Richardson Lake & Upper Scotch Lake Area Thunder Bay Mining … · 2017. 1. 16. · UPPER SCOTCH...
Transcript of Richardson Lake & Upper Scotch Lake Area Thunder Bay Mining … · 2017. 1. 16. · UPPER SCOTCH...
2012 Assessment Work Report
A Drilling Exploration Project
Richardson Lake & Upper Scotch Lake Area
Thunder Bay Mining Division, Ontario
Prepared and Submitted by
China Metallurgical Exploration Corp. (CME)
(145 Riviera Drive, Unit 7, Markham,
Ontario L3R 5J6, Canada)
July 20, 2012
Table of Content
List of Figures ............................................................................................................... 3
List of Tables ................................................................................................................. 3
List of Appendices ........................................................................................................ 3
1. Introduction ........................................................................................................... 4
2. Claims, Location, and Access ............................................................................... 4
2.1 Property Description and Ownership ...................................................... 4
3. Property Location and Access .............................................................................. 9
4. Previous Work Performed by CME .................................................................. 10
5. Regional Geological Setting ............................................................................... 11
5.1. Rock type .................................................................................................. 11
5.2. Stratum. .................................................................................................... 11
5.3. Mineralization .......................................................................................... 11
6. Drilling Exploration Project 2011 ...................................................................... 17
6.1. General information ................................................................................ 12
6.2. Products and Conclusion ........................................................................ 13
7. References ............................................................................................................ 25
List of Figures
Figure 1: Claim Map ......................................................................................................................... 8
Figure 2: Property Location Map ...................................................................................................... 9
Figure 3: Property Access Map ....................................................................................................... 10
Figure 4: Drilling Site Map ............................................................. Error! Bookmark not defined.
List of Tables
Table 1: Property Claim Identity ....................................................................................................... 4
Table 2: Property Co-ordinates ......................................................................................................... 8
List of Appendices
Appendix 1 Summary Report of Drilling Exploration…………..………….…independent File
1. Introduction
The whole CME’s Richardson Lake & Upper Scotch Lake Property and claims were acquired or staked / recorded by CME through 2009 and 2012due to its potential of hosting Copper, Zinc, and Gold. Since some of the current claims on this property were staked / recorded after the Drilling Exploration which was performed in March 2011, they are NOT part of this assessment work report. All the information, materials, and maps discussed in this report and its appendices only cover and refer to the claims recorded before the Drilling Exploration. Terms such as “the property”, “this property”, or “the Richardson Lake & Upper Scotch Lake Property” used below through the whole report for the purpose of convenient narration as well only refer to these claims recorded before the Drilling Exploration. In March 2011, a CME geology team did a traverse visit to the property; and in the same month, a Drilling Exploration was performed on this property to prove valuable magnetic and electromagnetic information gathered by the helicopter-borne survey carried in 2010 as basis for further exploration work. On the basis of interpretation and recommendations by Geotech, CME conducted a 12 hole diamond drill program totaling 1,658.72 metres to test selected airborne magnetic and electromagnetic anomalies. The drill program was conducted from March to May,2011 and focused on identification of potential base metal mineralization associated with the geophysical conductors.
2. Claims, Location, and Access
2.1 Property Description and Ownership
The Property consists of 51 contiguous unpatented claims within the Richardson Lake Area and Upper Scotch Lake Area. Specific claim information is provided in Table 1. The claims location and layout, along with their coordinates are given in Figure 1,
and Table 2.
Table 1: Property Claim Identity
Township/Area Claim
Number Recording
Date Claim Due Date
RICHARDSON LAKE AREA 4248129 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4248130 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252241 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252242 2009-Aug-04 2012-Aug-04
RICHARDSON LAKE AREA 4252243 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252244 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252245 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252246 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252247 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252248 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252249 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4252250 2009-Aug-04 2012-Aug-04 RICHARDSON LAKE AREA 4254299 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4256067 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4256068 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4256069 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4258300 2010-Nov-22 2012-Nov-22 RICHARDSON LAKE AREA 4258830 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4258831 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4258832 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4258833 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260202 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260205 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260206 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260210 2011-Sep-09 2013-Sep-09 RICHARDSON LAKE AREA 4260221 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260222 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260223 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260224 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260228 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260229 2011-Mar-02 2013-Mar-02 RICHARDSON LAKE AREA 4260230 2011-Mar-02 2013-Mar-02 UPPER SCOTCH LAKE AREA 4252233 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252234 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252235 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252236 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252237 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252238 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252239 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4252240 2009-Aug-04 2012-Aug-04 UPPER SCOTCH LAKE AREA 4259018 2011-Jan-31 2013-Jan-31 UPPER SCOTCH LAKE AREA 4259019 2011-Jan-31 2013-Jan-31 UPPER SCOTCH LAKE AREA 4261360 2011-Apr-26 2013-Apr-26
UPPER SCOTCH LAKE AREA 4263611 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263612 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263613 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263614 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263615 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263616 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263617 2011-Apr-26 2013-Apr-26 UPPER SCOTCH LAKE AREA 4263618 2011-Apr-26 2013-Apr-26
Table 2: Property Co-ordinates at Date of Drilling
Infl. Point
Longitude/Latitude Infl. Point
Longitude/Latitude
1 91° 9’ 10.19” W 49° 9’ 19.48” N 13 91° 9’ 37.38” W 49° 4’ 28.58” N 2 91° 6’ 31.13” W 49° 9’ 16.23” N 14 91° 10’ 55.73” W 49° 4’ 29.46” N
3 91° 6’ 33.80” W 49° 7’ 59.66” N 15 91° 10’ 56.02” W 49° 4’ 37.74” N 4 91° 5’ 55.07” W 49° 7’ 59.36” N 16 91° 12’ 14.07” W 49° 4’ 39.52” N
5 91° 5’ 56.55” W 49° 7’ 7.63” N 17 91° 12’ 12.59” W 49° 5’ 30.96” N 6 91° 5’ 17.52” W 49° 7’ 6.45” N 18 91° 11’ 18.79” W 49° 5’ 31.55” N
7 91° 5’ 20.18” W 49° 5’ 48.69” N 19 91° 11’ 15.83” W 49° 5’ 54.02” N 8 91° 7’ 58.64” W 49° 5’ 51.95” N 20 91° 10’ 56.32” W 49° 5’ 54.31” N
9 91° 8’ 0.71” W 49° 4’ 46.61” N 21 91° 10’ 54.84” W 49° 6’ 33.33” N 10 91° 8’ 40.03” W 49° 4’ 46.02” N 22 91° 10’ 15.52” W 49° 6’ 32.74” N
11 91° 8’ 41.51” W 49° 4’ 9.07” N 23 91° 10’ 11.68” W 49° 8’ 2.91” N 12 91° 9’ 38.27” W 49° 4’ 10.25” N 24 91° 9’ 13.44” W 49° 8’ 2.32” N
Figure 1: Claim Map at Date of Drilling
3. Property Location and Access
CME’s Richardson Lake & Upper Scotch Lake Property is located in Richardson Lake & Upper Scotch Lake areas, Thunder Bay Mining Division, ON. The closest town is Upsala, approximately 45 km² to the East of the property. Thunder Bay is approximately 190 km² in the Southeast (Figure 2).
Figure 2: Property Location Map
The TransCanada Highway 17 runs E-W through Upsala and to the East and North of the property. A trail off Hwy 17 at Graham Road leads to the property. . (Figure 3)
Figure 3: Property Access Map
4. Previous Work Performed by CME
A CME geology team did a preliminary a traverse visit to the property in May, 2010. Exploration products such as mapping or systematic sample assays were not intended or produced. The main objective of the visit was to acquire some valuable information regarding the geological setting, mineralization conditions of the property and provide reference in support of future geology work. The team observed and examined the outcrops and mineralization at the geological observation points. A NITON XL3t-500 handheld X-ray fluorescence ore analyzer was used to analyze the mineralized rocks (ore) to preliminarily determine the content of Cu and Zn in the field. A few samples were collected to analyze the grade of Cu and Au. A total of 24 geological points with a total length of approximately 16.6km were surveyed. In order to better understand the property’s geology and collect its magnetic and electromagnetic information, in September, 2010, a helicopter-borne geophysical survey was carried out by Geotech Ltd. on behalf of CME over its Richardson Lake & Upper Scotch Lake property. The total survey coverage for the area was 495.5 line-km.
The survey was flown at 100 metres line spacing with a West to East (N90º E/N 270°E) flight line direction.
5. Regional Geological Setting
The topography of the property shows low-to-moderate hills and the elevation is approximately 460-560 meters. Numerous rivers connect various lakes and the surrounding wetlands. Outcrops can be observed and the most areas are covered by sand, soil, and vegetation. In 1985, M.C. Jackson performed a research of the geological features in the Lumby Lake area. Much of the property is located in the area defined in Jackson’s study. According to Jackson’s research, Lumby Lake is in the Canadian Shield area, represented by Archean greenstone belt.
5.1. Rock type
According to the past research and the CME traverse survey, the rock types in the property include the Archaeozoic mafic metavolcanics, felsic metavolcanics, metamorphic sedimentary rocks, felsic intrusive rocks and mafic intrusive rocks. Mafic metavolcanics: widespread, the outcrops observed by the CME geo team are mostly mafic metavolcanics. Rock types are mainly massive and pillow lavas. Felsic intrusive rock: distributed at the western and northeastern edge of the property. Rock type is granite. According to CME team’s observation, Granite is light reddish, containing feldspar and quartz.
5.2. Stratum.
Stratums distributed in this area include Archaeozoic and Cenozoic strata. Archaean: mafic metavolcanic rocks, felsic - neutral metavolcanic rocks, metamorphic clastic sedimentary rocks and metamorphic sedimentary rocks. Mafic metavolcanics is the main lithology in this area, making up to 80 percent of the greenstone. The main rock types include massive or pillow lava, variolite, tuff, lapilli tuff, tuff breccia, plagioclase-porphyritic flows, etc. Cenozoic: in recent and pleistocene lake, stream and wetland deposits, glacial, glaciofluvial and glaciolacustrine deposits: sand, gravel, clay, till.
5.3. Mineralization
Mineral exploration in this area began in 1913. Minerals include iron, gold, and some base metals. Gold mineralization is mainly observed in the sedimentary rocks containing iron construction. Base metals (copper, lead, zinc) are mainly found in copper-nickel sulfide deposits.
The CME geo team observed limonitization in the mafic metavolcanics and the metamorphic sedimentary rocks in the property. Some outcrops (floats) exhibits minor Cu and Zn mineralization.
6. Drilling Exploration 2011
6.1. General information
On the basis of interpretation and recommendations by Geotech, CME conducted a 12 hole diamond drill program totaling 1,658.72 metres to test selected airborne magnetic and electromagnetic anomalies. The drill program was conducted from March to May, 2011 and focused on identification of potential base metal mineralization associated with the geophysical conductors. We analysed 458 pieces of sample for copper and gold. (The planned drilling hole ZK5 did not drilled)(表 3,图 9)
Table 3 Drilling Hole Information of Richardson Lake Property, 2011
Hole# Measured coordinate Designed
dip /azimuth
(°)
Designed
depth
(m)
Completion
depth (m)
Sample
analysis
(piece) X Y Z
ZK1 633682.998 5438207.218 497.124 45/90 150 163.68 62
ZK2 633404.587 5438233.876 501.690 45/70 120 123.44 9
ZK3 633025.454 5438170.008 510.101 55/60 150 150.88 33
ZK4 635010.358 5440603.521 540.182 60/250 200 177.39 18
ZK5 50/70 150 Undrilling /
ZK6 634089.253 5440803.821 510.628 60/90 160 141.73 95
ZK7 634713.398 5441172.069 507.698 50/55 120 124.05 33
ZK8 634409.031 5441157.381 511.544 55/65 150 150.88 8
ZK9 634321.713 5443331.717 502.892 65/270 120 133.20 40
ZK10 636738.912 5445230.614 514.427 55/110 120 123.44 38
ZK11 636874.032 5445451.449 507.698 50/120 80 117.35 62
ZK12 636708.874 5445441.670 511.544 55/110 80 105.16 9
ZK13 635309.305 5443119.607 564.416 45/150 150 147.52 10
Total 1600 1658.72 417
Figure 9 TAU、CVG anomaly isogram and geology map
(with site of planned drilling hole,ZK5 undrilled)
6.2. Products and Conclusion
Products:
Except drilling hole ZK2、ZK4、ZK8、ZK12 andZK13 show little sulfide, the other drilling hole met plenty of sulfide zone (table 4), no result of copper and gold mineralization, the airborne anomaly was almost caused by pyrrhotine and pyrite.
Table4 Sulfide Zone Information of Richardson Lake Property, 2011
Hole
#
Sulfide Zone depth(m) Rock/ore type
Sulfid
e type
Analysis result
Cu(%) Au(g/t)
Form To Coun tenor Tenor tenor Tenor
t Ave Ave
ZK1
9.75 20.05 10.30 Basalt ,pyrrho
tine
Po、bit
Py、
precio
us
little
Clp
0.026-0.052 0.036 / /
20.05 86.57 66.52 Metavolcanite
, pyrrhotine
Po、
Mag、
bit
Py、
precio
us
little
Clp
0.001-0.196 0.027 0.019-0.253 0.056
ZK2 Bit Po、Py 0.012-0.070 0.024 <0.005 <0.005
ZK3
7.02 10.67 3.65
Andesite,
pyrrhotine
Po 0.013-0.135 0.074 / /
80.02 113.99 33.97 Metavolcanite
, pyrrhotine
Po、
Py、
precio
us
little
Clp
0.004-0.099 0.034 0.012-0.064 0.031
ZK4 Bit Po 0.003-0.258 0.038 <0.005 <0.005
ZK6
18.06 42.86 24.80
Andesite,
pyrrhotine
Po、Py 0.006-0.116 0.039 0.007-0.025 0.015
45.86 68.28 22.42 Massive
sulfide Po、Py 0.015-0.064 0.032 0.009-0.026 0.016
68.28 82.46 14.18 Andesite,
pyrrhotine Po、Py 0.007-0.034 0.015 0.005-0.025 0.012
83.20 106.28 23.08 Massive
sulfide Py、Po 0.002-0.059 0.014 <0.005-0.012 0.005
108.00 116.31 8.31 Massive
sulfide Py、Po 0.004-0.017 0.012 0.009 0.009
ZK7
1.30 9.40 8.10 Andesite,
pyrrhotine Py、Po 0.011-0.044 0.021 <0.005 <0.005
29.87 33.81 3.94 Andesite,
pyrrhotine
Py、
Po、
precio
us
little
Clp
<0.001-0.031 0.018 0.006-0.010 0.008
44.81 57.27 12.46 Andesite,
pyrrhotine
Py、
Po、
precio
us
little
Clp
0.005-0.025 0.013 <0.005-0.006 <0.005
ZK8 Bit Py、precious little Clp 0.010-0.117 0.029 / /
ZK9
13.43 38.16 24.73 Andesite,
pyrrhotine
Po、bit
Py,、
precio
us
little
Clp
0.004-0.036 0.016 <0.005-0.036 0.017
38.16 52.09 13.93 Andesite,
pyrrhotine Bit Po 0.007-0.014 0.012 <0.005 <0.005
52.09 59.17 7.08 Andesite,
pyrrhotine
Po、
precio
us
little
Clp
0.008-0.027 0.019 <0.005-0.008 <0.005
ZK1
0
11.77 42.05 30.28
Andesite,
Massive
sulfide
Py、
Po、
precio
us
little
Clp
<0.001-0.756 0.078 <0.005-0.034 0.013
44.00 54.56 10.56
Andesite,
Massive
sulfide
Py、
Po、
precio
us
little
0.013-0.447 0.130 0.014 0.014
Clp
ZK1
1 16.51 86.87 70.36 Andesite
Py、
Po、
precio
us
little
Clp
0.020-0.142 0.036 <0.005-0.019 0.008
ZK1
2 61.52 61.92 0.40
Andesite,
pyrrhotine Py、Po 0.063 0.063 0.007 0.007
ZK1
3 8.80 10.76 1.96
Andesite,
pyrrhotine
Py、
Po、
Clp
0.133-0.301 0.217 0.095 0.095
6.2.1 Drill Logs & Assays
6.2.2 Conclusion
(1) A helicopter-borne geophysical survey and magnetic measurement interpreted some geophysical anomaly, The airborne anomaly was almost caused by Basalt, pyrrhotine and pyrite, some of the anomaly was caused by basic and ultrabasic rock what proved by drilling, (2)The result of the drilling shows that there are a lot of sulfides in the area, distributed as massive、denseness immerse、stripe. Sulfides almost pyrrhotine and pyrite are distributed as fine grained xenoblast-half idiomorphism condition.. There are some magnetite distributes in somewhere of anomaly area A, almost no chalcopyrite. The analysised sample shows no copper mineralization, representative sample and all samples from ZK9 shows no gold mineralization.
7. References(根据打钻公司、参与人员进行修改)
Geotech Ltd. September, 2010: Report on a Helicopter-borne Versatile Time Electromagnetic
(VTEM) and Aeromagnetic Geophysical Survey
Xianjun Li & Shawn Yang June, 2010: Summary of Geological Traverse Survey, Palmer Township and Ryan
Township, Sault Ste. Marie District, Ontario
Jackson, M.C. 1985: Geology of the Lumby Lake Area, Eastern Part, Districts of Kenora and Rainy
River; Ontario Geological Survey, Open File Report 5535,142p., 7 tables, 12 figures, 7 photographs, and l map in back pocket.
序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩(矿)石 名 称采
样日
期
No. DH No.Sample
No.to Lab自
(From)至
(To)样长
(Length)
Length of
core (m)
Recovery
factor(%)Size(mm) Weight(kg) Rock/Ore type
Samp
ling
date
ME Au AgAl
%
As
ppm
Ba
ppm
Be
ppm
Ca
%
Cd
ppm
Cr
ppm
Co
ppm
Cu
ppm
Fe
%
K
%
La
ppm
Li
ppm
Mg
%
Mn
ppm
Mo
ppm
Ni
ppm
P
%
Pb
ppm
Sb
ppm
Sc
ppm
Sn
ppm
1 ZK1 RL.H-1 9.75 11.28 1.53 0.93 61 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.6 90 180 <5 1.1 <10 670 100 390 7.99 2.7 10 40 1.41 1560 <10 280 0.05 70 <50 40 <50
2 ZK1 RL.H-2 12.68 1.40 1.40 100 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.7 40 170 <5 0.5 <10 730 90 260 7.56 2.7 10 30 1.12 1700 <10 260 0.02 60 <50 40 <50
3 ZK1 RL.H-3 14.08 1.40 1.40 100 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.8 <30 170 <5 0.7 <10 700 80 370 7.91 2.6 10 40 1.25 1980 <10 220 0.03 60 <50 41 <50
4 ZK1 RL.H-4 15.43 1.35 1.35 100 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.4 90 190 <5 0.5 <10 690 70 260 7.04 2.6 10 40 1.26 1890 <10 250 0.02 60 <50 40 <50
5 ZK1 RL.H-5 16.80 1.37 1.37 100 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.3 <30 170 <5 0.8 <10 680 120 520 9.75 2.5 10 40 1.25 1740 <10 350 0.02 80 <50 40 <50
6 ZK1 RL.H-6 18.17 1.37 1.37 100 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.7 <30 160 <5 1 <10 710 90 370 8.73 2.5 10 30 1.15 2010 <10 270 0.02 60 <50 41 <50
7 ZK1 RL.H-7 19.05 0.88 0.88 100 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.2 <30 160 <5 1.1 <10 700 80 380 9.75 2.2 <10 30 1.14 2620 <10 240 0.02 50 <50 41 <50
8 ZK1 RL.H-8 20.05 1.00 1.00 100 42/2 磁黄铁矿化(变)玄武岩/Pyrrhotite mineralization(altered), Basalt ICP90A 10.1 <30 150 <5 0.7 <10 760 100 330 11.4 2.1 10 30 1 2590 <10 290 0.02 40 <50 41 <50
9 ZK1 RL.H-9 21.35 1.30 1.30 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.73 <30 10 <5 3.8 <10 120 30 100 25.6 0.2 <10 <10 3.02 3860 <10 80 0.08 <20 <50 5 <50
10 ZK1 RL.H-10 22.70 1.35 1.35 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2.39 <30 70 <5 3.3 <10 160 40 110 27.1 0.4 <10 20 3.3 2850 <10 80 0.06 <20 <50 8 <50
11 RL.H-11 ICP90A 7.15 <30 480 5 0.7 <10 10 <10 <10 1.54 4.3 90 40 0.17 330 <10 <10 0.02 20 <50 <5 <50
12 ZK1 RL.H-12 23.97 1.27 1.27 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 4.68 50 160 <5 2.8 <10 300 70 170 22 1.1 <10 30 2.43 3030 <10 150 0.04 20 <50 16 <50
13 ZK1 RL.H-13 25.33 1.36 1.30 96 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2.84 <30 130 <5 3 <10 240 50 280 26.3 0.4 <10 20 2.86 3850 <10 100 0.06 <20 <50 11 <50
14 ZK1 RL.H-14 26.52 1.19 1.14 96 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.33 50 20 <5 4 <10 200 30 100 27.3 0.2 <10 <10 3.27 4270 <10 60 0.08 <20 <50 <5 <50
15 ZK1 RL.H-15 27.92 1.40 1.40 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 2.14 <30 50 <5 2.4 <10 140 50 310 27.6 0.1 <10 <10 2.55 3600 <10 120 0.08 <20 <50 6 <50
16 ZK1 RL.H-16 29.57 1.65 1.65 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.68 <30 10 <5 3.3 <10 40 <10 40 24.9 <0.1 <10 <10 2.93 4390 <10 30 0.06 <20 <50 <5 <50
17 ZK1 RL.H-17 30.86 1.29 1.20 93 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.7 80 130 <5 2.2 <10 320 70 200 14 0.7 30 50 1.58 2010 <10 160 0.04 30 <50 20 <50
18 ZK1 RL.H-18 32.26 1.40 1.30 93 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 9.98 <30 230 <5 3.1 <10 220 50 330 7.43 1.2 60 50 1.53 950 <10 100 0.05 40 <50 20 <50
19 ZK1 RL.H-19 33.66 1.40 1.33 95 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 7.82 <30 190 <5 3.2 <10 230 90 550 11.1 1 20 40 1.65 1170 <10 170 0.05 60 <50 19 <50
20 ZK1 RL.H-20 34.92 1.26 1.20 95 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.12 80 80 <5 2.2 <10 180 80 1960 13.2 0.6 <10 30 1.47 1270 <10 140 0.02 30 <50 14 <50
21 ZK1 RL.H-21 36.09 1.17 1.14 97 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.44 90 80 <5 2.1 <10 220 110 610 17 0.8 <10 30 1.94 1860 <10 200 0.03 50 <50 13 <50
22 RL.H-22 ICP90A 7.4 100 590 <5 0.8 20 30 20 4450 4.85 4.8 10 10 0.88 520 170 30 0.1 2080 70 12 260
23 ZK1 RL.H-23 37.41 1.32 1.32 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.84 <30 130 <5 1 <10 300 80 370 15.3 1 10 50 1.19 1840 <10 140 0.04 40 <50 18 <50
24 ZK1 RL.H-24 38.71 1.30 1.30 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 4.74 80 140 <5 0.7 <10 110 120 560 22.7 0.9 10 30 0.77 1070 <10 230 0.03 50 <50 12 <50
25 ZK1 RL.H-25 39.76 1.05 1.05 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.89 70 110 <5 1.1 <10 110 120 690 24.9 0.7 <10 20 1.2 1360 <10 210 0.02 50 <50 12 <50
26 ZK1 RL.H-26 40.91 1.15 1.15 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.56 <30 <10 <5 2 <10 30 20 100 10.5 <0.1 <10 <10 1.58 2030 <10 30 0.03 <20 <50 <5 <50
27 ZK1 RL.H-27 42.29 1.38 1.35 98 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.89 <30 10 <5 3 <10 40 20 100 18.5 <0.1 <10 <10 2.72 3580 <10 40 0.05 <20 <50 <5 <50
28 ZK1 RL.H-28 43.51 1.22 1.15 94 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.81 40 100 <5 2.8 <10 290 50 150 15.5 0.8 10 50 2.04 2590 <10 110 0.03 <20 <50 16 <50
29 ZK1 RL.H-29 44.81 1.30 1.23 94 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 8.09 <30 270 <5 1.2 <10 300 80 440 14.6 1.7 20 60 1.36 1750 <10 170 0.04 30 <50 22 <50
30 ZK1 RL.H-30 45.91 1.10 1.10 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2 <30 <10 <5 3.1 <10 130 60 240 20.4 0.2 <10 10 2.17 3180 <10 180 0.03 <20 <50 <5 <50
31 ZK1 RL.H-31 46.91 1.00 1.00 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.52 <30 60 <5 2.1 <10 250 50 540 22 0.2 <10 20 1.83 2880 <10 160 0.03 <20 <50 11 <50
32 ZK1 RL.H-32 47.85 0.94 0.94 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.17 <30 <10 <5 1.8 <10 310 40 290 22.6 <0.1 <10 20 2.08 4340 <10 130 0.04 <20 <50 13 <50
33 RL.H-33 ICP90A FAI323 Au AAS21E Ag 6.96 <30 380 <5 0.7 <10 10 <10 20 1.78 4.2 80 40 0.16 360 <10 <10 0.02 30 <50 <5 <50
34 ZK1 RL.H-34 49.07 1.22 1.22 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 2.09 <30 20 <5 2.8 <10 140 30 130 17.8 0.1 <10 10 2.27 2990 <10 90 0.05 <20 <50 6 <50
35 ZK1 RL.H-35 50.42 1.35 1.35 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 2.69 <30 100 <5 1.9 <10 190 40 360 17.3 0.5 <10 20 1.76 1940 <10 120 0.05 <20 <50 9 <50
36 ZK1 RL.H-36 51.87 1.45 1.44 99 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.98 <30 20 <5 3.6 <10 240 30 370 15.4 0.2 <10 10 2.27 3100 <10 100 0.05 <20 <50 7 <50
37 ZK1 RL.H-37 53.26 1.39 1.38 99 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.32 <30 <10 <5 1.9 <10 60 10 40 20.3 <0.1 <10 <10 1.98 5080 <10 50 0.03 <20 <50 <5 <50
38 ZK1 RL.H-38 54.56 1.30 1.30 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.77 <30 120 <5 2.1 <10 170 <10 10 17.7 0.2 <10 <10 2.59 5080 <10 70 0.03 <20 <50 <5 <50
39 ZK1 RL.H-39 56.01 1.45 1.45 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.8 <30 280 <5 3 <10 310 10 30 15.9 0.3 <10 10 3.32 4370 <10 100 0.05 <20 <50 6 <50
40 ZK1 RL.H-40 57.34 1.33 1.33 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.1 <30 80 <5 5.1 <10 140 10 70 9.38 0.3 <10 20 2.47 3130 10 50 0.04 <20 <50 7 <50
41 ZK1 RL.H-41 58.74 1.40 1.40 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 5.29 80 110 <5 2.5 <10 90 50 230 17.6 0.6 30 30 1.14 1330 <10 170 0.05 20 <50 11 <50
42 ZK1 RL.H-42 60.05 1.31 1.31 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.62 40 100 <5 2.4 <10 350 170 680 17.4 0.7 <10 30 1.31 1290 <10 260 0.04 30 <50 17 <50
43 ZK1 RL.H-43 61.25 1.20 1.20 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 8.38 <30 170 <5 2 <10 470 40 430 9.51 1.2 20 50 1.36 1600 <10 190 0.02 20 <50 25 <50
44 RL.H-44 ICP90A 6.06 460 1520 <5 2.6 60 350 30 25900 6.75 2.4 20 20 1.89 940 1280 260 0.13 7850 90 12 110
45 ZK1 RL.H-45 62.55 1.30 1.30 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 6.79 60 140 <5 2.4 <10 460 110 480 17.2 0.9 <10 40 1.39 1260 <10 260 0.03 20 <50 24 <50
46 ZK1 RL.H-46 63.95 1.40 1.40 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.86 <30 40 <5 4.3 <10 150 90 390 16.1 0.4 <10 10 2.22 2800 <10 160 0.05 <20 <50 8 <50
47 ZK1 RL.H-47 65.50 1.55 1.55 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 6.18 40 180 <5 14.6 <10 380 50 180 6.86 2.2 <10 20 2.3 3370 <10 130 0.04 <20 <50 32 <50
48 ZK1 RL.H-48 66.90 1.40 1.40 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 6.73 30 240 <5 7.6 <10 410 50 100 8.46 1.8 10 20 2.6 2510 <10 170 0.06 <20 <50 28 <50
49 ZK1 RL.H-49 68.11 1.21 1.20 98 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.82 <30 180 <5 3.4 <10 550 70 310 12 1.6 10 30 1.49 1350 <10 140 0.02 <20 <50 28 <50
50 ZK1 RL.H-50 69.19 1.08 1.06 98 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.69 30 140 <5 3.2 <10 680 50 140 11.1 1.4 10 30 1.48 1500 <10 130 0.02 <20 <50 31 <50
51 ZK1 RL.H-51 70.39 1.20 1.15 96 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 6.92 <30 130 <5 3.3 <10 420 70 130 13.3 1.2 <10 20 1.57 1710 <10 150 0.04 <20 <50 26 <50
52 ZK1 RL.H-52 71.58 1.19 1.14 96 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 5.36 <30 80 <5 2.9 <10 210 40 130 10.2 0.6 10 20 1.15 1480 <10 110 0.01 <20 <50 16 <50
53 ZK1 RL.H-53 72.91 1.33 1.30 98 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 5.91 <30 90 <5 2.4 <10 230 40 100 11.8 0.8 <10 20 1.02 1270 <10 130 0.03 20 <50 18 <50
54 ZK1 RL.H-54 74.13 1.22 1.22 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 9.64 <30 170 <5 2.4 <10 420 30 140 6.57 1.5 10 50 1.26 1880 <10 170 0.04 <20 <50 34 <50
55 RL.H-55 ICP90A 7.18 <30 380 <5 0.7 <10 <10 <10 <10 1.54 4.5 90 40 0.16 320 <10 10 0.01 20 <50 <5 <50
56 ZK1 RL.H-56 75.29 1.16 1.16 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 3.22 <30 80 <5 7.4 <10 140 50 190 19.5 0.6 <10 20 2.83 3780 <10 170 0.02 <20 <50 16 <50
57 ZK1 RL.H-57 76.59 1.30 1.30 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 2 30 10 <5 6.3 <10 130 110 210 22.2 0.2 <10 <10 2.53 4090 50 190 0.01 <20 <50 8 <50
58 ZK1 RL.H-58 77.79 1.20 1.20 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.53 <30 20 <5 4.2 <10 100 20 80 8.18 0.2 <10 <10 1.66 2680 <10 70 0.01 <20 <50 5 <50
59 ZK1 RL.H-59 78.94 1.15 1.15 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 0.24 <30 <10 <5 6.3 <10 20 20 70 8.49 <0.1 <10 <10 2.43 3960 <10 70 0.03 <20 <50 <5 <50
60 ZK1 RL.H-60 80.04 1.10 1.10 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 1.81 <30 <10 <5 8.6 <10 100 20 120 14.8 <0.1 <10 <10 3.4 5970 <10 130 0.01 <20 <50 6 <50
61 ZK1 RL.H-61 81.08 1.04 1.04 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 1.79 <30 <10 <5 6.1 <10 70 40 130 15.6 <0.1 <10 <10 2.53 4870 <10 140 0.01 <20 <50 5 <50
62 ZK1 RL.H-62 82.28 1.20 1.20 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.41 <30 30 <5 6.4 <10 90 20 110 12.9 0.4 <10 10 2.6 4900 <10 120 0.03 <20 <50 10 <50
63 ZK1 RL.H-63 83.48 1.20 1.20 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 7.98 30 130 <5 2 <10 310 40 60 6.41 1.5 20 50 0.9 1110 <10 140 0.03 <20 <50 21 <50
64 ZK1 RL.H-64 84.94 1.46 1.46 100 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A FAI323 Au AAS21E Ag 6.77 30 90 <5 2.1 <10 190 40 90 6.71 0.8 10 40 0.9 1200 <10 140 0.03 <20 <50 21 <50
65 ZK1 RL.H-65 86.57 1.63 1.60 98 42/2 磁黄铁矿化含铁(变)火山沉积岩/Pyrrhotite Mineralization (altered), volcanic sediment ICP90A 4.93 <30 80 <5 3.1 <10 170 30 70 5.77 0.4 <10 20 1.16 1750 <10 110 0.02 <20 <50 19 <50
66 RL.H-66 ICP90A FAI323 Au AAS21E Ag 7.45 100 590 <5 0.7 20 30 20 4500 4.76 4.7 10 10 0.88 520 180 30 0.09 2120 70 12 270
67 ZK1 RL.H-67 87.91 1.34 1.30 98 42/2 (变)安山岩/(Altered) Andesite ICP90A 8 <30 180 <5 7.8 <10 120 30 70 7.29 0.5 10 20 3.81 2740 <10 70 0.1 <20 <50 23 <50
68 ZK1 RL.H-68 89.03 1.12 1.10 98 42/2 (变)安山岩/(Altered) Andesite ICP90A 5.21 <30 210 <5 9.2 <10 190 50 110 7.84 0.5 <10 <10 3.35 3940 <10 200 0.02 <20 <50 23 <50
69 ZK2 RL.H-69 13.58 14.74 1.16 1.16 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.11 <30 20 <5 7.8 <10 280 50 120 9.34 0.2 <10 40 4.25 1780 <10 130 0.03 <20 <50 42 <50
70 ZK2 RL.H-70 15.94 1.20 1.20 100 42/2 (变)安山岩/(Altered) Andesite ICP90A FAI323 Au AAS21E Ag 7.93 <30 10 <5 8.9 <10 270 50 130 8.85 <0.1 <10 20 3.93 1700 <10 120 0.03 <20 <50 40 <50
71 ZK2 RL.H-71 19.36 20.38 1.02 1.02 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.75 <30 40 <5 12.5 <10 270 50 170 6.41 0.1 <10 10 2.2 1720 <10 140 0.04 <20 <50 38 <50
72 ZK2 RL.H-72 21.48 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.75 <30 820 <5 3.9 <10 100 70 360 6.79 1.9 20 30 2.35 760 <10 120 0.12 <20 <50 21 <50
73 ZK2 RL.H-73 91.08 92.23 1.15 1.15 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.76 <30 50 <5 8.9 <10 360 50 150 7.07 0.2 <10 20 4.37 1690 <10 80 0.01 <20 <50 44 <50
74 ZK2 RL.H-74 121.87 123.44 1.57 1.40 89 42/2 (变)安山岩/(Altered) Andesite ICP90A FAI323 Au AAS21E Ag 4.58 <30 40 6 18.4 <10 90 30 120 4.71 0.3 <10 30 2.8 2940 <10 50 0.04 <20 <50 27 <50
75 ZK3 RL.H-75 7.67 9.17 1.50 1.50 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (altered),Andesite ICP90A 6.1 <30 180 <5 8 <10 160 130 1350 13.1 0.6 <10 30 3.15 1970 <10 190 0.01 <20 <50 34 <50
76 ZK3 RL.H-76 10.67 1.50 1.50 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (altered),Andesite ICP90A 7.45 <30 90 <5 9.9 <10 210 50 130 8.45 0.5 <10 20 3.61 2040 <10 160 0.02 <20 <50 41 <50
77 RL.H-77 ICP90A 6.82 <30 400 5 0.8 <10 40 <10 <10 1.42 4.3 80 40 0.19 320 <10 <10 0.02 <20 <50 <5 <50
78 ZK3 RL.H-78 78.72 80.02 1.30 1.30 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 6.36 <30 160 <5 11.7 <10 180 40 190 7.63 0.4 <10 20 3.5 1920 <10 100 0.01 <20 <50 34 <50
79 ZK3 RL.H-79 81.22 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.74 <30 230 <5 6 <10 150 50 460 7.79 1.6 <10 20 2.06 1030 <10 90 0.04 <20 <50 29 <50
80 ZK3 RL.H-80 82.52 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 6.44 <30 140 <5 3 <10 80 120 630 11.1 1.2 20 20 1.37 570 <10 110 0.03 30 <50 10 <50
81 ZK3 RL.H-81 83.82 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 7.97 <30 200 <5 3.8 <10 210 60 620 7.32 2.1 20 20 1.86 600 <10 80 0.04 30 <50 17 <50
82 ZK3 RL.H-82 85.16 1.34 1.33 99 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.09 40 240 <5 3.4 <10 100 70 710 6.28 2.1 10 10 1.69 610 <10 90 0.03 40 <50 19 <50
83 ZK3 RL.H-83 86.47 1.31 1.30 99 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 10.6 80 350 <5 5.5 <10 190 60 320 4.52 2.7 10 20 3.37 630 <10 90 0.03 <20 <50 43 <50
84 ZK3 RL.H-84 87.68 1.21 1.20 99 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 4.74 350 140 <5 2.6 <10 60 40 170 4.69 1.1 10 60 1.65 430 <10 50 0.02 <20 <50 8 <50
85 ZK3 RL.H-85 88.68 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.22 70 220 <5 1.8 <10 60 30 130 7.5 2 10 80 2.18 540 <10 70 0.05 <20 <50 15 <50
86 ZK3 RL.H-86 89.59 0.91 0.91 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 2.82 <30 110 <5 6.2 <10 110 30 290 14.7 0.6 <10 <10 3.86 1800 <10 100 0.07 <20 <50 6 <50
87 ZK3 RL.H-87 90.52 0.93 0.93 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.38 <30 600 <5 5 <10 800 40 70 7.52 1.4 30 10 7.54 1230 <10 430 0.16 <20 <50 19 <50
88 RL.H-88 ICP90A FAI323 Au AAS21E Ag 5.81 460 1480 <5 2.6 60 380 30 24700 6.73 2.4 20 20 1.8 920 1250 350 0.13 7720 80 12 110
89 ZK3 RL.H-89 91.83 1.31 1.30 99 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 5.69 80 170 <5 1 <10 80 90 670 8.62 1.5 10 40 1.86 330 <10 90 0.04 30 <50 12 <50
90 ZK3 RL.H-90 92.96 1.13 1.12 99 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.6 40 300 <5 2 <10 90 100 990 7.92 2.9 20 10 1.35 510 <10 120 0.06 30 <50 18 <50
91 ZK3 RL.H-91 94.01 1.05 1.02 97 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 7.22 <30 270 <5 2.2 <10 70 60 560 12 2.6 20 20 1.84 1520 <10 100 0.04 30 <50 16 <50
92 ZK3 RL.H-92 95.45 1.44 1.40 97 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 0.42 <30 <10 <5 2.6 <10 60 <10 70 18.8 <0.1 <10 <10 2.38 2660 <10 20 0.06 <20 <50 <5 <50
93 ZK3 RL.H-93 96.61 1.16 1.10 95 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 0.94 <30 10 <5 5 <10 20 10 160 17.2 0.2 <10 <10 2.83 2990 <10 20 0.04 <20 <50 <5 <50
94 ZK3 RL.H-94 97.87 1.26 1.20 95 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.49 <30 320 <5 1.3 <10 30 30 220 6.2 3.7 20 <10 0.84 540 <10 130 0.08 <20 <50 11 <50
分析结果/Assay Result
基本析样品取样及分析结果登记表
取样位置Sampling location (m)
Sample Log
分析方法/Assay Method
正元国际矿业有限公司W W W . C N Z I M C . C O M
正元国际矿业有限公司W W W . C N Z I M C . C O M
第 1 页,共 10 页
序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩(矿)石 名 称采
样日
期
No. DH No.Sample
No.to Lab自
(From)至
(To)样长
(Length)
Length of
core (m)
Recovery
factor(%)Size(mm) Weight(kg) Rock/Ore type
Samp
ling
date
ME Au AgAl
%
As
ppm
Ba
ppm
Be
ppm
Ca
%
Cd
ppm
Cr
ppm
Co
ppm
Cu
ppm
Fe
%
K
%
La
ppm
Li
ppm
Mg
%
Mn
ppm
Mo
ppm
Ni
ppm
P
%
Pb
ppm
Sb
ppm
Sc
ppm
Sn
ppm
分析结果/Assay Result
基本析样品取样及分析结果登记表
取样位置Sampling location (m)
Sample Log
分析方法/Assay Method
正元国际矿业有限公司W W W . C N Z I M C . C O M
正元国际矿业有限公司W W W . C N Z I M C . C O M
95 ZK3 RL.H-95 99.06 1.19 1.13 95 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.49 <30 360 <5 1.1 <10 60 40 280 5.86 3.7 20 10 0.99 340 <10 110 0.05 <20 <50 12 <50
96 ZK3 RL.H-96 100.08 1.02 1.00 98 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.36 50 420 <5 1.1 <10 90 40 310 4.87 4.1 20 10 0.98 350 <10 140 0.05 30 <50 15 <50
97 ZK3 RL.H-97 101.10 1.02 1.00 98 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 6.54 40 370 <5 1.3 <10 120 50 470 6.06 3.3 20 10 1.36 530 <10 140 0.03 <20 <50 14 <50
98 ZK3 RL.H-98 102.11 1.01 1.00 99 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.6 <30 340 <5 1 <10 60 30 260 6.24 3.4 30 10 1.32 420 <10 80 0.05 <20 <50 12 <50
99 RL.H-99 ICP90A 6.9 <30 480 <5 0.8 <10 20 <10 <10 1.29 4.3 80 40 0.15 300 <10 <10 0.02 <20 <50 <5 <50
100 ZK3 RL.H-100 103.46 1.35 1.35 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.18 <30 380 <5 1.4 <10 110 30 130 5.13 3.7 30 20 1.41 420 <10 90 0.05 <20 <50 13 <50
101 ZK3 RL.H-101 104.86 1.40 1.40 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.17 <30 390 <5 0.7 <10 100 40 620 5.15 3.9 20 20 1.43 340 <10 100 0.04 <20 <50 13 <50
102 ZK3 RL.H-102 106.29 1.43 1.40 98 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.15 <30 450 <5 1.6 <10 100 60 300 5.88 4.2 20 10 1.47 410 <10 120 0.04 <20 <50 14 <50
103 ZK3 RL.H-103 107.80 1.51 1.48 98 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.98 <30 350 <5 2.9 <10 140 60 150 9.7 3.5 20 30 3.01 730 <10 130 0.03 <20 <50 32 <50
104 ZK3 RL.H-104 109.10 1.30 1.27 98 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.87 <30 430 <5 2.3 <10 70 20 260 4.07 3.2 20 10 1.87 480 <10 80 0.06 <20 <50 10 <50
105 ZK3 RL.H-105 110.40 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.36 <30 400 <5 1.6 <10 60 30 180 5.5 3.2 20 10 1.54 830 <10 70 0.04 <20 <50 11 <50
106 ZK3 RL.H-106 111.65 1.25 1.25 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A FAI323 Au AAS21E Ag 5.66 <30 280 <5 3.1 <10 80 50 390 7.52 2.6 20 <10 1.61 1230 <10 120 0.04 <20 <50 11 <50
107 ZK3 RL.H-107 112.75 1.10 1.10 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 7.78 <30 400 <5 1 <10 120 60 210 6.37 3.9 20 20 2.09 520 <10 130 0.05 <20 <50 17 <50
108 ZK3 RL.H-108 113.99 1.24 1.24 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 8.03 <30 500 <5 1 <10 80 30 40 4.52 3.7 20 30 2.15 440 <10 90 0.05 <20 <50 14 <50
109 ZK3 RL.H-109 115.19 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化含铁(变)火山沉积岩/Pyrrhotite&Pyrite Mineralization (Altered), volcanic Sediment ICP90A 6.45 <30 190 <5 5.3 <10 120 30 40 6.33 1.2 <10 20 4.92 1020 <10 100 0.02 <20 <50 24 <50
110 RL.H-110 ICP90A 7.39 100 580 <5 0.9 20 50 20 4450 4.81 4.9 10 10 0.87 530 160 40 0.1 2060 70 11 270
111 ZK3 RL.H-111 116.39 1.20 1.20 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.14 <30 300 <5 9 <10 160 50 80 7.58 1.6 <10 10 4.39 1390 <10 130 0.02 <20 <50 38 <50
112 ZK10 RL.H-112 10.67 11.77 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.43 <30 30 <5 8.1 <10 160 40 40 9.07 0.4 <10 30 3.73 1520 <10 90 0.09 <20 <50 36 <50
113 ZK10 RL.H-113 13.02 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.08 <30 30 <5 7.4 <10 310 50 70 7.83 0.4 <10 30 3.69 1870 <10 110 0.03 <20 <50 42 <50
114 ZK10 RL.H-114 14.46 1.44 1.40 97 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.79 <30 40 <5 6.9 <10 300 50 90 8.15 0.5 <10 40 3.98 1960 <10 110 0.02 <20 <50 41 <50
115 ZK10 RL.H-115 15.85 1.39 1.30 94 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.9 <30 40 <5 8.5 <10 310 50 160 7.95 0.5 <10 30 3.41 2200 <10 110 0.02 <20 <50 41 <50
116 ZK10 RL.H-116 17.07 1.22 1.15 94 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.9 <30 10 <5 12 <10 300 40 60 7.44 0.2 <10 20 2.97 2600 10 110 0.02 <20 <50 41 <50
117 ZK10 RL.H-117 18.29 1.22 1.20 98 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.57 <30 20 <5 8.2 <10 280 50 80 6.81 0.2 <10 20 3 1840 20 110 0.01 <20 <50 40 <50
118 ZK10 RL.H-118 19.66 1.37 1.35 98 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.06 <30 50 <5 9 <10 310 50 60 7.34 0.4 <10 20 3.16 2010 10 110 0.02 <20 <50 43 <50
119 ZK10 RL.H-119 20.66 1.00 1.00 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.73 <30 20 <5 10.5 <10 280 40 50 7.52 0.3 <10 20 3.09 2270 30 110 0.02 <20 <50 38 <50
120 ZK10 RL.H-120 20.99 0.33 0.33 100 42/2 块状硫化物 VMS ICP90A 1.69 <30 <10 <5 2.6 <10 130 100 840 >30 <0.1 <10 <10 0.49 500 70 100 <0.01 <20 <50 <5 <50
121 RL.H-121 ICP90A 6.95 <30 470 <5 0.9 <10 20 <10 <10 1.35 4.2 70 40 0.17 300 10 <10 0.01 <20 <50 <5 <50
122 ZK10 RL.H-122 22.06 1.07 1.07 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 6.37 <30 60 <5 7.8 <10 170 20 230 7.09 0.6 <10 20 3.08 1360 140 70 0.03 <20 <50 30 <50
123 ZK10 RL.H-123 23.31 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.94 <30 50 <5 8.2 <10 210 40 150 7.44 0.8 <10 40 3.96 1490 <10 90 0.02 <20 <50 40 <50
124 ZK10 RL.H-124 24.66 1.35 1.35 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.76 <30 80 <5 7.9 <10 330 50 80 8.08 1.7 <10 60 4.83 1460 20 120 0.02 <20 <50 40 <50
125 ZK10 RL.H-125 26.00 1.34 1.34 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.56 <30 20 <5 8.4 <10 280 40 90 8.05 0.6 <10 30 4.51 1570 <10 110 0.02 <20 <50 40 <50
126 ZK10 RL.H-126 26.94 0.94 0.94 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.96 <30 300 <5 3.1 <10 10 <10 <10 1.42 1.8 10 40 0.92 300 <10 10 0.03 <20 <50 <5 <50
127 ZK10 RL.H-127 27.94 1.00 1.00 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.89 <30 340 <5 3.2 <10 100 <10 <10 1.37 1.6 <10 40 0.94 320 <10 <10 0.03 <20 <50 <5 <50
128 ZK10 RL.H-128 28.96 1.02 1.02 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.16 <30 10 <5 11.5 <10 260 40 40 7.37 0.2 <10 20 3.97 2110 <10 90 0.02 <20 <50 40 <50
129 ZK10 RL.H-129 30.20 1.24 1.24 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.75 <30 10 <5 9.4 <10 270 40 100 7.88 0.4 <10 20 3.75 1700 30 100 0.02 <20 <50 41 <50
130 ZK10 RL.H-130 31.50 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.64 <30 20 <5 9.6 <10 250 30 90 7.08 0.4 <10 30 3.48 1460 <10 80 0.02 <20 <50 38 <50
131 ZK10 RL.H-131 32.60 1.10 1.10 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 2.34 50 30 <5 3.7 <10 60 120 2200 >30 0.4 <10 20 1.92 880 80 140 0.01 <20 <50 16 <50
132 RL.H-132 ICP90A 5.91 460 1460 <5 2.7 60 370 30 25700 6.67 2.4 20 20 1.84 940 1260 260 0.13 7840 90 12 110
133 ZK10 RL.H-133 33.52 0.92 0.92 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 1.6 90 10 <5 4 <10 60 100 5540 >30 0.2 <10 <10 1.63 720 110 120 <0.01 40 <50 8 <50
134 ZK10 RL.H-134 35.05 1.53 1.53 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.06 <30 60 <5 8.5 <10 300 40 190 7.71 0.6 <10 20 3.9 1730 <10 110 0.04 <20 <50 44 <50
135 ZK10 RL.H-135 36.15 1.10 1.10 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.65 <30 100 <5 8.3 <10 250 30 260 7.08 0.9 <10 40 4.48 1710 10 90 0.02 <20 <50 48 <50
136 ZK10 RL.H-136 37.35 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.48 <30 70 <5 7.8 <10 310 40 60 5.89 0.6 <10 20 4.37 1340 30 100 0.03 <20 <50 46 <50
137 ZK10 RL.H-137 38.70 1.35 1.35 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.31 <30 80 <5 6.9 <10 260 30 350 7.47 0.6 <10 20 3.85 1300 <10 100 0.02 <20 <50 35 <50
138 ZK10 RL.H-138 39.97 1.27 1.27 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.75 <30 40 <5 8.8 <10 290 40 120 7.27 0.4 <10 20 3.95 1580 <10 90 0.03 <20 <50 42 <50
139 ZK10 RL.H-139 41.15 1.18 1.18 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 0.44 120 <10 <5 2 <10 10 230 1860 >30 <0.1 <10 <10 0.35 330 20 140 <0.01 20 <50 <5 <50
140 ZK10 RL.H-140 42.05 0.90 0.90 100 42/2 块状硫化物/VMS ICP90A 1.38 <30 30 <5 4 <10 30 80 7560 >30 0.3 <10 10 2.03 910 60 430 0.01 40 <50 <5 <50
141 ZK10 RL.H-141 43.05 1.00 1.00 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.24 <30 30 <5 1 <10 <10 <10 180 1.05 1.5 <10 <10 0.04 190 <10 <10 <0.01 20 <50 7 <50
142 ZK10 RL.H-142 44.00 0.95 0.95 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 6.66 <30 30 <5 1.3 <10 30 <10 180 0.92 2.1 <10 <10 0.04 330 <10 <10 <0.01 30 <50 6 <50
143 RL.H-143 ICP90A FAI323 Au AAS21E Ag 6.87 <30 420 <5 1.3 <10 30 <10 20 1.16 4.1 70 40 0.14 280 <10 <10 0.02 20 <50 <5 <50
144 ZK10 RL.H-144 45.04 1.04 1.04 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 0.74 90 10 <5 3.9 <10 10 140 1930 >30 0.4 <10 <10 2.11 860 30 190 <0.01 30 <50 6 <50
145 ZK10 RL.H-145 46.29 1.25 1.25 100 42/2 块状硫化物/VMS ICP90A 0.92 80 <10 <5 2.6 <10 30 150 3410 >30 0.1 <10 <10 1.15 580 180 240 <0.01 50 <50 <5 <50
146 ZK10 RL.H-146 47.74 1.45 1.45 100 42/2 块状硫化物/VMS ICP90A FAI323 Au AAS21E Ag 0.95 <30 <10 <5 2 <10 10 80 4470 >30 0.5 <10 20 1.5 900 50 500 <0.01 40 <50 8 <50
147 ZK10 RL.H-147 48.84 1.10 1.10 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.69 <30 10 8 7.8 <10 110 20 640 9.51 0.8 <10 40 5.52 3140 <10 60 0.03 <20 <50 52 <50
148 ZK10 RL.H-148 50.29 1.45 1.45 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.19 <30 40 15 11.4 <10 80 20 360 5.91 0.9 <10 30 5.37 2870 <10 30 0.04 <20 <50 16 <50
149 ZK11 RL.H-149 15.31 16.51 1.20 1.20 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 6.76 <30 560 5 5.7 <10 480 40 40 6.53 1.5 20 70 6.1 1170 <10 290 0.15 <20 <50 19 <50
150 ZK11 RL.H-150 17.71 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.56 <30 140 7 6 <10 320 100 200 7.64 0.9 <10 30 3.24 1080 <10 380 0.03 <20 <50 39 <50
151 ZK11 RL.H-151 18.86 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.99 <30 80 8 7.9 <10 320 80 200 6.43 0.6 <10 20 2.65 1070 <10 280 0.03 <20 <50 41 <50
152 ZK11 RL.H-152 19.81 0.95 0.95 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.9 <30 130 6 7.5 <10 340 80 290 6.59 1.1 <10 40 2.99 1150 20 330 0.03 70 <50 40 <50
153 ZK11 RL.H-153 21.11 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.69 <30 40 9 11.6 <10 230 50 250 8.65 0.3 <10 20 4.05 1890 30 290 0.03 20 <50 30 <50
154 RL.H-154 ICP90A 7.48 100 590 <5 0.7 20 40 20 4440 4.89 4.7 10 10 0.9 540 200 30 0.09 2070 60 12 260
155 ZK11 RL.H-155 22.31 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.68 <30 80 6 4.5 <10 220 50 570 8.03 0.7 <10 40 1.76 650 40 230 0.02 30 <50 33 <50
156 ZK11 RL.H-156 23.61 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.06 <30 70 8 5 <10 240 80 370 6.95 0.8 <10 40 1.85 810 10 210 0.03 <20 <50 32 <50
157 ZK11 RL.H-157 24.71 1.10 1.10 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.07 <30 60 8 3.8 <10 260 70 410 6.59 0.7 <10 50 1.8 710 <10 270 0.03 <20 <50 33 <50
158 ZK11 RL.H-158 25.91 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.35 <30 30 7 5.6 <10 300 90 220 8.59 0.3 <10 30 2.43 1000 <10 370 0.02 <20 <50 38 <50
159 ZK11 RL.H-159 27.26 1.35 1.35 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.15 <30 40 6 4.4 <10 290 80 290 8.85 0.3 <10 30 2.78 930 <10 420 0.03 <20 <50 38 <50
160 ZK11 RL.H-160 28.41 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.2 <30 60 <5 5.6 <10 270 120 250 13.7 0.4 <10 30 2.04 810 <10 420 0.03 <20 <50 33 <50
161 ZK11 RL.H-161 29.66 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 70 5 7.6 <10 310 70 240 9.21 0.4 <10 30 1.8 940 40 320 0.03 <20 <50 37 <50
162 ZK11 RL.H-162 30.86 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.47 <30 100 5 6.5 <10 190 40 260 8.19 0.3 <10 20 0.87 760 20 300 0.03 <20 <50 22 <50
163 ZK11 RL.H-163 32.00 1.14 1.14 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.97 <30 130 7 4.7 <10 90 10 130 3.7 0.6 <10 30 1.03 520 <10 100 0.05 <20 <50 11 <50
164 ZK11 RL.H-164 33.10 1.10 1.10 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.34 <30 120 7 6 <10 210 130 710 11.8 0.6 <10 40 2.22 890 <10 440 0.05 <20 <50 28 <50
165 RL.H-165 ICP90A 7.04 <30 370 8 0.9 <10 10 <10 10 1.74 4.3 80 40 0.16 340 <10 <10 0.01 <20 <50 <5 <50
166 ZK11 RL.H-166 34.40 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.41 <30 80 5 8.6 <10 280 100 320 12.5 0.3 <10 20 2.11 1200 30 390 0.03 <20 <50 36 <50
167 ZK11 RL.H-167 35.75 1.35 1.35 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.25 <30 50 <5 8.3 <10 290 80 240 9.35 0.4 <10 30 2.64 1260 <10 270 0.04 <20 <50 38 <50
168 ZK11 RL.H-168 36.95 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.2 <30 30 <5 6.8 <10 270 150 330 13.8 0.3 <10 30 2.22 980 20 420 0.02 <20 <50 35 <50
169 ZK11 RL.H-169 38.10 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.13 <30 30 5 7.7 <10 310 70 210 8.92 0.3 <10 20 2.71 1140 <10 300 0.02 <20 <50 40 <50
170 ZK11 RL.H-170 39.35 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.25 <30 60 <5 7 <10 300 70 270 8.96 0.6 <10 40 2.29 1090 20 260 0.02 <20 <50 39 <50
171 ZK11 RL.H-171 40.65 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.46 <30 40 7 9 <10 280 90 240 10.7 0.2 <10 20 1.66 1250 <10 270 0.02 <20 <50 36 <50
172 ZK11 RL.H-172 41.80 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.73 <30 80 6 6.4 <10 320 50 220 7.2 0.6 <10 50 2.34 1010 <10 260 0.03 <20 <50 42 <50
173 ZK11 RL.H-173 43.10 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 8.23 <30 80 <5 6.6 <10 310 90 280 9.95 0.5 <10 50 2.61 1170 <10 270 0.02 <20 <50 40 <50
174 ZK11 RL.H-174 44.20 1.10 1.10 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.24 <30 80 6 6.7 <10 310 60 280 8.05 0.4 <10 40 2.16 950 <10 260 0.03 <20 <50 39 <50
175 ZK11 RL.H-175 44.84 0.64 0.64 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.28 <30 60 9 7.5 <10 270 60 260 7.28 0.4 <10 40 2.05 940 10 220 0.02 <20 <50 38 <50
176 RL.H-176 ICP90A 6.05 480 1510 6 2.6 60 370 30 25300 6.83 2.4 20 20 1.91 920 1280 260 0.13 7870 90 12 120
177 ZK11 RL.H-177 46.29 1.45 1.45 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.95 <30 20 7 8.9 <10 200 50 150 9.7 0.4 <10 40 4.44 1810 <10 70 0.03 <20 <50 43 <50
178 ZK11 RL.H-178 47.74 1.45 1.45 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.47 <30 50 <5 8.1 <10 200 40 130 9.35 0.4 <10 30 4.25 1700 <10 70 0.03 <20 <50 42 <50
179 ZK11 RL.H-179 48.99 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.16 <30 160 <5 7.3 <10 200 50 160 7.99 0.9 <10 40 3.79 1430 <10 80 0.02 <20 <50 38 <50
180 ZK11 RL.H-180 50.29 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 6.43 <30 130 7 9.5 <10 240 80 730 10.5 0.8 <10 30 1.83 2290 10 180 0.03 <20 <50 37 <50
181 ZK11 RL.H-181 51.44 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.22 <30 40 6 7.9 <10 190 40 160 8.9 0.5 <10 20 3.99 1710 <10 70 0.03 <20 <50 40 <50
182 ZK11 RL.H-182 52.59 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.06 <30 20 5 8.4 <10 180 30 100 8.25 0.3 <10 20 3.74 1550 <10 60 0.03 <20 <50 39 <50
183 ZK11 RL.H-183 53.74 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.41 <30 10 <5 7.9 <10 180 40 90 9.37 0.3 <10 20 4.17 1720 <10 60 0.03 <20 <50 42 <50
184 ZK11 RL.H-184 54.89 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.44 <30 30 8 6.6 <10 170 40 140 7.74 0.4 <10 20 3.5 1460 <10 80 0.03 <20 <50 37 <50
185 ZK11 RL.H-185 56.09 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.7 <30 40 8 8.6 <10 280 80 500 9.8 0.3 <10 <10 1.63 1150 20 340 0.03 <20 <50 36 <50
186 ZK11 RL.H-186 57.39 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.67 <30 <10 7 5.7 <10 90 190 1100 24.7 0.1 <10 <10 0.61 1040 60 540 0.01 <20 <50 10 <50
187 RL.H-187 ICP90A 7.06 <30 380 14 0.8 <10 20 <10 20 1.56 4.3 80 40 0.16 340 <10 <10 0.03 <20 <50 <5 <50
188 ZK11 RL.H-188 58.39 1.00 1.00 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.72 <30 40 9 6.2 <10 150 50 280 10.9 0.4 <10 10 0.7 950 160 250 0.03 <20 <50 23 <50
第 2 页,共 10 页
序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩(矿)石 名 称采
样日
期
No. DH No.Sample
No.to Lab自
(From)至
(To)样长
(Length)
Length of
core (m)
Recovery
factor(%)Size(mm) Weight(kg) Rock/Ore type
Samp
ling
date
ME Au AgAl
%
As
ppm
Ba
ppm
Be
ppm
Ca
%
Cd
ppm
Cr
ppm
Co
ppm
Cu
ppm
Fe
%
K
%
La
ppm
Li
ppm
Mg
%
Mn
ppm
Mo
ppm
Ni
ppm
P
%
Pb
ppm
Sb
ppm
Sc
ppm
Sn
ppm
分析结果/Assay Result
基本析样品取样及分析结果登记表
取样位置Sampling location (m)
Sample Log
分析方法/Assay Method
正元国际矿业有限公司W W W . C N Z I M C . C O M
正元国际矿业有限公司W W W . C N Z I M C . C O M
189 ZK11 RL.H-189 59.44 1.05 1.05 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.01 <30 70 7 5.1 <10 150 60 520 13.8 0.5 <10 30 0.68 850 40 340 0.02 <20 <50 22 <50
190 ZK11 RL.H-190 60.44 1.00 1.00 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 1.26 <30 <10 <5 2.2 <10 90 50 280 9.1 0.2 <10 <10 0.28 390 10 180 0.02 <20 <50 5 <50
191 ZK11 RL.H-191 61.44 1.00 1.00 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.06 <30 <10 <5 4.8 <10 50 130 970 26.3 <0.1 <10 <10 0.25 800 120 510 <0.01 <20 <50 <5 <50
192 ZK11 RL.H-192 62.48 1.04 1.04 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 8.09 <30 100 7 8.3 <10 210 40 170 8.22 0.7 <10 20 2.44 1400 <10 110 0.04 <20 <50 34 <50
193 ZK11 RL.H-193 63.73 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.63 <30 60 9 10.2 <10 270 60 280 8.17 0.4 <10 20 1.5 1730 70 190 0.04 <20 <50 32 <50
194 ZK11 RL.H-194 64.98 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.65 <30 70 7 5.5 <10 250 60 370 5.67 0.5 <10 10 0.93 690 <10 180 0.02 <20 <50 30 <50
195 ZK11 RL.H-195 66.23 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.98 <30 60 7 7.4 <10 280 70 360 7.45 0.3 <10 10 1.16 880 <10 240 0.03 <20 <50 34 <50
196 ZK11 RL.H-196 67.38 1.15 1.15 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.16 <30 60 <5 3.8 <10 260 90 920 10.1 0.5 <10 50 2.41 770 <10 370 0.02 <20 <50 33 <50
197 ZK11 RL.H-197 68.58 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.35 <30 80 7 3.9 <10 260 140 1210 11.3 1 <10 30 2.96 910 <10 390 0.03 <20 <50 34 <50
198 RL.H-198 ICP90A 7.39 110 580 <5 0.7 20 40 20 4380 4.91 4.8 10 10 0.87 530 180 30 0.1 2060 70 12 280
199 ZK11 RL.H-199 69.78 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.85 <30 100 7 2.9 <10 290 90 1310 8.78 1.3 <10 50 2.87 560 <10 380 0.03 <20 <50 36 <50
200 ZK11 RL.H-200 70.83 1.05 1.05 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.59 <30 80 5 6 <10 210 60 390 7.65 0.9 <10 30 2.42 1110 <10 160 0.03 <20 <50 35 <50
201 ZK11 RL.H-201 72.75 1.92 1.92 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 7.9 <30 260 <5 1.2 <10 20 <10 20 0.8 2.8 <10 10 0.11 130 <10 <10 <0.01 <20 <50 <5 <50
202 ZK11 RL.H-202 74.00 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 50 7 8.1 <10 220 40 70 8.85 0.7 <10 20 4.14 1710 <10 120 0.05 <20 <50 42 <50
203 ZK11 RL.H-203 75.20 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.86 <30 80 <5 4.2 <10 100 110 510 13.7 0.7 <10 10 0.97 680 20 530 0.02 <20 <50 14 <50
204 ZK11 RL.H-204 76.40 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 5.39 <30 270 <5 5 <10 670 140 290 13.6 0.9 10 40 4.21 810 <10 420 0.08 <20 <50 25 <50
205 ZK11 RL.H-205 77.72 1.32 1.32 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.95 <30 90 <5 3 <10 210 60 1420 10.6 0.7 <10 30 2.43 700 <10 340 0.02 <20 <50 41 <50
206 ZK11 RL.H-206 78.92 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 7.89 <30 80 6 3.2 <10 240 100 280 9.8 0.7 <10 30 2.38 1100 <10 190 0.04 <20 <50 41 <50
207 ZK11 RL.H-207 80.17 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.24 <30 130 <5 4 <10 240 100 180 10.9 0.6 <10 20 1.72 690 <10 260 0.02 <20 <50 31 <50
208 ZK11 RL.H-208 81.42 1.25 1.25 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 4.85 <30 360 <5 2.6 <10 200 30 60 5.68 1.4 20 30 2.44 590 <10 180 0.06 <20 <50 16 <50
209 RL.H-209 ICP90A 7.2 <30 380 11 1.2 <10 30 <10 10 1.77 4.4 80 40 0.19 360 <10 <10 0.02 <20 <50 <5 <50
210 ZK11 RL.H-210 82.62 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 6.84 <30 50 <5 8.2 <10 220 40 190 11.3 0.4 <10 <10 1.49 1200 <10 210 0.03 <20 <50 34 <50
211 ZK11 RL.H-211 83.82 1.20 1.20 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.76 40 <10 <5 6.9 <10 70 100 180 23.8 <0.1 <10 <10 0.2 1100 10 220 0.01 <20 <50 6 <50
212 ZK11 RL.H-212 84.82 1.00 1.00 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 0.31 <30 <10 <5 2.2 <10 40 70 210 14.8 <0.1 <10 <10 0.04 240 10 160 <0.01 <20 <50 <5 <50
213 ZK11 RL.H-213 85.82 1.00 1.00 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 0.32 <30 <10 <5 1 <10 60 30 150 4.66 <0.1 <10 <10 0.05 260 10 150 <0.01 <20 <50 <5 <50
214 ZK11 RL.H-214 86.87 1.05 1.05 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (Altered), Andesite ICP90A 2.65 <30 60 <5 1.9 <10 60 20 210 4.33 0.5 <10 <10 0.1 450 <10 190 0.01 <20 <50 <5 <50
215 ZK11 RL.H-215 88.02 1.15 1.15 100 42/2 长英质火山岩/Felsic Volcanics ICP90A 6.67 <30 320 7 1.1 <10 30 <10 30 1.54 1.6 <10 20 0.18 340 <10 10 0.01 <20 <50 <5 <50
216 ZK11 RL.H-216 89.32 1.30 1.30 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.09 <30 300 <5 1.2 <10 20 <10 30 1.02 2.1 <10 10 0.12 250 <10 <10 <0.01 <20 <50 <5 <50
217 ZK12 RL.H-217 4.57 5.85 1.28 1.25 98 42/2 (变)安山岩/(Altered) Andesite ICP90A 6.87 <30 70 <5 6.7 <10 40 50 100 12 0.4 <10 40 2.79 1720 <10 40 0.06 <20 <50 42 <50
218 ZK12 RL.H-218 46.64 48.04 1.40 1.40 100 42/2 弱黄铁矿化(变)安山岩/Weak Pyrite Mienralization (Altered) Andesite ICP90A 7.16 <30 650 <5 8.5 <10 200 40 160 6.79 1.1 70 50 3.66 1330 <10 100 0.14 <20 <50 27 <50
219 ZK12 RL.H-219 60.52 61.52 1.00 1.00 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.67 <30 40 <5 8.1 <10 300 50 100 8.68 0.4 <10 40 5.19 1590 <10 140 0.02 <20 <50 39 <50
220 RL.H-220 ICP90A FAI323 Au AAS21E Ag 6.06 450 1510 <5 2.7 60 380 30 25600 6.92 2.4 20 20 1.89 950 1290 300 0.13 7850 80 12 120
221 ZK12 RL.H-221 61.92 0.40 0.40 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Pyrrhotite&Pyrite Mineralization(altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.33 <30 140 <5 6.6 <10 390 90 630 15.3 0.6 10 20 0.96 940 20 190 0.03 <20 <50 13 <50
222 ZK12 RL.H-222 63.18 1.26 1.26 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.81 <30 410 <5 6.6 <10 180 70 130 5.1 1.2 30 50 2.27 960 <10 250 0.08 <20 <50 28 <50
223 ZK12 RL.H-223 64.48 1.30 1.30 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.68 <30 120 <5 6.6 <10 310 60 90 5.89 0.5 10 30 2.93 1310 <10 170 0.05 <20 <50 41 <50
224 ZK12 RL.H-224 66.13 1.65 1.65 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.74 <30 70 <5 6.6 <10 200 40 140 6.99 0.4 <10 30 2.29 1200 <10 110 0.04 <20 <50 35 <50
225 ZK12 RL.H-225 67.33 1.20 1.20 100 42/2 硅化(变)安山岩/Silicified (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 6.11 <30 360 <5 4.9 <10 120 20 40 2.88 1.2 20 10 0.35 570 10 90 0.03 <20 <50 15 <50
226 ZK12 RL.H-226 68.58 1.25 1.25 100 42/2 硅化(变)安山岩/Silicified (Altered) Andesite ICP90A 5.37 <30 340 <5 3.4 <10 50 30 120 3.44 1.6 20 20 0.89 600 <10 80 0.03 <20 <50 13 <50
227 ZK9 RL.H-227 12.38 13.43 1.05 1.05 100 42/2 (变)安山岩/(Altered) Andesite ICP90A FAI323 Au 6.67 <30 140 <5 9.2 <10 220 40 90 7.99 1.6 20 40 4.33 3360 <10 100 0.09 130 <50 32 <50
228 ZK9 RL.H-228 14.63 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 6.09 <30 90 <5 7.3 20 90 20 120 7.87 1.8 10 20 2.5 5150 <10 70 0.03 110 <50 18 <50
229 ZK9 RL.H-229 15.83 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 4.6 <30 80 <5 8.2 <10 100 30 190 8.59 1.2 10 30 3.04 4840 <10 80 0.03 <20 <50 14 <50
230 ZK9 RL.H-230 17.13 1.30 1.30 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 4.39 <30 80 <5 10.8 30 130 40 120 13.1 0.9 <10 20 3.99 6040 <10 110 0.03 <20 <50 24 <50
231 RL.H-231 ICP90A 7.02 <30 390 <5 0.8 <10 30 <10 <10 2.04 4.3 90 40 0.2 420 10 <10 0.01 <20 <50 <5 <50
232 ZK9 RL.H-232 18.37 1.24 1.24 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.51 <30 50 <5 6.8 <10 170 40 150 13.2 0.7 <10 10 2.12 2630 <10 120 0.03 <20 <50 11 <50
233 ZK9 RL.H-233 19.37 1.00 1.00 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.72 <30 60 <5 1.6 <10 110 60 210 16.8 1 <10 20 0.79 970 <10 150 0.03 20 <50 7 <50
234 ZK9 RL.H-234 20.42 1.05 1.05 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 0.35 <30 10 <5 2.1 <10 50 10 60 6.35 0.1 <10 <10 0.81 1770 <10 50 <0.01 <20 <50 <5 <50
235 ZK9 RL.H-235 21.62 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 0.91 <30 20 <5 3 <10 70 10 40 5.39 0.2 <10 <10 1.18 2870 <10 30 0.01 <20 <50 <5 <50
236 ZK9 RL.H-236 22.82 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 1.21 <30 10 <5 4 <10 60 10 80 6.81 0.2 <10 <10 1.92 3950 <10 40 0.02 <20 <50 7 <50
237 ZK9 RL.H-237 23.87 1.05 1.05 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 0.51 <30 <10 <5 4.5 <10 30 30 140 12.4 <0.1 <10 <10 2.01 5070 <10 100 0.03 <20 <50 <5 <50
238 ZK9 RL.H-238 25.12 1.25 1.25 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 1.52 <30 30 <5 1.9 <10 60 30 110 9.43 0.5 <10 <10 0.88 1260 <10 80 0.01 <20 <50 6 <50
239 ZK9 RL.H-239 26.27 1.15 1.15 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 4.28 <30 60 <5 2.4 <10 70 70 220 18.4 1.4 20 10 0.92 910 <10 170 0.03 20 <50 9 <50
240 ZK9 RL.H-240 27.37 1.10 1.10 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.67 <30 20 <5 3.1 <10 70 70 260 18.5 0.4 10 20 1.5 1080 <10 170 0.02 <20 <50 6 <50
241 ZK9 RL.H-241 28.57 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 5.2 <30 70 <5 1.8 <10 100 80 360 21.3 1.4 10 30 1.15 1010 <10 200 0.05 40 <50 13 <50
242 RL.H-242 ICP90A FAI323 Au AAS21E Ag 7.4 110 590 <5 0.8 20 40 20 4420 4.9 4.8 20 10 0.88 530 160 30 0.1 2110 70 11 280
243 ZK9 RL.H-243 29.57 1.00 1.00 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 2.31 <30 20 <5 1.7 <10 60 90 210 23.2 0.4 <10 10 1.07 650 <10 210 0.01 <20 <50 5 <50
244 ZK9 RL.H-244 30.77 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.24 <30 10 <5 1.8 <10 50 100 250 25.3 0.3 <10 <10 0.94 650 <10 220 0.02 <20 <50 5 <50
245 ZK9 RL.H-245 31.97 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 4.71 <30 30 <5 2.2 <10 70 40 220 12.1 0.6 20 20 2.31 880 <10 110 0.04 <20 <50 9 <50
246 ZK9 RL.H-246 33.17 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 5.62 30 50 <5 1.3 <10 80 70 170 18.6 0.6 <10 40 1.95 1130 <10 170 0.03 <20 <50 14 <50
247 ZK9 RL.H-247 34.27 1.10 1.10 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 3.96 <30 70 <5 2.9 <10 70 50 180 14.8 0.7 10 10 1.37 740 <10 130 0.03 <20 <50 9 <50
248 ZK9 RL.H-248 35.51 1.24 1.24 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 6.98 <30 60 <5 5.9 <10 250 40 100 10.7 0.5 10 20 3.63 1600 <10 100 0.08 <20 <50 34 <50
249 ZK9 RL.H-249 36.91 1.40 1.40 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au 6.75 <30 70 <5 3.9 <10 120 50 120 12.5 1.4 10 30 2.48 1130 <10 100 0.05 <20 <50 28 <50
250 ZK9 RL.H-250 38.16 1.25 1.25 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization (Altered) Andesite ICP90A FAI323 Au AAS21E Ag 2.72 <30 60 <5 4.2 <10 70 40 110 11 0.7 <10 10 1.34 1460 <10 80 0.02 <20 <50 11 <50
251 ZK9 RL.H-251 39.46 1.30 1.30 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.21 <30 90 <5 7.3 <10 130 40 120 10.3 0.7 <10 20 3.76 1980 <10 50 0.04 <20 <50 44 <50
252 ZK9 RL.H-252 40.66 1.20 1.20 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.43 <30 110 <5 8.5 <10 130 50 140 11 1.6 <10 30 3.05 4890 <10 80 0.06 60 <50 38 <50
253 RL.H-253 ICP90A FAI323 Au 7.12 <30 410 <5 0.8 <10 40 <10 <10 1.72 4.4 90 40 0.18 370 <10 <10 0.02 <20 <50 <5 <50
254 ZK9 RL.H-254 41.76 1.10 1.10 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 6.87 <30 40 <5 9.1 <10 130 40 110 10.4 0.5 <10 20 3.25 2280 <10 60 0.06 <20 <50 35 <50
255 ZK9 RL.H-255 42.96 1.20 1.20 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 6.88 <30 50 <5 9.5 <10 110 40 140 10 0.4 <10 20 2.76 2070 <10 70 0.06 <20 <50 34 <50
256 ZK9 RL.H-256 44.16 1.20 1.20 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.14 <30 <10 <5 6.7 <10 120 50 140 11 0.1 <10 20 3.61 1720 <10 70 0.06 <20 <50 36 <50
257 ZK9 RL.H-257 45.51 1.35 1.35 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.4 <30 10 <5 7.6 <10 120 50 110 10.7 0.1 <10 20 3.42 1870 <10 70 0.06 <20 <50 37 <50
258 ZK9 RL.H-258 46.71 1.20 1.20 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.37 <30 60 <5 8.1 <10 130 40 110 11 0.2 <10 20 3.46 2110 <10 70 0.07 <20 <50 36 <50
259 ZK9 RL.H-259 47.85 1.14 1.14 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.49 <30 260 <5 8.3 <10 140 50 120 10.5 0.6 <10 20 2.85 1920 <10 60 0.07 <20 <50 36 <50
260 ZK9 RL.H-260 49.05 1.20 1.20 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.57 <30 140 <5 7 <10 140 40 120 10.4 0.4 <10 20 3.47 1980 <10 60 0.07 <20 <50 37 <50
261 ZK9 RL.H-261 50.15 1.10 1.10 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.58 <30 180 <5 6.7 <10 270 50 90 9.39 0.5 10 20 4.13 1860 <10 130 0.08 <20 <50 34 <50
262 ZK9 RL.H-262 51.09 0.94 0.94 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.74 <30 200 <5 7.8 <10 240 40 70 7.93 0.7 10 40 3.54 1760 <10 120 0.07 <20 <50 31 <50
263 ZK9 RL.H-263 52.09 1.00 1.00 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au 7.79 <30 80 <5 8.2 <10 130 40 120 10.4 0.7 <10 20 2.97 1840 <10 60 0.07 <20 <50 38 <50
264 RL.H-264 ICP90A FAI323 Au 6.01 460 1510 <5 2.7 60 370 30 25800 6.69 2.4 20 20 1.84 930 1260 250 0.13 7790 80 12 120
265 ZK9 RL.H-265 53.29 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au 5.96 <30 100 <5 10.1 <10 100 30 170 7.92 1 <10 20 3.35 2110 <10 50 0.05 20 <50 26 <50
266 ZK9 RL.H-266 54.35 1.06 1.06 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au 6.72 <30 150 <5 3.9 <10 80 30 140 8.27 2 20 30 1.82 890 <10 70 0.05 <20 <50 20 <50
267 ZK9 RL.H-267 55.70 1.35 1.35 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au AAS21E Ag 4.21 <30 130 <5 2 <10 90 50 200 18.3 1.5 20 30 1.07 850 <10 130 0.04 <20 <50 8 <50
268 ZK9 RL.H-268 57.00 1.30 1.30 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au AAS21E Ag 0.76 <30 20 <5 2.6 <10 30 50 260 17 0.2 <10 <10 1.53 1210 <10 120 0.02 <20 <50 <5 <50
269 ZK9 RL.H-269 58.00 1.00 1.00 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Mineralization(altered), Andesite ICP90A FAI323 Au 4.53 <30 90 <5 4.9 <10 120 40 270 15 0.6 10 30 2.18 3600 <10 110 0.03 <20 <50 18 <50
270 ZK9 RL.H-270 59.17 1.17 1.17 100 42/2 (变)安山岩/(Altered) Andesite ICP90A FAI323 Au 7.75 <30 150 <5 8.2 <10 320 40 80 9.03 0.5 10 30 4.93 1640 <10 140 0.04 <20 <50 36 <50
271 ZK13 RL.H-271 6.62 7.75 1.13 1.13 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.68 <30 330 <5 6.3 <10 240 40 210 7.31 2.6 <10 50 1.76 1970 <10 130 0.03 <20 <50 43 <50
272 ZK13 RL.H-272 8.80 1.05 1.05 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.69 <30 140 <5 7.4 <10 250 50 290 8.55 2.7 <10 30 2 2200 <10 140 0.03 <20 <50 49 <50
273 ZK13 RL.H-273 9.90 1.10 1.10 100 42/2 磁黄铁矿化黄铁矿化黄铜矿化(变)安山岩/Pyrrhotite&Pyrite&Chalcopyrite Mineralization(Altered), Andesite ICP90A 7.89 <30 160 <5 5.6 <10 260 50 3010 8.83 2.4 <10 40 1.79 1730 <10 130 0.03 <20 <50 42 <50
274 ZK13 RL.H-274 10.76 0.86 0.86 100 42/2 磁黄铁矿化黄铁矿化黄铜矿化(变)安山岩/Pyrrhotite&Pyrite&Chalcopyrite Mineralization(Altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.06 <30 130 <5 4.2 <10 210 180 1330 14.2 2.2 <10 30 1.75 1300 <10 220 0.03 <20 <50 30 <50
275 RL.H-275 ICP90A FAI323 Au AAS21E Ag 7 <30 530 <5 1.5 <10 20 <10 <10 1.57 4.3 90 40 0.17 320 <10 <10 0.01 <20 <50 <5 <50
276 ZK13 RL.H-276 11.86 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.36 <30 140 <5 9.6 <10 230 50 300 7.23 2.4 <10 40 2.44 2090 <10 140 0.03 <20 <50 35 <50
277 ZK13 RL.H-277 12.96 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 9.71 <30 180 <5 5.1 <10 300 70 290 7.89 3.1 <10 50 1.76 1480 <10 190 0.03 <20 <50 47 <50
278 ZK13 RL.H-278 123.14 124.14 1.00 1.00 100 42/2 辉长岩/Gabbro ICP90A 7.99 <30 660 <5 6.4 <10 90 40 70 7.46 1.8 30 60 4.68 1070 <10 70 0.29 <20 <50 30 <50
279 ZK13 RL.H-279 125.14 1.00 1.00 100 42/2 辉长岩/Gabbro ICP90A 8.07 <30 640 <5 6.6 <10 100 40 80 7.74 1.7 30 50 4.93 1100 <10 70 0.3 <20 <50 31 <50
280 ZK7 RL.H-280 1.30 2.40 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.19 <30 70 <5 4.5 <10 310 50 120 9.29 0.3 <10 20 3.42 2780 <10 120 0.04 <20 <50 38 <50
281 ZK7 RL.H-281 3.60 1.20 1.20 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.14 <30 280 <5 7.1 <10 420 60 240 8.96 0.5 30 20 4.9 2280 <10 210 0.12 <20 <50 26 <50
282 ZK7 RL.H-282 4.90 1.30 1.30 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.1 <30 300 <5 3.9 <10 360 50 130 8.77 0.6 20 40 3.84 2400 <10 200 0.09 <20 <50 34 <50
第 3 页,共 10 页
序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩(矿)石 名 称采
样日
期
No. DH No.Sample
No.to Lab自
(From)至
(To)样长
(Length)
Length of
core (m)
Recovery
factor(%)Size(mm) Weight(kg) Rock/Ore type
Samp
ling
date
ME Au AgAl
%
As
ppm
Ba
ppm
Be
ppm
Ca
%
Cd
ppm
Cr
ppm
Co
ppm
Cu
ppm
Fe
%
K
%
La
ppm
Li
ppm
Mg
%
Mn
ppm
Mo
ppm
Ni
ppm
P
%
Pb
ppm
Sb
ppm
Sc
ppm
Sn
ppm
分析结果/Assay Result
基本析样品取样及分析结果登记表
取样位置Sampling location (m)
Sample Log
分析方法/Assay Method
正元国际矿业有限公司W W W . C N Z I M C . C O M
正元国际矿业有限公司W W W . C N Z I M C . C O M
283 ZK7 RL.H-283 6.12 1.22 1.20 98 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.73 <30 70 <5 2 <10 320 50 110 9.83 0.2 <10 40 2.43 2890 <10 120 0.04 <20 <50 42 <50
284 ZK7 RL.H-284 7.22 1.10 1.08 98 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 8.73 <30 240 <5 2.4 <10 330 80 250 10.5 0.3 <10 30 1.75 2750 <10 160 0.04 <20 <50 38 <50
285 ZK7 RL.H-285 8.23 1.01 1.00 98 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.63 <30 240 <5 2.4 <10 350 80 210 11 0.3 <10 20 1.69 2800 <10 170 0.04 <20 <50 31 <50
286 RL.H-286 ICP90A 6.94 90 540 <5 0.7 20 30 20 4150 4.49 4.4 20 10 0.84 500 160 30 0.08 1940 60 11 250
287 ZK7 RL.H-287 9.40 1.17 1.17 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.07 <30 80 <5 2.8 <10 280 90 440 12.7 0.2 <10 20 1.9 2810 <10 170 0.04 <20 <50 29 <50
288 ZK7 RL.H-288 10.50 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.6 <30 70 <5 5.5 <10 210 40 120 7.68 0.1 <10 <10 2.55 3010 <10 80 0.04 <20 <50 45 <50
289 ZK7 RL.H-289 28.77 29.87 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.93 <30 40 <5 3.8 <10 150 50 110 13.8 <0.1 <10 30 2.39 3360 <10 80 0.06 <20 <50 40 <50
290 ZK7 RL.H-290 30.81 0.94 0.94 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.38 <30 250 <5 2.5 <10 100 50 160 12.1 1 <10 40 1.79 2170 <10 80 0.05 <20 <50 27 <50
291 ZK7 RL.H-291 31.81 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.07 <30 820 <5 2.4 <10 30 <10 <10 1.85 2.1 10 20 0.58 420 <10 <10 0.06 <20 <50 <5 <50
292 ZK7 RL.H-292 32.81 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.85 <30 560 <5 1.8 <10 130 30 310 6.06 2.4 20 20 1.21 500 <10 80 0.07 <20 <50 10 <50
293 ZK7 RL.H-293 33.81 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.47 <30 180 <5 1.1 <10 60 60 250 12.6 1.4 10 30 1.12 1170 <10 130 0.04 <20 <50 14 <50
294 ZK7 RL.H-294 34.91 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.04 <30 40 <5 5.7 <10 130 40 70 11.4 0.2 <10 20 3.43 2570 <10 70 0.06 <20 <50 36 <50
295 ZK7 RL.H-295 36.11 1.20 1.20 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.64 <30 50 <5 5.3 <10 140 50 110 10.4 0.2 <10 20 3.66 2300 <10 60 0.07 <20 <50 37 <50
296 ZK7 RL.H-296 43.51 44.81 1.30 1.30 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.37 <30 700 <5 5.4 <10 140 50 130 10.6 1.4 <10 50 2.89 1730 <10 80 0.07 <20 <50 43 <50
297 RL.H-297 ICP90A 7.14 <30 470 6 0.7 <10 <10 <10 <10 1.61 4.3 90 40 0.18 350 <10 <10 0.02 <20 <50 <5 <50
298 ZK7 RL.H-298 46.01 1.20 1.20 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 8.05 <30 170 <5 3.4 <10 100 40 100 12.2 1.3 10 30 2.46 1420 <10 60 0.11 <20 <50 42 <50
299 ZK7 RL.H-299 46.91 0.90 0.90 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.37 <30 130 <5 6.7 <10 40 30 60 10.7 1.2 10 20 2.73 2390 <10 30 0.1 <20 <50 35 <50
300 ZK7 RL.H-300 47.91 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.48 <30 80 <5 5.7 <10 40 30 50 12.2 0.6 <10 10 2.7 2200 <10 20 0.11 <20 <50 35 <50
301 ZK7 RL.H-301 49.01 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.8 <30 90 <5 3.9 <10 80 30 110 11.2 0.7 10 60 2.1 1230 <10 60 0.07 <20 <50 19 <50
302 ZK7 RL.H-302 49.91 0.90 0.90 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 7.03 <30 160 <5 0.7 <10 80 40 110 13.1 1.4 20 50 1.33 610 <10 130 0.04 <20 <50 13 <50
303 ZK7 RL.H-303 50.90 0.99 0.99 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 3.96 <30 70 <5 3.8 <10 110 30 220 13.1 0.6 <10 10 1.5 1820 <10 100 0.02 <20 <50 13 <50
304 ZK7 RL.H-304 52.00 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 7.67 <30 100 <5 4.5 <10 240 40 130 11.4 0.9 <10 30 4.66 1710 <10 120 0.03 <20 <50 35 <50
305 ZK7 RL.H-305 53.10 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.85 <30 90 <5 4.4 <10 50 30 70 10.9 1 10 40 2.88 1570 <10 50 0.11 <20 <50 37 <50
306 ZK7 RL.H-306 54.20 1.10 1.10 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.33 <30 120 <5 0.3 <10 110 60 210 13.4 1.6 10 30 0.92 530 <10 120 0.03 <20 <50 16 <50
307 ZK7 RL.H-307 55.40 1.20 1.20 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 6.38 <30 140 <5 0.4 <10 70 40 130 8.85 1.4 20 60 1.44 430 <10 110 0.03 30 <50 10 <50
308 RL.H-308 ICP90A 6.14 470 1550 <5 2.6 60 370 30 26200 6.7 2.5 20 20 1.87 900 1260 260 0.12 8060 90 12 120
309 ZK7 RL.H-309 56.40 1.00 1.00 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 7.09 <30 80 <5 2.4 <10 50 50 250 12.7 0.6 10 70 2.14 1290 <10 60 0.08 20 <50 30 <50
310 ZK7 RL.H-310 57.27 0.87 0.87 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite Mineralization (altered), Andesite ICP90A 7.09 <30 90 <5 4.4 <10 40 40 80 12.3 0.6 10 20 2.47 1740 <10 30 0.11 <20 <50 36 <50
311 ZK7 RL.H-311 58.27 1.00 1.00 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 6.93 <30 20 <5 5 <10 40 40 40 12.6 <0.1 10 <10 2.17 1720 <10 20 0.11 <20 <50 36 <50
312 ZK7 RL.H-312 74.59 75.59 1.00 1.00 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 9.11 <30 270 <5 1.3 <10 160 30 110 5.23 3.3 20 20 1.6 1030 <10 80 0.03 <20 <50 21 <50
313 ZK7 RL.H-313 76.79 1.20 1.20 100 42/2 (变)安山岩夹黄铁矿细脉/(Altered) Andesite, associated with Pyrite veinlets ICP90A 8.47 <30 270 <5 0.5 <10 150 40 160 7.03 3 20 20 1.5 980 <10 100 0.03 <20 <50 22 <50
314 ZK7 RL.H-314 77.79 1.00 1.00 100 42/2 (变)安山岩夹黄铁矿细脉/(Altered) Andesite, associated with Pyrite veinlets ICP90A FAI323 Au AAS21E Ag 7.74 <30 390 <5 2 <10 200 30 110 6.6 2.4 20 20 2.21 1370 <10 110 0.05 <20 <50 19 <50
315 ZK7 RL.H-315 78.74 0.95 0.95 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.23 <30 420 <5 3.6 <10 310 40 100 8.54 1.3 20 20 3.57 1930 <10 140 0.08 <20 <50 25 <50
316 ZK2 RL.H-316 36.15 37.35 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A FAI323 Au AAS21E Ag 8.85 <30 690 <5 4.1 <10 250 40 700 7.09 2.2 20 30 2.42 930 <10 80 0.07 <20 <50 24 <50
317 ZK2 RL.H-317 38.10 0.75 0.75 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 7.91 <30 900 <5 4.7 <10 90 40 230 6.36 1.4 20 20 2.46 980 <10 50 0.14 <20 <50 17 <50
318 ZK2 RL.H-318 39.10 1.00 1.00 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.92 <30 690 <5 5.9 <10 230 30 190 6.87 0.9 20 20 3.96 1280 <10 70 0.14 <20 <50 24 <50
319 RL.H-319 ICP90A 6.89 <30 430 6 0.7 <10 20 <10 <10 1.58 4.2 90 40 0.17 340 <10 <10 0.02 <20 <50 <5 <50
320 ZK10 RL.H-320 50.29 51.39 1.10 1.10 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (altered), Andesite ICP90A 7.44 <30 80 <5 10.2 <10 270 30 130 5.86 1.2 <10 40 4.82 1970 <10 70 0.02 <20 <50 38 <50
321 ZK10 RL.H-321 52.69 1.30 1.30 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (altered), Andesite ICP90A 6.96 <30 80 6 10.2 <10 210 30 300 5.97 1.5 <10 50 4.48 2080 <10 60 0.04 <20 <50 34 <50
322 ZK10 RL.H-322 53.64 0.95 0.95 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (altered), Andesite ICP90A 7.42 <30 120 <5 4.9 <10 130 40 310 5.84 1.5 <10 30 2.81 1020 <10 60 0.05 <20 <50 34 <50
323 ZK10 RL.H-323 54.56 0.92 0.92 100 42/2 黄铁矿化(变)安山岩/Pyrite Mineralization (altered), Andesite ICP90A 8.22 <30 170 6 5.6 <10 170 40 180 9.02 2.7 <10 60 3.96 1250 <10 70 0.09 <20 <50 48 <50
324 ZK13 RL.H-324 104.85 105.95 1.10 1.10 100 42/2 辉长岩/Gabbro ICP90A 8.17 <30 720 <5 5.9 <10 110 30 100 7.12 1.8 30 40 4.27 1020 <10 60 0.26 <20 <50 28 <50
325 ZK13 RL.H-325 107.25 1.30 1.30 100 42/2 辉长岩/Gabbro ICP90A 8.29 <30 760 <5 6 <10 130 30 80 7.01 2 30 30 4.25 1020 <10 70 0.27 <20 <50 27 <50
326 ZK8 RL.H-326 41.15 42.30 1.15 1.15 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7.61 <30 70 <5 7.8 <10 190 50 110 13.4 0.6 <10 40 2.55 5140 <10 120 0.04 <20 <50 38 <50
327 ZK8 RL.H-327 43.55 1.25 1.25 100 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7.96 <30 80 <5 8 <10 200 60 100 11.2 0.6 <10 40 2.43 4470 <10 120 0.04 <20 <50 39 <50
328 ZK8 RL.H-328 58.69 60.00 1.31 1.30 99 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.81 <30 170 <5 6.9 <10 230 60 190 8.11 0.3 <10 30 2.13 3300 <10 150 0.04 <20 <50 41 <50
329 ZK8 RL.H-329 60.65 0.65 0.64 99 42/2 弱磁黄铁矿化黄铜矿化(变)安山岩/Weak Pyrrhotite&Chalcopyrite Mineralzation (Altered) Andesite ICP90A 6.4 <30 100 <5 11.2 <10 160 70 1170 14.2 0.5 <10 50 2 5330 <10 110 0.03 <20 <50 34 <50
330 RL.H-330 ICP90A 7.35 80 540 <5 0.8 20 40 20 4300 4.74 4.6 20 10 0.89 550 160 30 0.09 2030 70 12 250
331 ZK8 RL.H-331 61.91 1.26 1.25 99 42/2 (变)安山岩/(Altered) Andesite ICP90A 8.94 <30 190 <5 5.7 <10 220 60 160 6.87 0.4 <10 30 2.06 2670 <10 130 0.06 <20 <50 42 <50
332 ZK8 RL.H-332 114.30 115.58 1.28 1.25 98 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7 <30 90 <5 7.8 <10 80 50 170 13.4 0.3 <10 40 3.14 5090 <10 60 0.05 400 <50 46 <50
333 ZK8 RL.H-333 116.65 1.07 1.05 98 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7.03 <30 100 <5 7 <10 60 50 160 11.2 0.5 <10 40 2.75 4270 <10 60 0.05 <20 <50 45 <50
334 ZK8 RL.H-334 117.85 1.20 1.18 98 42/2 弱磁黄铁矿化(变)安山岩/Weak Pyrrhotite Mineralizaiton, (altered) Andesite ICP90A 7 <30 20 <5 8.3 <10 70 50 240 12.2 0.2 <10 30 2.42 4360 <10 60 0.05 <20 <50 45 <50
335 ZK6 RL.H-335 11.39 12.44 1.05 1.05 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 320 <5 8.5 <10 280 60 300 9.06 1.5 <10 40 3.86 1720 <10 140 0.03 <20 <50 39 <50
336 ZK6 RL.H-336 13.54 1.10 1.10 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.64 <30 140 <5 9 <10 300 40 130 7.57 1 <10 30 3.87 1470 <10 130 0.02 <20 <50 37 <50
337 ZK6 RL.H-337 14.62 1.08 1.08 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.34 <30 230 <5 7.8 <10 310 90 210 9.92 1.4 <10 50 4.55 1340 <10 140 0.03 <20 <50 34 <50
338 ZK6 RL.H-338 15.85 1.23 1.23 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.9 <30 160 <5 0.7 <10 60 <10 60 0.73 3.9 30 10 0.08 200 <10 <10 0.01 30 <50 <5 <50
339 ZK6 RL.H-339 16.60 0.75 0.75 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.17 <30 170 <5 8.6 <10 240 30 210 6.9 1.4 <10 50 3.19 1700 <10 100 0.03 <20 <50 29 <50
340 ZK6 RL.H-340 18.06 1.46 1.46 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.92 <30 360 <5 0.6 <10 30 <10 30 1.09 4 20 10 0.08 210 <10 <10 <0.01 30 <50 <5 <50
341 RL.H-341 ICP90A 7.12 <30 460 6 0.7 <10 20 <10 40 1.38 4.6 90 40 0.15 330 <10 <10 0.01 <20 <50 <5 <50
342 ZK6 RL.H-342 19.36 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 8.28 <30 120 <5 12.7 <10 360 40 100 8.23 1.3 <10 40 2.82 2470 20 110 0.03 <20 <50 40 <50
343 ZK6 RL.H-343 20.51 1.15 1.15 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 8.55 <30 230 <5 9 <10 340 50 140 7.67 2.4 <10 50 2.48 1500 <10 150 0.03 <20 <50 43 <50
344 ZK6 RL.H-344 21.66 1.15 1.15 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 6 <30 120 <5 9.8 <10 1060 20 280 8.1 1.3 <10 40 3.85 1760 <10 160 0.03 720 <50 33 <50
345 ZK6 RL.H-345 22.16 0.50 0.50 100 42/2 块状硫化物(Po)/VMS (Po) ICP90A 0.74 <30 <10 <5 3.3 <10 30 <10 1100 >30 0.2 <10 <10 0.57 540 20 220 <0.01 <20 <50 <5 <50
346 ZK6 RL.H-346 23.61 1.45 1.44 99 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 6.97 <30 620 <5 3.5 <10 440 20 110 6.16 1.7 20 30 2.56 1040 <10 70 0.07 <20 <50 17 <50
347 ZK6 RL.H-347 24.54 0.93 0.92 99 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 4.62 <30 700 <5 1.4 <10 80 70 730 23.7 1.7 30 20 0.92 710 <10 140 0.06 <20 <50 <5 <50
348 ZK6 RL.H-348 25.22 0.68 0.67 99 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A 0.93 <30 80 <5 1.4 <10 70 40 870 >30 0.3 <10 <10 0.59 430 <10 270 0.02 <20 <50 <5 <50
349 ZK6 RL.H-349 26.26 0.94 0.93 99 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 4.1 <30 150 <5 4.5 <10 720 20 790 20.3 0.7 <10 20 2.96 1300 <10 170 0.01 <20 <50 17 <50
350 ZK6 RL.H-350 27.23 1.07 1.07 100 42/2 中性侵入岩/Intermediate Intrusive ICP90A 7.69 <30 1220 <5 1.9 <10 90 <10 60 2.98 3 40 60 1.04 490 <10 50 0.07 <20 <50 <5 <50
351 ZK6 RL.H-351 28.60 1.37 1.37 100 42/2 块状-稠密浸染状硫化物(Po,Py)/Massive-deseminated VMS (Po,Py) ICP90A FAI323 Au AAS21E Ag 0.46 <30 <10 <5 1.3 <10 40 50 1160 >30 <0.1 <10 <10 0.55 580 <10 250 <0.01 <20 <50 <5 <50
352 RL.H-352 ICP90A FAI323 Au AAS21E Ag 5.89 410 1510 <5 2.6 60 370 30 24700 6.74 2.4 20 20 1.85 950 1240 250 0.11 7750 90 12 110
353 ZK6 RL.H-353 29.80 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 3.61 <30 10 <5 0.8 <10 50 <10 300 7.16 1.7 <10 <10 0.38 500 30 30 <0.01 20 <50 <5 <50
354 ZK6 RL.H-354 31.00 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.78 <30 10 <5 1.6 <10 40 10 210 9.13 0.1 <10 <10 0.72 830 20 40 0.02 <20 <50 <5 <50
355 ZK6 RL.H-355 32.00 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.4 <30 20 <5 2.6 <10 40 30 390 15.2 0.1 <10 <10 1.21 1250 <10 50 0.02 <20 <50 <5 <50
356 ZK6 RL.H-356 33.22 1.22 1.20 98 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.2 <30 20 <5 1.8 <10 60 10 460 18.9 0.3 <10 10 1.39 2130 <10 80 0.02 <20 <50 5 <50
357 ZK6 RL.H-357 34.49 1.27 1.25 98 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 3.7 <30 70 <5 5.8 <10 720 50 160 9.29 0.4 <10 20 3.7 1190 <10 120 0.03 <20 <50 22 <50
358 ZK6 RL.H-358 35.75 1.26 1.25 99 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 5.41 <30 40 <5 3.6 <10 1120 40 270 14.9 0.7 <10 50 6.01 1740 <10 260 0.03 <20 <50 30 <50
359 ZK6 RL.H-359 37.10 1.35 1.35 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.77 <30 <10 <5 1.9 <10 80 80 410 24.1 0.2 <10 90 1.9 1830 <10 80 0.03 <20 <50 6 <50
360 ZK6 RL.H-360 38.10 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.28 <30 80 <5 6.1 <10 860 40 140 7.78 0.6 <10 50 6.41 1980 <10 120 0.02 <20 <50 45 <50
361 ZK6 RL.H-361 39.10 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.78 <30 100 <5 5.7 <10 790 40 150 7.02 0.9 <10 60 5.83 2110 <10 130 0.02 <20 <50 47 <50
362 ZK6 RL.H-362 40.00 0.90 0.90 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.6 <30 <10 <5 1.5 <10 90 110 260 26.1 0.2 <10 10 1.23 1060 <10 170 <0.01 <20 <50 <5 <50
363 RL.H-363 ICP90A 7.02 <30 380 8 0.7 <10 30 <10 30 1.96 4.5 80 40 0.17 400 <10 <10 0.01 <20 <50 <5 <50
364 ZK6 RL.H-364 40.90 0.90 0.90 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.98 <30 50 <5 2.4 <10 30 60 350 >30 0.4 <10 10 1.02 1330 <10 170 0.02 <20 <50 <5 <50
365 ZK6 RL.H-365 41.79 0.89 0.89 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.66 <30 40 <5 2.1 <10 60 20 390 19.8 0.5 <10 30 1.43 1080 <10 110 <0.01 <20 <50 6 <50
366 ZK6 RL.H-366 42.86 1.07 1.07 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.05 <30 10 <5 1.9 <10 60 <10 100 8.49 0.3 <10 10 0.73 1140 20 40 <0.01 <20 <50 <5 <50
367 ZK6 RL.H-367 44.36 1.50 1.50 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.63 <30 200 <5 0.7 <10 40 <10 50 1.5 3.9 20 <10 0.16 360 <10 <10 0.01 20 <50 <5 <50
368 ZK6 RL.H-368 45.86 1.50 1.50 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.72 <30 320 <5 0.7 <10 30 <10 60 1.18 4 30 <10 0.06 300 <10 <10 0.01 30 <50 <5 <50
369 ZK6 RL.H-369 46.92 1.06 1.06 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.74 <30 30 <5 3.3 <10 60 <10 170 15.1 0.6 <10 <10 1.31 1880 <10 70 0.02 <20 <50 <5 <50
370 ZK6 RL.H-370 47.80 0.88 0.88 100 42/2 块状硫化物(Py,Po)/VMS (Py,Po) ICP90A 0.7 <30 <10 <5 2.2 <10 30 360 320 >30 0.1 <10 <10 0.6 2060 <10 110 0.02 <20 <50 <5 <50
371 ZK6 RL.H-371 48.90 1.10 1.10 100 42/2 块状硫化物(Py,Po)/VMS (Py,Po) ICP90A 0.42 <30 <10 <5 2.3 <10 40 40 290 >30 0.1 <10 <10 0.51 1840 <10 120 <0.01 <20 <50 <5 <50
372 ZK6 RL.H-372 50.10 1.20 1.20 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.25 <30 <10 5 4.4 <10 20 40 390 >30 <0.1 <10 <10 0.36 1770 <10 220 0.02 <20 <50 <5 <50
373 ZK6 RL.H-373 51.33 1.23 1.20 98 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.49 <30 <10 <5 2.1 <10 140 70 310 >30 0.2 <10 <10 0.42 2450 <10 200 0.01 <20 <50 <5 <50
374 RL.H-374 ICP90A 7.24 100 600 <5 0.8 20 50 20 4330 4.85 4.9 20 10 0.86 550 170 30 0.09 2130 80 12 270
375 ZK6 RL.H-375 52.59 1.26 1.22 97 42/2 块状-稠密浸染状硫化物(Po,Py)/Massive-deseminated VMS (Po,Py) ICP90A 0.21 <30 <10 <5 3 <10 90 <10 150 27 <0.1 <10 <10 0.98 2340 <10 140 <0.01 <20 <50 <5 <50
376 ZK6 RL.H-376 53.82 1.23 1.20 98 42/2 块状-稠密浸染状硫化物(Po,Py)/Massive-deseminated VMS (Po,Py) ICP90A 0.37 <30 <10 <5 4.7 <10 50 20 330 >30 <0.1 <10 <10 1.4 1390 <10 140 <0.01 20 <50 <5 <50
第 4 页,共 10 页
序号 工程编号 送样编号 岩矿心长 采取率 采样规格 样品重量 岩(矿)石 名 称采
样日
期
No. DH No.Sample
No.to Lab自
(From)至
(To)样长
(Length)
Length of
core (m)
Recovery
factor(%)Size(mm) Weight(kg) Rock/Ore type
Samp
ling
date
ME Au AgAl
%
As
ppm
Ba
ppm
Be
ppm
Ca
%
Cd
ppm
Cr
ppm
Co
ppm
Cu
ppm
Fe
%
K
%
La
ppm
Li
ppm
Mg
%
Mn
ppm
Mo
ppm
Ni
ppm
P
%
Pb
ppm
Sb
ppm
Sc
ppm
Sn
ppm
分析结果/Assay Result
基本析样品取样及分析结果登记表
取样位置Sampling location (m)
Sample Log
分析方法/Assay Method
正元国际矿业有限公司W W W . C N Z I M C . C O M
正元国际矿业有限公司W W W . C N Z I M C . C O M
377 ZK6 RL.H-377 55.08 1.26 1.25 99 42/2 块状-稠密浸染状硫化物(Po,Py)/Massive-deseminated VMS (Po,Py) ICP90A 0.42 <30 <10 <5 3.1 <10 30 10 370 >30 <0.1 <10 <10 0.76 1000 <10 210 <0.01 <20 <50 <5 <50
378 ZK6 RL.H-378 56.39 1.31 1.29 99 42/2 块状-稠密浸染状硫化物(Po,Py)/Massive-deseminated VMS (Po,Py) ICP90A FAI323 Au AAS21E Ag 0.75 <30 30 <5 2.9 <10 30 30 350 >30 0.1 <10 <10 0.94 5450 <10 180 <0.01 <20 <50 <5 <50
379 ZK6 RL.H-379 57.64 1.25 1.25 100 42/2 稠密浸染状硫化物(Po,Py)/intensively Diseminated VMS (Po,Py) ICP90A 1.01 <30 50 <5 1.9 <10 20 60 320 >30 0.3 <10 <10 0.63 5210 <10 140 0.01 <20 <50 <5 <50
380 ZK6 RL.H-380 58.94 1.30 1.30 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.86 <30 40 <5 2.2 <10 20 40 470 >30 0.3 <10 <10 0.91 3670 <10 170 <0.01 <20 <50 <5 <50
381 ZK6 RL.H-381 60.18 1.24 1.24 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.56 <30 <10 <5 2.1 <10 20 110 480 >30 0.1 <10 <10 0.89 2180 <10 130 0.01 <20 <50 <5 <50
382 ZK6 RL.H-382 61.38 1.20 1.20 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.4 <30 <10 <5 2.2 <10 20 160 640 >30 <0.1 <10 <10 0.97 2780 <10 110 0.02 30 <50 <5 <50
383 ZK6 RL.H-383 62.48 1.10 1.10 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A 0.75 <30 <10 <5 3.2 <10 10 110 260 >30 <0.1 <10 <10 1.4 3120 <10 100 <0.01 <20 <50 <5 <50
384 ZK6 RL.H-384 63.63 1.15 1.15 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.58 <30 20 <5 1.9 <10 20 160 250 >30 0.2 <10 <10 0.28 3340 <10 120 0.01 <20 <50 <5 <50
385 RL.H-385 ICP90A FAI323 Au AAS21E Ag 6.9 <30 510 8 0.9 <10 20 <10 40 2.63 4.5 80 40 0.17 450 <10 10 0.02 <20 <50 <5 <50
386 ZK6 RL.H-386 64.83 1.20 1.20 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A 0.94 <30 50 <5 2 <10 20 110 220 >30 0.4 <10 <10 0.33 4610 <10 140 0.01 <20 <50 <5 <50
387 ZK6 RL.H-387 66.13 1.30 1.30 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A 1.38 <30 50 <5 3.2 <10 20 80 260 >30 0.4 <10 <10 0.6 4810 <10 140 <0.01 <20 <50 <5 <50
388 ZK6 RL.H-388 67.13 1.00 1.00 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 1.11 <30 30 <5 2.2 <10 20 120 270 >30 0.3 <10 <10 0.33 6540 <10 150 0.01 <20 <50 <5 <50
389 ZK6 RL.H-389 68.28 1.15 1.15 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A 1.42 <30 50 <5 2.5 <10 20 90 270 >30 0.5 <10 <10 0.47 6560 <10 130 <0.01 <20 <50 <5 <50
390 ZK6 RL.H-390 69.48 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 4.55 <30 130 <5 4.2 <10 50 10 170 16.9 1.3 10 10 1.45 1410 <10 80 0.03 <20 <50 8 <50
391 ZK6 RL.H-391 70.68 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 6.26 <30 230 7 4.2 <10 60 <10 130 12.2 2 20 20 1.13 1290 <10 60 0.05 <20 <50 14 <50
392 ZK6 RL.H-392 71.98 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 4.98 <30 150 7 2.9 <10 50 30 180 18 1.7 <10 10 0.9 1840 <10 100 0.03 <20 <50 13 <50
393 ZK6 RL.H-393 72.98 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.28 <30 30 5 2.3 <10 30 160 160 >30 0.3 <10 <10 0.77 1870 <10 80 0.02 30 <50 5 <50
394 ZK6 RL.H-394 73.98 1.00 1.00 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 2.1 30 10 7 2.5 <10 40 130 340 >30 0.2 <10 <10 0.86 3090 <10 160 0.02 <20 <50 <5 <50
395 ZK6 RL.H-395 75.28 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 6.02 <30 130 8 4.9 <10 140 10 130 14.2 1.4 10 <10 1.66 2650 <10 90 0.03 <20 <50 18 <50
396 RL.H-396 ICP90A 6.13 450 1490 8 2.7 60 380 30 24900 6.94 2.4 20 20 1.88 1030 1250 260 0.14 7770 80 12 120
397 ZK6 RL.H-397 76.48 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 5.91 <30 150 7 4.7 <10 590 10 120 10.5 1.6 10 10 1.63 2810 <10 80 0.03 <20 <50 18 <50
398 ZK6 RL.H-398 77.72 1.24 1.24 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 5.95 <30 170 8 3.7 <10 70 10 110 9.63 1.4 10 10 0.97 1950 <10 60 0.02 <20 <50 17 <50
399 ZK6 RL.H-399 79.02 1.30 1.30 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 7.14 <30 310 7 4.1 <10 80 10 70 7.39 1.9 20 10 1.02 2330 <10 50 0.04 <20 <50 17 <50
400 ZK6 RL.H-400 79.82 0.80 0.80 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 3.78 <30 80 6 3.3 <10 80 <10 150 24.6 0.6 <10 10 1 2530 <10 130 0.02 <20 <50 10 <50
401 ZK6 RL.H-401 80.72 0.95 0.95 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 1.6 <30 <10 <5 2 <10 50 10 210 >30 <0.1 <10 <10 0.67 2030 <10 190 0.02 <20 <50 <5 <50
402 ZK6 RL.H-402 81.69 0.92 0.90 98 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 1.34 <30 <10 7 1.3 <10 40 130 150 >30 0.1 <10 <10 0.43 1390 <10 110 0.03 <20 <50 <5 <50
403 ZK6 RL.H-403 82.46 0.77 0.75 98 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 1.9 <30 40 7 2 <10 30 110 80 >30 0.6 <10 <10 0.56 2330 <10 70 0.02 <20 <50 <5 <50
404 ZK6 RL.H-404 83.20 0.74 0.73 98 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.74 <30 90 8 0.6 <10 30 <10 50 1.83 3.7 20 <10 0.08 280 <10 20 <0.01 <20 <50 <5 <50
405 ZK6 RL.H-405 84.45 1.25 1.25 100 42/2 块状硫化物(Py)/VMS(Py) ICP90A FAI323 Au AAS21E Ag 1.55 <30 30 6 2.8 <10 30 70 120 >30 0.4 <10 <10 0.4 2610 <10 50 0.02 30 <50 <5 <50
406 ZK6 RL.H-406 85.69 1.24 1.24 100 42/2 块状硫化物(Py)/VMS(Py) ICP90A 0.49 30 <10 6 1.8 <10 30 100 80 >30 <0.1 <10 <10 0.56 3870 <10 60 0.01 <20 <50 <5 <50
407 RL.H-407 ICP90A 7.25 <30 400 12 0.8 <10 20 <10 30 1.55 4.4 80 40 0.18 390 <10 10 0.04 20 <50 <5 <50
408 ZK6 RL.H-408 86.74 1.05 1.05 100 42/2 强硅化磁黄铁矿化黄铁矿化(变)安山岩/strong silicification, Pyrrhotite&Pyrite mineralization, (altered) Andesite ICP90A FAI323 Au AAS21E Ag 0.12 <30 <10 <5 0.4 <10 70 <10 40 1.66 <0.1 <10 <10 0.04 410 <10 30 0.02 <20 <50 <5 <50
409 ZK6 RL.H-409 87.89 1.15 1.15 100 42/2 强硅化磁黄铁矿化黄铁矿化(变)安山岩/strong silicification, Pyrrhotite&Pyrite mineralization, (altered) Andesite ICP90A 0.09 30 <10 <5 0.3 <10 100 <10 20 0.82 <0.1 <10 <10 0.05 270 <10 40 <0.01 <20 <50 <5 <50
410 ZK6 RL.H-410 88.89 1.00 1.00 100 42/2 块状硫化物(Py)/VMS(Py) ICP90A 0.26 40 <10 <5 1.2 <10 20 120 70 >30 <0.1 <10 <10 0.33 2480 <10 40 <0.01 <20 <50 <5 <50
411 ZK6 RL.H-411 89.92 1.03 1.03 100 42/2 块状硫化物(Py)/VMS(Py) ICP90A 0.43 <30 <10 5 2.1 <10 10 100 160 >30 <0.1 <10 <10 0.63 4770 <10 60 0.02 <20 <50 <5 <50
412 ZK6 RL.H-412 91.06 1.14 1.14 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.75 <30 <10 <5 2 <10 40 70 80 27.1 <0.1 <10 <10 0.5 3250 <10 30 <0.01 <20 <50 <5 <50
413 ZK6 RL.H-413 91.77 0.71 0.71 100 42/2 块状硫化物(Py,Po)/VMS (Py,Po) ICP90A 0.82 <30 <10 5 3 <10 20 70 160 >30 <0.1 <10 <10 1.45 8530 <10 140 0.01 <20 <50 5 <50
414 ZK6 RL.H-414 92.48 0.71 0.71 100 42/2 黄铁矿化磁黄铁矿化(变)安山岩/Pyrite&Pyrrhotite mineralization (altered), Andesite ICP90A 0.4 <30 <10 7 3.6 <10 80 <10 140 11.4 <0.1 <10 <10 0.91 6840 <10 40 <0.01 <20 <50 <5 <50
415 ZK6 RL.H-415 93.80 1.32 1.32 100 42/2 块状硫化物(Py,Po)/VMS (Py,Po) ICP90A 0.47 40 <10 6 2.3 <10 <10 100 120 >30 <0.1 <10 <10 0.89 7730 <10 70 0.01 <20 <50 <5 <50
416 ZK6 RL.H-416 95.00 1.20 1.20 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.5 40 30 6 2 <10 20 100 150 >30 0.1 <10 <10 0.57 4260 <10 60 0.02 <20 <50 <5 <50
417 ZK6 RL.H-417 96.01 1.01 1.01 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.19 <30 <10 <5 2.6 <10 20 70 150 >30 <0.1 <10 <10 0.76 3230 <10 80 <0.01 <20 <50 <5 <50
418 RL.H-418 ICP90A FAI323 Au AAS21E Ag 7.45 100 550 7 0.8 20 60 10 4250 4.91 4.6 10 10 0.89 560 170 30 0.11 2100 70 11 260
419 ZK6 RL.H-419 97.26 1.25 1.25 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.24 <30 <10 <5 2.9 <10 50 30 90 21.7 <0.1 <10 <10 0.81 4090 <10 60 <0.01 <20 <50 <5 <50
420 ZK6 RL.H-420 98.10 1.15 1.15 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.11 <30 10 <5 1.1 <10 40 10 140 25.8 <0.1 <10 <10 0.23 1810 <10 90 <0.01 <20 <50 <5 <50
421 ZK6 RL.H-421 99.64 1.23 1.23 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.42 30 <10 <5 1.7 <10 30 60 230 >30 <0.1 <10 <10 0.42 5290 <10 90 0.01 <20 <50 <5 <50
422 ZK6 RL.H-422 100.89 1.25 1.25 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.31 <30 <10 <5 2.4 <10 40 10 90 15.4 <0.1 <10 <10 0.73 5500 <10 60 <0.01 <20 <50 6 <50
423 ZK6 RL.H-423 102.11 1.22 1.22 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.67 30 30 <5 5 <10 40 50 590 29.1 0.1 <10 <10 0.62 5470 <10 70 0.01 <20 <50 <5 <50
424 ZK6 RL.H-424 103.21 1.10 1.10 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 1.21 <30 20 5 10.3 <10 20 60 340 >30 <0.1 <10 <10 0.44 4890 <10 80 0.02 <20 <50 <5 <50
425 ZK6 RL.H-425 104.41 1.20 1.20 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.34 <30 10 <5 0.8 <10 50 20 50 9.49 <0.1 <10 <10 0.25 2880 <10 30 <0.01 <20 <50 <5 <50
426 ZK6 RL.H-426 105.16 0.75 0.75 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.43 50 <10 <5 3.6 <10 10 100 70 >30 <0.1 <10 <10 0.79 3680 <10 50 <0.01 <20 <50 <5 <50
427 ZK6 RL.H-427 106.28 1.12 1.12 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.76 <30 10 <5 2.1 <10 20 50 180 >30 0.1 <10 <10 0.56 4760 <10 110 0.02 <20 <50 <5 <50
428 ZK6 RL.H-428 108.00 1.72 1.72 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.51 <30 180 6 0.6 <10 10 <10 50 1.13 3.5 20 <10 0.08 260 20 <10 <0.01 <20 <50 <5 <50
429 RL.H-429 ICP90A 7.11 <30 370 10 0.7 <10 20 <10 50 1.66 4.2 70 40 0.16 390 <10 10 0.02 20 <50 <5 <50
430 ZK6 RL.H-430 109.22 1.22 1.22 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 1.14 30 30 <5 1.9 <10 50 80 140 >30 0.2 <10 <10 0.79 11000 <10 60 0.01 <20 <50 <5 <50
431 ZK6 RL.H-431 110.42 1.20 1.20 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.59 <30 20 <5 2 <10 40 70 170 >30 <0.1 <10 <10 0.67 4110 <10 40 0.01 <20 <50 <5 <50
432 ZK6 RL.H-432 111.83 1.41 1.41 100 42/2 稠密浸染状-块状硫化物(Po,Py)/intensively diseminated-massive VMS(Po,Py) ICP90A 0.43 40 10 <5 1.9 <10 40 70 110 >30 <0.1 <10 <10 0.59 2690 <10 50 0.01 <20 <50 <5 <50
433 ZK6 RL.H-433 112.96 1.13 1.13 100 42/2 磁黄铁矿化黄铁矿化(变)安山岩/Weak Pyrrhotite&Pyrite Mineralization (Altered), Andesite ICP90A 0.24 <30 <10 <5 1.1 <10 70 20 40 17.9 <0.1 <10 <10 0.25 2310 <10 20 0.02 <20 <50 <5 <50
434 ZK6 RL.H-434 114.03 1.07 1.07 100 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A 0.65 40 <10 6 2.4 <10 20 80 90 >30 <0.1 <10 <10 0.82 7100 <10 50 0.02 <20 <50 <5 <50
435 ZK6 RL.H-435 115.15 1.12 1.11 99 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A FAI323 Au AAS21E Ag 0.57 <30 <10 <5 1.7 <10 20 70 120 >30 <0.1 <10 <10 0.67 6490 <10 50 0.01 <20 <50 <5 <50
436 ZK6 RL.H-436 116.31 1.16 1.14 98 42/2 块状硫化物(Po,Py)/VMS(Po,Py) ICP90A 1.05 30 30 <5 1.8 <10 10 80 160 >30 0.2 <10 <10 0.75 6830 <10 70 0.01 <20 <50 <5 <50
437 ZK6 RL.H-437 117.35 1.04 1.02 98 42/2 钾长花岗岩(少量硫化物)/Feldspar Granite(minor VMS) ICP90A 7.08 <30 270 6 1.1 <10 40 <10 30 1.97 3.1 10 30 0.29 680 10 10 0.02 100 <50 <5 <50
438 ZK6 RL.H-438 118.35 1.00 1.00 100 42/2 钾长花岗岩/Feldspar Granite ICP90A 6.89 30 340 7 0.6 <10 20 <10 40 1.16 4 20 10 0.12 450 <10 <10 0.02 40 <50 <5 <50
439 ZK4 RL.H-439 54.04 55.41 1.07 1.05 98 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 6.59 <30 130 7 7.7 <10 210 50 240 16.1 0.3 <10 30 3.4 4490 <10 120 0.04 <20 <50 30 <50
440 RL.H-440 ICP90A 6.08 420 1460 7 2.7 60 360 30 24900 6.75 2.3 20 20 1.89 940 1270 270 0.13 7880 80 12 120
441 ZK4 RL.H-441 89.92 90.82 0.90 0.90 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 7.47 <30 130 10 9.1 <10 230 40 290 11.3 0.3 <10 30 3.24 4860 <10 110 0.05 <20 <50 42 <50
442 ZK4 RL.H-442 91.66 0.84 0.84 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 6.5 <30 80 9 7.4 <10 530 60 280 13.4 0.4 <10 30 3.9 4300 <10 180 0.04 <20 <50 39 <50
443 ZK4 RL.H-443 114.13 115.58 1.45 1.41 97 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 7.13 <30 90 8 8.6 <10 120 50 170 15.6 0.2 <10 40 3.73 6280 <10 100 0.04 <20 <50 42 <50
444 ZK4 RL.H-444 117.00 1.42 1.38 97 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 6.89 <30 20 10 7.2 <10 170 50 370 15.1 0.2 <10 40 3.34 5650 <10 100 0.05 <20 <50 41 <50
445 ZK4 RL.H-445 139.88 141.08 1.20 1.20 100 42/2 磁黄铁矿化(变)安山岩夹石英脉/Pyrrhotite Mineralizaton (altered) Andesite, associated with quartz Vein ICP90A FAI323 Au AAS21E Ag 5.89 <30 70 8 6.3 <10 100 40 200 12.6 0.7 <10 50 2.86 4370 <10 60 0.03 <20 <50 35 <50
446 ZK4 RL.H-446 142.33 1.05 1.05 100 42/2 磁黄铁矿化(变)安山岩夹石英脉/Pyrrhotite Mineralizaton (altered) Andesite, associated with quartz Vein ICP90A 7.5 <30 130 8 6.3 <10 70 50 250 12.3 1.6 <10 100 2.71 4180 <10 100 0.07 <20 <50 45 <50
447 ZK4 RL.H-447 161.54 162.54 1.00 1.00 100 42/2 (变)安山岩/(Altered) Andesite ICP90A 7.68 <30 100 8 8.9 <10 30 40 230 12.4 1.4 <10 30 3.15 5370 <10 60 0.06 <20 <50 47 <50
448 ZK4 RL.H-448 163.42 0.88 0.88 100 42/2 磁黄铁矿化(变)安山岩夹石英脉/Pyrrhotite Mineralizaton (altered) Andesite, associated with quartz Vein ICP90A 4.23 <30 60 7 5.4 <10 60 30 190 7.7 0.6 <10 30 1.93 3160 <10 40 0.07 <20 <50 27 <50
449 ZK4 RL.H-449 164.47 1.05 1.05 100 42/2 硅化磁黄铁矿化(变)安山岩/Silicified Pyrrhotite Mineralization, (altered) Andesite ICP90A 8.47 <30 130 9 8.4 <10 30 50 240 13.6 1.3 <10 60 3.15 6040 <10 60 0.04 <20 <50 52 <50
450 ZK4 RL.H-450 165.62 1.15 1.15 100 42/2 石英脉夹磁黄铁矿化(变)安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A 1.06 <30 20 <5 1.5 <10 70 10 140 2.39 0.3 <10 10 0.48 1170 <10 30 0.02 20 <50 5 <50
451 RL.H-451 ICP90A 7.08 <30 440 12 0.8 <10 20 <10 170 1.47 4.3 70 40 0.18 400 10 10 0.02 30 <50 <5 <50
452 ZK4 RL.H-452 166.62 1.00 1.00 100 42/2 石英脉夹磁黄铁矿化(变)安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A 2.18 <30 40 11 3.5 <10 70 20 150 5.4 0.2 <10 10 1.23 2320 <10 30 0.03 <20 <50 12 <50
453 ZK4 RL.H-453 167.82 1.20 1.20 100 42/2 石英脉夹磁黄铁矿化(变)安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 2.4 <30 70 7 5.8 <10 170 40 210 6.88 0.1 <10 20 2.73 3240 <10 100 0.02 <20 <50 13 <50
454 ZK4 RL.H-454 168.72 0.90 0.90 100 42/2 石英脉夹磁黄铁矿化(变)安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A FAI323 Au AAS21E Ag 1.89 <30 100 6 2 <10 270 30 160 3.15 0.2 <10 20 2.16 930 <10 120 0.04 <20 <50 7 <50
455 ZK4 RL.H-455 169.77 1.05 1.04 99 42/2 石英脉夹磁黄铁矿化(变)安山岩/Quartz Vein, associated with Pyrrhotite Mineralization (Altered), Andesite ICP90A 0.12 <30 <10 5 0.4 <10 70 <10 30 0.57 <0.1 <10 <10 0.07 170 <10 10 <0.01 <20 <50 <5 <50
456 ZK4 RL.H-456 171.00 1.23 1.23 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A FAI323 Au AAS21E Ag 5.84 <30 170 8 6.6 <10 340 70 710 13.4 0.5 <10 40 5.06 3680 <10 250 0.08 <20 <50 32 <50
457 ZK4 RL.H-457 172.36 1.36 1.36 100 42/2 磁黄铁矿化(变)安山岩/Pyrrhotite Minralization (altered) Andesite ICP90A 5.2 <30 100 6 6.4 <10 860 70 2580 11.8 0.6 10 70 5.74 3290 <10 300 0.07 110 <50 22 <50
458 ZK4 RL.H-458 176.21 177.39 1.18 42/2 沙状粉末/sand power ICP91A FAI323 Au AAS21E Ag
第 5 页,共 10 页
备 注
Sr
ppm
Ti
%
V
ppm
W
ppm
Y
ppm
Zn
ppm
Au
ppb
Ag
g/t
Pt
ppb
Pd
ppbNote
140 0.61 300 <50 29 2100
90 0.61 290 <50 19 1680
100 0.62 290 <50 19 2050
70 0.6 290 <50 21 930
80 0.58 290 <50 18 1460
80 0.61 300 <50 22 1290
60 0.58 290 <50 19 1000
50 0.58 310 <50 18 830
30 0.1 80 <50 14 150
30 0.14 90 <50 11 290
90 0.12 10 <50 82 50 blank
40 0.25 150 <50 15 440 253 <0.3
40 0.16 110 <50 12 510
40 0.07 70 <50 12 260
30 0.11 80 <50 12 970 63 0.3
20 0.03 40 <50 9 80
100 0.34 160 <50 17 880
220 0.48 110 <50 42 590
180 0.41 140 <50 19 1130 43 0.6
60 0.21 100 4370 9 870
40 0.23 130 420 14 1610
270 0.35 160 <50 18 2610 ME-12
50 0.35 150 <50 14 1010
50 0.25 110 <50 13 1580 31 1
30 0.2 120 <50 11 1160
20 0.03 30 <50 8 90
30 0.05 50 <50 10 120
40 0.29 140 <50 14 630
80 0.41 180 <50 19 1100 31 <0.3
30 0.12 60 <50 11 180
20 0.2 110 <50 13 530
<10 0.25 130 <50 14 240
90 0.12 10 <50 81 50 Blank
10 0.13 70 <50 11 210
10 0.16 90 <50 11 950 76 <0.3
<10 0.16 80 <50 13 350
10 0.07 40 <50 10 80
80 0.05 40 <50 8 50
300 0.12 70 <50 10 80
60 0.16 80 <50 13 140
80 0.24 90 <50 21 290 29 0.3
90 0.32 150 <50 11 440
110 0.41 170 <50 27 310
380 0.32 150 <50 17 8990 ME-11
90 0.34 180 <50 17 2000 61 0.6
20 0.13 80 <50 12 1320
90 0.8 300 <50 21 170
120 0.68 250 <50 29 250
90 0.44 220 <50 17 640
80 0.43 230 <50 17 670
80 0.4 200 <50 14 240 30 <0.3
70 0.3 140 <50 10 190
70 0.3 140 <50 10 250 41 <0.3
120 0.53 250 <50 15 180
90 0.12 10 <50 77 40 Blank
40 0.18 130 <50 15 130
20 0.11 90 <50 11 260 19 0.3
20 0.1 60 <50 8 140
<10 0.02 20 <50 8 50
20 0.1 70 <50 12 100
30 0.1 60 <50 10 130 28 <0.3
50 0.21 100 <50 11 190
100 0.38 160 <50 11 160
80 0.41 170 <50 11 190 23 <0.3
70 0.31 140 <50 8 140
280 0.35 170 <50 17 2580 ME-12
820 0.37 180 <50 11 130
110 0.28 160 <50 18 110
120 0.53 290 <50 19 90
150 0.5 280 <50 18 90 <5 <0.3
90 0.49 260 <50 20 80
650 0.48 200 <50 20 180
130 0.45 280 <50 16 80
50 0.31 180 <50 18 80 <5 <0.3
80 0.4 260 <50 15 80
110 0.48 280 <50 18 120
90 0.12 10 <50 77 40 Blank
80 0.41 240 <50 16 100
90 0.43 210 <50 19 290
70 0.27 80 <50 14 1360 29 2.1
80 0.35 110 <50 17 630 22 1.6
60 0.32 120 <50 15 1380
120 0.49 270 <50 15 210
40 0.16 50 <50 10 70
50 0.31 90 <50 16 110
180 0.14 60 <50 12 110 21 0.8
940 0.41 160 <50 16 110
350 0.31 150 <50 17 9110 1410 78.4 ME-11
50 0.24 70 <50 14 1230
50 0.32 100 <50 18 1610
40 0.29 100 <50 18 1660 64 0.8
20 0.02 30 <50 7 170
30 0.04 30 <50 9 200
50 0.35 60 <50 19 680
分析结果/Assay Result
基本析样品取样及分析结果登记表Sample Log
第 6 页,共 10 页
备 注
Sr
ppm
Ti
%
V
ppm
W
ppm
Y
ppm
Zn
ppm
Au
ppb
Ag
g/t
Pt
ppb
Pd
ppbNote
分析结果/Assay Result
基本析样品取样及分析结果登记表Sample Log
40 0.3 70 <50 20 1600
40 0.32 90 <50 20 1550
40 0.25 80 <50 19 880 12 <0.3
30 0.31 80 <50 21 190
100 0.12 10 <50 78 50 Blank
40 0.27 80 <50 22 140
30 0.25 90 1280 23 350
40 0.27 90 <50 15 770
50 0.39 210 <50 19 90
40 0.21 60 <50 16 60
30 0.27 70 <50 16 190
40 0.22 80 <50 15 910 36 0.4
20 0.34 110 <50 18 140
20 0.36 90 <50 18 60
40 0.31 160 <50 11 80
270 0.35 160 <50 18 2600 ME-12
50 0.42 250 <50 14 100
100 1.3 370 <50 35 100
90 0.56 300 <50 20 150
100 0.47 270 <50 18 140
90 0.47 280 <50 18 170
120 0.46 290 <50 18 170
100 0.45 260 <50 17 100 <5 <0.3
70 0.48 280 <50 18 110
130 0.42 280 <50 17 180
40 0.07 80 <50 5 50
100 0.12 10 <50 75 50 Blank
110 0.43 210 <50 20 150 <5 <0.3
130 0.63 280 <50 23 120 <5 <0.3
150 0.43 250 <50 16 180
190 0.42 260 <50 17 150
100 0.16 20 <50 <5 30
80 0.16 20 <50 <5 30
130 0.44 260 <50 20 160
180 0.46 260 <50 19 120
90 0.42 250 <50 20 180
30 0.18 100 <50 13 290 34 1.4
350 0.31 140 <50 17 9240 ME-11
20 0.09 90 <50 5 300 20 4.6
90 0.49 280 <50 19 170
80 0.42 240 <50 20 170
100 0.52 270 <50 21 120
80 0.41 230 <50 18 130
90 0.49 270 <50 20 130
<10 0.03 40 <50 <5 80 22 1.6
30 0.07 60 <50 6 260
30 <0.01 <10 <50 39 <10
40 0.01 <10 <50 29 50
100 0.11 10 <50 74 50 <0.5 <0.3 Blank
20 0.02 40 <50 6 470 14 1.6
10 0.01 40 <50 <5 280
<10 0.02 50 <50 <5 220 14 3.4
40 0.33 220 <50 26 260
40 0.19 120 <50 15 170
940 0.54 160 <50 13 100
120 0.56 300 <50 18 80
120 0.58 300 <50 19 120
120 0.57 310 <50 17 220
100 0.4 210 <50 14 310
280 0.36 170 <50 18 2560 ME-12
90 0.34 170 <50 21 160 6 0.6
110 0.38 210 <50 19 160
110 0.4 200 <50 17 150
140 0.47 270 <50 15 160
110 0.47 260 <50 13 180
100 0.42 250 <50 13 140 <5 0.3
120 0.48 260 <50 13 130
120 0.33 160 <50 9 70
130 0.23 80 <50 7 60
110 0.37 220 <50 13 160
90 0.12 10 <50 79 40 Blank
100 0.44 260 <50 17 170 6 0.5
120 0.47 270 <50 16 260
120 0.43 250 <50 14 190
120 0.49 280 <50 15 160
110 0.47 270 <50 16 160
90 0.44 260 <50 15 140
90 0.51 290 <50 17 180
90 0.49 290 <50 17 140 6 <0.3
120 0.48 270 <50 16 120
130 0.47 270 <50 15 120
380 0.32 150 <50 18 8860 ME-11
130 0.55 310 <50 19 110
120 0.53 300 <50 17 100
80 0.44 270 <50 14 120
60 0.41 250 <50 20 130 12 0.5
70 0.5 280 <50 17 120
120 0.46 270 <50 17 100
130 0.52 300 <50 17 110
80 0.44 250 <50 16 140
110 0.46 240 <50 16 160 <5 0.6
40 0.14 100 <50 9 320 19 1.7
100 0.12 10 <50 78 50 Blank
90 0.33 190 <50 17 120
第 7 页,共 10 页
备 注
Sr
ppm
Ti
%
V
ppm
W
ppm
Y
ppm
Zn
ppm
Au
ppb
Ag
g/t
Pt
ppb
Pd
ppbNote
分析结果/Assay Result
基本析样品取样及分析结果登记表Sample Log
60 0.3 180 <50 12 470
10 0.08 40 <50 6 300
20 0.05 50 <50 9 160 7 1.7
100 0.55 290 <50 16 140
110 0.53 270 <50 11 270
110 0.36 210 <50 14 150
130 0.41 230 <50 17 200
100 0.4 240 <50 13 210
100 0.42 250 <50 13 320 8 0.9
280 0.35 160 <50 18 2590 ME-12
90 0.43 250 <50 14 210
90 0.41 220 <50 16 120
80 0.04 10 <50 7 10
100 0.56 300 <50 21 130
100 0.18 100 <50 8 190 10 0.3
250 0.31 190 <50 12 530
100 0.54 270 <50 19 290 9 0.7
80 0.56 310 <50 18 210
130 0.4 240 <50 12 460
250 0.26 130 <50 8 170
110 0.13 10 <50 79 50 Blank
90 0.45 260 <50 16 220
10 0.11 100 <50 <5 1210 15 0.3
10 0.02 20 <50 <5 380
<10 0.02 20 <50 <5 390
60 0.06 40 <50 <5 100
120 0.08 20 <50 7 40
250 0.05 10 <50 <5 10
90 0.94 420 <50 34 110
1010 0.4 200 <50 18 110
100 0.43 260 <50 16 100
390 0.33 150 <50 17 9020 1230 78.6 ME-11
60 0.21 100 <50 10 110 7 1.1
440 0.47 220 <50 16 140
280 0.5 280 <50 17 160
190 0.5 270 <50 17 90
80 0.23 120 <50 7 40 <5 <0.3
50 0.24 110 <50 9 170
150 0.64 280 <50 25 760 8
80 0.39 150 <50 18 1150 12
60 0.29 130 <50 21 550 18 0.6
60 0.37 200 <50 37 2640 36
90 0.12 10 <50 80 60 Blank
40 0.17 90 <50 14 600 11 1.4
30 0.17 80 <50 8 70 16 2.1
<10 0.05 20 <50 <5 100 7
10 0.09 50 <50 8 140 6
20 0.13 60 <50 11 390 13
<10 0.04 30 <50 9 360 15 1.8
10 0.13 60 <50 <5 110 10
40 0.24 90 <50 16 570 21
20 0.13 60 <50 11 1330 26 2.2
40 0.29 110 <50 15 730 26
280 0.35 170 <50 17 2600 311 53.7 ME-12
20 0.11 70 <50 10 390 27
20 0.11 70 <50 10 750 30 3.3
40 0.28 90 <50 14 320 18
50 0.32 120 <50 14 270 23
60 0.2 80 <50 13 450 19 1.6
210 0.73 290 <50 22 180 <5
70 0.58 230 <50 22 310 12
30 0.21 110 <50 8 260 9 0.8
70 0.72 350 <50 25 140 <5
80 1.03 380 <50 35 500 <5
100 0.13 10 <50 80 50 <5 Blank
90 0.96 360 <50 35 130 <5
100 0.92 330 <50 34 100 <5
170 0.99 360 <50 34 110 <5
110 1.01 360 <50 35 120 <5
90 0.99 360 <50 34 120 <5
110 0.98 360 <50 33 150 <5 <0.3
100 0.99 380 <50 33 110 <5
270 0.92 340 <50 29 120 <5
330 0.83 290 <50 28 110 <5
100 1.02 370 <50 34 90 <5
390 0.32 150 <50 17 8920 1260 ME-11
90 0.7 260 <50 27 170 7
70 0.56 200 <50 23 250 <5
40 0.26 90 <50 14 180 5 0.8
20 0.04 30 <50 6 180 5 1
70 0.31 140 <50 17 300 8
170 0.65 300 <50 21 110 <5
110 0.51 290 <50 19 60
90 0.58 300 <50 22 70
80 0.55 300 <50 17 70
50 0.49 260 <50 15 60 95 2.1
100 0.12 10 <50 79 110 <5 <0.3 Blank
70 0.56 290 <50 20 50
80 0.65 350 <50 21 60
1070 0.86 310 <50 24 80 <10 6
1060 0.91 320 <50 25 80 <10 <5
140 0.7 310 <50 22 210
470 0.57 220 <50 19 130 5 <0.3
270 0.68 280 <50 22 270
第 8 页,共 10 页
备 注
Sr
ppm
Ti
%
V
ppm
W
ppm
Y
ppm
Zn
ppm
Au
ppb
Ag
g/t
Pt
ppb
Pd
ppbNote
分析结果/Assay Result
基本析样品取样及分析结果登记表Sample Log
70 0.77 330 <50 24 490
40 0.77 360 <50 23 320 <5 0.3
30 0.78 370 <50 21 170
250 0.33 150 <50 16 2380 ME-12
40 0.74 350 <50 23 140
60 0.77 340 <50 25 90
90 1.03 400 <50 36 150
90 0.67 260 <50 24 150 6 <0.3
680 0.17 30 <50 <5 40
340 0.26 80 <50 13 1460
60 0.43 140 <50 19 370 10 0.5
120 0.97 360 <50 34 130
110 1.01 380 <50 33 140
100 1.11 410 <50 37 120
110 0.12 10 <50 79 50 Blank
110 1.22 280 <50 42 140
100 1.03 170 <50 48 110
100 1.06 160 <50 48 130
80 0.55 110 <50 29 220 5 <0.3
80 0.36 110 <50 21 410 6 <0.3
80 0.33 130 <50 18 320 <5 <0.3
80 0.6 280 <50 22 120
60 1.11 160 <50 49 110
50 0.33 130 <50 15 1130 6 1.4
50 0.23 90 <50 14 350
390 0.32 150 <50 18 9180 ME-11
80 0.88 150 <50 40 220
70 1.09 160 <50 50 180
90 1.11 150 <50 53 150
60 0.46 170 <50 15 170
30 0.44 170 <50 16 250
240 0.42 150 <50 14 310 5 <0.3
380 0.53 220 <50 17 230
370 0.44 200 <50 20 530 8 <0.3 Additonal Sampling840 0.45 180 <50 18 140 Additonal Sampling950 0.5 210 <50 20 110 Additonal Sampling110 0.12 10 <50 89 50 Blank
80 0.39 250 <50 16 150 Additonal Sampling70 0.54 250 <50 21 160 Additonal Sampling70 0.94 320 <50 35 70 Additonal Sampling70 1.45 440 <50 38 110 Additonal Sampling
1140 0.8 290 <50 24 80 <5 <10 <5 Additonal Sampling1150 0.79 290 <50 23 80 <5 <10 <5 Additonal Sampling50 0.71 330 <50 25 190
90 0.74 330 <50 24 140
140 0.81 360 <50 25 100
100 0.58 300 <50 23 190
260 0.35 160 <50 17 2570 ME-12
150 0.8 360 <50 23 100
70 0.84 410 <50 36 160
80 0.86 400 <50 33 150
70 0.81 390 <50 34 180
100 0.43 260 <50 18 160
80 0.45 270 <50 17 100
80 0.45 260 <50 16 210
80 0.06 <10 <50 7 20
110 0.36 210 <50 15 140
110 0.05 <10 <50 6 20
90 0.12 10 <50 83 60 Blank
110 0.48 290 <50 17 130
110 0.53 300 <50 16 120
130 0.3 210 <50 13 200
<10 0.03 50 <50 <5 60
600 0.25 110 <50 11 140
530 0.15 60 <50 6 90
60 0.05 50 <50 <5 50
180 0.17 130 <50 9 160
810 0.19 50 <50 7 50
10 0.02 50 <50 <5 110 25 2.8
350 0.32 140 <50 17 9120 1240 76.5 ME-11
20 0.04 20 <50 7 70
20 0.04 30 <50 6 90
50 0.08 40 <50 6 190 12 0.9
50 0.13 50 <50 8 260 23 0.9
130 0.17 140 <50 10 150
80 0.24 190 <50 13 290
60 0.18 80 <50 13 480 10 0.5
90 0.29 250 <50 16 170
110 0.3 250 <50 17 180
10 0.1 60 <50 6 210
80 0.12 10 <50 75 50 Blank
40 0.12 70 <50 9 260
40 0.17 80 <50 9 320 7 0.6
10 0.05 30 <50 <5 150
80 0.06 <10 <50 5 30
110 0.05 <10 <50 5 20
30 0.07 40 <50 9 110
10 0.04 60 <50 9 210
10 0.02 40 <50 7 90
20 0.02 50 <50 8 230 9 0.8
10 0.03 60 <50 7 100 11 0.8
260 0.35 170 <50 17 2690 ME-12
10 0.01 40 <50 6 180
<10 0.03 60 <50 15 60
第 9 页,共 10 页
备 注
Sr
ppm
Ti
%
V
ppm
W
ppm
Y
ppm
Zn
ppm
Au
ppb
Ag
g/t
Pt
ppb
Pd
ppbNote
分析结果/Assay Result
基本析样品取样及分析结果登记表Sample Log
<10 0.03 60 <50 9 150
<10 0.04 60 <50 11 590 26 1.2
20 0.06 50 <50 7 160
20 0.03 50 <50 6 200
<10 0.03 50 <50 6 110
<10 0.02 50 <50 8 130 14 1
<10 0.04 50 <50 11 250
20 0.03 50 <50 <5 130 15 0.6
90 0.12 10 <50 78 50 <5 <0.3 Blank
20 0.05 50 <50 <5 250
20 0.07 60 <50 7 1060
20 0.05 50 <50 5 240 21 0.8
20 0.07 50 <50 5 170
60 0.22 80 <50 16 220
70 0.31 100 <50 16 110 8 <0.3
70 0.23 90 <50 16 110 11 0.4
10 0.17 70 <50 10 70 25 0.5
10 0.13 100 <50 10 120
40 0.38 140 <50 18 330
340 0.34 150 <50 17 9140 ME-11
50 0.3 130 <50 19 230
60 0.33 120 <50 18 380 5 0.3
80 0.43 140 <50 21 430
30 0.24 100 <50 12 250
<10 0.1 80 <50 8 360
20 0.1 70 <50 6 80 9 0.4
20 0.09 60 <50 9 140
60 0.05 10 <50 <5 20
20 0.06 50 <50 8 150 12 <0.3
<10 0.03 60 <50 10 50
90 0.13 10 <50 86 60 Blank
<10 0.01 <10 <50 <5 40 <5 1.4
<10 <0.01 <10 <50 <5 20
<10 0.02 50 <50 5 60
10 0.02 60 <50 10 60
20 0.04 50 <50 8 60
<10 0.04 80 <50 19 100
10 0.02 30 <50 10 60
10 0.03 60 <50 13 90
10 0.03 60 <50 10 80 <5 0.5
<10 0.01 60 <50 11 50
240 0.36 160 <50 18 2640 332 48.3 ME-12
<10 0.02 50 <50 12 80
<10 <0.01 40 <50 <5 40
10 0.03 60 <50 7 90 12 1
<10 0.02 40 <50 9 50
50 0.03 60 <50 11 50
90 0.04 50 <50 10 120
<10 0.02 20 <50 <5 50
20 0.02 60 <50 10 60
10 0.05 70 <50 9 90 <5 0.9
70 0.06 <10 <50 5 20
80 0.13 10 <50 78 80 Blank
20 0.07 60 <50 13 90
20 0.03 50 <50 9 60
10 0.02 50 <50 7 50
<10 0.02 30 <50 <5 20
10 0.03 60 <50 14 70
<10 0.03 50 <50 8 80 9 0.7
10 0.06 60 <50 8 80
130 0.12 30 <50 7 100
150 0.06 10 <50 <5 40
70 0.57 250 <50 23 330
340 0.33 150 <50 18 9170 ME-11
80 0.69 320 <50 26 110
50 0.57 290 <50 23 160
60 0.58 320 <50 25 270
70 0.71 350 <50 30 380
40 0.69 350 <50 29 110 <5 <0.3
40 0.94 420 <50 33 130
50 0.95 430 <50 36 150
30 0.51 260 <50 22 170
60 1.03 460 <50 40 160
20 0.11 70 <50 6 30
90 0.13 20 <50 81 90 Blank
30 0.24 140 <50 12 60
100 0.2 130 <50 11 60 <5 <0.3
150 0.16 80 <50 7 40 <5 <0.3
<10 <0.01 10 <50 <5 10
240 0.59 280 <50 24 120 <5 <0.3
50 0.36 170 <50 17 470
<5 4.8
第 10 页,共 10 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
RL.H-1 10.6 90 180 <5 1.1 <10 670 100 390 7.99 2.7 10 40 1.41 1560 <10 280 0.05 70 <50 40 <50 140 0.61 300 <50 29 2100
RL.H-2 10.7 40 170 <5 0.5 <10 730 90 260 7.56 2.7 10 30 1.12 1700 <10 260 0.02 60 <50 40 <50 90 0.61 290 <50 19 1680
RL.H-3 10.8 <30 170 <5 0.7 <10 700 80 370 7.91 2.6 10 40 1.25 1980 <10 220 0.03 60 <50 41 <50 100 0.62 290 <50 19 2050
RL.H-4 10.4 90 190 <5 0.5 <10 690 70 260 7.04 2.6 10 40 1.26 1890 <10 250 0.02 60 <50 40 <50 70 0.6 290 <50 21 930
RL.H-5 10.3 <30 170 <5 0.8 <10 680 120 520 9.75 2.5 10 40 1.25 1740 <10 350 0.02 80 <50 40 <50 80 0.58 290 <50 18 1460
RL.H-6 10.7 <30 160 <5 1 <10 710 90 370 8.73 2.5 10 30 1.15 2010 <10 270 0.02 60 <50 41 <50 80 0.61 300 <50 22 1290
RL.H-7 10.2 <30 160 <5 1.1 <10 700 80 380 9.75 2.2 <10 30 1.14 2620 <10 240 0.02 50 <50 41 <50 60 0.58 290 <50 19 1000
RL.H-8 10.1 <30 150 <5 0.7 <10 760 100 330 11.4 2.1 10 30 1 2590 <10 290 0.02 40 <50 41 <50 50 0.58 310 <50 18 830
RL.H-9 1.73 <30 10 <5 3.8 <10 120 30 100 25.6 0.2 <10 <10 3.02 3860 <10 80 0.08 <20 <50 5 <50 30 0.1 80 <50 14 150
RL.H-10 2.39 <30 70 <5 3.3 <10 160 40 110 27.1 0.4 <10 20 3.3 2850 <10 80 0.06 <20 <50 8 <50 30 0.14 90 <50 11 290
RL.H-11 7.15 <30 480 5 0.7 <10 10 <10 <10 1.54 4.3 90 40 0.17 330 <10 <10 0.02 20 <50 <5 <50 90 0.12 10 <50 82 50
RL.H-12 4.68 50 160 <5 2.8 <10 300 70 170 22 1.1 <10 30 2.43 3030 <10 150 0.04 20 <50 16 <50 40 0.25 150 <50 15 440 253 <0.3
RL.H-13 2.84 <30 130 <5 3 <10 240 50 280 26.3 0.4 <10 20 2.86 3850 <10 100 0.06 <20 <50 11 <50 40 0.16 110 <50 12 510
RL.H-14 1.33 50 20 <5 4 <10 200 30 100 27.3 0.2 <10 <10 3.27 4270 <10 60 0.08 <20 <50 <5 <50 40 0.07 70 <50 12 260
RL.H-15 2.14 <30 50 <5 2.4 <10 140 50 310 27.6 0.1 <10 <10 2.55 3600 <10 120 0.08 <20 <50 6 <50 30 0.11 80 <50 12 970 63 0.3
RL.H-16 0.68 <30 10 <5 3.3 <10 40 <10 40 24.9 <0.1 <10 <10 2.93 4390 <10 30 0.06 <20 <50 <5 <50 20 0.03 40 <50 9 80
RL.H-17 7.7 80 130 <5 2.2 <10 320 70 200 14 0.7 30 50 1.58 2010 <10 160 0.04 30 <50 20 <50 100 0.34 160 <50 17 880
RL.H-18 9.98 <30 230 <5 3.1 <10 220 50 330 7.43 1.2 60 50 1.53 950 <10 100 0.05 40 <50 20 <50 220 0.48 110 <50 42 590
RL.H-19 7.82 <30 190 <5 3.2 <10 230 90 550 11.1 1 20 40 1.65 1170 <10 170 0.05 60 <50 19 <50 180 0.41 140 <50 19 1130 43 0.6
RL.H-20 4.12 80 80 <5 2.2 <10 180 80 1960 13.2 0.6 <10 30 1.47 1270 <10 140 0.02 30 <50 14 <50 60 0.21 100 4370 9 870
RL.H-21 4.44 90 80 <5 2.1 <10 220 110 610 17 0.8 <10 30 1.94 1860 <10 200 0.03 50 <50 13 <50 40 0.23 130 420 14 1610
RL.H-22 7.4 100 590 <5 0.8 20 30 20 4450 4.85 4.8 10 10 0.88 520 170 30 0.1 2080 70 12 260 270 0.35 160 <50 18 2610
RL.H-23 5.84 <30 130 <5 1 <10 300 80 370 15.3 1 10 50 1.19 1840 <10 140 0.04 40 <50 18 <50 50 0.35 150 <50 14 1010
RL.H-24 4.74 80 140 <5 0.7 <10 110 120 560 22.7 0.9 10 30 0.77 1070 <10 230 0.03 50 <50 12 <50 50 0.25 110 <50 13 1580 31 1
RL.H-25 3.89 70 110 <5 1.1 <10 110 120 690 24.9 0.7 <10 20 1.2 1360 <10 210 0.02 50 <50 12 <50 30 0.2 120 <50 11 1160
RL.H-26 0.56 <30 <10 <5 2 <10 30 20 100 10.5 <0.1 <10 <10 1.58 2030 <10 30 0.03 <20 <50 <5 <50 20 0.03 30 <50 8 90
RL.H-27 0.89 <30 10 <5 3 <10 40 20 100 18.5 <0.1 <10 <10 2.72 3580 <10 40 0.05 <20 <50 <5 <50 30 0.05 50 <50 10 120
RL.H-28 5.81 40 100 <5 2.8 <10 290 50 150 15.5 0.8 10 50 2.04 2590 <10 110 0.03 <20 <50 16 <50 40 0.29 140 <50 14 630
RL.H-29 8.09 <30 270 <5 1.2 <10 300 80 440 14.6 1.7 20 60 1.36 1750 <10 170 0.04 30 <50 22 <50 80 0.41 180 <50 19 1100 31 <0.3
RL.H-30 2 <30 <10 <5 3.1 <10 130 60 240 20.4 0.2 <10 10 2.17 3180 <10 180 0.03 <20 <50 <5 <50 30 0.12 60 <50 11 180
RL.H-31 3.52 <30 60 <5 2.1 <10 250 50 540 22 0.2 <10 20 1.83 2880 <10 160 0.03 <20 <50 11 <50 20 0.2 110 <50 13 530
RL.H-32 4.17 <30 <10 <5 1.8 <10 310 40 290 22.6 <0.1 <10 20 2.08 4340 <10 130 0.04 <20 <50 13 <50 <10 0.25 130 <50 14 240
RL H 33 6 96 <30 380 <5 0 7 <10 10 <10 20 1 78 4 2 80 40 0 16 360 <10 <10 0 02 30 <50 <5 <50 90 0 12 10 <50 81 50
Richardson Lake 2011 Assay Results
RL.H-33 6.96 <30 380 <5 0.7 <10 10 <10 20 1.78 4.2 80 40 0.16 360 <10 <10 0.02 30 <50 <5 <50 90 0.12 10 <50 81 50
RL.H-34 2.09 <30 20 <5 2.8 <10 140 30 130 17.8 0.1 <10 10 2.27 2990 <10 90 0.05 <20 <50 6 <50 10 0.13 70 <50 11 210
RL.H-35 2.69 <30 100 <5 1.9 <10 190 40 360 17.3 0.5 <10 20 1.76 1940 <10 120 0.05 <20 <50 9 <50 10 0.16 90 <50 11 950 76 <0.3
RL.H-36 1.98 <30 20 <5 3.6 <10 240 30 370 15.4 0.2 <10 10 2.27 3100 <10 100 0.05 <20 <50 7 <50 <10 0.16 80 <50 13 350
RL.H-37 1.32 <30 <10 <5 1.9 <10 60 10 40 20.3 <0.1 <10 <10 1.98 5080 <10 50 0.03 <20 <50 <5 <50 10 0.07 40 <50 10 80
RL.H-38 0.77 <30 120 <5 2.1 <10 170 <10 10 17.7 0.2 <10 <10 2.59 5080 <10 70 0.03 <20 <50 <5 <50 80 0.05 40 <50 8 50
RL.H-39 1.8 <30 280 <5 3 <10 310 10 30 15.9 0.3 <10 10 3.32 4370 <10 100 0.05 <20 <50 6 <50 300 0.12 70 <50 10 80
RL.H-40 3.1 <30 80 <5 5.1 <10 140 10 70 9.38 0.3 <10 20 2.47 3130 10 50 0.04 <20 <50 7 <50 60 0.16 80 <50 13 140
RL.H-41 5.29 80 110 <5 2.5 <10 90 50 230 17.6 0.6 30 30 1.14 1330 <10 170 0.05 20 <50 11 <50 80 0.24 90 <50 21 290 29 0.3
RL.H-42 5.62 40 100 <5 2.4 <10 350 170 680 17.4 0.7 <10 30 1.31 1290 <10 260 0.04 30 <50 17 <50 90 0.32 150 <50 11 440
RL.H-43 8.38 <30 170 <5 2 <10 470 40 430 9.51 1.2 20 50 1.36 1600 <10 190 0.02 20 <50 25 <50 110 0.41 170 <50 27 310
RL.H-44 6.06 460 1520 <5 2.6 60 350 30 25900 6.75 2.4 20 20 1.89 940 1280 260 0.13 7850 90 12 110 380 0.32 150 <50 17 8990
RL.H-45 6.79 60 140 <5 2.4 <10 460 110 480 17.2 0.9 <10 40 1.39 1260 <10 260 0.03 20 <50 24 <50 90 0.34 180 <50 17 2000 61 0.6
RL.H-46 1.86 <30 40 <5 4.3 <10 150 90 390 16.1 0.4 <10 10 2.22 2800 <10 160 0.05 <20 <50 8 <50 20 0.13 80 <50 12 1320
RL.H-47 6.18 40 180 <5 14.6 <10 380 50 180 6.86 2.2 <10 20 2.3 3370 <10 130 0.04 <20 <50 32 <50 90 0.8 300 <50 21 170
RL.H-48 6.73 30 240 <5 7.6 <10 410 50 100 8.46 1.8 10 20 2.6 2510 <10 170 0.06 <20 <50 28 <50 120 0.68 250 <50 29 250
RL.H-49 7.82 <30 180 <5 3.4 <10 550 70 310 12 1.6 10 30 1.49 1350 <10 140 0.02 <20 <50 28 <50 90 0.44 220 <50 17 640
RL.H-50 7.69 30 140 <5 3.2 <10 680 50 140 11.1 1.4 10 30 1.48 1500 <10 130 0.02 <20 <50 31 <50 80 0.43 230 <50 17 670
RL.H-51 6.92 <30 130 <5 3.3 <10 420 70 130 13.3 1.2 <10 20 1.57 1710 <10 150 0.04 <20 <50 26 <50 80 0.4 200 <50 14 240 30 <0.3
RL.H-52 5.36 <30 80 <5 2.9 <10 210 40 130 10.2 0.6 10 20 1.15 1480 <10 110 0.01 <20 <50 16 <50 70 0.3 140 <50 10 190
RL.H-53 5.91 <30 90 <5 2.4 <10 230 40 100 11.8 0.8 <10 20 1.02 1270 <10 130 0.03 20 <50 18 <50 70 0.3 140 <50 10 250 41 <0.3
RL.H-54 9.64 <30 170 <5 2.4 <10 420 30 140 6.57 1.5 10 50 1.26 1880 <10 170 0.04 <20 <50 34 <50 120 0.53 250 <50 15 180
RL.H-55 7.18 <30 380 <5 0.7 <10 <10 <10 <10 1.54 4.5 90 40 0.16 320 <10 10 0.01 20 <50 <5 <50 90 0.12 10 <50 77 40
RL.H-56 3.22 <30 80 <5 7.4 <10 140 50 190 19.5 0.6 <10 20 2.83 3780 <10 170 0.02 <20 <50 16 <50 40 0.18 130 <50 15 130
第 1 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-57 2 30 10 <5 6.3 <10 130 110 210 22.2 0.2 <10 <10 2.53 4090 50 190 0.01 <20 <50 8 <50 20 0.11 90 <50 11 260 19 0.3
RL.H-58 1.53 <30 20 <5 4.2 <10 100 20 80 8.18 0.2 <10 <10 1.66 2680 <10 70 0.01 <20 <50 5 <50 20 0.1 60 <50 8 140
RL.H-59 0.24 <30 <10 <5 6.3 <10 20 20 70 8.49 <0.1 <10 <10 2.43 3960 <10 70 0.03 <20 <50 <5 <50 <10 0.02 20 <50 8 50
RL.H-60 1.81 <30 <10 <5 8.6 <10 100 20 120 14.8 <0.1 <10 <10 3.4 5970 <10 130 0.01 <20 <50 6 <50 20 0.1 70 <50 12 100
RL.H-61 1.79 <30 <10 <5 6.1 <10 70 40 130 15.6 <0.1 <10 <10 2.53 4870 <10 140 0.01 <20 <50 5 <50 30 0.1 60 <50 10 130 28 <0.3
RL.H-62 4.41 <30 30 <5 6.4 <10 90 20 110 12.9 0.4 <10 10 2.6 4900 <10 120 0.03 <20 <50 10 <50 50 0.21 100 <50 11 190
RL.H-63 7.98 30 130 <5 2 <10 310 40 60 6.41 1.5 20 50 0.9 1110 <10 140 0.03 <20 <50 21 <50 100 0.38 160 <50 11 160
RL.H-64 6.77 30 90 <5 2.1 <10 190 40 90 6.71 0.8 10 40 0.9 1200 <10 140 0.03 <20 <50 21 <50 80 0.41 170 <50 11 190 23 <0.3
RL.H-65 4.93 <30 80 <5 3.1 <10 170 30 70 5.77 0.4 <10 20 1.16 1750 <10 110 0.02 <20 <50 19 <50 70 0.31 140 <50 8 140
RL.H-66 7.45 100 590 <5 0.7 20 30 20 4500 4.76 4.7 10 10 0.88 520 180 30 0.09 2120 70 12 270 280 0.35 170 <50 17 2580
RL.H-67 8 <30 180 <5 7.8 <10 120 30 70 7.29 0.5 10 20 3.81 2740 <10 70 0.1 <20 <50 23 <50 820 0.37 180 <50 11 130
RL.H-68 5.21 <30 210 <5 9.2 <10 190 50 110 7.84 0.5 <10 <10 3.35 3940 <10 200 0.02 <20 <50 23 <50 110 0.28 160 <50 18 110
RL.H-69 8.11 <30 20 <5 7.8 <10 280 50 120 9.34 0.2 <10 40 4.25 1780 <10 130 0.03 <20 <50 42 <50 120 0.53 290 <50 19 90
RL.H-70 7.93 <30 10 <5 8.9 <10 270 50 130 8.85 <0.1 <10 20 3.93 1700 <10 120 0.03 <20 <50 40 <50 150 0.5 280 <50 18 90 <5 <0.3
RL.H-71 7.75 <30 40 <5 12.5 <10 270 50 170 6.41 0.1 <10 10 2.2 1720 <10 140 0.04 <20 <50 38 <50 90 0.49 260 <50 20 80
RL.H-72 8.75 <30 820 <5 3.9 <10 100 70 360 6.79 1.9 20 30 2.35 760 <10 120 0.12 <20 <50 21 <50 650 0.48 200 <50 20 180
RL.H-73 7.76 <30 50 <5 8.9 <10 360 50 150 7.07 0.2 <10 20 4.37 1690 <10 80 0.01 <20 <50 44 <50 130 0.45 280 <50 16 80
RL.H-74 4.58 <30 40 6 18.4 <10 90 30 120 4.71 0.3 <10 30 2.8 2940 <10 50 0.04 <20 <50 27 <50 50 0.31 180 <50 18 80 <5 <0.3
RL.H-75 6.1 <30 180 <5 8 <10 160 130 1350 13.1 0.6 <10 30 3.15 1970 <10 190 0.01 <20 <50 34 <50 80 0.4 260 <50 15 80
RL.H-76 7.45 <30 90 <5 9.9 <10 210 50 130 8.45 0.5 <10 20 3.61 2040 <10 160 0.02 <20 <50 41 <50 110 0.48 280 <50 18 120
RL.H-77 6.82 <30 400 5 0.8 <10 40 <10 <10 1.42 4.3 80 40 0.19 320 <10 <10 0.02 <20 <50 <5 <50 90 0.12 10 <50 77 40
RL.H-78 6.36 <30 160 <5 11.7 <10 180 40 190 7.63 0.4 <10 20 3.5 1920 <10 100 0.01 <20 <50 34 <50 80 0.41 240 <50 16 100
RL.H-79 7.74 <30 230 <5 6 <10 150 50 460 7.79 1.6 <10 20 2.06 1030 <10 90 0.04 <20 <50 29 <50 90 0.43 210 <50 19 290
RL.H-80 6.44 <30 140 <5 3 <10 80 120 630 11.1 1.2 20 20 1.37 570 <10 110 0.03 30 <50 10 <50 70 0.27 80 <50 14 1360 29 2.1
RL.H-81 7.97 <30 200 <5 3.8 <10 210 60 620 7.32 2.1 20 20 1.86 600 <10 80 0.04 30 <50 17 <50 80 0.35 110 <50 17 630 22 1.6
RL.H-82 7.09 40 240 <5 3.4 <10 100 70 710 6.28 2.1 10 10 1.69 610 <10 90 0.03 40 <50 19 <50 60 0.32 120 <50 15 1380
RL.H-83 10.6 80 350 <5 5.5 <10 190 60 320 4.52 2.7 10 20 3.37 630 <10 90 0.03 <20 <50 43 <50 120 0.49 270 <50 15 210
RL.H-84 4.74 350 140 <5 2.6 <10 60 40 170 4.69 1.1 10 60 1.65 430 <10 50 0.02 <20 <50 8 <50 40 0.16 50 <50 10 70
RL.H-85 7.22 70 220 <5 1.8 <10 60 30 130 7.5 2 10 80 2.18 540 <10 70 0.05 <20 <50 15 <50 50 0.31 90 <50 16 110
RL.H-86 2.82 <30 110 <5 6.2 <10 110 30 290 14.7 0.6 <10 <10 3.86 1800 <10 100 0.07 <20 <50 6 <50 180 0.14 60 <50 12 110 21 0.8
RL.H-87 6.38 <30 600 <5 5 <10 800 40 70 7.52 1.4 30 10 7.54 1230 <10 430 0.16 <20 <50 19 <50 940 0.41 160 <50 16 110
RL.H-88 5.81 460 1480 <5 2.6 60 380 30 24700 6.73 2.4 20 20 1.8 920 1250 350 0.13 7720 80 12 110 350 0.31 150 <50 17 9110 1410 78.4
RL H 89 5 69 80 170 <5 1 <10 80 90 670 8 62 1 5 10 40 1 86 330 <10 90 0 04 30 <50 12 <50 50 0 24 70 <50 14 1230RL.H-89 5.69 80 170 <5 1 <10 80 90 670 8.62 1.5 10 40 1.86 330 <10 90 0.04 30 <50 12 <50 50 0.24 70 <50 14 1230
RL.H-90 7.6 40 300 <5 2 <10 90 100 990 7.92 2.9 20 10 1.35 510 <10 120 0.06 30 <50 18 <50 50 0.32 100 <50 18 1610
RL.H-91 7.22 <30 270 <5 2.2 <10 70 60 560 12 2.6 20 20 1.84 1520 <10 100 0.04 30 <50 16 <50 40 0.29 100 <50 18 1660 64 0.8
RL.H-92 0.42 <30 <10 <5 2.6 <10 60 <10 70 18.8 <0.1 <10 <10 2.38 2660 <10 20 0.06 <20 <50 <5 <50 20 0.02 30 <50 7 170
RL.H-93 0.94 <30 10 <5 5 <10 20 10 160 17.2 0.2 <10 <10 2.83 2990 <10 20 0.04 <20 <50 <5 <50 30 0.04 30 <50 9 200
RL.H-94 6.49 <30 320 <5 1.3 <10 30 30 220 6.2 3.7 20 <10 0.84 540 <10 130 0.08 <20 <50 11 <50 50 0.35 60 <50 19 680
RL.H-95 6.49 <30 360 <5 1.1 <10 60 40 280 5.86 3.7 20 10 0.99 340 <10 110 0.05 <20 <50 12 <50 40 0.3 70 <50 20 1600
RL.H-96 7.36 50 420 <5 1.1 <10 90 40 310 4.87 4.1 20 10 0.98 350 <10 140 0.05 30 <50 15 <50 40 0.32 90 <50 20 1550
RL.H-97 6.54 40 370 <5 1.3 <10 120 50 470 6.06 3.3 20 10 1.36 530 <10 140 0.03 <20 <50 14 <50 40 0.25 80 <50 19 880 12 <0.3
RL.H-98 6.6 <30 340 <5 1 <10 60 30 260 6.24 3.4 30 10 1.32 420 <10 80 0.05 <20 <50 12 <50 30 0.31 80 <50 21 190
RL.H-99 6.9 <30 480 <5 0.8 <10 20 <10 <10 1.29 4.3 80 40 0.15 300 <10 <10 0.02 <20 <50 <5 <50 100 0.12 10 <50 78 50
RL.H-100 7.18 <30 380 <5 1.4 <10 110 30 130 5.13 3.7 30 20 1.41 420 <10 90 0.05 <20 <50 13 <50 40 0.27 80 <50 22 140
RL.H-101 7.17 <30 390 <5 0.7 <10 100 40 620 5.15 3.9 20 20 1.43 340 <10 100 0.04 <20 <50 13 <50 30 0.25 90 1280 23 350
RL.H-102 7.15 <30 450 <5 1.6 <10 100 60 300 5.88 4.2 20 10 1.47 410 <10 120 0.04 <20 <50 14 <50 40 0.27 90 <50 15 770
RL.H-103 7.98 <30 350 <5 2.9 <10 140 60 150 9.7 3.5 20 30 3.01 730 <10 130 0.03 <20 <50 32 <50 50 0.39 210 <50 19 90
RL.H-104 6.87 <30 430 <5 2.3 <10 70 20 260 4.07 3.2 20 10 1.87 480 <10 80 0.06 <20 <50 10 <50 40 0.21 60 <50 16 60
RL.H-105 6.36 <30 400 <5 1.6 <10 60 30 180 5.5 3.2 20 10 1.54 830 <10 70 0.04 <20 <50 11 <50 30 0.27 70 <50 16 190
RL.H-106 5.66 <30 280 <5 3.1 <10 80 50 390 7.52 2.6 20 <10 1.61 1230 <10 120 0.04 <20 <50 11 <50 40 0.22 80 <50 15 910 36 0.4
RL.H-107 7.78 <30 400 <5 1 <10 120 60 210 6.37 3.9 20 20 2.09 520 <10 130 0.05 <20 <50 17 <50 20 0.34 110 <50 18 140
RL.H-108 8.03 <30 500 <5 1 <10 80 30 40 4.52 3.7 20 30 2.15 440 <10 90 0.05 <20 <50 14 <50 20 0.36 90 <50 18 60
RL.H-109 6.45 <30 190 <5 5.3 <10 120 30 40 6.33 1.2 <10 20 4.92 1020 <10 100 0.02 <20 <50 24 <50 40 0.31 160 <50 11 80
RL.H-110 7.39 100 580 <5 0.9 20 50 20 4450 4.81 4.9 10 10 0.87 530 160 40 0.1 2060 70 11 270 270 0.35 160 <50 18 2600
RL.H-111 8.14 <30 300 <5 9 <10 160 50 80 7.58 1.6 <10 10 4.39 1390 <10 130 0.02 <20 <50 38 <50 50 0.42 250 <50 14 100
RL.H-112 7.43 <30 30 <5 8.1 <10 160 40 40 9.07 0.4 <10 30 3.73 1520 <10 90 0.09 <20 <50 36 <50 100 1.3 370 <50 35 100
第 2 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-113 8.08 <30 30 <5 7.4 <10 310 50 70 7.83 0.4 <10 30 3.69 1870 <10 110 0.03 <20 <50 42 <50 90 0.56 300 <50 20 150
RL.H-114 7.79 <30 40 <5 6.9 <10 300 50 90 8.15 0.5 <10 40 3.98 1960 <10 110 0.02 <20 <50 41 <50 100 0.47 270 <50 18 140
RL.H-115 7.9 <30 40 <5 8.5 <10 310 50 160 7.95 0.5 <10 30 3.41 2200 <10 110 0.02 <20 <50 41 <50 90 0.47 280 <50 18 170
RL.H-116 7.9 <30 10 <5 12 <10 300 40 60 7.44 0.2 <10 20 2.97 2600 10 110 0.02 <20 <50 41 <50 120 0.46 290 <50 18 170
RL.H-117 7.57 <30 20 <5 8.2 <10 280 50 80 6.81 0.2 <10 20 3 1840 20 110 0.01 <20 <50 40 <50 100 0.45 260 <50 17 100 <5 <0.3
RL.H-118 8.06 <30 50 <5 9 <10 310 50 60 7.34 0.4 <10 20 3.16 2010 10 110 0.02 <20 <50 43 <50 70 0.48 280 <50 18 110
RL.H-119 7.73 <30 20 <5 10.5 <10 280 40 50 7.52 0.3 <10 20 3.09 2270 30 110 0.02 <20 <50 38 <50 130 0.42 280 <50 17 180
RL.H-120 1.69 <30 <10 <5 2.6 <10 130 100 840 >30 <0.1 <10 <10 0.49 500 70 100 <0.01 <20 <50 <5 <50 40 0.07 80 <50 5 50
RL.H-121 6.95 <30 470 <5 0.9 <10 20 <10 <10 1.35 4.2 70 40 0.17 300 10 <10 0.01 <20 <50 <5 <50 100 0.12 10 <50 75 50
RL.H-122 6.37 <30 60 <5 7.8 <10 170 20 230 7.09 0.6 <10 20 3.08 1360 140 70 0.03 <20 <50 30 <50 110 0.43 210 <50 20 150 <5 <0.3
RL.H-123 7.94 <30 50 <5 8.2 <10 210 40 150 7.44 0.8 <10 40 3.96 1490 <10 90 0.02 <20 <50 40 <50 130 0.63 280 <50 23 120 <5 <0.3
RL.H-124 7.76 <30 80 <5 7.9 <10 330 50 80 8.08 1.7 <10 60 4.83 1460 20 120 0.02 <20 <50 40 <50 150 0.43 250 <50 16 180
RL.H-125 7.56 <30 20 <5 8.4 <10 280 40 90 8.05 0.6 <10 30 4.51 1570 <10 110 0.02 <20 <50 40 <50 190 0.42 260 <50 17 150
RL.H-126 7.96 <30 300 <5 3.1 <10 10 <10 <10 1.42 1.8 10 40 0.92 300 <10 10 0.03 <20 <50 <5 <50 100 0.16 20 <50 <5 30
RL.H-127 7.89 <30 340 <5 3.2 <10 100 <10 <10 1.37 1.6 <10 40 0.94 320 <10 <10 0.03 <20 <50 <5 <50 80 0.16 20 <50 <5 30
RL.H-128 7.16 <30 10 <5 11.5 <10 260 40 40 7.37 0.2 <10 20 3.97 2110 <10 90 0.02 <20 <50 40 <50 130 0.44 260 <50 20 160
RL.H-129 7.75 <30 10 <5 9.4 <10 270 40 100 7.88 0.4 <10 20 3.75 1700 30 100 0.02 <20 <50 41 <50 180 0.46 260 <50 19 120
RL.H-130 7.64 <30 20 <5 9.6 <10 250 30 90 7.08 0.4 <10 30 3.48 1460 <10 80 0.02 <20 <50 38 <50 90 0.42 250 <50 20 180
RL.H-131 2.34 50 30 <5 3.7 <10 60 120 2200 >30 0.4 <10 20 1.92 880 80 140 0.01 <20 <50 16 <50 30 0.18 100 <50 13 290 34 1.4
RL.H-132 5.91 460 1460 <5 2.7 60 370 30 25700 6.67 2.4 20 20 1.84 940 1260 260 0.13 7840 90 12 110 350 0.31 140 <50 17 9240
RL.H-133 1.6 90 10 <5 4 <10 60 100 5540 >30 0.2 <10 <10 1.63 720 110 120 <0.01 40 <50 8 <50 20 0.09 90 <50 5 300 20 4.6
RL.H-134 8.06 <30 60 <5 8.5 <10 300 40 190 7.71 0.6 <10 20 3.9 1730 <10 110 0.04 <20 <50 44 <50 90 0.49 280 <50 19 170
RL.H-135 7.65 <30 100 <5 8.3 <10 250 30 260 7.08 0.9 <10 40 4.48 1710 10 90 0.02 <20 <50 48 <50 80 0.42 240 <50 20 170
RL.H-136 8.48 <30 70 <5 7.8 <10 310 40 60 5.89 0.6 <10 20 4.37 1340 30 100 0.03 <20 <50 46 <50 100 0.52 270 <50 21 120
RL.H-137 7.31 <30 80 <5 6.9 <10 260 30 350 7.47 0.6 <10 20 3.85 1300 <10 100 0.02 <20 <50 35 <50 80 0.41 230 <50 18 130
RL.H-138 7.75 <30 40 <5 8.8 <10 290 40 120 7.27 0.4 <10 20 3.95 1580 <10 90 0.03 <20 <50 42 <50 90 0.49 270 <50 20 130
RL.H-139 0.44 120 <10 <5 2 <10 10 230 1860 >30 <0.1 <10 <10 0.35 330 20 140 <0.01 20 <50 <5 <50 <10 0.03 40 <50 <5 80 22 1.6
RL.H-140 1.38 <30 30 <5 4 <10 30 80 7560 >30 0.3 <10 10 2.03 910 60 430 0.01 40 <50 <5 <50 30 0.07 60 <50 6 260
RL.H-141 7.24 <30 30 <5 1 <10 <10 <10 180 1.05 1.5 <10 <10 0.04 190 <10 <10 <0.01 20 <50 7 <50 30 <0.01 <10 <50 39 <10
RL.H-142 6.66 <30 30 <5 1.3 <10 30 <10 180 0.92 2.1 <10 <10 0.04 330 <10 <10 <0.01 30 <50 6 <50 40 0.01 <10 <50 29 50
RL.H-143 6.87 <30 420 <5 1.3 <10 30 <10 20 1.16 4.1 70 40 0.14 280 <10 <10 0.02 20 <50 <5 <50 100 0.11 10 <50 74 50 <0.5 <0.3
RL.H-144 0.74 90 10 <5 3.9 <10 10 140 1930 >30 0.4 <10 <10 2.11 860 30 190 <0.01 30 <50 6 <50 20 0.02 40 <50 6 470 14 1.6
RL H 145 0 92 80 <10 <5 2 6 <10 30 150 3410 >30 0 1 <10 <10 1 15 580 180 240 <0 01 50 <50 <5 <50 10 0 01 40 <50 <5 280RL.H-145 0.92 80 <10 <5 2.6 <10 30 150 3410 >30 0.1 <10 <10 1.15 580 180 240 <0.01 50 <50 <5 <50 10 0.01 40 <50 <5 280
RL.H-146 0.95 <30 <10 <5 2 <10 10 80 4470 >30 0.5 <10 20 1.5 900 50 500 <0.01 40 <50 8 <50 <10 0.02 50 <50 <5 220 14 3.4
RL.H-147 5.69 <30 10 8 7.8 <10 110 20 640 9.51 0.8 <10 40 5.52 3140 <10 60 0.03 <20 <50 52 <50 40 0.33 220 <50 26 260
RL.H-148 5.19 <30 40 15 11.4 <10 80 20 360 5.91 0.9 <10 30 5.37 2870 <10 30 0.04 <20 <50 16 <50 40 0.19 120 <50 15 170
RL.H-149 6.76 <30 560 5 5.7 <10 480 40 40 6.53 1.5 20 70 6.1 1170 <10 290 0.15 <20 <50 19 <50 940 0.54 160 <50 13 100
RL.H-150 8.56 <30 140 7 6 <10 320 100 200 7.64 0.9 <10 30 3.24 1080 <10 380 0.03 <20 <50 39 <50 120 0.56 300 <50 18 80
RL.H-151 8.99 <30 80 8 7.9 <10 320 80 200 6.43 0.6 <10 20 2.65 1070 <10 280 0.03 <20 <50 41 <50 120 0.58 300 <50 19 120
RL.H-152 8.9 <30 130 6 7.5 <10 340 80 290 6.59 1.1 <10 40 2.99 1150 20 330 0.03 70 <50 40 <50 120 0.57 310 <50 17 220
RL.H-153 6.69 <30 40 9 11.6 <10 230 50 250 8.65 0.3 <10 20 4.05 1890 30 290 0.03 20 <50 30 <50 100 0.4 210 <50 14 310
RL.H-154 7.48 100 590 <5 0.7 20 40 20 4440 4.89 4.7 10 10 0.9 540 200 30 0.09 2070 60 12 260 280 0.36 170 <50 18 2560
RL.H-155 7.68 <30 80 6 4.5 <10 220 50 570 8.03 0.7 <10 40 1.76 650 40 230 0.02 30 <50 33 <50 90 0.34 170 <50 21 160 6 0.6
RL.H-156 8.06 <30 70 8 5 <10 240 80 370 6.95 0.8 <10 40 1.85 810 10 210 0.03 <20 <50 32 <50 110 0.38 210 <50 19 160
RL.H-157 8.07 <30 60 8 3.8 <10 260 70 410 6.59 0.7 <10 50 1.8 710 <10 270 0.03 <20 <50 33 <50 110 0.4 200 <50 17 150
RL.H-158 8.35 <30 30 7 5.6 <10 300 90 220 8.59 0.3 <10 30 2.43 1000 <10 370 0.02 <20 <50 38 <50 140 0.47 270 <50 15 160
RL.H-159 8.15 <30 40 6 4.4 <10 290 80 290 8.85 0.3 <10 30 2.78 930 <10 420 0.03 <20 <50 38 <50 110 0.47 260 <50 13 180
RL.H-160 7.2 <30 60 <5 5.6 <10 270 120 250 13.7 0.4 <10 30 2.04 810 <10 420 0.03 <20 <50 33 <50 100 0.42 250 <50 13 140 <5 0.3
RL.H-161 7.78 <30 70 5 7.6 <10 310 70 240 9.21 0.4 <10 30 1.8 940 40 320 0.03 <20 <50 37 <50 120 0.48 260 <50 13 130
RL.H-162 7.47 <30 100 5 6.5 <10 190 40 260 8.19 0.3 <10 20 0.87 760 20 300 0.03 <20 <50 22 <50 120 0.33 160 <50 9 70
RL.H-163 7.97 <30 130 7 4.7 <10 90 10 130 3.7 0.6 <10 30 1.03 520 <10 100 0.05 <20 <50 11 <50 130 0.23 80 <50 7 60
RL.H-164 7.34 <30 120 7 6 <10 210 130 710 11.8 0.6 <10 40 2.22 890 <10 440 0.05 <20 <50 28 <50 110 0.37 220 <50 13 160
RL.H-165 7.04 <30 370 8 0.9 <10 10 <10 10 1.74 4.3 80 40 0.16 340 <10 <10 0.01 <20 <50 <5 <50 90 0.12 10 <50 79 40
RL.H-166 7.41 <30 80 5 8.6 <10 280 100 320 12.5 0.3 <10 20 2.11 1200 30 390 0.03 <20 <50 36 <50 100 0.44 260 <50 17 170 6 0.5
RL.H-167 8.25 <30 50 <5 8.3 <10 290 80 240 9.35 0.4 <10 30 2.64 1260 <10 270 0.04 <20 <50 38 <50 120 0.47 270 <50 16 260
RL.H-168 7.2 <30 30 <5 6.8 <10 270 150 330 13.8 0.3 <10 30 2.22 980 20 420 0.02 <20 <50 35 <50 120 0.43 250 <50 14 190
第 3 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-169 8.13 <30 30 5 7.7 <10 310 70 210 8.92 0.3 <10 20 2.71 1140 <10 300 0.02 <20 <50 40 <50 120 0.49 280 <50 15 160
RL.H-170 8.25 <30 60 <5 7 <10 300 70 270 8.96 0.6 <10 40 2.29 1090 20 260 0.02 <20 <50 39 <50 110 0.47 270 <50 16 160
RL.H-171 7.46 <30 40 7 9 <10 280 90 240 10.7 0.2 <10 20 1.66 1250 <10 270 0.02 <20 <50 36 <50 90 0.44 260 <50 15 140
RL.H-172 8.73 <30 80 6 6.4 <10 320 50 220 7.2 0.6 <10 50 2.34 1010 <10 260 0.03 <20 <50 42 <50 90 0.51 290 <50 17 180
RL.H-173 8.23 <30 80 <5 6.6 <10 310 90 280 9.95 0.5 <10 50 2.61 1170 <10 270 0.02 <20 <50 40 <50 90 0.49 290 <50 17 140 6 <0.3
RL.H-174 8.24 <30 80 6 6.7 <10 310 60 280 8.05 0.4 <10 40 2.16 950 <10 260 0.03 <20 <50 39 <50 120 0.48 270 <50 16 120
RL.H-175 8.28 <30 60 9 7.5 <10 270 60 260 7.28 0.4 <10 40 2.05 940 10 220 0.02 <20 <50 38 <50 130 0.47 270 <50 15 120
RL.H-176 6.05 480 1510 6 2.6 60 370 30 25300 6.83 2.4 20 20 1.91 920 1280 260 0.13 7870 90 12 120 380 0.32 150 <50 18 8860
RL.H-177 7.95 <30 20 7 8.9 <10 200 50 150 9.7 0.4 <10 40 4.44 1810 <10 70 0.03 <20 <50 43 <50 130 0.55 310 <50 19 110
RL.H-178 7.47 <30 50 <5 8.1 <10 200 40 130 9.35 0.4 <10 30 4.25 1700 <10 70 0.03 <20 <50 42 <50 120 0.53 300 <50 17 100
RL.H-179 7.16 <30 160 <5 7.3 <10 200 50 160 7.99 0.9 <10 40 3.79 1430 <10 80 0.02 <20 <50 38 <50 80 0.44 270 <50 14 120
RL.H-180 6.43 <30 130 7 9.5 <10 240 80 730 10.5 0.8 <10 30 1.83 2290 10 180 0.03 <20 <50 37 <50 60 0.41 250 <50 20 130 12 0.5
RL.H-181 7.22 <30 40 6 7.9 <10 190 40 160 8.9 0.5 <10 20 3.99 1710 <10 70 0.03 <20 <50 40 <50 70 0.5 280 <50 17 120
RL.H-182 7.06 <30 20 5 8.4 <10 180 30 100 8.25 0.3 <10 20 3.74 1550 <10 60 0.03 <20 <50 39 <50 120 0.46 270 <50 17 100
RL.H-183 7.41 <30 10 <5 7.9 <10 180 40 90 9.37 0.3 <10 20 4.17 1720 <10 60 0.03 <20 <50 42 <50 130 0.52 300 <50 17 110
RL.H-184 7.44 <30 30 8 6.6 <10 170 40 140 7.74 0.4 <10 20 3.5 1460 <10 80 0.03 <20 <50 37 <50 80 0.44 250 <50 16 140
RL.H-185 7.7 <30 40 8 8.6 <10 280 80 500 9.8 0.3 <10 <10 1.63 1150 20 340 0.03 <20 <50 36 <50 110 0.46 240 <50 16 160 <5 0.6
RL.H-186 2.67 <30 <10 7 5.7 <10 90 190 1100 24.7 0.1 <10 <10 0.61 1040 60 540 0.01 <20 <50 10 <50 40 0.14 100 <50 9 320 19 1.7
RL.H-187 7.06 <30 380 14 0.8 <10 20 <10 20 1.56 4.3 80 40 0.16 340 <10 <10 0.03 <20 <50 <5 <50 100 0.12 10 <50 78 50
RL.H-188 6.72 <30 40 9 6.2 <10 150 50 280 10.9 0.4 <10 10 0.7 950 160 250 0.03 <20 <50 23 <50 90 0.33 190 <50 17 120
RL.H-189 5.01 <30 70 7 5.1 <10 150 60 520 13.8 0.5 <10 30 0.68 850 40 340 0.02 <20 <50 22 <50 60 0.3 180 <50 12 470
RL.H-190 1.26 <30 <10 <5 2.2 <10 90 50 280 9.1 0.2 <10 <10 0.28 390 10 180 0.02 <20 <50 5 <50 10 0.08 40 <50 6 300
RL.H-191 1.06 <30 <10 <5 4.8 <10 50 130 970 26.3 <0.1 <10 <10 0.25 800 120 510 <0.01 <20 <50 <5 <50 20 0.05 50 <50 9 160 7 1.7
RL.H-192 8.09 <30 100 7 8.3 <10 210 40 170 8.22 0.7 <10 20 2.44 1400 <10 110 0.04 <20 <50 34 <50 100 0.55 290 <50 16 140
RL.H-193 7.63 <30 60 9 10.2 <10 270 60 280 8.17 0.4 <10 20 1.5 1730 70 190 0.04 <20 <50 32 <50 110 0.53 270 <50 11 270
RL.H-194 7.65 <30 70 7 5.5 <10 250 60 370 5.67 0.5 <10 10 0.93 690 <10 180 0.02 <20 <50 30 <50 110 0.36 210 <50 14 150
RL.H-195 7.98 <30 60 7 7.4 <10 280 70 360 7.45 0.3 <10 10 1.16 880 <10 240 0.03 <20 <50 34 <50 130 0.41 230 <50 17 200
RL.H-196 7.16 <30 60 <5 3.8 <10 260 90 920 10.1 0.5 <10 50 2.41 770 <10 370 0.02 <20 <50 33 <50 100 0.4 240 <50 13 210
RL.H-197 7.35 <30 80 7 3.9 <10 260 140 1210 11.3 1 <10 30 2.96 910 <10 390 0.03 <20 <50 34 <50 100 0.42 250 <50 13 320 8 0.9
RL.H-198 7.39 110 580 <5 0.7 20 40 20 4380 4.91 4.8 10 10 0.87 530 180 30 0.1 2060 70 12 280 280 0.35 160 <50 18 2590
RL.H-199 7.85 <30 100 7 2.9 <10 290 90 1310 8.78 1.3 <10 50 2.87 560 <10 380 0.03 <20 <50 36 <50 90 0.43 250 <50 14 210
RL.H-200 7.59 <30 80 5 6 <10 210 60 390 7.65 0.9 <10 30 2.42 1110 <10 160 0.03 <20 <50 35 <50 90 0.41 220 <50 16 120
RL H 201 7 9 <30 260 <5 1 2 <10 20 <10 20 0 8 2 8 <10 10 0 11 130 <10 <10 <0 01 <20 <50 <5 <50 80 0 04 10 <50 7 10RL.H-201 7.9 <30 260 <5 1.2 <10 20 <10 20 0.8 2.8 <10 10 0.11 130 <10 <10 <0.01 <20 <50 <5 <50 80 0.04 10 <50 7 10
RL.H-202 7.78 <30 50 7 8.1 <10 220 40 70 8.85 0.7 <10 20 4.14 1710 <10 120 0.05 <20 <50 42 <50 100 0.56 300 <50 21 130
RL.H-203 5.86 <30 80 <5 4.2 <10 100 110 510 13.7 0.7 <10 10 0.97 680 20 530 0.02 <20 <50 14 <50 100 0.18 100 <50 8 190 10 0.3
RL.H-204 5.39 <30 270 <5 5 <10 670 140 290 13.6 0.9 10 40 4.21 810 <10 420 0.08 <20 <50 25 <50 250 0.31 190 <50 12 530
RL.H-205 7.95 <30 90 <5 3 <10 210 60 1420 10.6 0.7 <10 30 2.43 700 <10 340 0.02 <20 <50 41 <50 100 0.54 270 <50 19 290 9 0.7
RL.H-206 7.89 <30 80 6 3.2 <10 240 100 280 9.8 0.7 <10 30 2.38 1100 <10 190 0.04 <20 <50 41 <50 80 0.56 310 <50 18 210
RL.H-207 6.24 <30 130 <5 4 <10 240 100 180 10.9 0.6 <10 20 1.72 690 <10 260 0.02 <20 <50 31 <50 130 0.4 240 <50 12 460
RL.H-208 4.85 <30 360 <5 2.6 <10 200 30 60 5.68 1.4 20 30 2.44 590 <10 180 0.06 <20 <50 16 <50 250 0.26 130 <50 8 170
RL.H-209 7.2 <30 380 11 1.2 <10 30 <10 10 1.77 4.4 80 40 0.19 360 <10 <10 0.02 <20 <50 <5 <50 110 0.13 10 <50 79 50
RL.H-210 6.84 <30 50 <5 8.2 <10 220 40 190 11.3 0.4 <10 <10 1.49 1200 <10 210 0.03 <20 <50 34 <50 90 0.45 260 <50 16 220
RL.H-211 1.76 40 <10 <5 6.9 <10 70 100 180 23.8 <0.1 <10 <10 0.2 1100 10 220 0.01 <20 <50 6 <50 10 0.11 100 <50 <5 1210 15 0.3
RL.H-212 0.31 <30 <10 <5 2.2 <10 40 70 210 14.8 <0.1 <10 <10 0.04 240 10 160 <0.01 <20 <50 <5 <50 10 0.02 20 <50 <5 380
RL.H-213 0.32 <30 <10 <5 1 <10 60 30 150 4.66 <0.1 <10 <10 0.05 260 10 150 <0.01 <20 <50 <5 <50 <10 0.02 20 <50 <5 390
RL.H-214 2.65 <30 60 <5 1.9 <10 60 20 210 4.33 0.5 <10 <10 0.1 450 <10 190 0.01 <20 <50 <5 <50 60 0.06 40 <50 <5 100
RL.H-215 6.67 <30 320 7 1.1 <10 30 <10 30 1.54 1.6 <10 20 0.18 340 <10 10 0.01 <20 <50 <5 <50 120 0.08 20 <50 7 40
RL.H-216 7.09 <30 300 <5 1.2 <10 20 <10 30 1.02 2.1 <10 10 0.12 250 <10 <10 <0.01 <20 <50 <5 <50 250 0.05 10 <50 <5 10
RL.H-217 6.87 <30 70 <5 6.7 <10 40 50 100 12 0.4 <10 40 2.79 1720 <10 40 0.06 <20 <50 42 <50 90 0.94 420 <50 34 110
RL.H-218 7.16 <30 650 <5 8.5 <10 200 40 160 6.79 1.1 70 50 3.66 1330 <10 100 0.14 <20 <50 27 <50 1010 0.4 200 <50 18 110
RL.H-219 7.67 <30 40 <5 8.1 <10 300 50 100 8.68 0.4 <10 40 5.19 1590 <10 140 0.02 <20 <50 39 <50 100 0.43 260 <50 16 100
RL.H-220 6.06 450 1510 <5 2.7 60 380 30 25600 6.92 2.4 20 20 1.89 950 1290 300 0.13 7850 80 12 120 390 0.33 150 <50 17 9020 1230 78.6
RL.H-221 5.33 <30 140 <5 6.6 <10 390 90 630 15.3 0.6 10 20 0.96 940 20 190 0.03 <20 <50 13 <50 60 0.21 100 <50 10 110 7 1.1
RL.H-222 7.81 <30 410 <5 6.6 <10 180 70 130 5.1 1.2 30 50 2.27 960 <10 250 0.08 <20 <50 28 <50 440 0.47 220 <50 16 140
RL.H-223 8.68 <30 120 <5 6.6 <10 310 60 90 5.89 0.5 10 30 2.93 1310 <10 170 0.05 <20 <50 41 <50 280 0.5 280 <50 17 160
RL.H-224 7.74 <30 70 <5 6.6 <10 200 40 140 6.99 0.4 <10 30 2.29 1200 <10 110 0.04 <20 <50 35 <50 190 0.5 270 <50 17 90
第 4 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-225 6.11 <30 360 <5 4.9 <10 120 20 40 2.88 1.2 20 10 0.35 570 10 90 0.03 <20 <50 15 <50 80 0.23 120 <50 7 40 <5 <0.3
RL.H-226 5.37 <30 340 <5 3.4 <10 50 30 120 3.44 1.6 20 20 0.89 600 <10 80 0.03 <20 <50 13 <50 50 0.24 110 <50 9 170
RL.H-227 6.67 <30 140 <5 9.2 <10 220 40 90 7.99 1.6 20 40 4.33 3360 <10 100 0.09 130 <50 32 <50 150 0.64 280 <50 25 760 8
RL.H-228 6.09 <30 90 <5 7.3 20 90 20 120 7.87 1.8 10 20 2.5 5150 <10 70 0.03 110 <50 18 <50 80 0.39 150 <50 18 1150 12
RL.H-229 4.6 <30 80 <5 8.2 <10 100 30 190 8.59 1.2 10 30 3.04 4840 <10 80 0.03 <20 <50 14 <50 60 0.29 130 <50 21 550 18 0.6
RL.H-230 4.39 <30 80 <5 10.8 30 130 40 120 13.1 0.9 <10 20 3.99 6040 <10 110 0.03 <20 <50 24 <50 60 0.37 200 <50 37 2640 36
RL.H-231 7.02 <30 390 <5 0.8 <10 30 <10 <10 2.04 4.3 90 40 0.2 420 10 <10 0.01 <20 <50 <5 <50 90 0.12 10 <50 80 60
RL.H-232 2.51 <30 50 <5 6.8 <10 170 40 150 13.2 0.7 <10 10 2.12 2630 <10 120 0.03 <20 <50 11 <50 40 0.17 90 <50 14 600 11 1.4
RL.H-233 2.72 <30 60 <5 1.6 <10 110 60 210 16.8 1 <10 20 0.79 970 <10 150 0.03 20 <50 7 <50 30 0.17 80 <50 8 70 16 2.1
RL.H-234 0.35 <30 10 <5 2.1 <10 50 10 60 6.35 0.1 <10 <10 0.81 1770 <10 50 <0.01 <20 <50 <5 <50 <10 0.05 20 <50 <5 100 7
RL.H-235 0.91 <30 20 <5 3 <10 70 10 40 5.39 0.2 <10 <10 1.18 2870 <10 30 0.01 <20 <50 <5 <50 10 0.09 50 <50 8 140 6
RL.H-236 1.21 <30 10 <5 4 <10 60 10 80 6.81 0.2 <10 <10 1.92 3950 <10 40 0.02 <20 <50 7 <50 20 0.13 60 <50 11 390 13
RL.H-237 0.51 <30 <10 <5 4.5 <10 30 30 140 12.4 <0.1 <10 <10 2.01 5070 <10 100 0.03 <20 <50 <5 <50 <10 0.04 30 <50 9 360 15 1.8
RL.H-238 1.52 <30 30 <5 1.9 <10 60 30 110 9.43 0.5 <10 <10 0.88 1260 <10 80 0.01 <20 <50 6 <50 10 0.13 60 <50 <5 110 10
RL.H-239 4.28 <30 60 <5 2.4 <10 70 70 220 18.4 1.4 20 10 0.92 910 <10 170 0.03 20 <50 9 <50 40 0.24 90 <50 16 570 21
RL.H-240 2.67 <30 20 <5 3.1 <10 70 70 260 18.5 0.4 10 20 1.5 1080 <10 170 0.02 <20 <50 6 <50 20 0.13 60 <50 11 1330 26 2.2
RL.H-241 5.2 <30 70 <5 1.8 <10 100 80 360 21.3 1.4 10 30 1.15 1010 <10 200 0.05 40 <50 13 <50 40 0.29 110 <50 15 730 26
RL.H-242 7.4 110 590 <5 0.8 20 40 20 4420 4.9 4.8 20 10 0.88 530 160 30 0.1 2110 70 11 280 280 0.35 170 <50 17 2600 311 53.7
RL.H-243 2.31 <30 20 <5 1.7 <10 60 90 210 23.2 0.4 <10 10 1.07 650 <10 210 0.01 <20 <50 5 <50 20 0.11 70 <50 10 390 27
RL.H-244 2.24 <30 10 <5 1.8 <10 50 100 250 25.3 0.3 <10 <10 0.94 650 <10 220 0.02 <20 <50 5 <50 20 0.11 70 <50 10 750 30 3.3
RL.H-245 4.71 <30 30 <5 2.2 <10 70 40 220 12.1 0.6 20 20 2.31 880 <10 110 0.04 <20 <50 9 <50 40 0.28 90 <50 14 320 18
RL.H-246 5.62 30 50 <5 1.3 <10 80 70 170 18.6 0.6 <10 40 1.95 1130 <10 170 0.03 <20 <50 14 <50 50 0.32 120 <50 14 270 23
RL.H-247 3.96 <30 70 <5 2.9 <10 70 50 180 14.8 0.7 10 10 1.37 740 <10 130 0.03 <20 <50 9 <50 60 0.2 80 <50 13 450 19 1.6
RL.H-248 6.98 <30 60 <5 5.9 <10 250 40 100 10.7 0.5 10 20 3.63 1600 <10 100 0.08 <20 <50 34 <50 210 0.73 290 <50 22 180 <5
RL.H-249 6.75 <30 70 <5 3.9 <10 120 50 120 12.5 1.4 10 30 2.48 1130 <10 100 0.05 <20 <50 28 <50 70 0.58 230 <50 22 310 12
RL.H-250 2.72 <30 60 <5 4.2 <10 70 40 110 11 0.7 <10 10 1.34 1460 <10 80 0.02 <20 <50 11 <50 30 0.21 110 <50 8 260 9 0.8
RL.H-251 7.21 <30 90 <5 7.3 <10 130 40 120 10.3 0.7 <10 20 3.76 1980 <10 50 0.04 <20 <50 44 <50 70 0.72 350 <50 25 140 <5
RL.H-252 7.43 <30 110 <5 8.5 <10 130 50 140 11 1.6 <10 30 3.05 4890 <10 80 0.06 60 <50 38 <50 80 1.03 380 <50 35 500 <5
RL.H-253 7.12 <30 410 <5 0.8 <10 40 <10 <10 1.72 4.4 90 40 0.18 370 <10 <10 0.02 <20 <50 <5 <50 100 0.13 10 <50 80 50 <5
RL.H-254 6.87 <30 40 <5 9.1 <10 130 40 110 10.4 0.5 <10 20 3.25 2280 <10 60 0.06 <20 <50 35 <50 90 0.96 360 <50 35 130 <5
RL.H-255 6.88 <30 50 <5 9.5 <10 110 40 140 10 0.4 <10 20 2.76 2070 <10 70 0.06 <20 <50 34 <50 100 0.92 330 <50 34 100 <5
RL.H-256 7.14 <30 <10 <5 6.7 <10 120 50 140 11 0.1 <10 20 3.61 1720 <10 70 0.06 <20 <50 36 <50 170 0.99 360 <50 34 110 <5
RL H 257 7 4 <30 10 <5 7 6 <10 120 50 110 10 7 0 1 <10 20 3 42 1870 <10 70 0 06 <20 <50 37 <50 110 1 01 360 <50 35 120 <5RL.H-257 7.4 <30 10 <5 7.6 <10 120 50 110 10.7 0.1 <10 20 3.42 1870 <10 70 0.06 <20 <50 37 <50 110 1.01 360 <50 35 120 <5
RL.H-258 7.37 <30 60 <5 8.1 <10 130 40 110 11 0.2 <10 20 3.46 2110 <10 70 0.07 <20 <50 36 <50 90 0.99 360 <50 34 120 <5
RL.H-259 7.49 <30 260 <5 8.3 <10 140 50 120 10.5 0.6 <10 20 2.85 1920 <10 60 0.07 <20 <50 36 <50 110 0.98 360 <50 33 150 <5 <0.3
RL.H-260 7.57 <30 140 <5 7 <10 140 40 120 10.4 0.4 <10 20 3.47 1980 <10 60 0.07 <20 <50 37 <50 100 0.99 380 <50 33 110 <5
RL.H-261 7.58 <30 180 <5 6.7 <10 270 50 90 9.39 0.5 10 20 4.13 1860 <10 130 0.08 <20 <50 34 <50 270 0.92 340 <50 29 120 <5
RL.H-262 7.74 <30 200 <5 7.8 <10 240 40 70 7.93 0.7 10 40 3.54 1760 <10 120 0.07 <20 <50 31 <50 330 0.83 290 <50 28 110 <5
RL.H-263 7.79 <30 80 <5 8.2 <10 130 40 120 10.4 0.7 <10 20 2.97 1840 <10 60 0.07 <20 <50 38 <50 100 1.02 370 <50 34 90 <5
RL.H-264 6.01 460 1510 <5 2.7 60 370 30 25800 6.69 2.4 20 20 1.84 930 1260 250 0.13 7790 80 12 120 390 0.32 150 <50 17 8920 1260
RL.H-265 5.96 <30 100 <5 10.1 <10 100 30 170 7.92 1 <10 20 3.35 2110 <10 50 0.05 20 <50 26 <50 90 0.7 260 <50 27 170 7
RL.H-266 6.72 <30 150 <5 3.9 <10 80 30 140 8.27 2 20 30 1.82 890 <10 70 0.05 <20 <50 20 <50 70 0.56 200 <50 23 250 <5
RL.H-267 4.21 <30 130 <5 2 <10 90 50 200 18.3 1.5 20 30 1.07 850 <10 130 0.04 <20 <50 8 <50 40 0.26 90 <50 14 180 5 0.8
RL.H-268 0.76 <30 20 <5 2.6 <10 30 50 260 17 0.2 <10 <10 1.53 1210 <10 120 0.02 <20 <50 <5 <50 20 0.04 30 <50 6 180 5 1
RL.H-269 4.53 <30 90 <5 4.9 <10 120 40 270 15 0.6 10 30 2.18 3600 <10 110 0.03 <20 <50 18 <50 70 0.31 140 <50 17 300 8
RL.H-270 7.75 <30 150 <5 8.2 <10 320 40 80 9.03 0.5 10 30 4.93 1640 <10 140 0.04 <20 <50 36 <50 170 0.65 300 <50 21 110 <5
RL.H-271 7.68 <30 330 <5 6.3 <10 240 40 210 7.31 2.6 <10 50 1.76 1970 <10 130 0.03 <20 <50 43 <50 110 0.51 290 <50 19 60
RL.H-272 8.69 <30 140 <5 7.4 <10 250 50 290 8.55 2.7 <10 30 2 2200 <10 140 0.03 <20 <50 49 <50 90 0.58 300 <50 22 70
RL.H-273 7.89 <30 160 <5 5.6 <10 260 50 3010 8.83 2.4 <10 40 1.79 1730 <10 130 0.03 <20 <50 42 <50 80 0.55 300 <50 17 70
RL.H-274 7.06 <30 130 <5 4.2 <10 210 180 1330 14.2 2.2 <10 30 1.75 1300 <10 220 0.03 <20 <50 30 <50 50 0.49 260 <50 15 60 95 2.1
RL.H-275 7 <30 530 <5 1.5 <10 20 <10 <10 1.57 4.3 90 40 0.17 320 <10 <10 0.01 <20 <50 <5 <50 100 0.12 10 <50 79 110 <5 <0.3
RL.H-276 8.36 <30 140 <5 9.6 <10 230 50 300 7.23 2.4 <10 40 2.44 2090 <10 140 0.03 <20 <50 35 <50 70 0.56 290 <50 20 50
RL.H-277 9.71 <30 180 <5 5.1 <10 300 70 290 7.89 3.1 <10 50 1.76 1480 <10 190 0.03 <20 <50 47 <50 80 0.65 350 <50 21 60
RL.H-278 7.99 <30 660 <5 6.4 <10 90 40 70 7.46 1.8 30 60 4.68 1070 <10 70 0.29 <20 <50 30 <50 1070 0.86 310 <50 24 80 <10 6
RL.H-279 8.07 <30 640 <5 6.6 <10 100 40 80 7.74 1.7 30 50 4.93 1100 <10 70 0.3 <20 <50 31 <50 1060 0.91 320 <50 25 80 <10 <5
RL.H-280 8.19 <30 70 <5 4.5 <10 310 50 120 9.29 0.3 <10 20 3.42 2780 <10 120 0.04 <20 <50 38 <50 140 0.7 310 <50 22 210
第 5 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-281 7.14 <30 280 <5 7.1 <10 420 60 240 8.96 0.5 30 20 4.9 2280 <10 210 0.12 <20 <50 26 <50 470 0.57 220 <50 19 130 5 <0.3
RL.H-282 8.1 <30 300 <5 3.9 <10 360 50 130 8.77 0.6 20 40 3.84 2400 <10 200 0.09 <20 <50 34 <50 270 0.68 280 <50 22 270
RL.H-283 8.73 <30 70 <5 2 <10 320 50 110 9.83 0.2 <10 40 2.43 2890 <10 120 0.04 <20 <50 42 <50 70 0.77 330 <50 24 490
RL.H-284 8.73 <30 240 <5 2.4 <10 330 80 250 10.5 0.3 <10 30 1.75 2750 <10 160 0.04 <20 <50 38 <50 40 0.77 360 <50 23 320 <5 0.3
RL.H-285 8.63 <30 240 <5 2.4 <10 350 80 210 11 0.3 <10 20 1.69 2800 <10 170 0.04 <20 <50 31 <50 30 0.78 370 <50 21 170
RL.H-286 6.94 90 540 <5 0.7 20 30 20 4150 4.49 4.4 20 10 0.84 500 160 30 0.08 1940 60 11 250 250 0.33 150 <50 16 2380
RL.H-287 8.07 <30 80 <5 2.8 <10 280 90 440 12.7 0.2 <10 20 1.9 2810 <10 170 0.04 <20 <50 29 <50 40 0.74 350 <50 23 140
RL.H-288 7.6 <30 70 <5 5.5 <10 210 40 120 7.68 0.1 <10 <10 2.55 3010 <10 80 0.04 <20 <50 45 <50 60 0.77 340 <50 25 90
RL.H-289 7.93 <30 40 <5 3.8 <10 150 50 110 13.8 <0.1 <10 30 2.39 3360 <10 80 0.06 <20 <50 40 <50 90 1.03 400 <50 36 150
RL.H-290 5.38 <30 250 <5 2.5 <10 100 50 160 12.1 1 <10 40 1.79 2170 <10 80 0.05 <20 <50 27 <50 90 0.67 260 <50 24 150 6 <0.3
RL.H-291 8.07 <30 820 <5 2.4 <10 30 <10 <10 1.85 2.1 10 20 0.58 420 <10 <10 0.06 <20 <50 <5 <50 680 0.17 30 <50 <5 40
RL.H-292 6.85 <30 560 <5 1.8 <10 130 30 310 6.06 2.4 20 20 1.21 500 <10 80 0.07 <20 <50 10 <50 340 0.26 80 <50 13 1460
RL.H-293 5.47 <30 180 <5 1.1 <10 60 60 250 12.6 1.4 10 30 1.12 1170 <10 130 0.04 <20 <50 14 <50 60 0.43 140 <50 19 370 10 0.5
RL.H-294 8.04 <30 40 <5 5.7 <10 130 40 70 11.4 0.2 <10 20 3.43 2570 <10 70 0.06 <20 <50 36 <50 120 0.97 360 <50 34 130
RL.H-295 7.64 <30 50 <5 5.3 <10 140 50 110 10.4 0.2 <10 20 3.66 2300 <10 60 0.07 <20 <50 37 <50 110 1.01 380 <50 33 140
RL.H-296 8.37 <30 700 <5 5.4 <10 140 50 130 10.6 1.4 <10 50 2.89 1730 <10 80 0.07 <20 <50 43 <50 100 1.11 410 <50 37 120
RL.H-297 7.14 <30 470 6 0.7 <10 <10 <10 <10 1.61 4.3 90 40 0.18 350 <10 <10 0.02 <20 <50 <5 <50 110 0.12 10 <50 79 50
RL.H-298 8.05 <30 170 <5 3.4 <10 100 40 100 12.2 1.3 10 30 2.46 1420 <10 60 0.11 <20 <50 42 <50 110 1.22 280 <50 42 140
RL.H-299 6.37 <30 130 <5 6.7 <10 40 30 60 10.7 1.2 10 20 2.73 2390 <10 30 0.1 <20 <50 35 <50 100 1.03 170 <50 48 110
RL.H-300 6.48 <30 80 <5 5.7 <10 40 30 50 12.2 0.6 <10 10 2.7 2200 <10 20 0.11 <20 <50 35 <50 100 1.06 160 <50 48 130
RL.H-301 5.8 <30 90 <5 3.9 <10 80 30 110 11.2 0.7 10 60 2.1 1230 <10 60 0.07 <20 <50 19 <50 80 0.55 110 <50 29 220 5 <0.3
RL.H-302 7.03 <30 160 <5 0.7 <10 80 40 110 13.1 1.4 20 50 1.33 610 <10 130 0.04 <20 <50 13 <50 80 0.36 110 <50 21 410 6 <0.3
RL.H-303 3.96 <30 70 <5 3.8 <10 110 30 220 13.1 0.6 <10 10 1.5 1820 <10 100 0.02 <20 <50 13 <50 80 0.33 130 <50 18 320 <5 <0.3
RL.H-304 7.67 <30 100 <5 4.5 <10 240 40 130 11.4 0.9 <10 30 4.66 1710 <10 120 0.03 <20 <50 35 <50 80 0.6 280 <50 22 120
RL.H-305 6.85 <30 90 <5 4.4 <10 50 30 70 10.9 1 10 40 2.88 1570 <10 50 0.11 <20 <50 37 <50 60 1.11 160 <50 49 110
RL.H-306 5.33 <30 120 <5 0.3 <10 110 60 210 13.4 1.6 10 30 0.92 530 <10 120 0.03 <20 <50 16 <50 50 0.33 130 <50 15 1130 6 1.4
RL.H-307 6.38 <30 140 <5 0.4 <10 70 40 130 8.85 1.4 20 60 1.44 430 <10 110 0.03 30 <50 10 <50 50 0.23 90 <50 14 350
RL.H-308 6.14 470 1550 <5 2.6 60 370 30 26200 6.7 2.5 20 20 1.87 900 1260 260 0.12 8060 90 12 120 390 0.32 150 <50 18 9180
RL.H-309 7.09 <30 80 <5 2.4 <10 50 50 250 12.7 0.6 10 70 2.14 1290 <10 60 0.08 20 <50 30 <50 80 0.88 150 <50 40 220
RL.H-310 7.09 <30 90 <5 4.4 <10 40 40 80 12.3 0.6 10 20 2.47 1740 <10 30 0.11 <20 <50 36 <50 70 1.09 160 <50 50 180
RL.H-311 6.93 <30 20 <5 5 <10 40 40 40 12.6 <0.1 10 <10 2.17 1720 <10 20 0.11 <20 <50 36 <50 90 1.11 150 <50 53 150
RL.H-312 9.11 <30 270 <5 1.3 <10 160 30 110 5.23 3.3 20 20 1.6 1030 <10 80 0.03 <20 <50 21 <50 60 0.46 170 <50 15 170
RL H 313 8 47 <30 270 <5 0 5 <10 150 40 160 7 03 3 20 20 1 5 980 <10 100 0 03 <20 <50 22 <50 30 0 44 170 <50 16 250RL.H-313 8.47 <30 270 <5 0.5 <10 150 40 160 7.03 3 20 20 1.5 980 <10 100 0.03 <20 <50 22 <50 30 0.44 170 <50 16 250
RL.H-314 7.74 <30 390 <5 2 <10 200 30 110 6.6 2.4 20 20 2.21 1370 <10 110 0.05 <20 <50 19 <50 240 0.42 150 <50 14 310 5 <0.3
RL.H-315 7.23 <30 420 <5 3.6 <10 310 40 100 8.54 1.3 20 20 3.57 1930 <10 140 0.08 <20 <50 25 <50 380 0.53 220 <50 17 230
RL.H-316 8.85 <30 690 <5 4.1 <10 250 40 700 7.09 2.2 20 30 2.42 930 <10 80 0.07 <20 <50 24 <50 370 0.44 200 <50 20 530 8 <0.3
RL.H-317 7.91 <30 900 <5 4.7 <10 90 40 230 6.36 1.4 20 20 2.46 980 <10 50 0.14 <20 <50 17 <50 840 0.45 180 <50 18 140
RL.H-318 7.92 <30 690 <5 5.9 <10 230 30 190 6.87 0.9 20 20 3.96 1280 <10 70 0.14 <20 <50 24 <50 950 0.5 210 <50 20 110
RL.H-319 6.89 <30 430 6 0.7 <10 20 <10 <10 1.58 4.2 90 40 0.17 340 <10 <10 0.02 <20 <50 <5 <50 110 0.12 10 <50 89 50
RL.H-320 7.44 <30 80 <5 10.2 <10 270 30 130 5.86 1.2 <10 40 4.82 1970 <10 70 0.02 <20 <50 38 <50 80 0.39 250 <50 16 150
RL.H-321 6.96 <30 80 6 10.2 <10 210 30 300 5.97 1.5 <10 50 4.48 2080 <10 60 0.04 <20 <50 34 <50 70 0.54 250 <50 21 160
RL.H-322 7.42 <30 120 <5 4.9 <10 130 40 310 5.84 1.5 <10 30 2.81 1020 <10 60 0.05 <20 <50 34 <50 70 0.94 320 <50 35 70
RL.H-323 8.22 <30 170 6 5.6 <10 170 40 180 9.02 2.7 <10 60 3.96 1250 <10 70 0.09 <20 <50 48 <50 70 1.45 440 <50 38 110
RL.H-324 8.17 <30 720 <5 5.9 <10 110 30 100 7.12 1.8 30 40 4.27 1020 <10 60 0.26 <20 <50 28 <50 1140 0.8 290 <50 24 80 <5 <10 <5
RL.H-325 8.29 <30 760 <5 6 <10 130 30 80 7.01 2 30 30 4.25 1020 <10 70 0.27 <20 <50 27 <50 1150 0.79 290 <50 23 80 <5 <10 <5
RL.H-326 7.61 <30 70 <5 7.8 <10 190 50 110 13.4 0.6 <10 40 2.55 5140 <10 120 0.04 <20 <50 38 <50 50 0.71 330 <50 25 190
RL.H-327 7.96 <30 80 <5 8 <10 200 60 100 11.2 0.6 <10 40 2.43 4470 <10 120 0.04 <20 <50 39 <50 90 0.74 330 <50 24 140
RL.H-328 8.81 <30 170 <5 6.9 <10 230 60 190 8.11 0.3 <10 30 2.13 3300 <10 150 0.04 <20 <50 41 <50 140 0.81 360 <50 25 100
RL.H-329 6.4 <30 100 <5 11.2 <10 160 70 1170 14.2 0.5 <10 50 2 5330 <10 110 0.03 <20 <50 34 <50 100 0.58 300 <50 23 190
RL.H-330 7.35 80 540 <5 0.8 20 40 20 4300 4.74 4.6 20 10 0.89 550 160 30 0.09 2030 70 12 250 260 0.35 160 <50 17 2570
RL.H-331 8.94 <30 190 <5 5.7 <10 220 60 160 6.87 0.4 <10 30 2.06 2670 <10 130 0.06 <20 <50 42 <50 150 0.8 360 <50 23 100
RL.H-332 7 <30 90 <5 7.8 <10 80 50 170 13.4 0.3 <10 40 3.14 5090 <10 60 0.05 400 <50 46 <50 70 0.84 410 <50 36 160
RL.H-333 7.03 <30 100 <5 7 <10 60 50 160 11.2 0.5 <10 40 2.75 4270 <10 60 0.05 <20 <50 45 <50 80 0.86 400 <50 33 150
RL.H-334 7 <30 20 <5 8.3 <10 70 50 240 12.2 0.2 <10 30 2.42 4360 <10 60 0.05 <20 <50 45 <50 70 0.81 390 <50 34 180
RL.H-335 7.78 <30 320 <5 8.5 <10 280 60 300 9.06 1.5 <10 40 3.86 1720 <10 140 0.03 <20 <50 39 <50 100 0.43 260 <50 18 160
RL.H-336 7.64 <30 140 <5 9 <10 300 40 130 7.57 1 <10 30 3.87 1470 <10 130 0.02 <20 <50 37 <50 80 0.45 270 <50 17 100
第 6 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-337 7.34 <30 230 <5 7.8 <10 310 90 210 9.92 1.4 <10 50 4.55 1340 <10 140 0.03 <20 <50 34 <50 80 0.45 260 <50 16 210
RL.H-338 6.9 <30 160 <5 0.7 <10 60 <10 60 0.73 3.9 30 10 0.08 200 <10 <10 0.01 30 <50 <5 <50 80 0.06 <10 <50 7 20
RL.H-339 7.17 <30 170 <5 8.6 <10 240 30 210 6.9 1.4 <10 50 3.19 1700 <10 100 0.03 <20 <50 29 <50 110 0.36 210 <50 15 140
RL.H-340 6.92 <30 360 <5 0.6 <10 30 <10 30 1.09 4 20 10 0.08 210 <10 <10 <0.01 30 <50 <5 <50 110 0.05 <10 <50 6 20
RL.H-341 7.12 <30 460 6 0.7 <10 20 <10 40 1.38 4.6 90 40 0.15 330 <10 <10 0.01 <20 <50 <5 <50 90 0.12 10 <50 83 60
RL.H-342 8.28 <30 120 <5 12.7 <10 360 40 100 8.23 1.3 <10 40 2.82 2470 20 110 0.03 <20 <50 40 <50 110 0.48 290 <50 17 130
RL.H-343 8.55 <30 230 <5 9 <10 340 50 140 7.67 2.4 <10 50 2.48 1500 <10 150 0.03 <20 <50 43 <50 110 0.53 300 <50 16 120
RL.H-344 6 <30 120 <5 9.8 <10 1060 20 280 8.1 1.3 <10 40 3.85 1760 <10 160 0.03 720 <50 33 <50 130 0.3 210 <50 13 200
RL.H-345 0.74 <30 <10 <5 3.3 <10 30 <10 1100 >30 0.2 <10 <10 0.57 540 20 220 <0.01 <20 <50 <5 <50 <10 0.03 50 <50 <5 60
RL.H-346 6.97 <30 620 <5 3.5 <10 440 20 110 6.16 1.7 20 30 2.56 1040 <10 70 0.07 <20 <50 17 <50 600 0.25 110 <50 11 140
RL.H-347 4.62 <30 700 <5 1.4 <10 80 70 730 23.7 1.7 30 20 0.92 710 <10 140 0.06 <20 <50 <5 <50 530 0.15 60 <50 6 90
RL.H-348 0.93 <30 80 <5 1.4 <10 70 40 870 >30 0.3 <10 <10 0.59 430 <10 270 0.02 <20 <50 <5 <50 60 0.05 50 <50 <5 50
RL.H-349 4.1 <30 150 <5 4.5 <10 720 20 790 20.3 0.7 <10 20 2.96 1300 <10 170 0.01 <20 <50 17 <50 180 0.17 130 <50 9 160
RL.H-350 7.69 <30 1220 <5 1.9 <10 90 <10 60 2.98 3 40 60 1.04 490 <10 50 0.07 <20 <50 <5 <50 810 0.19 50 <50 7 50
RL.H-351 0.46 <30 <10 <5 1.3 <10 40 50 1160 >30 <0.1 <10 <10 0.55 580 <10 250 <0.01 <20 <50 <5 <50 10 0.02 50 <50 <5 110 25 2.8
RL.H-352 5.89 410 1510 <5 2.6 60 370 30 24700 6.74 2.4 20 20 1.85 950 1240 250 0.11 7750 90 12 110 350 0.32 140 <50 17 9120 1240 76.5
RL.H-353 3.61 <30 10 <5 0.8 <10 50 <10 300 7.16 1.7 <10 <10 0.38 500 30 30 <0.01 20 <50 <5 <50 20 0.04 20 <50 7 70
RL.H-354 0.78 <30 10 <5 1.6 <10 40 10 210 9.13 0.1 <10 <10 0.72 830 20 40 0.02 <20 <50 <5 <50 20 0.04 30 <50 6 90
RL.H-355 1.4 <30 20 <5 2.6 <10 40 30 390 15.2 0.1 <10 <10 1.21 1250 <10 50 0.02 <20 <50 <5 <50 50 0.08 40 <50 6 190 12 0.9
RL.H-356 2.2 <30 20 <5 1.8 <10 60 10 460 18.9 0.3 <10 10 1.39 2130 <10 80 0.02 <20 <50 5 <50 50 0.13 50 <50 8 260 23 0.9
RL.H-357 3.7 <30 70 <5 5.8 <10 720 50 160 9.29 0.4 <10 20 3.7 1190 <10 120 0.03 <20 <50 22 <50 130 0.17 140 <50 10 150
RL.H-358 5.41 <30 40 <5 3.6 <10 1120 40 270 14.9 0.7 <10 50 6.01 1740 <10 260 0.03 <20 <50 30 <50 80 0.24 190 <50 13 290
RL.H-359 2.77 <30 <10 <5 1.9 <10 80 80 410 24.1 0.2 <10 90 1.9 1830 <10 80 0.03 <20 <50 6 <50 60 0.18 80 <50 13 480 10 0.5
RL.H-360 7.28 <30 80 <5 6.1 <10 860 40 140 7.78 0.6 <10 50 6.41 1980 <10 120 0.02 <20 <50 45 <50 90 0.29 250 <50 16 170
RL.H-361 7.78 <30 100 <5 5.7 <10 790 40 150 7.02 0.9 <10 60 5.83 2110 <10 130 0.02 <20 <50 47 <50 110 0.3 250 <50 17 180
RL.H-362 1.6 <30 <10 <5 1.5 <10 90 110 260 26.1 0.2 <10 10 1.23 1060 <10 170 <0.01 <20 <50 <5 <50 10 0.1 60 <50 6 210
RL.H-363 7.02 <30 380 8 0.7 <10 30 <10 30 1.96 4.5 80 40 0.17 400 <10 <10 0.01 <20 <50 <5 <50 80 0.12 10 <50 75 50
RL.H-364 1.98 <30 50 <5 2.4 <10 30 60 350 >30 0.4 <10 10 1.02 1330 <10 170 0.02 <20 <50 <5 <50 40 0.12 70 <50 9 260
RL.H-365 2.66 <30 40 <5 2.1 <10 60 20 390 19.8 0.5 <10 30 1.43 1080 <10 110 <0.01 <20 <50 6 <50 40 0.17 80 <50 9 320 7 0.6
RL.H-366 1.05 <30 10 <5 1.9 <10 60 <10 100 8.49 0.3 <10 10 0.73 1140 20 40 <0.01 <20 <50 <5 <50 10 0.05 30 <50 <5 150
RL.H-367 6.63 <30 200 <5 0.7 <10 40 <10 50 1.5 3.9 20 <10 0.16 360 <10 <10 0.01 20 <50 <5 <50 80 0.06 <10 <50 5 30
RL.H-368 6.72 <30 320 <5 0.7 <10 30 <10 60 1.18 4 30 <10 0.06 300 <10 <10 0.01 30 <50 <5 <50 110 0.05 <10 <50 5 20
RL H 369 1 74 <30 30 <5 3 3 <10 60 <10 170 15 1 0 6 <10 <10 1 31 1880 <10 70 0 02 <20 <50 <5 <50 30 0 07 40 <50 9 110RL.H-369 1.74 <30 30 <5 3.3 <10 60 <10 170 15.1 0.6 <10 <10 1.31 1880 <10 70 0.02 <20 <50 <5 <50 30 0.07 40 <50 9 110
RL.H-370 0.7 <30 <10 <5 2.2 <10 30 360 320 >30 0.1 <10 <10 0.6 2060 <10 110 0.02 <20 <50 <5 <50 10 0.04 60 <50 9 210
RL.H-371 0.42 <30 <10 <5 2.3 <10 40 40 290 >30 0.1 <10 <10 0.51 1840 <10 120 <0.01 <20 <50 <5 <50 10 0.02 40 <50 7 90
RL.H-372 0.25 <30 <10 5 4.4 <10 20 40 390 >30 <0.1 <10 <10 0.36 1770 <10 220 0.02 <20 <50 <5 <50 20 0.02 50 <50 8 230 9 0.8
RL.H-373 0.49 <30 <10 <5 2.1 <10 140 70 310 >30 0.2 <10 <10 0.42 2450 <10 200 0.01 <20 <50 <5 <50 10 0.03 60 <50 7 100 11 0.8
RL.H-374 7.24 100 600 <5 0.8 20 50 20 4330 4.85 4.9 20 10 0.86 550 170 30 0.09 2130 80 12 270 260 0.35 170 <50 17 2690
RL.H-375 0.21 <30 <10 <5 3 <10 90 <10 150 27 <0.1 <10 <10 0.98 2340 <10 140 <0.01 <20 <50 <5 <50 10 0.01 40 <50 6 180
RL.H-376 0.37 <30 <10 <5 4.7 <10 50 20 330 >30 <0.1 <10 <10 1.4 1390 <10 140 <0.01 20 <50 <5 <50 <10 0.03 60 <50 15 60
RL.H-377 0.42 <30 <10 <5 3.1 <10 30 10 370 >30 <0.1 <10 <10 0.76 1000 <10 210 <0.01 <20 <50 <5 <50 <10 0.03 60 <50 9 150
RL.H-378 0.75 <30 30 <5 2.9 <10 30 30 350 >30 0.1 <10 <10 0.94 5450 <10 180 <0.01 <20 <50 <5 <50 <10 0.04 60 <50 11 590 26 1.2
RL.H-379 1.01 <30 50 <5 1.9 <10 20 60 320 >30 0.3 <10 <10 0.63 5210 <10 140 0.01 <20 <50 <5 <50 20 0.06 50 <50 7 160
RL.H-380 0.86 <30 40 <5 2.2 <10 20 40 470 >30 0.3 <10 <10 0.91 3670 <10 170 <0.01 <20 <50 <5 <50 20 0.03 50 <50 6 200
RL.H-381 0.56 <30 <10 <5 2.1 <10 20 110 480 >30 0.1 <10 <10 0.89 2180 <10 130 0.01 <20 <50 <5 <50 <10 0.03 50 <50 6 110
RL.H-382 0.4 <30 <10 <5 2.2 <10 20 160 640 >30 <0.1 <10 <10 0.97 2780 <10 110 0.02 30 <50 <5 <50 <10 0.02 50 <50 8 130 14 1
RL.H-383 0.75 <30 <10 <5 3.2 <10 10 110 260 >30 <0.1 <10 <10 1.4 3120 <10 100 <0.01 <20 <50 <5 <50 <10 0.04 50 <50 11 250
RL.H-384 0.58 <30 20 <5 1.9 <10 20 160 250 >30 0.2 <10 <10 0.28 3340 <10 120 0.01 <20 <50 <5 <50 20 0.03 50 <50 <5 130 15 0.6
RL.H-385 6.9 <30 510 8 0.9 <10 20 <10 40 2.63 4.5 80 40 0.17 450 <10 10 0.02 <20 <50 <5 <50 90 0.12 10 <50 78 50 <5 <0.3
RL.H-386 0.94 <30 50 <5 2 <10 20 110 220 >30 0.4 <10 <10 0.33 4610 <10 140 0.01 <20 <50 <5 <50 20 0.05 50 <50 <5 250
RL.H-387 1.38 <30 50 <5 3.2 <10 20 80 260 >30 0.4 <10 <10 0.6 4810 <10 140 <0.01 <20 <50 <5 <50 20 0.07 60 <50 7 1060
RL.H-388 1.11 <30 30 <5 2.2 <10 20 120 270 >30 0.3 <10 <10 0.33 6540 <10 150 0.01 <20 <50 <5 <50 20 0.05 50 <50 5 240 21 0.8
RL.H-389 1.42 <30 50 <5 2.5 <10 20 90 270 >30 0.5 <10 <10 0.47 6560 <10 130 <0.01 <20 <50 <5 <50 20 0.07 50 <50 5 170
RL.H-390 4.55 <30 130 <5 4.2 <10 50 10 170 16.9 1.3 10 10 1.45 1410 <10 80 0.03 <20 <50 8 <50 60 0.22 80 <50 16 220
RL.H-391 6.26 <30 230 7 4.2 <10 60 <10 130 12.2 2 20 20 1.13 1290 <10 60 0.05 <20 <50 14 <50 70 0.31 100 <50 16 110 8 <0.3
RL.H-392 4.98 <30 150 7 2.9 <10 50 30 180 18 1.7 <10 10 0.9 1840 <10 100 0.03 <20 <50 13 <50 70 0.23 90 <50 16 110 11 0.4
第 7 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-393 2.28 <30 30 5 2.3 <10 30 160 160 >30 0.3 <10 <10 0.77 1870 <10 80 0.02 30 <50 5 <50 10 0.17 70 <50 10 70 25 0.5
RL.H-394 2.1 30 10 7 2.5 <10 40 130 340 >30 0.2 <10 <10 0.86 3090 <10 160 0.02 <20 <50 <5 <50 10 0.13 100 <50 10 120
RL.H-395 6.02 <30 130 8 4.9 <10 140 10 130 14.2 1.4 10 <10 1.66 2650 <10 90 0.03 <20 <50 18 <50 40 0.38 140 <50 18 330
RL.H-396 6.13 450 1490 8 2.7 60 380 30 24900 6.94 2.4 20 20 1.88 1030 1250 260 0.14 7770 80 12 120 340 0.34 150 <50 17 9140
RL.H-397 5.91 <30 150 7 4.7 <10 590 10 120 10.5 1.6 10 10 1.63 2810 <10 80 0.03 <20 <50 18 <50 50 0.3 130 <50 19 230
RL.H-398 5.95 <30 170 8 3.7 <10 70 10 110 9.63 1.4 10 10 0.97 1950 <10 60 0.02 <20 <50 17 <50 60 0.33 120 <50 18 380 5 0.3
RL.H-399 7.14 <30 310 7 4.1 <10 80 10 70 7.39 1.9 20 10 1.02 2330 <10 50 0.04 <20 <50 17 <50 80 0.43 140 <50 21 430
RL.H-400 3.78 <30 80 6 3.3 <10 80 <10 150 24.6 0.6 <10 10 1 2530 <10 130 0.02 <20 <50 10 <50 30 0.24 100 <50 12 250
RL.H-401 1.6 <30 <10 <5 2 <10 50 10 210 >30 <0.1 <10 <10 0.67 2030 <10 190 0.02 <20 <50 <5 <50 <10 0.1 80 <50 8 360
RL.H-402 1.34 <30 <10 7 1.3 <10 40 130 150 >30 0.1 <10 <10 0.43 1390 <10 110 0.03 <20 <50 <5 <50 20 0.1 70 <50 6 80 9 0.4
RL.H-403 1.9 <30 40 7 2 <10 30 110 80 >30 0.6 <10 <10 0.56 2330 <10 70 0.02 <20 <50 <5 <50 20 0.09 60 <50 9 140
RL.H-404 6.74 <30 90 8 0.6 <10 30 <10 50 1.83 3.7 20 <10 0.08 280 <10 20 <0.01 <20 <50 <5 <50 60 0.05 10 <50 <5 20
RL.H-405 1.55 <30 30 6 2.8 <10 30 70 120 >30 0.4 <10 <10 0.4 2610 <10 50 0.02 30 <50 <5 <50 20 0.06 50 <50 8 150 12 <0.3
RL.H-406 0.49 30 <10 6 1.8 <10 30 100 80 >30 <0.1 <10 <10 0.56 3870 <10 60 0.01 <20 <50 <5 <50 <10 0.03 60 <50 10 50
RL.H-407 7.25 <30 400 12 0.8 <10 20 <10 30 1.55 4.4 80 40 0.18 390 <10 10 0.04 20 <50 <5 <50 90 0.13 10 <50 86 60
RL.H-408 0.12 <30 <10 <5 0.4 <10 70 <10 40 1.66 <0.1 <10 <10 0.04 410 <10 30 0.02 <20 <50 <5 <50 <10 0.01 <10 <50 <5 40 <5 1.4
RL.H-409 0.09 30 <10 <5 0.3 <10 100 <10 20 0.82 <0.1 <10 <10 0.05 270 <10 40 <0.01 <20 <50 <5 <50 <10 <0.01 <10 <50 <5 20
RL.H-410 0.26 40 <10 <5 1.2 <10 20 120 70 >30 <0.1 <10 <10 0.33 2480 <10 40 <0.01 <20 <50 <5 <50 <10 0.02 50 <50 5 60
RL.H-411 0.43 <30 <10 5 2.1 <10 10 100 160 >30 <0.1 <10 <10 0.63 4770 <10 60 0.02 <20 <50 <5 <50 10 0.02 60 <50 10 60
RL.H-412 0.75 <30 <10 <5 2 <10 40 70 80 27.1 <0.1 <10 <10 0.5 3250 <10 30 <0.01 <20 <50 <5 <50 20 0.04 50 <50 8 60
RL.H-413 0.82 <30 <10 5 3 <10 20 70 160 >30 <0.1 <10 <10 1.45 8530 <10 140 0.01 <20 <50 5 <50 <10 0.04 80 <50 19 100
RL.H-414 0.4 <30 <10 7 3.6 <10 80 <10 140 11.4 <0.1 <10 <10 0.91 6840 <10 40 <0.01 <20 <50 <5 <50 10 0.02 30 <50 10 60
RL.H-415 0.47 40 <10 6 2.3 <10 <10 100 120 >30 <0.1 <10 <10 0.89 7730 <10 70 0.01 <20 <50 <5 <50 10 0.03 60 <50 13 90
RL.H-416 0.5 40 30 6 2 <10 20 100 150 >30 0.1 <10 <10 0.57 4260 <10 60 0.02 <20 <50 <5 <50 10 0.03 60 <50 10 80 <5 0.5
RL.H-417 0.19 <30 <10 <5 2.6 <10 20 70 150 >30 <0.1 <10 <10 0.76 3230 <10 80 <0.01 <20 <50 <5 <50 <10 0.01 60 <50 11 50
RL.H-418 7.45 100 550 7 0.8 20 60 10 4250 4.91 4.6 10 10 0.89 560 170 30 0.11 2100 70 11 260 240 0.36 160 <50 18 2640 332 48.3
RL.H-419 0.24 <30 <10 <5 2.9 <10 50 30 90 21.7 <0.1 <10 <10 0.81 4090 <10 60 <0.01 <20 <50 <5 <50 <10 0.02 50 <50 12 80
RL.H-420 0.11 <30 10 <5 1.1 <10 40 10 140 25.8 <0.1 <10 <10 0.23 1810 <10 90 <0.01 <20 <50 <5 <50 <10 <0.01 40 <50 <5 40
RL.H-421 0.42 30 <10 <5 1.7 <10 30 60 230 >30 <0.1 <10 <10 0.42 5290 <10 90 0.01 <20 <50 <5 <50 10 0.03 60 <50 7 90 12 1
RL.H-422 0.31 <30 <10 <5 2.4 <10 40 10 90 15.4 <0.1 <10 <10 0.73 5500 <10 60 <0.01 <20 <50 6 <50 <10 0.02 40 <50 9 50
RL.H-423 0.67 30 30 <5 5 <10 40 50 590 29.1 0.1 <10 <10 0.62 5470 <10 70 0.01 <20 <50 <5 <50 50 0.03 60 <50 11 50
RL.H-424 1.21 <30 20 5 10.3 <10 20 60 340 >30 <0.1 <10 <10 0.44 4890 <10 80 0.02 <20 <50 <5 <50 90 0.04 50 <50 10 120
RL H 425 0 34 <30 10 <5 0 8 <10 50 20 50 9 49 <0 1 <10 <10 0 25 2880 <10 30 <0 01 <20 <50 <5 <50 <10 0 02 20 <50 <5 50RL.H-425 0.34 <30 10 <5 0.8 <10 50 20 50 9.49 <0.1 <10 <10 0.25 2880 <10 30 <0.01 <20 <50 <5 <50 <10 0.02 20 <50 <5 50
RL.H-426 0.43 50 <10 <5 3.6 <10 10 100 70 >30 <0.1 <10 <10 0.79 3680 <10 50 <0.01 <20 <50 <5 <50 20 0.02 60 <50 10 60
RL.H-427 0.76 <30 10 <5 2.1 <10 20 50 180 >30 0.1 <10 <10 0.56 4760 <10 110 0.02 <20 <50 <5 <50 10 0.05 70 <50 9 90 <5 0.9
RL.H-428 6.51 <30 180 6 0.6 <10 10 <10 50 1.13 3.5 20 <10 0.08 260 20 <10 <0.01 <20 <50 <5 <50 70 0.06 <10 <50 5 20
RL.H-429 7.11 <30 370 10 0.7 <10 20 <10 50 1.66 4.2 70 40 0.16 390 <10 10 0.02 20 <50 <5 <50 80 0.13 10 <50 78 80
RL.H-430 1.14 30 30 <5 1.9 <10 50 80 140 >30 0.2 <10 <10 0.79 11000 <10 60 0.01 <20 <50 <5 <50 20 0.07 60 <50 13 90
RL.H-431 0.59 <30 20 <5 2 <10 40 70 170 >30 <0.1 <10 <10 0.67 4110 <10 40 0.01 <20 <50 <5 <50 20 0.03 50 <50 9 60
RL.H-432 0.43 40 10 <5 1.9 <10 40 70 110 >30 <0.1 <10 <10 0.59 2690 <10 50 0.01 <20 <50 <5 <50 10 0.02 50 <50 7 50
RL.H-433 0.24 <30 <10 <5 1.1 <10 70 20 40 17.9 <0.1 <10 <10 0.25 2310 <10 20 0.02 <20 <50 <5 <50 <10 0.02 30 <50 <5 20
RL.H-434 0.65 40 <10 6 2.4 <10 20 80 90 >30 <0.1 <10 <10 0.82 7100 <10 50 0.02 <20 <50 <5 <50 10 0.03 60 <50 14 70
RL.H-435 0.57 <30 <10 <5 1.7 <10 20 70 120 >30 <0.1 <10 <10 0.67 6490 <10 50 0.01 <20 <50 <5 <50 <10 0.03 50 <50 8 80 9 0.7
RL.H-436 1.05 30 30 <5 1.8 <10 10 80 160 >30 0.2 <10 <10 0.75 6830 <10 70 0.01 <20 <50 <5 <50 10 0.06 60 <50 8 80
RL.H-437 7.08 <30 270 6 1.1 <10 40 <10 30 1.97 3.1 10 30 0.29 680 10 10 0.02 100 <50 <5 <50 130 0.12 30 <50 7 100
RL.H-438 6.89 30 340 7 0.6 <10 20 <10 40 1.16 4 20 10 0.12 450 <10 <10 0.02 40 <50 <5 <50 150 0.06 10 <50 <5 40
RL.H-439 6.59 <30 130 7 7.7 <10 210 50 240 16.1 0.3 <10 30 3.4 4490 <10 120 0.04 <20 <50 30 <50 70 0.57 250 <50 23 330
RL.H-440 6.08 420 1460 7 2.7 60 360 30 24900 6.75 2.3 20 20 1.89 940 1270 270 0.13 7880 80 12 120 340 0.33 150 <50 18 9170
RL.H-441 7.47 <30 130 10 9.1 <10 230 40 290 11.3 0.3 <10 30 3.24 4860 <10 110 0.05 <20 <50 42 <50 80 0.69 320 <50 26 110
RL.H-442 6.5 <30 80 9 7.4 <10 530 60 280 13.4 0.4 <10 30 3.9 4300 <10 180 0.04 <20 <50 39 <50 50 0.57 290 <50 23 160
RL.H-443 7.13 <30 90 8 8.6 <10 120 50 170 15.6 0.2 <10 40 3.73 6280 <10 100 0.04 <20 <50 42 <50 60 0.58 320 <50 25 270
RL.H-444 6.89 <30 20 10 7.2 <10 170 50 370 15.1 0.2 <10 40 3.34 5650 <10 100 0.05 <20 <50 41 <50 70 0.71 350 <50 30 380
RL.H-445 5.89 <30 70 8 6.3 <10 100 40 200 12.6 0.7 <10 50 2.86 4370 <10 60 0.03 <20 <50 35 <50 40 0.69 350 <50 29 110 <5 <0.3
RL.H-446 7.5 <30 130 8 6.3 <10 70 50 250 12.3 1.6 <10 100 2.71 4180 <10 100 0.07 <20 <50 45 <50 40 0.94 420 <50 33 130
RL.H-447 7.68 <30 100 8 8.9 <10 30 40 230 12.4 1.4 <10 30 3.15 5370 <10 60 0.06 <20 <50 47 <50 50 0.95 430 <50 36 150
RL.H-448 4.23 <30 60 7 5.4 <10 60 30 190 7.7 0.6 <10 30 1.93 3160 <10 40 0.07 <20 <50 27 <50 30 0.51 260 <50 22 170
第 8 页,共 9 页
Elements Al As Ba Be Ca Cd Cr Co Cu Fe K La Li Mg Mn Mo Ni P Pb Sb Sc Sn Sr Ti V W Y Zn Au Ag Pt Pd
Method ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A ICP90A FAI323 AAS21E FAI323 FAI323
Limit 0.01 30 10 5 0.1 10 10 10 10 0.01 0.1 10 10 0.01 10 10 10 0.01 20 50 5 50 10 0.01 10 50 5 10 5 0.3 10 5
Unit % ppm ppm ppm % ppm ppm ppm ppm % % ppm ppm % ppm ppm ppm % ppm ppm ppm ppm ppm % ppm ppm ppm ppm ppb g/t ppb ppb
Richardson Lake 2011 Assay Results
RL.H-449 8.47 <30 130 9 8.4 <10 30 50 240 13.6 1.3 <10 60 3.15 6040 <10 60 0.04 <20 <50 52 <50 60 1.03 460 <50 40 160
RL.H-450 1.06 <30 20 <5 1.5 <10 70 10 140 2.39 0.3 <10 10 0.48 1170 <10 30 0.02 20 <50 5 <50 20 0.11 70 <50 6 30
RL.H-451 7.08 <30 440 12 0.8 <10 20 <10 170 1.47 4.3 70 40 0.18 400 10 10 0.02 30 <50 <5 <50 90 0.13 20 <50 81 90
RL.H-452 2.18 <30 40 11 3.5 <10 70 20 150 5.4 0.2 <10 10 1.23 2320 <10 30 0.03 <20 <50 12 <50 30 0.24 140 <50 12 60
RL.H-453 2.4 <30 70 7 5.8 <10 170 40 210 6.88 0.1 <10 20 2.73 3240 <10 100 0.02 <20 <50 13 <50 100 0.2 130 <50 11 60 <5 <0.3
RL.H-454 1.89 <30 100 6 2 <10 270 30 160 3.15 0.2 <10 20 2.16 930 <10 120 0.04 <20 <50 7 <50 150 0.16 80 <50 7 40 <5 <0.3
RL.H-455 0.12 <30 <10 5 0.4 <10 70 <10 30 0.57 <0.1 <10 <10 0.07 170 <10 10 <0.01 <20 <50 <5 <50 <10 <0.01 10 <50 <5 10
RL.H-456 5.84 <30 170 8 6.6 <10 340 70 710 13.4 0.5 <10 40 5.06 3680 <10 250 0.08 <20 <50 32 <50 240 0.59 280 <50 24 120 <5 <0.3
RL.H-457 5.2 <30 100 6 6.4 <10 860 70 2580 11.8 0.6 10 70 5.74 3290 <10 300 0.07 110 <50 22 <50 50 0.36 170 <50 17 470
RL.H-458 N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. N.A. <5 4.8
第 9 页,共 9 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 633682.998 East: Original Units: M North: North: 5438207.218 North: Storage: Markham Elevation: Elevation: 497.124 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFFFFFF
Page 1 of 12
Control Drilling: Cutting Sampled: YesGeophysics:
Deviation Tests
Target: VETM anomaly supported by Geotech reportComments: ZK1 returned 147 ppb Au over a 6.57 metre core length from 21.35 to 27.92 metres including 236 ppb Au over a 2.62 metre core length from 21.35 to 23.97 metres.This anomalous gold intersection lies within siltstone-magnetite-richargillite metasedimentary unit containing foliation parallel pyrrhotite bands and disseminations.
Contractor: TOPRANKSpotted by: ShawnCoord Type:Surveyed Date: Logged by: ShawnRe-logged by: Water Source: Water Line: Left in hole: Casing + Shoe
CHINA METALLURGICAL EXPLORATION CORP. Diamond Drill Hole Report
Casing
Completed: 13-March-11Logged: 14-March-11Wedged: NoWedged from:
Capped: YesCemented: No
Hole Number: ZK1
Project Number:
Other
Distance(m)
89.488.487.7
133.20154.53
Length: 163.68 metersStarted: 10-March-11
LocationTownship: Richardson Lake AreaClaim No: 4248129NTS:
Length: 9.75 metersPulled: No
DrillingAzimuth: 90Dip: -45
16-Nov-12
Azimuth11.28 79.541.76 93.972.24 93.6
102.72
0B
From To From To
ZK1 01 Overburden 0 9.75 9.75 Overburden\casing. 9.55-9.75m,K-feldspar granite,light flesh red color,medium-coarse grained,not see the contact with the underlying volcanic rocks,probably is float.
ZK1 02Pyrrhotite meta-basalt
9.75 20.05 10.3 9.7 94
Dark,fine-grained,rare porphyritic texture,amygdaloidal structure,diameter of amygdaloid is <1mm,calcspar filling,composed of pyroxene and a small amount of quartz and biotite. The rock development epidotization, pyrrhotite, partial see a small amount of pyrite and chalcopyrite. Pyrrhotite veinlets were banded, some of them were small lumpy, the width of pyrrhotite stringer was about 1-5mm, fine-grained, content was about 5%, partial up to 20%; pyrite, chalcopyrite distributed localy, mainly in rock fracture surface as fine-grained, often coexist with pyrrhotite, content is <1%. 14.15-15.53m, rock crushing. 13.26m ,a little bit chalcopyrite.
RL.H-1 9.75 11.28 1.53 0.93 61 390 70 2100 280 <10 670 100
RL.H-2 12.68 1.40 1.40 100 260 60 1680 260 <10 730 90
RL.H-3 14.08 1.40 1.40 100 370 60 2050 220 <10 700 80
RL.H-4 15.43 1.35 1.35 100 260 60 930 250 <10 690 70
RL.H-5 16.8 1.37 1.37 100 520 80 1460 350 <10 680 120
RL.H-6 18.17 1.37 1.37 100 370 60 1290 270 <10 710 90
RL.H-7 19.05 0.88 0.88 100 380 50 1000 240 <10 700 80
RL.H-8 20.05 1.00 1.00 100 330 40 830 290 <10 760 100
RL.H-9 21.35 1.30 1.30 100 100 <20 150 80 <10 120 30
RL.H-10 22.7 1.35 1.35 100 110 <20 290 80 <10 160 40
RL.H-12 23.97 1.27 1.27 100 170 20 440 150 <10 253 <0.3 300 70
RL.H-13 25.33 1.36 1.30 96 280 <20 510 100 <10 240 50
RL.H-14 26.52 1.19 1.14 96 100 <20 260 60 <10 200 30
RL.H-15 27.92 1.40 1.40 100 310 <20 970 120 <10 63 0.3 140 50
Moppm
Auppb
Agg/t
Assay Results
Cuppm
Pbppm
Znppm
Nippm
Length of
core (m)
Recovery
factor(%)
Thickness
(m)
Length of core (m)
Recovery
factor(%)
DescriptionHole No.
No.Rock/Ore
type Crppm
Location (m)
Gray-dark gray, fine-grained to aphanitic structure, banded structure, composed of pyroxene, hornblende and quartz and biotite. Magnetic to weak magnetic, magnetic minerals are mainly magnetite and pyrrhotite. Generally developed pyrrhotite, magnetite , locally developed pyrite and minor chalcopyrite. Pyrrhotite were mainly distributed as irregular banded veinlets and lumpy shape, content was about 5-50%; magnetite was distributed as black banded vein; partial can see some pyrite and chalcopyrite, and often coexist with pyrrhotite. Development of the chlorite and(or) epidotization. Two group joint,30°and 50°to core axis. 20.05-29.57m,iron formation,pyrrhotite were mainly distributed as irregular banded veinlets,the width of veinlets were about 5-30mm, 60°to core axis,content was >70%,some pyrrhotite were in banded veinlets,contnt was about 5-10%;26.65-26.75m,10cm width massive pyrrhotite。 29.57-32.61m,banded,veined pyrrhotite, about 20%;31.70m,a little bit lumpy chalcopyrite were distributed in pyrrhotite.
32 61-39 76m Intensive distribution of irregular banded veined and lumpy
Coppm
Drill Log of Hole #RLP-11-01
Depth(m)
Sample log
Sample No.
Length(m)
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-16 29.57 1.65 1.65 100 40 <20 80 30 <10 40 <10
RL.H-17 30.86 1.29 1.20 93 200 30 880 160 <10 320 70
RL.H-18 32.26 1.40 1.30 93 330 40 590 100 <10 220 50
RL.H-19 33.66 1.40 1.33 95 550 60 1130 170 <10 43 0.6 230 90
RL.H-20 34.92 1.26 1.20 95 1960 30 870 140 <10 180 80
RL.H-21 36.09 1.17 1.14 97 610 50 1610 200 <10 220 110
RL.H-23 37.41 1.32 1.32 100 370 40 1010 140 <10 300 80
RL.H-24 38.71 1.30 1.30 100 560 50 1580 230 <10 31 1 110 120
RL.H-25 39.76 1.05 1.05 100 690 50 1160 210 <10 110 120
RL.H-26 40.91 1.15 1.15 100 100 <20 90 30 <10 30 20
RL.H-27 42.29 1.38 1.35 98 100 <20 120 40 <10 40 20
RL.H-28 43.51 1.22 1.15 94 150 <20 630 110 <10 290 50
RL.H-29 44.81 1.30 1.23 94 440 30 1100 170 <10 31 <0.3 300 80
RL.H-30 45.91 1.10 1.10 100 240 <20 180 180 <10 130 60
RL.H-31 46.91 1.00 1.00 100 540 <20 530 160 <10 250 50
RL.H-32 47.85 0.94 0.94 100 290 <20 240 130 <10 310 40
RL.H-34 49.07 1.22 1.22 100 130 <20 210 90 <10 140 30
RL.H-35 50.42 1.35 1.35 100 360 <20 950 120 <10 76 <0.3 190 40
RL.H-36 51.87 1.45 1.44 99 370 <20 350 100 <10 240 30
RL.H-37 53.26 1.39 1.38 99 40 <20 80 50 <10 60 10
RL.H-38 54.56 1.30 1.30 100 10 <20 50 70 <10 170 <10
RL.H-39 56.01 1.45 1.45 100 30 <20 80 100 <10 310 10
RL.H-40 57.34 1.33 1.33 100 70 <20 140 50 10 140 10
03ZK1 86.5720.05Iron
Formation
32.61 39.76m,Intensive distribution of irregular banded,veined and lumpy pyrrhotite,about 50-70%;32.86m、34.56m、38.93m see minor chalcopyrit. 39.76-42.29m,sulphide <5%. 42.29-47.85m,banded pyrrhotite,30%;45.80m,a little bit lumpy chalcopyrit. 47.85-57.34m,content of pyrrhotite was about 10%. 57.34-63.95m,content of sulphide was about 40%,mainly pyrrhotite,irregular banded and lumpy;62.23m intensive distribution of irregular banded and veined pyrrhotite. 63.95-66.90m,sulphide <5%. 66.90-74.13m,aphanitic-glassy, black, banded pyrrhotite development,local see lumpy Prr, content was about 20%; 70.00m ,the pyrite and pyrrhotite coexist distribution. 74.13-81.04m,pyrrhotite,minor pyrite,content of sulphide was about 20%;75.70m,Py=1/5 Po. 81.04-86.57m,aphanitic-glassy,pyrrhotite about 10%,minor pyrite,Py=1/10 Po.
9965.6466.52
第 1 页,共 19 页
From To From To
Moppm
Auppb
Agg/t
Assay Results
Cuppm
Pbppm
Znppm
Nippm
Length of
core (m)
Recovery
factor(%)
Thickness
(m)
Length of core (m)
Recovery
factor(%)
DescriptionHole No.
No.Rock/Ore
type Crppm
Location (m)Coppm
Drill Log of Hole #RLP-11-01
Depth(m)
Sample log
Sample No.
Length(m)
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-41 58.74 1.40 1.40 100 230 20 290 170 <10 29 0.3 90 50
RL.H-42 60.05 1.31 1.31 100 680 30 440 260 <10 350 170
RL.H-43 61.25 1.20 1.20 100 430 20 310 190 <10 470 40
RL.H-45 62.55 1.30 1.30 100 480 20 2000 260 <10 61 0.6 460 110
RL.H-46 63.95 1.40 1.40 100 390 <20 1320 160 <10 150 90
RL.H-47 65.5 1.55 1.55 100 180 <20 170 130 <10 380 50
RL.H-48 66.9 1.40 1.40 100 100 <20 250 170 <10 410 50
RL.H-49 68.11 1.21 1.20 98 310 <20 640 140 <10 550 70
RL.H-50 69.19 1.08 1.06 98 140 <20 670 130 <10 680 50
RL.H-51 70.39 1.20 1.15 96 130 <20 240 150 <10 30 <0.3 420 70
RL.H-52 71.58 1.19 1.14 96 130 <20 190 110 <10 210 40
RL.H-53 72.91 1.33 1.30 98 100 20 250 130 <10 41 <0.3 230 40
RL.H-54 74.13 1.22 1.22 100 140 <20 180 170 <10 420 30
RL.H-56 75.29 1.16 1.16 100 190 <20 130 170 <10 140 50
RL.H-57 76.59 1.30 1.30 100 210 <20 260 190 50 19 0.3 130 110
RL.H-58 77.79 1.20 1.20 100 80 <20 140 70 <10 100 20
RL.H-59 78.94 1.15 1.15 100 70 <20 50 70 <10 20 20
RL.H-60 80.04 1.10 1.10 100 120 <20 100 130 <10 100 20
RL.H-61 81.08 1.04 1.04 100 130 <20 130 140 <10 28 <0.3 70 40
RL.H-62 82.28 1.20 1.20 100 110 <20 190 120 <10 90 20
RL.H-63 83.48 1.20 1.20 100 60 <20 160 140 <10 310 40
RL.H-64 84.94 1.46 1.46 100 90 <20 190 140 <10 23 <0.3 190 40
RL.H-65 86.57 1.63 1.60 98 70 <20 140 110 <10 170 30
RL.H-67 87.91 1.34 1.30 98 70 <20 130 70 <10 120 30
RL.H-68 89.03 1.12 1.10 98 110 <20 110 200 <10 190 50
04meta-
andesite86.57 102.72ZK1 16.15 15.91 99
Gray to dark green,medium to fine grained,massive structure,mineral compositionare mainly amphibole, feldspar and a small amount of quartz, biotite,scattereddistribution Prr and Py,general development of the chlorite and epidotization. One group joint,50°to core axis.
86.58-88.28m,lumpy Po, 5%;92.49m,minor Py。
ZK1 05 lamprophyre 102.72 104.02 1.3 1.3 100 Dark gray,porphyritic texture,massive structure,mineral composition are mainly feldspar,hornblende and biotite, phenocrysts were biotite.
ZK1 06meta-
andesite104.02 130.15 26.13 26.13 100
Gray to dark green,medium to fine grained,massive structure,mineral composition are mainly amphibole, feldspar and a small amount of quartz and biotite.
ZK1 07 lamprophyre 130.15 131.93 1.78 1.78 100 Dark gray,porphyritic texture,massive structure,mineral composition are mainly feldspar,hornblende and biotite, phenocrysts were biotite.
ZK1 08meta-
andesite131.93 163.68 31.75 31.6 100
Gray to dark green,medium to fine grained,massive structure,mineral composition are mainly amphibole, feldspar and quartz .Chlorite and epidotization were common.
86.58 88.28m,lumpy Po, 5%;92.49m,minor Py。
第 2 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 633404.587 East: Original Units: M North: North: 5438233.876 North: Storage: Markham Elevation: Elevation: 501.69 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFFF
Page 2 of 12
68.58 85.1114.30 84.3
Deviation TestsDistance(m)
25.91 86.6Azimuth
Geophysics: Target: VETM anomaly supported by Geotech reportComments: ZK2 intersected 5-10% wispy Po veinlets and minor Cpy from 36.15m to 37.35m that may explain the targeted EM conductor. Limited assays returned no significant gold or base metal content.
Control Drilling: Cutting Sampled: Yes
Wedged from: Water Line: Left in hole: Casing + Shoe
Logged: 17-March-11 Re-logged by: Wedged: No Water Source:
Started: 13-March-11 Cemented: No Surveyed Date: Completed: 16-March-11 Logged by: Shawn
Length: 123.44 meters Capped: Yes NTS: Coord Type: Dip: -45 Pulled: No Claim No: 4248129 Spotted by: Shawn
OtherAzimuth: 70 Length: 1.11 meters Township: Richardson Lake Area Contractor: TOPRANK
Drilling Casing Location
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK2
Diamond Drill Hole Report Project Number:
16-Nov-12
1B
From To From To
ZK2 01 Overburden 0 1.11 1.11 0 0 Overburden\casing.
RL.H-69 13.58 14.74 1.16 1.16 100 120 <20 90 130 <10 280 50
RL.H-70 15.94 1.20 1.20 100 130 <20 90 120 <10 <5 <0.3 270 50
RL.H-71 19.36 20.38 1.02 1.02 100 170 <20 80 140 <10 270 50
RL.H-72 21.48 1.10 1.10 100 360 <20 180 120 <10 100 70
RL.H-316 36.15 37.35 1.20 1.20 100 700 <20 530 80 <10 8 <0.3 250 40
RL.H-317 38.10 0.75 0.75 100 230 <20 140 50 <10 90 40
RL.H-318 39.10 1.00 1.00 100 190 <20 110 70 <10 230 30
ZK2 03 lamprophyre 68.3 71.79 3.49 3.49 100 Dark gray to dark, porphyritic texture and massive structure, mineral composition are plagioclase, hornblende and biotite, phenocrysts were biotite.
RL.H-73 91.08 92.23 1.15 1.15 100 150 <20 80 80 <10 360 50
RL.H-74 121.87 123.44 1.57 1.40 89 120 <20 80 50 <10 <5 <0.3 90 30
Drill Log of Hole #RLP-11-02
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Pbppm
Znppm
Coppm
67.19 67.19 100
Gray to gray-green, fine-grained texture and massive structure, main mineral composition are amphibole, feldspar, biotite. General development of the chlorite ,epidotization and silification. Calcite veins are common , showed a single vein or stockwork distribution, vein width is about 0.1-4cm. Pyrrhotite is occasionally to find. Two group joint,25°and 40°to core axis. 13.72m,small amounts of pyrite. 19.81m,silicified quartz vein, also see a little bit pyrrhotite,the content is about <1%. 33.90-47.32m, the rock was gray white to gray, the content of light colored and dark colored minerals are almost same; in 34.87m and 40.15m see some pyrrhotite in the rock joint. 47.32-52.00m, gray-green rocks, porphyritic texture, 50.09m see pyrrhotite, the content is about 5%. 57.64m,4cm wide calcite vein
Nippm
Moppm
Auppb
Agg/t
ZK2meta-
andesite1.11 68.302
Crppm
ZK2 123.4471.79meta-
andesite04
Gray to gray-green, fine to medium grained texture and massive structure, main mineral composition are amphibole, feldspar, quartz and biotite. General development of the chlorite ,epidotization and silification. Calcite and quartz veins are common.Pyrrhotite is occasionally to find. 78.08-87.29m,gray white to gray,silification, medium to fine grained,pyrrhotite is occasionally to see. 91.72m,lumpy pyrrhotite. 96.36m,strong epidotization,chlorite and silification 112.78-113.18m,calcite veins filled between volcanic fragments. 111.35-111.45m,111.60-111.75m ,strong silification. 122.42-122.72m,strong silification,also see some calcite veins. 122.99-123.44m,calcite veins filled between volcanic fragments.
9951.0951.65
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
第 3 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 633025.454 East: Original Units: M North: North: 5438170.008 North: Storage: Markham Elevation: Elevation: 510.101 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFFF
Page 3 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK3
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 60 Length: 7.02 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4248129 Spotted by: ShawnLength: 150.88 meters Capped: Yes NTS: Coord Type: Started: 16-March-11 Cemented: No Surveyed Date: Completed: 19-March-11 Logged by: ShawnLogged: 20-March-11 Re-logged by: Wedged: Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments: ZK3 intersected minor to moderate Po veinlets from 7.02m to 10.67m that might explain the targeted EM conductor. Assays returned no significant gold or base metal content within the iron formation although the zinc content is somewhatanomalous.
Deviation TestsDistance(m)
16-Nov-12
Azimuth36.58 62.386.87 59.4
128.02 61.3
2B
From To From To
ZK3 01 Overburden 0 7.02 7.02 0 0 Overburden\casing.
RL.H-75 7.67 9.17 1.50 1.50 100 1350 <20 80 190 <10 160 130
RL.H-76 10.67 1.50 1.50 100 130 <20 120 160 <10 210 50
ZK3 03meta-
andesite10.67 21.61 10.94 10.94 100
Gray-green to gray-white, fine-grained texture and massive structure, main mineral composition are amphibole, feldspar and a little quartz and biotite. General development of the chlorite ,epidotization. Occasionally to see pyrrhotite,the content is <1%. 10.67-11.87m,gray white to gray, medium-fine grained,the content of light colored and dark colored minerals are almost same;11.25m,al little bit pyrrhotite. 16.96m,17.60m,some pyrrhotite are distributed in calcite veins.
ZK3 04 lamprophyre 21.61 24.95 3.34 3.34 100 Dark gray, porphyritic texture and massive structure, mineral composition are plagioclase, hornblende and biotite, phenocrysts were biotite.
meta-andesite
3.6510.677.02
Crppm
Coppm
Gray to gray-green, fine-grained texture and massive structure, main mineral composition are amphibole, feldspar, quartz and a little biotite. General development of the chlorite ,epidotization. Generally developed pyrrhotite, distributed as irregular veinlets and lumpy shape in rocks cracks,also see some calcite veins. 7.02-7.67m,meta-andesite,occasionally to see pyrrhotite. 8.02-8.42m,see more pyrrhotite, irregular veins,the content is about 20%. 8.42-10.67m,occasionally to see pyrrhotite in rock joints,the content is about 2%.
100
Nippm
Moppm
Auppb
Agg/t
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery factor(%)
Cuppm
Pbppm
Znppm
Drill Log of Hole #RLP-11-03
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
24.95 80.02 55.07 54.65
02ZK3Pyrrhotite
meta-andesite
ZK3 05
3.65
99
Gray to gray-green, medium-fine grained texture and massive structure, main mineral composition are amphibole, feldspar and a little quartz and biotite. General development of the chlorite ,epidotization,rock cracks are filled with calcite as veins,vein width is about 2-6mm,also see some quartz veins. Occasionally to see sulphide as scattered specks,the content is <1%. Two group joints,25°and 40°to core axis. 24.95-32.68m,fine grained,contain a little bit biotite. 32.68-55.89m,medium-fine grained,more biotite;35.45-35.47m and 47.64-47.65m ,white quartz veins. 55.89-80.02m,fine grained,a little bit biotite;66.71-68.18m,calcite veins
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-78 78.72 80.02 1.30 1.30 100 190 <20 100 100 <10 180 40
RL.H-79 81.22 1.20 1.20 100 460 <20 290 90 <10 150 50
RL.H-80 82.52 1.30 1.30 100 630 30 1360 110 <10 29 2.1 80 120
RL.H-81 83.82 1.30 1.30 100 620 30 630 80 <10 22 1.6 210 60
RL.H-82 85.16 1.34 1.33 99 710 40 1380 90 <10 100 70
RL.H-83 86.47 1.31 1.30 99 320 <20 210 90 <10 190 60
RL.H-84 87.68 1.21 1.20 99 170 <20 70 50 <10 60 40
RL.H-85 88.68 1.00 1.00 100 130 <20 110 70 <10 60 30
RL.H-86 89.59 0.91 0.91 100 290 <20 110 100 <10 21 0.8 110 30
RL.H-87 90.52 0.93 0.93 100 70 <20 110 430 <10 800 40
RL.H-89 91.83 1.31 1.30 99 670 30 1230 90 <10 80 90
RL.H-90 92.96 1.13 1.12 99 990 30 1610 120 <10 90 100
RL.H-91 94.01 1.05 1.02 97 560 30 1660 100 <10 64 0.8 70 60
RL.H-92 95.45 1.44 1.40 97 70 <20 170 20 <10 60 <10
RL.H-93 96.61 1.16 1.10 95 160 <20 200 20 <10 20 10
RL.H-94 97.87 1.26 1.20 95 220 <20 680 130 <10 30 30
RL.H-95 99.06 1.19 1.13 95 280 <20 1600 110 <10 60 40
RL.H-96 100.08 1.02 1.00 98 310 30 1550 140 <10 90 40
RL.H-97 101.10 1.02 1.00 98 470 <20 880 140 <10 12 <0.3 120 50
RL.H-98 102.11 1.01 1.00 99 260 <20 190 80 <10 60 30
RL.H-100 103.46 1.35 1.35 100 130 <20 140 90 <10 110 30
RL.H-101 104.86 1.40 1.40 100 620 <20 350 100 <10 100 40
RL.H-102 106.29 1.43 1.40 98 300 <20 770 120 <10 100 60
RL.H-103 107.80 1.51 1.48 98 150 <20 90 130 <10 140 60
RL.H-104 109.10 1.30 1.27 98 260 <20 60 80 <10 70 20
Dark gray to dark, fine-grained to aphanitic texture and banded structure, main mineral composition are amphibole, feldspar, quartz and a little biotite.Magnetic to weak magnetic,magnetic minerals are mainly magnetite and pyrrhotite. Generally developed pyrrhotite, pyrite and minor chalcopyrite. Sulphide are mainly distributed as banded veins and lumpy shape,the content is about 10-40%,the width of veins is about 1-5mm,some is up to 40mm,the bands are 45°to core axis. 81.96m,Po and Py,lumpy,banded vein. 83.71m,30mm Po vein. 88.66-89.42m,wide sulphide banded veins,densely distributed,the content is about 40%. 89.59-90.52m,contain some lamprophyre, occasionally sulfide 90.52-102.11m,Po and minor Clp,the content of sulphide is about 15%,;100.44m Po=10Py. 102.11-106.29m,the content of sulphide is anout 10%. 106.29-107.80m,gray andesite,vesicular and amygdaloidal structure,occasionally to see sulphide. 107.80-113.99m,the content of sulphide is anout 5%,banded veins.
9933.53
filled between volcanic fragments.
06ZK3 33.97113.99Iron
Formation80.02
第 4 页,共 19 页
From To From To
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery factor(%)
Cuppm
Pbppm
Znppm
Drill Log of Hole #RLP-11-03
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-105 110.40 1.30 1.30 100 180 <20 190 70 <10 60 30
RL.H-106 111.65 1.25 1.25 100 390 <20 910 120 <10 36 0.4 80 50
RL.H-107 112.75 1.10 1.10 100 210 <20 140 130 <10 120 60
RL.H-108 113.99 1.24 1.24 100 40 <20 60 90 <10 80 30
RL.H-109 115.19 1.20 1.20 100 40 <20 80 100 <10 120 30
RL.H-111 116.39 1.20 1.20 100 80 <20 100 130 <10 160 50ZK3 07
meta-andesite
113.99 150.88 36.89Gray to gray-green, medium to fine grained texture and massive structure, main mineral composition are amphibole, feldspar and few quartz and biotite. General development of the chlorite ,epidotization,calcite veins are common to see.
36.55 99
第 5 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 635010.358 East: Original Units: M North: North: 5440603.521 North: Storage: Markham Elevation: Elevation: 540.182 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFFF
Page 4 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK4
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 250 Length: 2.02 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -60 Pulled: No Claim No: 4252244 Spotted by: ShawnLength: 177.39 meters Capped: Yes NTS: Coord Type: Started: 23-May-11 Cemented: No Surveyed Date: Completed: 26-May-11 Logged by: ShawnLogged: 27-May-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected approximately 176 metres of mafic metavolcanic rocks at least portions of which are pillowed .
Deviation TestsDistance(m)
16-Nov-12
Azimuth38.10 243.483.82 247.6
129.54 250
3B
From To From To
ZK4 01 Overburden 0.00 2.02 0.00 2.02 0 Overburden\casing.
RL.H-439 54.04 55.41 1.07 1.05 98 240 <20 330 120 <10 210 50
RL.H-441 89.92 90.82 0.90 0.90 100 290 <20 110 110 <10 230 40
RL.H-442 91.66 0.84 0.84 100 280 <20 160 180 <10 530 60
RL.H-443 114.13 115.58 1.45 1.41 97 170 <20 270 100 <10 120 50
RL.H-444 117.00 1.42 1.38 97 370 <20 380 100 <10 170 50
RL.H-445 139.88 141.08 1.20 1.20 100 200 <20 110 60 <10 <5 <0.3 100 40
RL.H-446 142.33 1.05 1.05 100 250 <20 130 100 <10 70 50
RL.H-447 161.54 162.54 1.00 1.00 100 230 <20 150 60 <10 30 40
RL.H-448 163.42 0.88 0.88 100 190 <20 170 40 <10 60 30
RL.H-449 164.47 1.05 1.05 100 240 <20 160 60 <10 30 50
RL.H-450 165.62 1.15 1.15 100 140 20 30 30 <10 70 10
RL.H-452 166.62 1.00 1.00 100 150 <20 60 30 <10 70 20
RL.H-453 167.82 1.20 1.20 100 210 <20 60 100 <10 <5 <0.3 170 40
RL.H-454 168.72 0.90 0.90 100 160 <20 40 120 <10 <5 <0.3 270 30
RL.H-455 169.77 1.05 1.04 99 30 <20 10 10 <10 70 <10
RL.H-456 171.00 1.23 1.23 100 710 <20 120 250 <10 <5 <0 3 340 70
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Pbppm
Znppm
Drill Log of Hole #RLP-11-04
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
2.02meta-
andesite02
Gray to dark green, fine-grained texture and massive structure, main mineral composition are amphibole and quartz. Quartz and calcite veins are common to see as irregular distribution. Occasionally to see pyrrhotite,the content is <1%. Two group joints,20°and 40°to core axis. 42.45-42.65m,strong silicification,white color. 48.97m,20mm width calcite vein. 54.04-55.39m,weak magnetic,strong epidotization,develop pyrrhotite veins,40°to core axis,the content is about 5%. 59.44-60.14m,develop pyrrhotite,weak magnetic,the content is about 2%. 78.27-78.50m,white quartz veins,also some calcite veins. 86.00m,lumpy pyrrhotite. 89.92-91.66m,weak magnetic,develop pyrrhotite veins,the content is about 5%. 100.61-103.01m,mafic intrusive rock,medium grained,more biotite,a little bit sulphide. 114.13-117.00m,weak magnetic,strong epidotization,the content of pyrrhotite is about 5%. 130.64m,20mm width pyrrhotite vein. 139.88-142.13m,weak magnetic,strong silicification,the content of pyrrhotite is about 5%. 151.72-155.22m,white quartz vein,occasionally to see sulphide.
99160.52159.84
169.77 7.22 7.23 100
ZK4
ZK4
quzrtz vein and stong
silicification meta-andesite
162.5403
162.54
White,strong silicification,develop quartz veins,chlorite and epidotization,weak magnetic,the content of pyrrhotite is about 2%. 162.54-163.07m,quartz vein,epidotization,Po=2%. 163.07-164.47m,strong silicification meta-andesite,weak magnetic,Po=2%. 164.47-169.77m,quartz vein and silicification meta-andesite,Po=2%.
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H 456 171.00 1.23 1.23 100 710 <20 120 250 <10 <5 <0.3 340 70
RL.H-457 172.36 1.36 1.36 100 2580 110 470 300 <10 860 70
RL.H-458 176.21 177.39 N.A. N.A. N.A. N.A. N.A. <5 4.8 N.A. N.A.
ZK4 04meta-
andesite169.77 175.91 5.74 6.14 93
Gray to dark green, fine-grained texture and massive structure, main mineral composition are amphibole and quartz.169.77-172.36m,Po=5%, irregular veins.
light flesh red color,medium-fine grained,main mineral composition are quartz and felspar.176.21-177.39m,the core look like sand,only collect some of them as sample.
177.39 0.66 1.48 45ZK4 05 granite 175.91
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634089.253 East: Original Units: M North: North: 5440803.821 North: Storage: Markham Elevation: Elevation: 510.628 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFFF
Page 5 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK6
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 90 Length: 0.22 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -60 Pulled: No Claim No: 4252243 Spotted by: ShawnLength: 141.73 meters Capped: Yes NTS: Coord Type: Started: 18-May-11 Cemented: No Surveyed Date: Completed: 20-May-11 Logged by: ShawnLogged: 21-May-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected approximately 77 metres of chert-sulphide iron formation from 39.1 metres to 116.31 metres flanked by mafic volcanics.
Deviation TestsDistance(m)
16-Nov-12
Azimuth38.10 128.883.82 101.4
129.54 105.5
4B
From To From To
ZK6 01 Overburden 0.00 0.22 0.22 0.00 0 Overburden\casing.
ZK6 02meta-
andesite0.22 4.78 4.56 4.51 99
Grey green- grey,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization, sulfide is occasionally to find,the content is <1%.
ZK6 03K-feldspar granite
4.78 6.70 1.92 1.92 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.Occasionally to see pyrrhotite,the content is <1%.
RL.H-335 11.39 12.44 1.05 1.05 100 300 <20 160 140 <10 280 60
RL.H-336 13.54 1.10 1.10 100 130 <20 100 130 <10 300 40
RL.H-337 14.62 1.08 1.08 100 210 <20 210 140 <10 310 90
RL.H-338 15.85 1.23 1.23 100 60 30 20 <10 <10 60 <10
RL.H-339 16.60 0.75 0.75 100 210 <20 140 100 <10 240 30
RL.H-340 18.06 1.46 1.46 10030 30 20 <10 <10 30 <10
RL.H-342 19.36 1.30 1.30 100 100 <20 130 110 20 360 40
RL.H-343 20.51 1.15 1.15 100 140 <20 120 150 <10 340 50
RL.H-344 21.66 1.15 1.15 100 280 720 200 160 <10 1060 20
RL.H-345 22.16 0.50 0.50 100 1100 <20 60 220 20 30 <10
RL.H-346 23.61 1.45 1.44 99 110 <20 140 70 <10 440 20
RL.H-347 24.54 0.93 0.92 99 730 <20 90 140 <10 80 70
RL.H-348 25.22 0.68 0.67 99 870 <20 50 270 <10 70 40
RL.H-349 26.26 0.94 0.93 99 790 <20 160 170 <10 720 20
RL.H-350 27.23 1.07 1.07 100 60 <20 50 50 <10 90 <10
RL.H-351 28.60 1.37 1.37 100 1160 <20 110 250 <10 25 2.8 40 50
RL.H-353 29.80 1.20 1.20 100 300 20 70 30 30 50 <10
RL.H-354 31.00 1.20 1.20 100 210 <20 90 40 20 40 1042.8618.06
meta-andesite
with06ZK6
100
Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar. 15.85-16.60m is neta andesite ,occasionally to see pyrrhotite,the content is <1%.
Grey-green to grey-white,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization.One group joint,70°to core axis,the core length is <0.6m。 The rock developed much pyrrhotite and pyrite,distributed as spot-like,irregular veinlets,heavily disseminated and massive,sulphide occur as subhedral to xenomorphic granular aggregates,the content is about 80%. 18.06-21.66m,Po and minor Py,occur as spot-like and irregular veinlets the content is about 2%. 21.66-22.16m,massive sulphide,Po and Py,the content of sulphide is >95%,and Py=5%. 22.16-23.61m,Po,occur as spot-like,PO=2%,silicification. 23.61-23.95m,massive sulphide,Po and Py,the content of sulphide is >95%,and Py=20%.
23 95-24 54m Po and a little bit Clp occur as spot-like and irregular10024.7224.80
0.92 100 Dark green,fine-grained,massive structure,Quartz and calcite veins are common to see as irregular distribution..Occasionally to see pyrrhotite.11.39-12.00m more Po and Py,the content is about 2%.
ZK6 05K-feldspar granite
14.62 18.06 3.44 3.44
ZK6 04meta-
andesite6.70 14.62 7.92
Drill Log of Hole #RLP-11-06
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H 354 31.00 1.20 1.20 100 210 <20 90 40 20 40 10
RL.H-355 32.00 1.00 1.00 100 390 <20 190 50 <10 12 0.9 40 30
RL.H-356 33.22 1.22 1.20 98 460 <20 260 80 <10 23 0.9 60 10
RL.H-357 34.49 1.27 1.25 98 160 <20 150 120 <10 720 50
RL.H-358 35.75 1.26 1.25 99 270 <20 290 260 <10 1120 40
RL.H-359 37.10 1.35 1.35 100 410 <20 480 80 <10 10 0.5 80 80
RL.H-360 38.10 1.00 1.00 100 140 <20 170 120 <10 860 40
RL.H-361 39.10 1.00 1.00 100 150 <20 180 130 <10 790 40
RL.H-362 40.00 0.90 0.90 100 260 <20 210 170 <10 90 110
RL.H-364 40.90 0.90 0.90 100 350 <20 260 170 <10 30 60
RL.H-365 41.79 0.89 0.89 100 390 <20 320 110 <10 7 0.6 60 20
RL.H-366 42.86 1.07 1.07 100 100 <20 150 40 20 60 <10
RL.H-367 44.36 1.50 1.50 100 50 20 30 <10 <10 40 <10
RL.H-368 45.86 1.50 1.50 100 60 30 20 <10 <10 30 <10
RL.H-369 46.92 1.06 1.06 100 170 <20 110 70 <10 60 <10
RL.H-370 47.80 0.88 0.88 100 320 <20 210 110 <10 30 360
RL.H-371 48.90 1.10 1.10 100 290 <20 90 120 <10 40 40
RL.H-372 50.10 1.20 1.20 100 390 <20 230 220 <10 9 0.8 20 40
RL.H-373 51.33 1.23 1.20 98 310 <20 100 200 <10 11 0.8 140 70
RL.H-375 52.59 1.26 1.22 97 150 <20 180 140 <10 90 <10
RL.H-376 53.82 1.23 1.20 98 330 20 60 140 <10 50 20
RL.H-377 55.08 1.26 1.25 99 370 <20 150 210 <10 30 10
RL.H-378 56.39 1.31 1.29 99 350 <20 590 180 <10 26 1.2 30 30
Dark-brassy to dark-bronze,sulphide are Py and Po, occur as subhedral to xenomorphic granular aggregates, and devloped as massive and dense disseminated,the content of sulfide is >80%, the content of pyrrhotite is slightly higher than pyrite. 45.86-46.92m,meta-andesite with Py and Po,silicification,sulphide is about 10%. 46.92-47.80m,masiive sulphide,>95%,the content of pyrrhotite is almost same to pyrite. 47.80-48.34m,meta-andesite with Py and Po,sulphide is about 10%. 48.34-51.33m,masiive sulphide,>95%, the content of pyrrhotite is slightly
3.00 3.00 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.
massive to h il
42.8618.06with pyrrhotite and pyrite
06ZK6
ZK6 07K-feldspar granite
42.86 45.86
23.95 24.54m,Po and a little bit Clp, occur as spot like and irregular veinlets,the content of sulphide is about 10%. 24.54-25.22m,massive sulphide,Po and Py,the content of sulphide is >95%,and Py=10%. 25.22-26.16m,heavily disseminated sulphide,Po and minor Py,the content of sulphide is about 60%. 26.16-27.23m,medium-grained intermediate intrusive,grey to grey-white,mineral composition are amphibole,feldspar and quartz,development of the Po and Py as fine granular aggregates,about 3%. 27.23-28.60m,massive to heavily disseminated sulphide,Po and Py,the content of sulphide is about 80%,and Py=20%. 28.60-37.10m,the content of sulphide is about 30%,irregular veinlets,Py=Po. 37.10-39.10m,pot-like sulphide,about 2%. 39.10-41.79m,dense veinlets,the content of sulfhide is about 60%,Py=25.
41 79-42 86m pot-like and lumpy Po about 5% silicification
10024.7224.80
第 7 页,共 19 页
From To From To
Drill Log of Hole #RLP-11-06
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-379 57.64 1.25 1.25 100 320 <20 160 140 <10 20 60
RL.H-380 58.94 1.30 1.30 100 470 <20 200 170 <10 20 40
RL.H-381 60.18 1.24 1.24 100 480 <20 110 130 <10 20 110
RL.H-382 61.38 1.20 1.20 100 640 30 130 110 <10 14 1 20 160
RL.H-383 62.48 1.10 1.10 100 260 <20 250 100 <10 10 110
RL.H-384 63.63 1.15 1.15 100 250 <20 130 120 <10 15 0.6 20 160
RL.H-386 64.83 1.20 1.20 100 220 <20 250 140 <10 20 110
RL.H-387 66.13 1.30 1.30 100 260 <20 1060 140 <10 20 80
RL.H-388 67.13 1.00 1.00 100 270 <20 240 150 <10 21 0.8 20 120
RL.H-389 68.28 1.15 1.15 100 270 <20 170 130 <10 20 90
RL.H-390 69.48 1.20 1.20 100 170 <20 220 80 <10 50 10
RL.H-391 70.68 1.20 1.20 100 130 <20 110 60 <10 8 <0.3 60 <10
RL.H-392 71.98 1.30 1.30 100 180 <20 110 100 <10 11 0.4 50 30
RL.H-393 72.98 1.00 1.00 100 160 30 70 80 <10 25 0.5 30 160
RL.H-394 73.98 1.00 1.00 100 340 <20 120 160 <10 40 130
RL.H-395 75.28 1.30 1.30 100 130 <20 330 90 <10 140 10
RL.H-397 76.48 1.20 1.20 100 120 <20 230 80 <10 590 10
RL.H-398 77.72 1.24 1.24 100 110 <20 380 60 <10 5 0.3 70 10
RL.H-399 79.02 1.30 1.30 100 70 <20 430 50 <10 80 10
RL.H-400 79.82 0.80 0.80 100 150 <20 250 130 <10 80 <10
RL.H-401 80.72 0.95 0.95 100 210 <20 360 190 <10 50 10
RL.H-402 81.69 0.92 0.90 98 150 <20 80 110 <10 9 0.4 40 130
RL.H-403 82.46 0.77 0.75 98 80 <20 140 70 <10 30 110
ZK6 10K-feldspar granite
82.46 83.20 0.74 0.73 98 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.
RL.H-404 83.20 0.74 0.73 98
50 <20 20 20 <10 30 <10
RL.H-405 84.45 1.25 1.25 100 120 30 150 50 <10 12 <0.3 30 70
RL.H-406 85.69 1.24 1.24 100 80 <20 50 60 <10 30 100
100
Grey-green to grey-white,fine-grained texture and massive structure,Po and Py,the sulphide is about 60%,occur as irregular veinlets,heavily disseminated and massive. 68.28-71.98m,Po,about 10%,irregular veinlets. 71.98-73.98m,Po and Py,dense disseminated,about 80%,the content of pyrrhotite is slightly higher than pyrite 73.98-79.25m,Po and minor Py,spot like and veinlets,about 10%。 79.25-80.77m,dense disseminated to masiive sulphide,Po and minor Py,about 70%。 80.77-82.46m,dense disseminated to masiive sulphide,Py and minor Po,about 70%。
22.29 99 higher than pyrite. 51.33-51.70m,meta-andesite with Py and Po,sulphide is about 20%. 51.70-52.02m,masiive sulphide,>95%, the content of pyrrhotite is slightly higher than pyrite. 52.02-52.59m,meta-andesite with Py and Po,silicification,sulphide is about 2%. 52.59-68.28m,massive to dense disseminated,sulphide,>90%, the content of pyrrhotite is slightly higher than pyrite.
ZK6 09
meta-andesite
with pyrrhotite and pyrite
68.28 82.46 14.18 14.15
ZK6heavily
disseminated sulfide
08 45.86 68.28 22.42
RL.H-408 86.74 1.05 1.05 100 40 <20 40 30 <10 <5 1.4 70 <10
RL.H-409 87.89 1.15 1.15 100 20 <20 20 40 <10 100 <10
RL.H-410 88.89 1.00 1.00 100 70 <20 60 40 <10 20 120
RL.H-411 89.92 1.03 1.03 100 160 <20 60 60 <10 10 100
RL.H-412 91.06 1.14 1.14 100 80 <20 60 30 <10 40 70
RL.H-413 91.77 0.71 0.71 100 160 <20 100 140 <10 20 70
RL.H-414 92.48 0.71 0.71 100 140 <20 60 40 <10 80 <10
RL.H-415 93.80 1.32 1.32 100 120 <20 90 70 <10 <10 100
RL.H-416 95.00 1.20 1.20 100 150 <20 80 60 <10 <5 0.5 20 100
RL.H-417 96.01 1.01 1.01 100 150 <20 50 80 <10 20 70
RL.H-419 97.26 1.25 1.25 100 90 <20 80 60 <10 50 30
RL.H-420 98.10 1.15 1.15 100 140 <20 40 90 <10 40 10
RL.H-421 99.64 1.23 1.23 100 230 <20 90 90 <10 12 1 30 60
RL.H-422 100.89 1.25 1.25 100 90 <20 50 60 <10 40 10
RL.H-423 102.11 1.22 1.22 100 590 <20 50 70 <10 40 50
RL.H-424 103.21 1.10 1.10 100 340 <20 120 80 <10 20 60
RL.H-425 104.41 1.20 1.20 100 50 <20 50 30 <10 50 20
RL.H-426 105.16 0.75 0.75 100 70 <20 60 50 <10 10 100
RL.H-427 106.28 1.12 1.12 100 180 <20 90 110 <10 <5 0.9 20 50
ZK6 12K-feldspar granite
106.28 108.00 1.72 1.72 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.
RL.H-428 108.00 1.72 1.72 100
50 <20 20 <10 20 10 <10
RL.H-430 109.22 1.22 1.22 100 140 <20 90 60 <10 50 80
Py and Po,the content of sulfide is about 70%,the content of Py is slightly higher than Po. 83.20-85.69m,massive sulfide,Py and minor Po,>95. 85.69-87.89m,meta-andesite with Py and Po,silicification,sulphide is about 5%. 87.89-89.92m,massive sulfide,Py and minor Po,>90. 89.92-91.06m,meta-andesite with Py and Po,sulphide is about 10%. 91.06-91.77m,massive sulfide,Py and minor Po,>90. 91.77-92.48m,sulphide is about 10%. 92.48-99.64m,dense disseminated to masiive sulphide,>80%,Py and Po,Po=30%. 99.64-101.48m,sulphide is about 40%,Po=Py. 101.48-102.21m,dense disseminated to masiive sulphide, about 60%, 102.21-102.73m,sulphide is about 25%. 102.73-103.46m,dense disseminated to masiive sulphide,>80%. 103.46-104.41m,sulphide is about 5%. 104.41-106.28m,ense disseminated to masiive sulphide,>90%,Py = Po
Sulphid ur m ii t d n di min t d P nd P th nt nt f P i
ZK6
heavily disseminated to massive
sulfide
11 83.20 106.28 23.08 23.06 100
第 8 页,共 19 页
From To From To
Drill Log of Hole #RLP-11-06
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-431 110.42 1.20 1.20 100 170 <20 60 40 <10 40 70
RL.H-432 111.83 1.41 1.41 100 110 <20 50 50 <10 40 70
RL.H-433 112.96 1.13 1.13 100 40 <20 20 20 <10 70 20
RL.H-434 114.03 1.07 1.07 100 90 <20 70 50 <10 20 80
RL.H-435 115.15 1.12 1.11 99 120 <20 80 50 <10 9 0.7 20 70
RL.H-436 116.31 1.16 1.14 98 160 <20 80 70 <10 10 80
RL.H-437 117.35 1.04 1.02 98 30 100 100 10 10 40 <10
RL.H-438 118.35 1.00 1.00 100 40 40 40 <10 <10 20 <10100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz and K-felspar.Sulfide is occasionally to find,One group joint,40°to core axis.
116.31 141.73 25.42 25.35
108.00
massive to heavily
disseminated sulfide
13ZK6
ZK6 14K-feldspar granite
Sulphide occur asmasiive to dense disseminated,Po and Py,the content of Py is slightly higher than Po. The content of sulphide is >80%; 108.00-111.83m,massive sulfide,>90. 111.83-112.96m,meta-andesite with Py and Po,irregular veinlets,sulphide is about 10%. 112.96-116.31m,dense disseminated to masiive sulphide, the content of sulfide is >90%;
998.278.31116.31
第 9 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634713.398 East: Original Units: M North: North: 5441172.069 North: Storage: Markham Elevation: Elevation: 507.698 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
Type
Page 6 of 12
Drilling Casing Location
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK7
Diamond Drill Hole Report Project Number:
OtherAzimuth: 55 Length: 1.30 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -50 Pulled: No Claim No: 4252244 Spotted by: ShawnLength: 124.05 meters Capped: Yes NTS: Coord Type: Started: 4-April-11 Cemented: No Surveyed Date: Completed: 6-April-11 Logged by: ShawnLogged: 7-April-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments: The drill hole also intersected another much narrower (1 metre) interval of metasediment with pyrrhotite bands and lamination from 32.40 to 33.65 metres. Pyrrhotite stringers were also locally intersected in the mafic metavolcanics in theupper portion of the drill hole.
AzimuthDeviation Tests
Distance(m)
16-Nov-12
The date was lost by drilling company.
5B
From To From To
ZK7 01 Overburden 0.00 1.30 1.30 0.00 0 Overburden\casing.
RL.H-280 1.30 2.40 1.10 1.10 100 120 <20 210 120 <10 310 50
RL.H-281 3.60 1.20 1.20 100 240 <20 130 210 <10 5 <0.3 420 60
RL.H-282 4.90 1.30 1.30 100 130 <20 270 200 <10 360 50
RL.H-283 6.12 1.22 1.20 98 110 <20 490 120 <10 320 50
RL.H-284 7.22 1.10 1.08 98 250 <20 320 160 <10 <5 0.3 330 80
RL.H-285 8.23 1.01 1.00 98 210 <20 170 170 <10 350 80
RL.H-287 9.40 1.17 1.17 100 440 <20 140 170 <10 280 90
RL.H-288 10.50 1.10 1.10 100 120 <20 90 80 <10 210 40
RL.H-289 28.77 29.87 1.10 1.10 100 110 <20 150 80 <10 150 50
RL.H-290 30.81 0.94 0.94 100160 <20 150 80 <10 6 <0.3 100 50
RL.H-291 31.81 1.00 1.00 100<10 <20 40 <10 <10 30 <10
RL.H-292 32.81 1.00 1.00 100310 <20 1460 80 <10 130 30
RL.H-293 33.81 1.00 1.00 100
250 <20 370 130 <10 10 0.5 60 60
RL.H-294 34.91 1.10 1.10 100 70 <20 130 70 <10 130 40
RL.H-295 36.11 1.20 1.20 100 110 <20 140 60 <10 140 50
RL.H-296 43.51 44.81 1.30 1.30 100 130 <20 120 80 <10 140 50
RL.H-298 46.01 1.20 1.20 100 100 <20 140 60 <10 100 40
RL.H-299 46.91 0.90 0.90 100 60 <20 110 30 <10 40 30
RL.H-300 47.91 1.00 1.00 100 50 <20 130 20 <10 40 30
RL.H-301 49.01 1.10 1.10 100 110 <20 220 60 <10 5 <0.3 80 30
Drill Log of Hole #RLP-11-07
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery
factor(%)
Description
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Nippm
Moppm
Pbppm
Znppm
Auppb
Agg/t
Crppm
Coppm
29.87 20.47 20.44 100
Grey to grey-white,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. Calcite and quartz veins are common to see.The content of sulphide is <1%.
Grey to grey green,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification.Po and Py occur as spot-like and irregular veinlets,subhedral to xenomorphic granular,the content is about 2-6%. Two group joint,20°and 40°to core axis.
998.038.109.401.30
meta-andesite
with pyrrhotite and pyrite
meta-andesite
9.40
02ZK7
ZK7 04
ZK7 03
ZK7 05meta-
andesite 33.81 44.81 11.00
3.94 10033.81
Grey to dark-green,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization. The rock developed pyrrhotite and pyrite,locally developed minor chalcopyrite.Sulphide occur as banded veinlets and irregular veinlets,the length of the vein is aboout 1-10mm。The content of sulphide is about 10%,Po=Py,and the content of Clp is<1%。The banded vein is 50°to core axis. 30.53m occur a little bit chalcopyrite.
meta-andesite
with pyrite and
pyrrhotite
29.87 3.94
11.00 100 Grey to grey-green,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar,quartz,dark minerals are directional arrangement,50°to core axis.
Grey to grey-green fine-grained texture and massive structure main mineral
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-302 49.91 0.90 0.90 100 110 <20 410 130 <10 6 <0.3 80 40
RL.H-303 50.90 0.99 0.99 100 220 <20 320 100 <10 <5 <0.3 110 30
RL.H-304 52.00 1.10 1.10 100 130 <20 120 120 <10 240 40
RL.H-305 53.10 1.10 1.10 100 70 <20 110 50 <10 50 30
RL.H-306 54.20 1.10 1.10 100 210 <20 1130 120 <10 6 1.4 110 60
RL.H-307 55.40 1.20 1.20 100 130 30 350 110 <10 70 40
RL.H-309 56.40 1.00 1.00 100 250 20 220 60 <10 50 50
RL.H-310 57.27 0.87 0.87 100 80 <20 180 30 <10 40 40
RL.H-311 58.27 1.00 1.00 100 40 <20 150 20 <10 40 40
RL.H-312 74.59 75.59 1.00 1.00 100 110 <20 170 80 <10 160 30
RL.H-313 76.79 1.20 1.20 100 160 <20 250 100 <10 150 40
RL.H-314 77.79 1.00 1.00 100 110 <20 310 110 <10 5 <0.3 200 30
RL.H-315 78.74 0.95 0.95 100 100 <20 230 140 <10 310 40
12.46
66.78
ZK7
meta-andesite
with pyrite and
pyrrhotite
06 44.81 57.27 12.46
100
100
Grey to grey green,fine grained texture and massive structure,main mineral composition are amphibole,feldspar,quartz and biotite.Development of the chlorite,epidotization and silicification.Sulphide occur as banded veinlets and irregular veinlets,is about 20%,P0=Py.The banded vein is 60°to core axis. 44.81-50.90m,Py and Po,Py=4Po;49.85m a little bit Clp. 50.90-57.27m,Po and Py,Po=3Py.
Grey to grey-green,fine-grained texture and massive structure,main mineral composition are amphibole,feldspar,quartz and biotite.Development of the chlorite,epidotizatiohe and silicification.Calcite and quartz veins are common to see.The content of sulphide is <1%。 75.77m,pyrite vein,about 2mm length; 76.11m,pyrite vein,about 5mm length; 76.87m,pyrite vein,about 5mm length; 81.74m,quartz vein,about 6mm length; 95.50m,quartz vein,about 5mm length;
ZK7 07meta-
andesite 57.27 124.05 66.78
第 10 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634409.031 East: Original Units: M North: North: 5441157.381 North: Storage: Markham Elevation: Elevation: 511.544 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
Azimuth Dip Type61.3 53 F64.3 52.5 F64.9 51.7 F64.8 51.4 F
Page 7 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK8
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 65 Length: 2.59 meters Township: Richardson Lake Area Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4252243 Spotted by: ShawnLength: 150.88 meters Capped: Yes NTS: Coord Type: Started: 15-May-11 Cemented: No Surveyed Date: Completed: 17-May-11 Logged by: ShawnLogged: 18-May-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected approximately 3.5 metres of metasediment with magnetite bands from 36.8 metres to 40.35 metres flanked by mafic volcanics cut by intermittent granite dykes.
141.73
Deviation TestsDistance(m)
16-Nov-12
38.1083.82
129.54
6B
From To From To
ZK8 01 Overburden 0.00 2.59 2.59 0.00 0 Overburden\casing.
ZK8 02meta-
andesite2.59 15.46 12.87 12.82 100
Dark grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization.Quartz veins are common and occur as irregular veinlets.One group joint, 40°to core axis.The core length are between 0.4 to 1.0m.
ZK8 03K-feldspar granite
15.46 17.61 2.15 2.15 100 Grey and light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.One group joint, 40°to core axis.
RL.H-326 41.15 42.30 1.15 1.15 100 110 <20 190 120 <10 190 50
RL.H-327 43.55 1.25 1.25 100 100 <20 140 120 <10 200 60
ZK8 05K-feldspar granite
50.29 52.64 2.35 2.35 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.
RL.H-328 58.69 60.00 1.31 1.30 99 190 <20 100 150 <10 230 60
RL.H-329 60.65 0.65 0.64 99 1170 <20 190 110 <10 160 70
RL.H-331 61.91 1.26 1.25 99 160 <20 100 130 <10 220 60
ZK8 07K-feldspar granite
91.21 98.64 7.43 7.38 99 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.The rock are broken.
RL.H-332 114.30 115.58 1.28 1.25 98 170 400 160 60 <10 80 50meta-
38.5791.21ZK8 06meta-
andesite
Grey green to grey,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization . Quartz and calcite veins are common and occur as irregular veinlets. Two group joint,20°and 50°to core axis.The core length are between 0.2 to 1.2m. Pyrrhotite is occasional to find,the content is <1%.62.00-62.65m,alittle bit Clp and Po cccur together.
9932.2852.64
Dark grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization .
ZK8 04meta-
andesite17.61
Pbppm
Description
Dark grey to grey,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization . Quartz and calcite veins are common and occur as irregular veinlets.One group joint, 40°to core axis.The core length are between 0.2 to 1.2m. 31.82-31.90m,white quartz vein; 36.25-50.29m,strong epidotization,occur as small banded veins. Pyrrhotite is occasional to find,the content is <1%.
Recovery
factor(%)
50.29 32.68 32.24 99
Auppb
Nippm
Moppm
Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Znppm
Crppm
Coppm
Drill Log of Hole #RLP-11-08
Hole No.
No.Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Agg/t
Sample log
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-333 116.65 1.07 1.05 98 160 <20 150 60 <10 60 50
RL.H-334 117.85 1.20 1.18 98 240 <20 180 60 <10 70 50
ZK8 09K-feldspar granite
143.56 147.31 3.75 3.75 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.The core length are between 0.4 to 1.0m.
ZK8 10meta-
andesite147.31 150.88 3.57 3.57 100
Grey to grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar and quartz,development of the chlorite and epidotization .
metaandesite
08ZK8 143.5698.64 Quartz and calcite veins are common.The content of Po is <1%. 114.30-117.85m,Po>1%. 132.58-136.24m,Granite and meta-andesite.
10044.7544.92
第 11 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 634321.713 East: Original Units: M North: North: 5443331.717 North: Storage: Markham Elevation: Elevation: 502.892 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
Type
Page 8 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK9
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 270 Length: 1.51 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -65 Pulled: No Claim No: 4252236 Spotted by: ShawnLength: 133.20 meters Capped: Yes NTS: Coord Type: Started: 30-March-11 Cemented: No Surveyed Date: Completed: 1-April-11 Logged by: ShawnLogged: 2-April-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments: The 16.7 metres of granite intersected at the end of ZK9 may represent the main body of the Norway Lake pluton; the 10.5 metres of mafic metavolcanic immediately uphole of this granite exhibits deformation and biotite-chlorite alterationindicative of a contact metamorphic aureole.
Deviation TestsDistance(m) Azimuth
16-Nov-12
The date was lost by drilling company.
7B
From To From To
ZK9 01 Overburden 0.00 1.51 1.51 0.00 0 Overburden\casing.
RL.H-227 12.38 13.43 1.05 1.05 100 90 130 760 100 <10 8 220 40
RL.H-228 14.63 1.20 1.20 100 120 110 1150 70 <10 12 90 20
RL.H-229 15.83 1.20 1.20 100 190 <20 550 80 <10 18 0.6 100 30
RL.H-230 17.13 1.30 1.30 100 120 <20 2640 110 <10 36 130 40
RL.H-232 18.37 1.24 1.24 100 150 <20 600 120 <10 11 1.4 170 40
RL.H-233 19.37 1.00 1.00 100 210 20 70 150 <10 16 2.1 110 60
RL.H-234 20.42 1.05 1.05 100 60 <20 100 50 <10 7 50 10
RL.H-235 21.62 1.20 1.20 100 40 <20 140 30 <10 6 70 10
RL.H-236 22.82 1.20 1.20 100 80 <20 390 40 <10 13 60 10
RL.H-237 23.87 1.05 1.05 100 140 <20 360 100 <10 15 1.8 30 30
RL.H-238 25.12 1.25 1.25 100 110 <20 110 80 <10 10 60 30
RL.H-239 26.27 1.15 1.15 100 220 20 570 170 <10 21 70 70
RL.H-240 27.37 1.10 1.10 100 260 <20 1330 170 <10 26 2.2 70 70
RL.H-241 28.57 1.20 1.20 100 360 40 730 200 <10 26 100 80
RL.H-243 29.57 1.00 1.00 100 210 <20 390 210 <10 27 60 90
RL.H-244 30.77 1.20 1.20 100 250 <20 750 220 <10 30 3.3 50 100
RL.H-245 31.97 1.20 1.20 100 220 <20 320 110 <10 18 70 40
RL.H-246 33.17 1.20 1.20 100 170 <20 270 170 <10 23 80 70
RL.H-247 34.27 1.10 1.10 100 180 <20 450 130 <10 19 1.6 70 50
RL.H-248 35.51 1.24 1.24 100 100 <20 180 100 <10 <5 250 40
RL.H-249 36.91 1.40 1.40 100 120 <20 310 100 <10 12 120 50
RL.H-250 38.16 1.25 1.25 100 110 <20 260 80 <10 9 0.8 70 40
RL H-251 39 46 1 30 1 30 100 120 <20 140 50 <10 <5 130 40
Depth(m) Thickness
(m)
Length of core (m)
Agg/t
Sample log
Recovery
factor(%)
Cuppm
Znppm
Crppm
Coppm
Drill Log of Hole #RLP-11-09
Hole No.
No.Rock/Ore
type
Recovery
factor(%)
13.43 11.92 11.92 100
Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Auppb
ZK9 02meta-
andesite1.51
Pbppm
Description
Grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite, epidotization and silicification.Pyrrhotite is occasional to find,the content is <1%,occur as xenomorphic granular. One group joint, 60°to core axis.The core length are <0.4m.
Nippm
Moppm
10024.7338.16ZK9meta-
andesite with Po
03 13.43
Grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite, epidotization and silicification. Generally developed pyrrhotite, locally developed minor pyrite and chalcopyrite.Pyrrhotite occur as subhedral to xenomorphic granular,distributed as irregular veinlets,also spot-like, lumpy and disseminated,the content is 5-20%. One group joint, 60°to core axis.The core length are <0.5m. 13.43-25.12m,Po occur asirregular veinlets,lumpy and spot-like,the content is about 5%.18.50m,a little bit Clp. 25.12-38.16m,distributed Po,the content is about 20%. 31.46m,32.94m and 33.76m,a little bit Clp.
24.73
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-251 39.46 1.30 1.30 100 120 <20 140 50 <10 <5 130 40
RL.H-252 40.66 1.20 1.20 100 140 60 500 80 <10 <5 130 50
RL.H-254 41.76 1.10 1.10 100 110 <20 130 60 <10 <5 130 40
RL.H-255 42.96 1.20 1.20 100 140 <20 100 70 <10 <5 110 40
RL.H-256 44.16 1.20 1.20 100 140 <20 110 70 <10 <5 120 50
RL.H-257 45.51 1.35 1.35 100 110 <20 120 70 <10 <5 120 50
RL.H-258 46.71 1.20 1.20 100 110 <20 120 70 <10 <5 130 40
RL.H-259 47.85 1.14 1.14 100 120 <20 150 60 <10 <5 <0.3 140 50
RL.H-260 49.05 1.20 1.20 100 120 <20 110 60 <10 <5 140 40
RL.H-261 50.15 1.10 1.10 100 90 <20 120 130 <10 <5 270 50
RL.H-262 51.09 0.94 0.94 100 70 <20 110 120 <10 <5 240 40
RL.H-263 52.09 1.00 1.00 100 120 <20 90 60 <10 <5 130 40
RL.H-265 53.29 1.20 1.20 100 170 20 170 50 <10 7 100 30
RL.H-266 54.35 1.06 1.06 100 140 <20 250 70 <10 <5 80 30
RL.H-267 55.70 1.35 1.35 100 200 <20 180 130 <10 5 0.8 90 50
RL.H-268 57.00 1.30 1.30 100 260 <20 180 120 <10 5 1 30 50
RL.H-269 58.00 1.00 1.00 100 270 <20 300 110 <10 8 120 40
RL.H-270 59.17 1.17 1.17 100 80 <20 110 140 <10 <5 320 40
ZK9 06K-feldspar granite
59.17 61.35 2.18 2.18 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.
38.16
meta-andesite
with minor Po
meta-andesite with Po
52.09 59.17
Grey green to grey, fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite, epidotization.Calcite veins are common,the length of vein is between 2 to 10mm. Pyrrhotite is occasional to find,the content is <1%.
10013.9304
Grey white to grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. Generally developed pyrrhotite, locally developed minor chalcopyrite.Pyrrhotite occur as irregular veinlets and lumpy,the content is 5-10%. 56.20m,56.44m,56.90m and 56.96m,a little bit Clp. 58.00-59.17m,Po<1%。
7.087.08 100
ZK9
ZK9 05
13.9352.09
第 12 页,共 19 页
From To From To
Depth(m) Thickness
(m)
Length of core (m)
Agg/t
Sample log
Recovery
factor(%)
Cuppm
Znppm
Crppm
Coppm
Drill Log of Hole #RLP-11-09
Hole No.
No.Rock/Ore
type
Recovery
factor(%)
Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Auppb
Pbppm
DescriptionNippm
Moppm
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
ZK9 07meta-
andesite 61.35 116.20 54.85 54.70 100
Grey to dark grey green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and calcite veins. Two group joint,30°and 60°to core axis.The core length are between 0.3 to 1.0m. 78.83m and 83.73m,white quartz veins,the length is 17mm and 12mm.
ZK9 08K-feldspar granite
116.20 133.20 17.00 17.00 100 Light flesh red color,medium-fine grained,massive structure,main mineral composition are quartz ,felspar and biotite.
第 13 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 636738.912 East: Original Units: M North: North: 5445230.614 North: Storage: Markham Elevation: Elevation: 514.427 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFFF
Page 9 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK10
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 110 Length: 3.70 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4252235 Spotted by: ShawnLength: 123.44 meters Capped: Yes NTS: Coord Type: Started: 23-March-11 Cemented: No Surveyed Date: Completed: 25-March-11 Logged by: ShawnLogged: 26-March-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments: The 13.74 metres of quartz monzonite/granite intersected at the end of ZK10 may represent the main body of the Chill Lake Lake pluton.
Deviation TestsDistance(m)
16-Nov-12
Azimuth36.58 98.985.34 109.6
114.30 108.1
8B
From To From To
ZK10 01 Overburden 0.00 3.70 3.70 0.00 0 Overburden\casing.
RL.H-112 10.67 11.77 1.10 1.10 100 40 <20 100 90 <10 160 40RL.H-113 13.02 1.25 1.25 100 70 <20 150 110 <10 310 50RL.H-114 14.46 1.44 1.40 97 90 <20 140 110 <10 300 50RL.H-115 15.85 1.39 1.30 94 160 <20 170 110 <10 310 50RL.H-116 17.07 1.22 1.15 94 60 <20 170 110 10 300 40RL.H-117 18.29 1.22 1.20 98 80 <20 100 110 20 <5 <0.3 280 50RL.H-118 19.66 1.37 1.35 98 60 <20 110 110 10 310 50RL.H-119 20.66 1.00 1.00 100 50 <20 180 110 30 280 40
ZK10 04 massive sulfide 20.66 20.99 0.33 0.33 100 Brass-yellow hue,massive sulphide,Py=90%,Po=2%,a little bit Clp. RL.H-120 20.99 0.33 0.33 100
840 <20 50 100 70 130 100RL.H-122 22.06 1.07 1.07 100 230 <20 150 70 140 <5 <0.3 170 20RL.H-123 23.31 1.25 1.25 100 150 <20 120 90 <10 <5 <0.3 210 40RL.H-124 24.66 1.35 1.35 100 80 <20 180 120 20 330 50RL.H-125 26.00 1.34 1.34 100 90 <20 150 110 <10 280 40RL.H-126 26.94 0.94 0.94 100 <10 <20 30 10 <10 10 <10RL.H-127 27.94 1.00 1.00 100 <10 <20 30 <10 <10 100 <10RL.H-128 28.96 1.02 1.02 100 40 <20 160 90 <10 260 40RL.H-129 30.20 1.24 1.24 100 100 <20 120 100 30 270 40RL.H-130 31.50 1.30 1.30 100 90 <20 180 80 <10 250 30
RL.H-131 32.60 1.10 1.10 100 2200 <20 290 140 80 34 1.4 60 120
RL.H-133 33.52 0.92 0.92 100 5540 40 300 120 110 20 4.6 60 100RL H 134 35 05 1 53 1 53 100
Drill Log of Hole #RLP-11-10
Hole No. No. Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery factor(%)
Description
Sample log Assay Results
Sample No.
Location (m) Length(m)
Length of core (m)
Recovery factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
11.77 Grey to grey green,development of the chlorite and epidotization;Py=2%,Py occur as ubhedral to xenomorphic granular aggregates.Two group joint, 60° and 80°to core axis.
Nippm
Moppm
Auppb
Agg/t
8.708.8920.66 98
ZK10
ZK10 03meta-
andesite with Py
11.773.70meta-andesite02
Grey green,development of the chlorite and epidotization,quartz veinlet,orientation arrangement; Py=2%,speckles and irregular veinlet; 21.21m,quartz veinlet(5cm),Py speckles; 21.67m,22.40m,quartz veinlet(3cm); 21.21-22.52m,Py speckles,the content is about 3%; 26.00-27.94m,grey white, felsic volcanics;
10010.5110.51
Grey,medium-fine grained,massive structure, the content of Py is <1%.One group joint, 60°to core axis.977.818.07
ZK10
ZK10 06 massive sulfide
31.5020.99meta-
andesite with Py
05
100 Brass-yellow hue,massive sulphide,Py=80%,Po=10%,a little bit Clp. 31.95-32.32m,meta-andesite with Py.31.50 33.52 2.02 2.02
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-134 35.05 1.53 1.53 100 190 <20 170 110 <10 300 40RL.H-135 36.15 1.10 1.10 100 260 <20 170 90 10 250 30RL.H-136 37.35 1.20 1.20 100 60 <20 120 100 30 310 40RL.H-137 38.70 1.35 1.35 100 350 <20 130 100 <10 260 30RL.H-138 39.97 1.27 1.27 100 120 <20 130 90 <10 290 40
RL.H-139 41.15 1.18 1.18 1001860 20 80 140 20 22 1.6 10 230
RL.H-140 42.05 0.90 0.90 1007560 40 260 430 60 30 80
RL.H-141 43.05 1.00 1.00 100 180 20 <10 <10 <10 <10 <10RL.H-142 44.00 0.95 0.95 100 180 30 50 <10 <10 30 <10
RL.H-144 45.04 1.04 1.04 100 1930 30 470 190 30 14 1.6 10 140
RL.H-145 46.29 1.25 1.25 100 3410 50 280 240 180 30 150
RL.H-146 47.74 1.45 1.45 100 4470 40 220 500 50 14 3.4 10 80RL.H-147 48.84 1.10 1.10 100 640 <20 260 60 <10 110 20RL.H-148 50.29 1.45 1.45 100 360 <20 170 30 <10 80 20RL.H-320 51.39 1.10 1.10 100 130 <20 150 70 <10 270 30RL.H-321 52.69 1.30 1.30 100 300 <20 160 60 <10 210 30RL.H-322 53.64 0.95 0.95 100 310 <20 70 60 <10 130 40RL.H-323 54.56 0.92 0.92 100 180 <20 110 70 <10 170 40
Grey green-grey,development of the chlorite ,epidotization and siliconization. Py=2%,speckles and irregular veinlet; 37.65-37.90m,Py speckles.
1006.456.45ZK10 07meta-
andesite with Py
33.52 39.97
42.05 2.08 2.08 100ZK10 08 massive sulfide 39.97
Brass-yellow hue,massive sulphide,Py=55%,Po=35%,a little bit Clp. 41.15-42.05m,Py=Po=45%;
41.23m,Py,Po and Clp.
ZK10 09 felsic volcanics 42.05 44.00 1.95 1.95 100 Grey white,fine-grained to aphanitic texture,massive structure,main mineral composition are
feldspar,quatz.a little bit sulphide in.
47.7444.00massive sulfide10
Brass-yellow hue,massive sulphide,Py,Po and a little bit Clp. 45.04-45.30m,more Po,Po=40%,Py=50%;
46.00-47.14m,Po=Py; 45.30-45.50m,grey white, felsic volcanics;
1003.743.74ZK10
Grey green-grey,development of the chlorite,epidotization and siliconization. 48.69-49.04m,52.60-52.74m,52.89-53.04m,grey white, felsic volcanics,a little bit Py in.1006.826.8254.5647.74
meta-andesite with
Py11ZK10
第 14 页,共 19 页
From To From To
Drill Log of Hole #RLP-11-10
Hole No. No. Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery factor(%)
Description
Sample log Assay Results
Sample No.
Location (m) Length(m)
Length of core (m)
Recovery factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
ZK10 12 felsic volcanics 54.56 75.73 21.17 21.17 99
Grey white,fine-grained to aphanitic texture,massive structure.main mineral composition are feldspar,quatz.a little bit Py in,Py<1%. One group joint, 50°to core axis.; 74.02-74.38m,grey-green,meta-mafic volcanics.
ZK10 13 meta-andesite 75.73 109.78 34.05 34.05 100
Grey,grey green,fine-grained,a little bit Py in. 75.98-76.33m、77.51-77.73m、78.52-78.95m、80.35-81.57m、88.47-88.32m,grey white, felsic volcanics; 92.61-93.06m、93.36-94.16m、95.53-96.75m、100.30-101.15m、102.01-102.26m,yellowish pink,felsic volcanics; 102.6-104.29m,104.78-105.46m,yellowish pink,felsic volcanics; 107.18-107.50m,grey white, felsic volcanics;
ZK10 14 K-feldspar granite 109.78 123.44 13.66 13.66 100 Light flesh red, main mineral composition are K-feldspar,quatz and biotite.
第 15 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 636874.032 East: Original Units: M North: North: 5445451.449 North: Storage: Markham Elevation: Elevation: 507.698 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFF
Page 10 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK11
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 120 Length: 2.27 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -50 Pulled: No Claim No: 4252235 Spotted by: ShawnLength: 117.35 meters Capped: Yes NTS: Coord Type: Started: 25-March-11 Cemented: No Surveyed Date: Completed: 27-March-11 Logged by: ShawnLogged: 28-March-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: Yes
Deviation TestsDistance(m)
Geophysics: Target: VETM anomaly supported by Geotech reportComments: The approximately 30 metres of quartz monzonite/granite intersected at the end of ZK11 may represent the main body of the Chill Lake Lake pluton.
16-Nov-12
Azimuth47.24 125.4
102.11 118.9
9B
From To From To
ZK11 01 Overburden 0 2.27 0 2.27 0 Overburden\casing.
RL.H-149 15.31 16.51 1.20 1.20 100 40 <20 100 290 <10 480 40RL.H-150 17.71 1.20 1.20 100 200 <20 80 380 <10 320 100RL.H-151 18.86 1.15 1.15 100 200 <20 120 280 <10 320 80RL.H-152 19.81 0.95 0.95 100 290 70 220 330 20 340 80RL.H-153 21.11 1.30 1.30 100 250 20 310 290 30 230 50RL.H-155 22.31 1.20 1.20 100 570 30 160 230 40 6 0.6 220 50RL.H-156 23.61 1.30 1.30 100 370 <20 160 210 10 240 80RL.H-157 24.71 1.10 1.10 100 410 <20 150 270 <10 260 70RL.H-158 25.91 1.20 1.20 100 220 <20 160 370 <10 300 90RL.H-159 27.26 1.35 1.35 100 290 <20 180 420 <10 290 80RL.H-160 28.41 1.15 1.15 100 250 <20 140 420 <10 <5 0.3 270 120RL.H-161 29.66 1.25 1.25 100 240 <20 130 320 40 310 70RL.H-162 30.86 1.20 1.20 100 260 <20 70 300 20 190 40RL.H-163 32.00 1.14 1.14 100 130 <20 60 100 <10 90 10RL.H-164 33.10 1.10 1.10 100 710 <20 160 440 <10 210 130RL.H-166 34.40 1.30 1.30 100 320 <20 170 390 30 6 0.5 280 100RL.H-167 35.75 1.35 1.35 100 240 <20 260 270 <10 290 80RL.H-168 36.95 1.20 1.20 100 330 <20 190 420 20 270 150RL.H-169 38.10 1.15 1.15 100 210 <20 160 300 <10 310 70RL.H-170 39.35 1.25 1.25 100 270 <20 160 260 20 300 70RL.H-171 40.65 1.30 1.30 100 240 <20 140 270 <10 280 90
02
Grey to grey green,development of the chlorite,epidotization and some quartz vein.Py=<1%, scattered specks.One group joint, 50°to core axis. 7.47m,white quartz vein(7cm),a little bit Py in,Py=1%; 7.70m,white quartz vein(7cm); 7.95m,white quartz vein(3.5cm),a little bit Py in,Py=1%;
10014.2414.2416.512.27meta-andesiteZK11
Grey to Grey green, development of the chlorite,epidotization and some quartz vein.Py=2-15%,Po=1-5%,a little bit Clp,the content <1%.One group joint, 55°to core axis. 16.51-19.81m,Py=2%,scattered specks,irregular veinlets; 19.81-44.84m.Py and a little bit Po,the content is about 6%;
44.84-47.74m.Py=1%,scattered specks; 47.74-50.29m,Py=3%, irregular veinlets; 50.29-54.89m.Py=2%;54.25m,54.41m,white quartz vein(2-3cm),a little bit Py in; 54.89-61.44m,Py=12%,Po=1%,irregular veinlets,in lumps and heavily disseminated; 61.44-70.83m,the content of sulphide is about 5%,Py and minor Po, irregular veinlets; 70.83-72.75m,felsic volcanics, grey-white and light flesh red,a little bit Py in; 72.75-82.97m,Py,Po and minor Clp, the content of sulphide is about 6%. 77.30m,a little bit Clp. 82.97-83.27m,massive sulphide,Py=90%;
83.27-83.57m,heavily disseminated Py, Py=40%; 83.57-83.63m,massive sulphide, Py, sulphide =95%; 83.63-84.58m,Py,irregular veinlets, sulphide=15%; 84.58-84.64m,massive sulphide, Py, sulphide >95%; 84.64-86.87m, Py irregular veinlets, sulphide=2%;
Drill Log of Hole #RLP-11-11
Hole No. No. Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery factor(%)
Description
Sample log Assay Results
Sample No.
Location (m) Length(m)
Length of core (m)
Recovery factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-172 41.80 1.15 1.15 100 220 <20 180 260 <10 320 50RL.H-173 43.10 1.30 1.30 100 280 <20 140 270 <10 6 <0.3 310 90RL.H-174 44.20 1.10 1.10 100 280 <20 120 260 <10 310 60RL.H-175 44.84 0.64 0.64 100 260 <20 120 220 10 270 60RL.H-177 46.29 1.45 1.45 100 150 <20 110 70 <10 200 50RL.H-178 47.74 1.45 1.45 100 130 <20 100 70 <10 200 40RL.H-179 48.99 1.25 1.25 100 160 <20 120 80 <10 200 50RL.H-180 50.29 1.30 1.30 100 730 <20 130 180 10 12 0.5 240 80RL.H-181 51.44 1.15 1.15 100 160 <20 120 70 <10 190 40RL.H-182 52.59 1.15 1.15 100 100 <20 100 60 <10 180 30RL.H-183 53.74 1.15 1.15 100 90 <20 110 60 <10 180 40RL.H-184 54.89 1.15 1.15 100 140 <20 140 80 <10 170 40RL.H-185 56.09 1.20 1.20 100 500 <20 160 340 20 <5 0.6 280 80RL.H-186 57.39 1.30 1.30 100 1100 <20 320 540 60 19 1.7 90 190RL.H-188 58.39 1.00 1.00 100 280 <20 120 250 160 150 50RL.H-189 59.44 1.05 1.05 100 520 <20 470 340 40 150 60RL.H-190 60.44 1.00 1.00 100 280 <20 300 180 10 90 50RL.H-191 61.44 1.00 1.00 100 970 <20 160 510 120 7 1.7 50 130RL.H-192 62.48 1.04 1.04 100 170 <20 140 110 <10 210 40RL.H-193 63.73 1.25 1.25 100 280 <20 270 190 70 270 60RL.H-194 64.98 1.25 1.25 100 370 <20 150 180 <10 250 60RL.H-195 66.23 1.25 1.25 100 360 <20 200 240 <10 280 70
ZK11meta-
andesite with Py
03 10070.3670.3686.8716.51
第 16 页,共 19 页
From To From To
Drill Log of Hole #RLP-11-11
Hole No. No. Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery factor(%)
Description
Sample log Assay Results
Sample No.
Location (m) Length(m)
Length of core (m)
Recovery factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-196 67.38 1.15 1.15 100 920 <20 210 370 <10 260 90RL.H-197 68.58 1.20 1.20 100 1210 <20 320 390 <10 8 0.9 260 140RL.H-199 69.78 1.20 1.20 100 1310 <20 210 380 <10 290 90RL.H-200 70.83 1.05 1.05 100 390 <20 120 160 <10 210 60RL.H-201 72.75 1.92 1.92 100 20 <20 10 <10 <10 20 <10RL.H-202 74.00 1.25 1.25 100 70 <20 130 120 <10 220 40RL.H-203 75.20 1.20 1.20 100 510 <20 190 530 20 10 0.3 100 110RL.H-204 76.40 1.20 1.20 100 290 <20 530 420 <10 670 140RL.H-205 77.72 1.32 1.32 100 1420 <20 290 340 <10 9 0.7 210 60RL.H-206 78.92 1.20 1.20 100 280 <20 210 190 <10 240 100RL.H-207 80.17 1.25 1.25 100 180 <20 460 260 <10 240 100RL.H-208 81.42 1.25 1.25 100 60 <20 170 180 <10 200 30RL.H-210 82.62 1.20 1.20 100 190 <20 220 210 <10 220 40RL.H-211 83.82 1.20 1.20 100 180 <20 1210 220 10 15 0.3 70 100RL.H-212 84.82 1.00 1.00 100 210 <20 380 160 10 40 70RL.H-213 85.82 1.00 1.00 100 150 <20 390 150 10 60 30RL.H-214 86.87 1.05 1.05 100 210 <20 100 190 <10 60 20RL.H-215 88.02 1.15 1.15 100 30 <20 40 10 <10 30 <10RL.H-216 89.32 1.30 1.30 100 30 <20 10 <10 <10 20 <10
ZK11 05 K-feldspar granite 90.73 117.35 26.07 26.62 98 Light flesh red, main mineral composition are K-feldspar,quatz and biotite.
93.80-94.30m、107.60-108.90m、110.85-111.20m,potassium alteration.
04ZK11 3.8690.7386.87meta-andesite
Grey green-grey,development of the chlorite,epidotization and siliconization. 88.02-89.32m,grey white, felsic volcanics.1003.86
第 17 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 636708.874 East: Original Units: M North: North: 5445441.67 North: Storage: Markham Elevation: Elevation: 511.544 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFF
Page 11 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK12
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 110 Length: 2.95 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -55 Pulled: No Claim No: 4252235 Spotted by: ShawnLength: 105.16 meters Capped: Yes NTS: Coord Type: Started: 27-March-11 Cemented: No Surveyed Date: Completed: 29-March-11 Logged by: ShawnLogged: 30-March-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: Yes
Deviation TestsDistance(m)
Geophysics: Target: VETM anomaly supported by Geotech reportComments: The drill hole intersected a 0.4 metre interval of metasediment or shear zone from 61.52 to 61.92 metres containing 20-30% py/po as disseminations/laminations within mafic metavolcanic sequence.
16-Nov-12
Azimuth44.20 114.583.82 116.8
10B
From To From To
ZK12 01 Overburden 0 2.95 0 2.95 100 Overburden\casing.
RL.H-217 4.57 5.85 1.28 1.25 98 100 <20 110 40 <10 40 50
RL.H-218 46.64 48.04 1.40 1.40 100 160 <20 110 100 <10 200 40
RL.H-219 60.52 61.52 1.00 1.00 100 100 <20 100 140 <10 300 50
ZK12 03meta-
andesite with Py and Po
61.52 61.92 0.40 0.40 100
Gray - gray green,fine-grained texture and massive structure, mineral composition mainly amphibole, albite and a small amount of quartz and biotite.Rock development pyritization, pyrrhotite, showed a fine hypautomorphic -xenomorphic, a concentrated veinlets distribution, local arranged in mass, pyrite and pyrrhotite content quite, each account for about 15% of the overall content of about 30%, sulfide.
RL.H-221 61.92 0.40 0.40 100 630 <20 110 190 20 7 1.1 390 90
RL.H-222 63.18 1.26 1.26 100 130 <20 140 250 <10 180 70RL.H-223 64.48 1.30 1.30 100 90 <20 160 170 <10 310 60RL.H-224 66.13 1.65 1.65 100 140 <20 90 110 <10 200 40RL.H-225 67.33 1.20 1.20 100 40 <20 40 90 10 <5 <0.3 120 20RL.H-226 68.58 1.25 1.25 100 120 <20 170 80 <10 50 30
Grey - dark green, fine-grained texture and massive structure,mineral composition mainly amphibole, albite and a small amount of quartz and biotite. Rock development chloritization epidotization, quartz veins and calcite veinlets, occasionally pyrite, content < 1%;66.13-72.83m, rock was gray, cryptocrystalline structure, development is strong silicification, occasionally sulfide, content < 1%;82.32-86.00m, rock is fine, with more black mica, mica particles visible black;99.36-101.81m, rock is fine, with more black mica.
10043.2443.24105.1661.9204
58.5061.522.95meta-andesite
ZK12
02ZK12
meta-andesite
Drill Log of Hole #RLP-11-12
Hole No. No. Rock/Ore
type
Depth(m) Thickness
(m)
Length of core (m)
Recovery factor(%)
Description
Sample log
Grey to dark-green,fine-grained texture and massive structure,main mineral composition are Hornblende, feldspar and small amounts of quartz and biotite.Rock development chloritization epidotization and silicification. Generally see vein quartz and calcite veinlets, pulse width of about 0.1-5.0cm, more irregular shape distribution;more quartz veinlets than calcite veinlets, quartz veins occasionally a small amount of pyrite and pyrrhotite.The core is in a short column ( < 0.5m ) - long column, development of two groups of joints, 40 tocore axis and 60 to core axis..The rock I see pyrite were mainly scattered, fine shape distribution, also see a few scattered magnetic pyrite, sulfur content < 1%;2.95-7.01m, rock shows fine structure; pyrite films can be see at 4.70m rock joints ,width about 1.5cm quartz vein at 3.7m, the distribution amount of pyrite and pyrrhotite.7.01-10.87m,almond structure , almond body mainly calcite and quartz;46.64-47.74m,pore structure and pyrite drain hole, see a little pyrite distribution, content of about 1%.
10058.57
Sample No.
Location (m) Length(m)
Length of core (m)
Recovery factor(%)
Cuppm
Coppm
Nippm
Moppm
Auppb
Agg/t
Assay Results
Pbppm
Znppm
Crppm
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
第 18 页,共 19 页
Project: RICHARDSON LAKE
Surface Hole: Yes Level:
Core Coordinate-Gemcom Coordinate-UTM Coordinate-GridDimension: NQ East: East: 635309.305 East: Original Units: M North: North: 5443119.607 North: Storage: Markham Elevation: Elevation: 564.416 Elevation:
UTM Zone: NAD 15,ZONE Grid Name:
TypeFFF
Page 12 of 12
CHINA METALLURGICAL EXPLORATION CORP. Hole Number: ZK13
Diamond Drill Hole Report Project Number:
Drilling Casing Location OtherAzimuth: 150 Length: 1.20 meters Township: UPPER SCOTCH LAKE AREA Contractor: TOPRANKDip: -45 Pulled: No Claim No: 4252237 Spotted by: ShawnLength: 147.52 meters Capped: Yes NTS: Coord Type: Started: 1-April-11 Cemented: No Surveyed Date: Completed: 3-April-11 Logged by: ShawnLogged: 4-April-11 Re-logged by: Wedged: No Water Source: Wedged from: Water Line:
Left in hole: Casing + ShoeControl Drilling: Cutting Sampled: YesGeophysics:
Target: VETM anomaly supported by Geotech reportComments:The hole intersected approximately 71 metres of mafic metavolcanic before intersecting approximately 76 metres of relatively unaltered and un-deformed weakly to moderately magnetic diorite .
Deviation TestsDistance(m)
16-Nov-12
Azimuth45.72 149.591.44 155
138.38 160.3
11B
From To From To
ZK11 01 Overburden 0.00 1.22 0.00 1.22 100 Overburden\casing.
RL.H-271 6.62 7.75 1.13 1.13 100 210 <20 60 130 <10 240 40
RL.H-272 8.80 1.05 1.05 100 290 <20 70 140 <10 250 50
RL.H-273 9.90 1.10 1.10 100 3010 <20 70 130 <10 260 50
RL.H-274 10.76 0.86 0.86 100 1330 <20 60 220 <10 95 2.1 210 180
RL.H-324 104.85 105.95 1.10 1.10 100 300 <20 50 140 <10 <10 <5 230 50
RL.H-325 107.25 1.30 1.30 100 290 <20 60 190 <10 <10 <5 300 70
RL.H-278 123.14 124.14 1.00 1.00 100 70 <20 80 70 <10 <10 6 90 40
Drill Log of Hole #RLP-11-13
Dark grey to black,medium-coarse grained,massive structure,main mineral composition are pyroxene and feldspar,the content of them are almost same.Fine-grained pyrite are occasional to find. 88.91-89.36m,quartz vein.
119 29-120 79m white quartz vein
Ptppb
Pdppb
147.52 56.61 56.61 100
Grey to grey-green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. The rock developed Py,Po and Clp,occur as ubhedral to xenomorphic granular aggregates,Py=3%,Po=5%,Clp=2%; 8.90m,Clp vein,the width is 4mm,the length is 7cm. 10.06m,more Clp,Po=10%,Clp=10%.
90.91 80.15
ZK11 05 gabbro 90.91
ZK11 04meta-
andesite10.76 80.15 100
Grey to grey-green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. Po is occasional to find,the content is < 1%. One group joint,45°to core axis.The core length are <0.5m. Calcite and quartz veins are common,the width is about 0.1-5cm. 47.50-49.80m、70.00-71.32m,the core are broken。
ZK11
ZK11 1001.961.9610.768.80
Grey to grey-green,fine-grained,massive structure,main mineral composition are amphibole,feldspar,quartz and biotite,development of the chlorite,epidotization and silicification. Calcite and quartz veins are common,the width is about 0.1-4cm. Pyrite is occasional to find,the content is about 1%.The core are broken,the length of the core are <0.4m.
1007.587.58
meta-andesite
with Py,Po and Clp
03
8.801.22meta-
andesite02
Thickness
(m)
Length of core (m)
Recovery
factor(%)
DescriptionHole No.
No.Rock/Ore
type
Depth(m)
Sample log Assay Results
Sample No.
Location (m)Length(m)
Length of
core (m)
Recovery
factor(%)
Cuppm
Pbppm
Znppm
Crppm
Coppm
Nippm
Moppm
Auppb
Agg/t
正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M正元国际矿业有限公司W W W . C N Z I M C . C O M
RL.H-279 125.14 1.00 1.00 100 80 <20 80 70 <10 <10 <5 100 40
119.29 120.79m,white quartz vein. 135.63-135.90m,quartz vein.
第 19 页,共 19 页
LEGEND
ARCHEAN
• Van Nostrand Stock Cornpos11l0D
14a Granite 14b Granodiorite J4c Mmronite
Features 14f Medium grained 14h lnequigranular 14j Biotite 14k Hornblende 14n Potassimn feldspar
phenocrysts
~Norway Lake Pluton ~Composition
13a Granite 13b Granodiorite 13c Tonalite !3d Mmronite 13e Quartz mmzonite 13f Diorite 13gMmmdiorite 13h Quartz diorite 13j Syenite Features 13k Pegmatitic 13mlll:e 13n Medium grained 13p Coan!e grained 13q Equigranular 13r Inequigranular 13s Biotite 13t Hornblende 13u Potassium feldspar phyric 13v Amphihclite xenoliths
Intrusive Mafic to Ultramafic Rocks OJmposition 9a Gabbro 9b Melanogabbro 9c Peridotite 9d Pyroxenite 9e Homblendite Features 9f Magnetite 9g Asbestos 9h Plagioclase phyric 9j Talcose 9k Actinolite 9m Serpentine
~ Synvolcanic Intrusive L____"_____j Mafic Rocks
Composition Sa Gabbro
• Chemical Metasedilrentary Rocks Sa Chert 5b Ferruginous chert 5c Oxide facies ironstone
(magnetite bearing) Sd Sulfide facies ironstone
(pyrite ± pyrrhotite bearing)
5e Silicate facies ironstone Sf Oastic ironstone
~ Oastic Meta~ sedimentary Rocks
lithofacies 4a Slate, argillite 4b Mudstone 4c lithic wacke 4d lithic arenite 4e Quartz arenite 4f Polymictic conglorrnrate.
matrix supported 4g Polymictic conglomerate,
clast supported Features 4h Graded 4j l1llninated 4k Schistose 4m Gamet porphyroblasts 4n Chert
~Intermediate and Felsic L_____:'_____j Metavolcanic Rocks
Pyroclastic Deposits 3a Tuff Features 3f Quartz phyric
D Mafic Metavolcanic Rocks Lithofacies of Flows 2a Massive flows 2b PillOIWd flow.; 2c Autobreccia,
flow-top breccia, hyaloclastite breccia
2d Coan;e-grained flow 1o synvolcanic gabbroic
dikes and sillsd Pyroclastic Deposits 2e Tuff 2f Lapilli tuff Features 2g Dikes 2h Magnetite 2j Plagioclase phyric 2k Variolitic 2m Gamet porphyroblasts 2n Amygdaloidal 2p Schistose 2q Vesicular 2r Amphihclite 2s Hyaloclastite
• Ultramafic Metavolcanic Rocks lithofacies of Flows la Massive flows 1 b Autobreccia, flow-top
breccia Pyroclastic Deposits
Features I d Spinifex textured
/ /
/
/ /
/
I
I
I
I
I
-<--@ I
RLP- 11 c::09 1 ~-~ -1
I
I
~ 4252234 50
D
SYMBOL
C2JRoad
1/~//1 Geologic boundary
~ Small bedrock ~exposure
I / / /I Fault, interpreted
1/l Strike and dip l___"_"'_J of schistosity
~ Pillov.ed flow, ~ facing knomWnknown
~ Volcanic bedding ~ facing known/unknown
0 Foliation, inclined
[1:2] Property boundary
I ~~-09 1 Location of DDH
RLP-11 -01
10m
20
30
40
50
60
70
80
90
100
110
120
130
140
150
160
Cu
o ~ N
00 00 00
Zn
0 "' 0 0
A I
IS) 1\.) .t:>. (J) 0 (Jl 0 (Jl 0 0 0 0 0 0 0 0
Ba
ON .l::>. G:lQ:I --"--" g........o...p.VJ .t::r. OlG:l-..JCXD Ol --"--" N ON.t:>.aJDOOOOOO 0 0 Ol 0
00000000 0 0 0 0 "'
OOl --" --"NNVJC OOOlOOlO C
00000(
480
470
460
450
440
430
420
410
400
STRIP LOG: RLP-11-01 Easting
633683.0
STRIP
Northing 5438207.2
RL 497.1
Azimuth 90.0
Dip -45.0
Depth 163.7
1 Rock_code PAT LABEL DESCRIPTION
And meta-andesite Bas-S Pyrrhotite meta-basalt IF Iron Formation Lamp lamprophyre Ovb Overburden
CME Corp. Richardson Lake Project
RLP-11-02
10m
20
30
40
50
60
70
80
90
100
110
120
ON 0
Ag Cu
o~
0 0 0
Zn AI Ba Ca Cr Co
o<n~
00 0
Fe K Sc Sr
0 (Jl ~
Ti v
OOl---"---"NNW OOOlOOlO
00000
RL
500
495
490
485
480
475
470
465
460
455
450
445
440
435
430
425
420
STRIP LOG: RLP-11-02 Easting
633404.6 Northing
5438233.9
STRIP
1 Rock_code
RL 501.7
PAT
Azimuth 70.0
LABEL
And Lamp Ovb
CME Corp.
Dip -45.0
Depth 123.4
DESCRIPTION
meta-andesite lamprophyre Overburden
Richardson Lake Project
RLP-11 -03
10m
20
30
40
50
60
70
80
90
100
110
120
130
140
150
Ag Cu
o~N
00 00 00
Zn A I Ba Ca Cr Co
0 N .t:>. G:l CO --" --" 0--"NW .l::>. OlG:l-.JOD Ol --" --" 0 f\.) 00000000 0 0 (Jl
00000000 0 0
OOl --"--" NNW OOOlOOlO
00000
STRIP LOG: RLP-11-03 Easting
633025.5 Northing
5438170.0
STRIP
1 Rock_code
RL 510.1
PAT
Azimuth 60.0
Dip -55.0
Depth 150.9
LABEL DESCRIPTION
And And-S
IF Lamp Ovb
meta-andesite meta-andesite with pyrrhotite and pyrite Iron Formation lamprophyre Overburden
CME Corp. Richardson Lake Project
STRIP LOG: RLP-11-04 Easting Northing RL Azimuth Dip Depth
635010.4 5440603.5 540.2 250.0 -60.0 177.4 RLP-11 -04 Ag Cu Zn AI Ba Ca Cr Co Fe K Mg Sc Sr Ti v
STRIP
1 Rock_code PAT LABEL DESCRIPTION 10m
530 And meta-andesite Gran2 granite
20 Ovb Overburden
520 QV-Sil quartz vein and stong silicification
30 meta-andesite
510
40
500
50
60 490
70 480
80 470
90
460
100
450
110
440 120
130
140 420
150
410
160
400
170
390
00 --"--" f\Jf\.)VJ G)~ =><>a) 0 --" NVJ .J::>. OlG:I-..Jm~N ON .t:>. G:ICO --" 0 --" NVJ .l::>. OlG:l-....JCXIJ!DOl --" 0 "' c; ~ NOO --"--" N 0 --" N VJ .t:>. OlCIJ:l c; "' 0J Q::>. F\.X.Jl .l::>. (J) 0 0 0 0 0 .....~Q-45~ --"--" 1'\JNVJ C
"' "' "' "'008 000 00 0 0000000000 0 0 "' "' 0 0 ocooo rv :.::.. meo f.SlOOlOOlO C 000 00 000000000 0 0 0 00000(
000
CME Corp. Richardson Lake Project
RLP-11 -06
10m
20
30
40
50
60
70
80
90
100
110
120
130
140
ON_,. =
Ag Cu Zn
~ = = = 0 --" NVJ .J::>. OlG:I-..JmCDN .t:>. (J) ())Q--P>..) .I» (J)....€0 --"--"9 N
0 0 0 0 0 N .t:>. ON .t:>. 0 0000000 0
0 0 0
v RL
510
500
490
480
470
460
450
440
430
420
410
STRIP LOG: RLP-11-06 Easting Northing RL Azimuth Dip Depth
634089.3 5440803.8 510.6 90.0 -60.0 141.7
STRIP
1 Rock_code PAT LABEL DESCRIPTION
And meta-andesite And-S meta-andesite with
pyrrhotite and pyrite - Gran K-feldspar granite (1:1~4',\"l HDS-MS heavily disseminated
to massive sulfide MS-HDS massive to heavily
disseminated sulfide - Ovb Overburden
CME Corp. Richardson Lake Project
RLP-11 -07
10m
20
30
40
50
60
70
80
90
100
110
120
ON 0
Ag Cu
o ~
0 0 0
Zn A I Ba Ca Cr
0 --" 1\JW .l::>. Ol 00000 00000
Co
o<n ~
00 0
STRIP LOG: RLP-11-07 Easting Northing RL Azimuth Dip Depth
634713.4 5441172.1 507.7 55.0 -50.0 124.1
STRIP
1 Rock_code PAT LABEL DESCRIPTION
And meta-andesite And-S meta-andesite with
pyrrhotite and pyrite - Ovb Overburden
CME Corp. Richardson Lake Project
STRIP LOG: RLP-11-08 Easting Northing RL Azimuth Dip Depth
634409.0 5441157.4 511.5 65.0 -55.0 150.9 RLP-11 -08 Ag Cu Zn AI Ba Ca Cr Co Fe K Mg Sc Sr Ti v RL __ __, __ __, --
510 STRIP
1 Rock_code PAT LABEL DESCRIPTION 10m
And meta-andesite 500 Gran K-feldspar granite
20 ---f---- f---- Ovb Overburden
490
30 --- --- --
40 480
50 470
60
460
70 --- --- --
450
80
90 440
100 --- -----
430
110
420
120
410 130 --------
140 400
150
0 "' ON 0 --" NVJ .l::>. OlG:I-..Jmt;eN ON .l::>. G:IC:0 --"--" 0 "' ..,. o<n~
0 "' --" --" NOO --" 0--"NW .l::>. OOl --"--"NNW~ 0 0 0 0 0 --'OOl --"--" f\Jf\.)(JJ ( 0 0 00 ON 0 0 00 0"' 0 "' OOlOOlOOlaill1IO N ~ G:IO:l OOOlOOlO C 0 0 00 0 0 0 00 00000( 0
CME Corp. Richardson Lake Project
RLP-11 -09
10m
20
30
40
50
60
70
80
90
100
110
120
130
ON-" 00
Ag Cu
00--" --" NNW G> --" (.n(n(.n(n8
0
Zn
0 "' 0 0
A I Ba Ca Cr
ISJ--" NVJ4>il0lm-..Jm--"rvw OOlOOlO 000 00000 000 0 0 0 0 0
Co
o<n~
00 0
Fe K
0 .t:>. anJl --"--" NNW~W.t:>. OOlOOlOOlailltDOO
0000
Ti v RL
500
490
480
470
460
450
440
430
420
410
400
390
STRIP LOG: RLP-11-09 Easting Northing RL Azimuth Dip Depth
634321.7 5443331.7 502.9 270.0 -65.0 133.2
STRIP
1 Rock_code PAT LABEL DESCRIPTION
And meta-andesite And-S meta-andesite with
pyrrhotite and pyrite Gran K-feldspar granite Ovb Overburden
CME Corp. Richardson Lake Project
RLP-11-10
10m
20
30
40
50
60
70
80
90
100
110
120
ON-" 00
Ag Cu Zn AI Ba --v---v---
L
I I I I I I I I I I I O --" NW.t::r.Olm-..Jmc;gf\JW.t::.
o=o o=o
OOl --"--" Nf\DOl OOOlOOl
0000
Sc Sr Ti v RL
STRIP LOG: RLP-11-10 Easting
636738.9 Northing
5445230.6 RL
514.4 Azimuth
110.0 Dip
-55.0 Depth 123.4
STRIP
1 Rock_code PAT LABEL DESCRIPTION
And meta-andesite And-S meta-andesite with
pyrrhotite and pyrite FV felsic volcanics Gran K-feldspar granite MS massive sulfide Ovb Overburden
CME Corp. Richardson Lake Project
RLP-11-11
10m
20
30
40
50
60
70
80
90
100
110
ON 0
Ag Cu
o ~ rv
00 00 00
Zn
~ = == = 0 --" NW.l::>.UlG:I-..Jm~NW .l::>.UlG:I
000000 000000
0 "'
505
500
495
490
485
480
475
470
465
460
455
450
445
440
435
430
425
420
~ ~ ~~~ ~ N ~ UD --" N W ~ Ul~~~~~~88§§8§8~ ~ ~ ~ 0
STRIP LOG: RLP-11-11 Easting
636874.0
STRIP
Northing 5445451.4
1 Rock_code
RL 507.7
PAT
Azimuth 120.0
LABEL
And And-S
Gran Ovb
Dip -50.0
Depth 117.3
DESCRIPTION
meta-andesite meta-andesite with pyrrhotite and pyrite K-feldspar granite Overburden
CME Corp. Richardson Lake Project
STRIP LOG: RLP-11-12 Easting Northing RL Azimuth Dip Depth
636708.9 5445441.7 511.5 110.0 -55.0 105.2 RLP-11-12 Au Ag Cu Zn AI Ba Ca Cr Co Fe K
510 STRIP
505 1 Rock_code PAT LABEL DESCRIPTION 10m
And meta-andesite 500 And-S meta-andesite with
20 495 pyrrhotite and pyrite - Ovb Overburden
490
30 485
480 40
475
50 470
465
60 460
455 70
450
80 445
440
90 435
430 100
425
ON 09--":-" o~ ON o __.. N w .t:>. Ol m -..J mc;ervw.t:>.Olm-..J ON.l::>.G:lQ:I--" 0--"NVJ.t:>. o<n~ 0 "' ;::; ~ NOO--"--"N 0 --" N W .t:>. OlanJl--"--"NNWUCJ::>..t>J ..,. Ol CXCl-@ 9 0 0 --'OOl--"--"NN VJC
0
"' "' 0 0 0000000 0 0000 00 0 "' "' 00l00l00l0(l1D 0 0
:5 :!9 ~"'"' OOOlOOlO C
0 0 0000000 0000 0 0 0 0 00000( 0 0 0
CME Corp. Richardson Lake Project
RLP-11-13 Ag Cu Zn
10m
20
30
40
50
60
70
80
90
100
110
120
130
140
0--"NVJ .l::>. 0\J 0 0 0 0 0 0 0 0 0 0 0000
AI Ba Ca
0 --" 1\JW .l::>. OlG:I-..Jmc;gJ>..:KJJ.t>.OlG:I-..JO:lO 1"0 .t:>. G:l CO --" 00000000 0 00000000
Cr
.t:>. CIJlJl --" --"NNVJUQ::>..to.X.Jl .t:>. G:l 00l00l00l0(11l00 0
0 0 0
550
545
540
535
530
525
520
51 5
510
505
500
495
490
485
480
475
470
STRIP LOG: RLP-11-13 Easting Northing RL Azimuth Dip Depth
635309.3 5443119.6 564.4 150.0 -45.0 147.5
STRIP
1 Rock_code PAT LABEL DESCRIPTION
And meta-andesite And-S meta-andesite with
pyrrhotite and pyrite Gab gabbro Ovb Overburden
CME Corp. Richardson Lake Project