Submitted by: Paul Coad, Senior Project Geologist, …Senior Project Geologist, Regional Exploration...

32E12SE80M 63.6823 NOSEWORTHY 010

PAMOREX MINERALS INC.

TIMMINS DIVISION

REGIONAL EXPLORATION DEPT.

MIKWAM JOINT VENTURE (0703)

O.M.I.P. REPORT - 1990

Submitted by:

Paul Coad,Senior Project Geologist,Regional Exploration Dept.

February 1991

32EI2SE00M 63.6023 NOSEWORTHY 010C

CONTENTS

COMMODITIES

DEPOSIT TYPE

LOCATION

ACCESS

PROPERTY/OWNERSHIP

EXPENDITURES

REGIONAL GEOLOGY

PROPERTY GEOLOGY

1990 DIAMOND DRILL PROGRAM

Introduction

Tadpole-Noseworthy Lake Area Till Anomalies Section 2550 West - D.D.H. MK-90-1 and MK-90-3 Section 1900 West - D.D.H. MK-90-2 and MK-90-4

"85-B8 Area" (Noseworthy Lake Area)Section 600 West - D.D.H. MK-90-5; Section 400 East - D.D.H. MK-90-6

"85-A8 Area"Section 3912 East - D.D.H. MK-90-7

Bradette Township EM Conductor Section 8400 West - D.D.H. MK-90-8

Future Work

REFERENCES

Page

l

l

I

1

2

2

3

3

4

4

4

II

14

15

17

18

APPENDIX A

APPENDIX B

APPENDIX C

APPENDIX D

APPENDICES

Assay Certificates

Wholerock Certificates

Borsurv Data - Survey Data, Summary Lithologs, Assays

Diamond Drill Logs

MAP POCKETS

Section 2550 West

Section 1900 West

Section 600 West 400 West

Section 3912 East 8400 West

D.D.H. MK-90-1, 3

D.D.H. MK-90-2, 4

D.D.H. MK-90-5 D.D.H. MK-90-6

D.D.H. MK-90-7 D.D.H. MK-90-8

PLAN MAPS

Detailed Compilation: Noseworthy Lake Area (1:5,000)

Detailed Compilation: A-8 Area (1:2,500)

Compilation Map: Mikwam Property (1:100,000)

(1)

NOTE: The Mikwam J.V, Project is a joint venture between Pamorex Minerals Inc. (5096) and Norfree (Noranda and Freewest - 5096). Noranda is the operator of this project. The contents of this O.M.I.P. report (1990) have been extracted from a "Report on 1990 Mikwam Diamond Drilling - Noseworthy and Bradette Townships, Ontario" by W. Corstorphine, dated January, 1991. This report was received by Pamorex on February 19, 1991.

COMMODITIES

Au, Ag, Cu, Zn, Pb.

DEPOSIT TYPE

MAIN TARGET

Epigenetic gold deposit (i.e. the Golden Pond deposit owned by TVX Minerals, located 15 km ENE of the east boundary, would be a type-deposit model).

SECONDARY TARGET

Volcanogenic massive sulphide deposit (i.e. the Golden Hope (Estrades) deposit owned by Breakwater Resources located 20 km east of the Golden Pond deposit, would be a type-deposit model).

LOCATION (NTS 32E/5, 6, 11,12 - 490 30'n, 790 30' W)

The Mikwam property is situated 155 kms northeast of Timmins, Ontario, in the Larder Lake Mining Division, District of Cochrane.

ACCESS

Access to the Mikwam property is limited to helicopter and in rare locations to fixed wing aircraft during the summer and fall periods. Larger tracked, muskeg-type vehicles can negotiate local terrain in this period but creeks and rivers offer major obstacles to complete access.

n D DH

n Hi

Gtroffon

y

BtVliiP

Regional Location Map

Figure l

NORANDA EXPLORATION CO. LTD.

Hearst

A Ir*liMikwam Project \

(2)

In winter it is possible to traverse the entire property on an existing network of winter roads which have been generated over the last eight to ten years by Newmont and other major companies such as Noranda and Esso Minerals who have also been active in the area.

Ice bridges however must be constructed on the Turgeon River, if access is desired from the east via La Sarre, Quebec, or on the Burntbush River, if access directly to the central and/or western parts of the property via Cochrane, Ontario, is preferred.

A winter road system currently extends across Bradette, Noseworthy and Hoblitzell Townships. In the east it links up with the all-weather Casa Berardi road in Dieppe Township, Quebec. The Casa Berardi road itself originates 34 kms north of Ville Bois, off the Selbaie road. In the west, Newmont's road connects with the northern winter extension of the gravelled Tomlinson (Township) road which in turn adjoins Abitibi's all-weather Trans Limit Road which runs between Cochrane and Iroquois Falls and the Quebec-Ontario border north of Lake Abitibi.

PROPERTY/OWNERSHIP

All claims subject to the Joint Venture Agreement are unpatented and wholly owned by the J.V. partners [Norfree (Noranda-Freewest) and Pamorex Minerals Inc.], Golden Shield Resources Ltd. retains a 1596 net profits interest in the western-most 97 claims as per an underlying agreement with Newmont. All claims are currently on lease extension.

The combined properties - Mikwam plus Golden Shield - total 588 claims and extend in a contiguous fashion from Dieppe Township in Quebec (12 claims) through Bradette and Noseworthy Townships and into Hoblitzell Township (see Figure 2 and Table 1).

The property forms a narrow east-west band of claims in Bradette and Dieppe Townships where 2396 of the claims are located. The property "blossoms" in Noseworthy Township to 366 claims or 6296 of the total. Hoblitzell Township hosts a band of 87 Golden Shield claims (an additional 10 Golden Shield claims lie in Noseworthy Township west of the Burntbush River). The property is about 38 kms long and in Noseworthy Township - its widest point - is 7 kms across.

EXPENDITURES

Expenditures for 1990 are tabulated in Table 2 (prepared by J. Houle, Pamorex Minerals Inc.).

GOWEN POND

Property Map Figure 2

m.

TABLE l

CLAIM LIST

Bradette TWP.. Ontario

Hoblitzell TWP.. Ontario

Noseworthv TWP.. Ontario

Dieppe TWP.. Quebec

L591375-378 incl.- L591380-394 incl.- L624881-884 incl- L633372-411 incl.- L633452-491 incb L633628-634 incl. L633637-638 incl. L634392-394incl.' L636955-962 incl.

L628595-630 incl. L628634-684 incl.

L624885-900incl.' L624981-990 incl. L628685-694 incl. L633106-107 incl. L633130-132 incl. L633269-273 incl.- L633312-371 incl.- L633412-451 incl. L633548-566 incl. L633627L633641-656 incl.- L634364-391 incl. L733738-758incl.- L733761L784535-536 incl. L810232-273 incl. L814606-615 incl.- L839437-475incl.- L839487-527 incl.

420620. 1-5 incl.420621. 1-5 incl.420622. 1-2 incl.

GRAND TOTAL

TOTAL ACRES

(4) (15) (4) (40) (40) (7)(2)(3)

123

(36)J(5JQ

87

(16) (10) (10)(2)(3) (5) (60) (40) (19)(1) (16)(28) (21)(1)(2) (42) (10) (39)

366

(5) (5)

12

588

24,042 (9,729 hectares)

TABLE 2

PAMOREX MINERALS INC. 1990 O.M.I.P. COST REPORTBY PROJECT AND PROPERTY

FOR MAY l TO DEC. 31 PERIOD

PROJECT NAME: MIKWAM

PROPERTY NAME: MIKWAM

REFERENCE NO.: 0287

PAMOREX % INTEREST (VESTED): 50*

% EXPENDITURES APPLIED: 100%

ACCT. NO.

A2

1 D6

G2 G364 65

DESCRIPTION OF ACTIVITY MAJOR MINOR

TECHNICAL

GEOPHYSICS

DRILLING

e ^ S SS S^ SS S* "^ ^ ^ S ^ S

RESEARCH

I. P.

ANOMALY DRILLING CORE SPLIT/ASSAYS ENGINEERING CAMP COSTS

APRIL 30 YTD TOTAL

0.00

0.00

0.00 0.00 0.00 0.00

DEC. 31 YTD TOTAL

55,024.04

18,700.00

204,870.87 12,677.76 17,965.66 20,378.62

MAY 1 - DEC. 31

1990 COST

55,024.04

18,700.00

204,870.87 12,677.76 17,965.66 20,378.62

iTAL EXPENDITURES

JOINT VENTURE CONTRIBUTIONS

NET EXPENDITURES

0.00 329,616.95 329,616.95

0.00 164,658.48 164,658.48

0.00 164,958.47 164,958.47

(3)

REGIONAL GEOLOGY

The Mikwam property lies within the northern part of the Early Precambrian Abitibi Greenstone Belt of the Superior Structural Province. It occupies a position on the north flank of a northwesterly-trending lobe of the main Abitibi Belt between the northernmost Detour lobe and the main Timmins-Noranda-Val d'Or trend to the south.

Regional reconnaissance mapping was most recently conducted in the area by the Ontario Geological Survey in 1978 as part of a larger regional mapping program. The resulting Geological Map, No. 2453 (1:100,000 scale) by G.W. Johns, depicts a thick mafic to intermediate volcanic succession centred in St. Laurent and Hurtubise Townships.

Overlying the mafic volcanics to the north is a thick sequence of intermediate to felsic metavolcanic rocks centred in Bradette Township. This mixed volcanic sequence extends westward into southern Noseworthy and northeastern Hurtubise Townships where they abruptly appear to fade out. The more felsic stratigraphy is capped by a thick series of epiclastic and chemically derived metasediments. The sediments directly overlie the mafic volcanic pile in Hoblitzell Township. No major intrusive bodies have been identified as yet in the upper part of the volcano-sedimentary pile on or about the Mikwam property. North of the sediments the terrain is gneissic.

PROPERTY GEOLOGY

The property covers approximately 36 kms of projected westerly strike extension of the Casa Berardi Fault Zone (CBFZ), commencing some 15 kms west of the Golden Pond Au deposits (three zones totalling 11.4 m tonnes at 7.94 g.p.t. Au). In Quebec, the CBFZ is developed within argillaceous sediments in the lower portion of the Taibi Group Domain (Lacroix et al, 1990). Work by Noranda on either side of the interprovincial boundary has traced a sediment-hosted, graphitic conductive zone westward to the Bradette "1-80"- Mikwam boundary (Figure 2 in Cooper, 1990). This zone is locally quartz-veined.

Regionally, both Au and polymetallic VMS (Au-bearing) deposits in the Quebec portion of the Harricana-Turgeon Belt (Lacroix et al, 1990) tend to occur near the intersection of east to northeast-trending transverse structures and east to southeast-trending stratigraphy and/or primary longitudinal structures.

Two deposit types in Quebec occurring at such structural intersections along the CBFZ provide models for exploration on the Mikwam property. Both the Golden Pond (Au) and Estrades (Au-Ag-Zn-Cu-Pb) deposits, although different in terms of mineralogy and host lithology, occur near the western end of adjacent (south) lenses of Cartwright basaltic-komatiitic rocks (Figure 3 in Cooper, 1990).

(4)

1990 DIAMOND DRILL PROGRAM

INTRODUCTION

Diamond drilling commenced September 15 and ended September 30, 1990. Eight holes were drilled for a total metrage of 2,326.3 m with 416.1 m of casing (IT.9% of total - Table 3). Project field supervision was provided by W. Corstorphine with assistance by S. Harding.

A base camp was established at the north end of the Tomlinson Road where the all- weather gravel portion of the road ends. All drill sites were accessed from this point by helicopter. Two drills were utilized during the program and a Hughes 500D helicopter provided the necessary air support. The drilling contractor was Norex Drilling of Timmins and the helicopter, under contract directly to the drill company, was supplied by Nordic Helicopters of La Sarre, Quebec. Both companies provided excellent services during the program.

All drill core from this 1990 drill program is stored in Timmins. Rejects and pulps from the analytical work are currently stored at XRAL Assay Laboratories in Toronto.

The purpose and results of drilling are reviewed separately for each drill hole. Summary logs with best assay results are included with these individual descriptions. In addition, detailed logs for each drill hole are appended. Assay and wholerock certificates for each drill hole are also appended. Jensen plots for wholerock data from each drill hole are included with the appended wholerock data. In addition, a detailed account of the assay results are tabulated and appended under the section "Borsurv Data".

TADPOLE-NOSEWORTHY LAKE AREA TILL ANOMALIES

Section 2550 West - D.D.H, MK-90-1 and MK-90-3

The stratigraphy tested on this section lies between 3496S and 3818S. The interval represented an untested gap in the geology up-ice from overburden holes 84-26, 85-13 and 84-27,85-14. These RC holes carried heavy sulphide concentrations of pyrite and pyrrhotite and in the case of 84-27 highly anomalous gold in their till heavy metal concentrates.

MK-90-l's section contained a major HLEM conductor centred at 3725S. MK-90- 3, 160 m behind 90-1, completed the geological cross section northwards.

D.D.H. MK-90-1

Hole 90-1 encountered deeper than expected overburden (55 m vertical) and almost immediately intersected mineralized volcanic rock. After an initial section of intermediate volcanic a 100 m section of more felsic rock, termed "dacitic", was encountered containing an average of lG-15% semi-massive and massive pyrite. The "dacitic" volcanic is aphanitic

ft l

1990 DDH Locations Figure 3

NORANO^BXPLORATION COiUt

*DRILL SUMMRY PROJECTi 287KIKWAH

TABLE 3 ^Hole Property

MK-90-1 Nfkwam

MK-90-2 Nfkwan

KK-90-3 Mlkwam

NK-90-4 Mlkwam

KK-90-5 Mlkwaa

MK-90-6 M i kwan

MK-90-7 Mtkwem

MK-90-8 Mfkuam

TOTALS

ChargeNo.

287

287

287

287

287

287

287

287

Gridlocation

2550W/36258

1900V/3400S

2550W/34658

1900W/32088

600W/34008

400E/30448

3912E/18958

8400W/mow

Start/Finish

15/9-18/91990

15/9-20/91990

19/9-22/91990

29/9-24/91990

22/9-24/91990

24/9-26/91990

26/9-39/91990

28/9-30/91990

Azimuth

1800G.8.

1800G.S.

18006.8.

18000.8.

18000.8.

1800G.S.

1550

18000.8.

Plunge Casing Final CumulativeDepth Footage

50 73.15 285.3 285.3

50 46.3 325.0 610.3

50 46.3 321.9 932.2

-50 56.1 223.2 1155.4

50 48.1 309.7 1465.1

50 32.3 297.0 1762.1

60 82.3 357.2 2119.3

55 31.5 207.0 2326.3

416.05 2326.3 2326.3(17.9XCasing)

Dip

61122183244

60120180240300

61123183244305

120180

61123183244305

60120180240

61123182244355

60120

Tests

48048470460

"o"53054OH!530

"S

470450440

480460

480470470450460

51'51OSO0480

600580ST0^o560

540510

No. ofSampleTaken

95 Assay11 WR

73 Assay4 WR

42 Assay15 WR

32 Assay5 WR

9 Assay0 WR

32 AssayOWR

39 Assay2UR

69 Assay6WR

391 Assay43 WR

LoggedBy

we

8H

we

8H

we

SK

we

8H

(5)

and pale, buffish grey in colour. The groundmass is massive in appearance. There is an overall fragmental texture to the unit - that of a monolithic, lapilli tuff to microagglomerate (32-64 mm), with pyrite acting as matrix. The fragments are usually moderately to tightly packed (i.e. clast supported). The sulphide-rich sections are matrix supported.

Three principal sections starting at 80.6,112.6 and 133.7 m, respectively, and varying between 7.7 and 10.5 m in drilled width, contained the heaviest sulphide concentrations (3096, 3596 and 6096, respectively). These, particularly the latter two, are the main contributors to the HLEM conductor. The sulphides display primary growth features and laminations characteristic of sediments. The sulphides have a fine-grained silica-rich matrix. Traces of black, graphitic sediment fragments occur in at least one of the main sulphide- rich sections.

Stratigraphy below the dacite pyroclastic consists of a 19.4 m section of more andesitic volcanic and a 29.4 m interval of sediments (siltstone).

A short section of sericite schist (possibly a rhyolite tuff) separates the sedimentary unit from an unusual looking unit hi which the hole was terminated. This bottom unit is a more coarsely textured, porphyritic rock of dark green colour. The colour is due to the chlorite or hornblende content. Quartz and feldspar phenocrysts are abundant (2-496). Fine-grained, lensoid, quartzo-feldspathic patches form much of the remaining identifiable groundmass material. The texture and foliation fabric of this melanocratic dacite unit is somewhat variable, but on the whole it displays a well foliated rock. It is also variably magnetic due to changing magnetite content. There is also weak to moderate development of reddish hematite in the groundmass and in association with fine fractures.

SUMMARY LOG (in meters) BEST ASSAYS

0.0 - 73.5 casing 73.5 - 77.3 andesite 77.3 - 177.3 dacite fragmental/sulphide zone 101.46-102.9

80.6 - 90.7: 3096 smsv py (po) 0.051 ppm Au112.6 - 120.3: 3596 smsv py (po)133.7 - 144.2: 6096 smsv-msv py (po)

177.3 - 196.7 andesite196.7 - 203.4 graphitic argillite (locally conductive) 203.4 - 232.9 siltstone-wacke 232.9 - 242.3 sericite schist 242.3 - 285.3 chloritic dacite porphyry 285.3 end of hole

(6)

The volcanic and sedimentary sections in this hole do not exhibit obvious alteration effects. It is possible that the main "dacite" fragmental unit is pervasively altered in a weak fashion given its slightly beige cast. Several wholerock results indicate little if any carbonatization in the unit.

The melanocratic dacite porphyry at the bottom of the hole is of unusual appearance. It looks to have a significant chlorite or hornblende content based on overall colour but geochemical analysis indicates it is chemically similar to the overlying "dacitic" fragmental. The porphyry also possesses the strongest fabric development of any unit in the hole other than the sericite schist, suggesting perhaps an intrusive origin for the unit.

Secondary structural features such as shears or breccias are absent from the section. Likewise, notable veining and sulphide development exclusive of that found in the dacite is sparse to absent.

The sericite schist unit is chemically equivalent to a dacite or a rhyolite based on SiO2 and TiO2 values from two analysis.

Assay samples from MK-90-1 produced no significant precious or base metal values. The highest gold value was 51 ppb with several more in the 27 to 34 ppb range. All were widely separated. Arsenic was also assayed for; the highest value was 110 ppm with 11 or 12 more greater than 25 ppm. Base metal sampling was intermittent but the upper portion of the sulphide zone which was reasonably well sampled, was distinctly barren.

D.D.H. MK-90-3

Hole 90-3 was set up 160 m behind hole 90-1. The hole intersected intermediate volcanic rocks to a depth of 173.0 m. The more foliated sections are considered tuffs. Within this unit there are several strongly foliated intervals of relatively narrow width. They contain no significant alteration or mineralization.

The remainder of the hole is dacitic in appearance, resembling in colour and grain size the dacite in hole 90-1. Some sections contain moderately well mineralized intervals of up to 2096 semi-massive pyrite and minor pyrrhotite. The better mineralized widths are usually less than 3 m across. The strongest zone occurs at 231.6 m and contains 2096 pyrite over 9.5 m. The main sulphide-bearing section is between 196.9 and 245.0 m but it in no way compares to the sulphide interval in MK-90-1 in terms of the quantity of sulphides.

Wholerock data indicates that in terms of silica and titanium content most of the section drilled by this hole is a silica-rich andesite comparable to the initial unit in hole 90- 1. Titanium values are particularly uniform.

The principal sulphide sections are similar to those in hole 90-1 in that they display a fragmental look with pyrite acting as matrix. They differ principally in width, being much

(7)

narrower than those in 90-1. The bulk of the "dacitic" rock in 90-3, between the sulphide- bearing sections, is more massively structured.


0.0 - 46.3 casing 46.3 - 77.3 andesite 77.3 - 78.2 2096 smsv py, andesite 78.2 - 86.9 dacite/andesite, strongly foliated 86.9 - 120.7 dacite/andesite

120.7 - 121.9 shear zone, andesite, lC-15% diss py 121.9 - 173.0 dacite/andesite, foliated, several qv, minor py

142.0 - 145.5: strongly foliated 173.0 - 196.0 dacite

183.6- 189.1: 596 qv, tr py 196.0 - 199.9 mineralized dacite fragmental, 1596 diss to

smsv py, po199.9 - 203.0 andesite 203.0 - 204.4 dacite/andesite 204.4 - 204.7 mineralized dacite/andesite fragmental, 1596

diss to smsv py 204.7 - 210.15 dacite, andesite (intermixed)

205.6 - 206.3: lS-20% qv, 1096 py208.0 - 209.3: shear, 1096 py

210.15 - 210.8 mineralized dacite fragmental, 2096 smsv py 210.8 - 212.1 dacite 212.1 - 215.2 dacite, 2096 py locally 215.2 - 241.6 mineralized dacite fragmental

215.2 - 231.6: 5-896 diss py locally rare qtz phen231.6 - 241.1: 20% smsv-msv to diss and str py

241.6 - 244.8 dacite (msv), 59fc qv, tr py 244.8 - 245.1 mineralized dacite fragmental, 10-1596 py 245.1 - 250.1 dacite, 596 py

245.7 - 246.2: qv, 1096 py 250.1 - 254.81 fault, minor qv, 10-2096 py 254.81- 279.6 dacite

254.81 - 256.2: breccia, 5-1096 qv270.7 -272.7: breccia

279.6 - 283.0 mineralized dacite fragmental, 1096 diss andstr py, po

283.0 - 321.9 dacite 310.8-312.3305.8-306.6: 1096 qv, trpy 0.02ppmAu312.8 - 313.2: qv, 2096 str py

321.9 end of hole

(8)

No significant alteration effects were noted in 90-3. Weak carbonatization may be present but because of its weakness is difficult to identify.

Notable zones of stress as reflected by shear fabrics are sporadic and narrow in width, e.g. 120.7 to 121.9 m, a shear with lG-15% disseminated pyrite. At 250.0 m there is a 4.7 m fault zone bearing minor quartz and lG-20% pyrite. Neither structure displays hydrothermal alteration effects.

Sulphide mineralization occurs intermittently throughout much of the hole in minor to locally heavy amounts. The most significant is, as has been mentioned, in the "dacite" below 196 m and relates to primary stratigraphic sulphide development.

Veining was not a significant feature of this stratigraphic interval. All individual veins are narrow (less than 10 cm). None exhibited alteration association. Sulphides associated with veins and veinlets ranged from trace to 2096 and occurred mainly in the host rocks.

A 4.6 m section of graphitic argillite hosting quartz-carbonate veinlets and minor sulphides averaged 60 ppb Au (24 to 86 ppm range). Within this same interval a 2.0 m section assay .2792* Zn. A second zinc-bearing graphitic argillite section at 85.6 to 87.1 m assayed .339fc Zn with slightly elevated gold (110 and 31 ppb). These values are not considered significant, particularly the zinc, given the nature of the host rock.

Section 1900 West - D.D.H. MK-90-2 and MK-90-4

The section of stratigraphy that was designated for drilling on this line lay in an up- ice direction from a "HMC" till anomaly in RC hole 85-11 and an anomalous gold in till anomaly in RC hole 84-25.

MK-90-2 was positioned so as to intersect a strong HLEM conductor with coincident mag centred at 3585S. This conductor was interpreted as the on-strike continuation of the conductor tested by MK-90-1,650 m to the west on Line 2550W. The section's second hole, MK-90-4, was collared 200 m behind 90-2. The two holes totalled 548 m with 102.4 m, or IS.7%, being casing. In vertical projection 350 m of stratigraphy was drilled. Hole 90-4 had to be aborted due to heavy sanding at 223 m, and ended 77 m short of its proposed depth. This shortfall in depth has left a 72 m vertical gap between the two holes.

D.D.H. MK-90-2

Hole 90-2 collared into an andesite unit which becomes progressively more intermixed with argillite as its lower contact is reached at 86.4. The volcanic is largely tuffaceous and the argillite is dark and weakly graphitic. Below the andesite the sediments are greywackes, with interbanded graphitic argillite in the upper part of the unit and two greenish, chloritic zones in the central part.

(9)

Between 216.5 and 272.4 m siliceous, oxide iron formation predominates. The I.F. is unusual in that there is a strong glassy quartz component that resembles more a quartz vein-type of material than chert. There are chert beds as well, and laminae of fine-grained magnetite. Heavy pyrite/pyrrhotite mineralization (up to 3096) is also intermixed in with silicates and oxide components. The remaining lithotype in the I.F. is a chloritic argillite- wacke.

Graphitic argillite, well veined with 1596 quartz-carbonate stringers and 10-1596 pyrite-pyrrhotite, immediately underlies the iron formation for 25.6 m. The hole ends in an interbedded unit of greywacke and graphitic argillite with minor disseminated pyrite/pyrrhotite.

SUMMARY LOG (in meters)

0.0 - 46.3 casing46.3 - 63.5 andesite tuff63.5 - 66.2 interbedded argillite, andesite tuff66.2 - 75.7 andesite tuff75.7 - 86.4 interbedded andesite tuff, argillite (gf)

86.4 - 93.5 graphitic argillite

BEST ASSAYS

93.5 - 98.4

98.4216.5

223.4229.4

216.5223.4

229.4272.4

graphitic argillite, greywacke

greywacke, loc chloriticiron formation, 7096 qtz + cht, 3%magnetite lam, lS-20% py, po, 7-1296 sedgreywackeiron formation229.4 - 238.0: 6096 qtz * cht, 1096 magnetite

lam, 10-1596 py, po, lS-20%cbl sed

238.0 - 252.0: 4096 qtz, 3096 cbl sed, 1296596 magnetite lam, 1396 py, po

252.0 - 265.0: 1596 qtz, 3596 cbl sed, 3596 cht,1396 magnetite lam, 296 py,po

265.0 - 272.4: 2596 qtz, 35-6096 cbl sed, 5-3096py, po locally, 596 magnetitelam, 596 cht

85.6-86.3: 0.11 ppm Au 85.6-87.1: 3335 ppm Zn 89.6-93.5: 0.06 ppm Au 90.6-92.6: 2705 ppm Zn 96.4-97.4: 0.141 ppm Au, 15 ppm As

230.7-236.5: 0.3 ppm Au

238.0-244.0: 0.29 ppm Au

(10)

SUMMARY LOG (in meters) cont'd. BEST ASSAYS

272.4 - 298.0 graphitic argillite, 1596 qtz-carb str, 272.35-280.8: locally heavy py, po, 10-1596 overall 0.091 ppm Au

282.8-284.5: 0.74 ppm Au 289.0-290.8: 0.15 ppm Au

298.0 - 325.0 interbedded greywacke and graphitic argillite(50/50)

325.0 end of hole

The HLEM anomaly is attributed to the heavy sulphide zones in the iron formation.

There are no readily identifiable occurrences of hydrothermal alteration in the hole. The 1596 quartz-carbonate veining with 10-1596 total sulphide at 272.4 m is the most notable zone of veining and increased sulphide content in any non-iron formation lithology.

No fault or shear structures of significant scale or intensity were observed in the section.

An abrupt change is noted in the character of the conductor and the nature of the host rock between Line 2550W and Line 1900W, a distance of only 650 m - pyrite hosted by dacitic pyroclastic rocks vs sulphide-quartz-chert-magnetite iron formation hosted by clastic metasediments.

Assay results were low in the hole except for two intervals in the iron formation which were found to be anomalous in gold. One 5.8 m section from 230.7 to 236.5 assayed 0.33 ppm Au while another of 6.0 m, from 238.0 to 244.0, assayed 0.29 ppm Au. The two sections lacked any distinctive features that would alert the logging geologist to possibly expect anomalous gold values. These two assay intervals were the best obtained in the drilling program. The elevated zinc assays present in the hole are attributed to the graphitic component in the host and are not considered significant.

D.D.H. MK-90-4

Spotted 190 m north of 90-2, hole 90-4 intersected intermediate volcanic stratigraphy. The initial 154 m was interpreted as being more andesitic while the bottom portion was considered more felsic. Wholerock results indicate however that in terms of silica (SiO2) content, there is little change through the entire section and that the rock is of dacitic affinity. TiO2 values were also quite uniform with the exception of one sample; and based on this immobile element the section is more andesitic (the exception was one "dacitic" value). The silica and titania from this section are very similar to those from hole 90-4.

(11)


0.0 - 56.1 casing 56.1 - 154.0 andesite, scattered, narrow qv with tr pb

113.4 - 122.0: 2596 carbonate str, tr py,well foliated

154.0 - 223.2 dacite volcanic171.5 - 178.3: shear zone, weak carbonate 175.2-176.1:+ sericite, 596 diss py, minor qv 0.07 ppm Au183.1 -184.2: breccia, 2096 carb str,minor qtz, tr py, po194.6 - 200.0: weak shear zone, weak carb+ sericite, 3% diss to str py210.7 - 213.2: weak shear zone, S-10%qtz-carb str, 1096 diss py214.2 - 223.0: 1096 diss and str py, 396 po 215.2-216.7:

18 ppm As 223.2 end of hole

Signs of hydrothermal alteration were restricted to weak carbonate-sericite alteration in two shear structures noted in the summary log. In these locations and elsewhere, in both the upper and lower litho-units, increased concentrations of carbonate and carbonate-quartz stringers occur in several locations. The occurrence of the weak shear at 210.7 m and a nearby interval of 1096 disseminated and stringer pyrite from 214.2 to 223.0 m represents the widest zone of vein and sulphide mineralization in the hole.

Assay results were low throughout the section. The highest gold was an isolated 70 ppb; the best arsenic was 18 ppm.

"85-B8 AREA" (NOSEWORTHY LAKE AREA)

D.D.H. MK-90-5

Drill hole MK-90-5 tested a section of stratigraphy 200 m east-southeast of drill hole 85-B8 which carried two closely spaced anomalous gold intersections of 1.1 g.p.t/1.25 m and 1.52 g.p.t./O.SS m in epiclastic sediments. The zones occur in a breccia quartz vein stockwork with 3-5 96 pyrite-pyrrhotite. Anomalous gold and arsenic was also encountered 250 m south of hole 85-B8, in till samples from RC hole 84-22. MK-90-5 sectioned 179 m of stratigraphy between 3432S and 361 IS.

Hole 90-5 intersected a continuous, unbroken section of siltstones, greywacke and argillite. Fine-grained, siliceous sediments of black to dark grey colour dominate the section. They are separated from an initial argillite unit by 45 m of greywacke.

(12)

i


0.0 - 48.1 casing48.1 - 70.0 graphitic argillite and interbedded greywacke 70.0 - 116.8 greywacke and interbedded argillite

74.6 - 80.0: brittle fault zone98.2 - 101.6: 4096 graphitic argillite

116.8 - 169.7 argillaceous siltstone163.37 - 167.9: local breccia with qtz veinlets 163.3-164.5:

0.02 ppm Au169.7 - 171.8 graphitic argillite 171.8 - 178.8 siltstone-wacke 178.8 - 309.7 siliceous siltstone-wacke

189.4 - 192.7: minor qv193.9-211.5: local breccia with qv 210.3-211.6:

191 ppm As 309.7 end of hole

The hole contained very little of interest. Breccias with some quartz veinlet matrix material occur at two locations but hydrothermal alteration effects, such as carbonatization, show no real signs of development here or anywhere else in the drill hole. Sulphides are sparse and never attained more than the normally expected background concentrations.

The section bore no signs of containing or being proximal to a high stress area except for the brittle breccia structures already mentioned.

Only 7.35 m of sampling was undertaken in this hole. Gold values were low and only one arsenic value from 210.3 m in a breccia zone was slightly anomalous at 191 ppm.

Section 400 East - D.D.H. MK-90-6

The small untested gap in stratigraphy tested by hole MK-90-6 is 600 m northeast of RC hole 84-20 which contained some anomalous arsenic, precious, and base metal concentrations. With the completion of hole 90-6, a continuous stratigraphic profile now exists between 2950S and 3450S on Line 400E.

As with MK-90-5, this hole intersected a continuous sequence of coarsely interbedded argillites and greywackes. Occasionally there will be a slight greenish, chloritic cast to the sediment, otherwise they are grey to black in colour.

A number of narrow quartz veins (-c 10 cm) with trace to 89fc pyrite-pyrrhotite and occasional carbonate or sericite, occur locally in the section but none show significant pervasive hydrothermal alteration effects.

(13)

The shear zone centred at 260.0 to 262.7 m is the singular most significant structure in the hole. Its low 10 degree core angle extends the related fabric envelope considerably in the hole - 255.4 to 288.0 m.


0.0 - 32.0 32.0 - 160.5

160.5

181.6

201.5

255.4

288.0

181.6

201.5

255.4

288.0

297.0

casinginterbedded argillite and greywacke - minor qvand associated carb and sericite alteration106.5 - 110.0: graphitic argillitegreywacke, minor interbedded argillite andsiltstoneargillite with interbedded greywacke andsiltstonegreywacke with interbedded argillite andsiltstoneshear zone in greywacke260.0 - 262.7: main shear, 10s, S-15% diss pygreywacke with interbedded argillite andsiltstone, locally sheared, lS-20% qtz-carbveinlets, S-15% py, po

Average: 0.179 ppm Au/5.2 m

291.8-292.8: 0.14 pp, Au 292.8-293.6: 0.15 ppm Au 293.6-294.8: 0.29 ppm Au 183 ppm As 294.8-296.0: 0.02 ppm, Au 192 ppm As 296.0-297.0: 0.28 ppm Au 193 ppm As

The strongest shear interval at 255.4 to 288.0 m was assayed between 259.4 and 263.0 m. It contained no anomalous values. The section of locally sheared and quartz-carbonate veined sediment between 288.0 and 297.0 m (end of hole) carried increasingly anomalous amounts of both gold and arsenic with the 291.8 to 297.0 interval being the most elevated in both elements.

Newmont's 85-B2, immediately in front of 90-6, also encountered an interval of deformation which probably correlates to the zone in 90-6. Correlation would necessitate a steep northward dip of about 80 degrees which approximates lithological dips in the area. The low core angles in 90-6 may reflect localized deformation fabric more than the dip of the larger scale structure it is part of.

O*)

Sampling in hole 85-B2 tended to be specific to an individual feature, consequently numerous unsampled gaps occur in the upper part of the hole. No significant assays were reported (highest Au - 59 ppb; arsenic - 60 ppm).

"85-A8 AREA"

Section 3912 East - D.D.H, MK-90-7

D.D.H. MK-90-7

This additional hole in the A8 area probed for an eastward rake extension of the A8 mineralization. Hole 86-8 suggested a possible trend to the east with intersections of 2.14 g.p.t. Au/4.8 m and 4.29 g.p.t. Au/2.5 m. MK-90-7 was collared at -60" and drilled on a 1650 azimuth to a depth of 357.2 m.

Overburden was particularly deep at 70 m vertical. The initial 87 m produced a uniform section of dacitic tuff. The last 10 m are graphitic reflecting proximity to the underlying graphitic argillites. The thick graphitic argillite (187.3 m cored) is a very uniform unit. Both lithologies contain a number of narrow shear zones and a thin massive pyrite lens occurs at 159.85 m, near the contact between the two units.


0.0 - 82.6 casing 82.6 - 159.1 dacite tuff, locally strongly foliated to sheared

120.5 -128.0: shear zone, 1096 qtz-carbveining, 1-296 py131.1 - 133.0: weak breccia, 596 py143.0 - 144.3: shear zone, minor qtz, tr py145.7 - 148.5: shear zone, minor qtz, tr py

159.1 - 169.7 graphitic dacite tuff159.85 -161.0: 8596 msv py 159.8-161.0:

0.2 ppm Au 144 ppm As

161.45 - 162.05: sericitic 169.7 - 324.3 argillite, locally graphitic

179.4 - 192.9: graphitic, 596 diss py198.2 - 207.1: graphitic, 5-896 eg py, localfault gouge214.8 - 248.2: graphitic, 5-1096 qtz-carb str,3-596 py257.2 - 307.6: graphitic, 10-1596 qtz-carb 299.8-300.8:associated with thin shear structures 0.07 ppm Au

14 ppm As

(15)


309.0-319.8: graphitic324.3 - 352.5 graphitic argillite

330.8 - 331.8: shear, 2096 qtz, Wo py338.5 - 340.1: shear, 509& qtz, t-2% diss py341.4 - 342.0: shear + qtz, 5% py )344.1 - 344.7: shear, S-8% qtz, 5% py348.7 - 352.5: shear (contorted)

352.5 - 357.2 argillite-wacke357.2 end of hole

The dacite unit exhibits a moderate to strong structural fabric throughout. Several intervals actually display very strong shearing effects but any associated vein and sulphide mineralization is only weakly developed. The unit gives some suggestion of a weak pervasive carbonate alteration but it is only weakly developed if present at all. Wholerock information does not indicate significant carbonatization.

In the sediments there are a number of narrow quartz and quartz-carbonate veinlets 1-10 cm wide associated with small, isolated shears - the widest is 1.5 m at 338.5 m. A weak ankeritic alteration may be present in this unit also but it is very poorly defined if present.

The overall lack of more pervasive shear structures, mineralization and carbonatization indicates the mineralized A8 zone has not been intersected. This is also reflected directly in the assay results which are low. The highest gold and arsenic at 0.2 ppm and 144 ppm, respectively, occurred in the massive sulphide band at 159.85 m.

The intersection of volcanic stratigraphy in this hole was not anticipated. Wholerock data suggests the volcanic dacite encountered in this hole corresponds to dacites belonging to a stratigraphic interval well north of the A8 Zone. This suggests, in turn, that the A8 stratigraphy and the associated mineralization of interest is further to the south than expected.

BRADETTE TOWNSHIP EM CONDUCTOR

Section 8400 West - D.D.H. MK-90-8

D.D.H. MK-90-8

Hole 90-8 tested a conductor and its enclosing stratigraphy for indications of Casa Berardi-type structure, alteration and/or mineralization. The favourability of this northern terrain is reflected in its proximity to conductive trends that can be traced from the Casa Berardi Area.

(16)

The hole collared into mafic volcanic rocks and remained in them to termination. A sulphide-bearing section between 77.7 and 104.8 m averaged 596 sulphides (po/py). The sulphides occurred as narrow semi-massive lenses and stringers of both pyrite and pyrrhotite. The local concentrations of sulphide were sufficient to produce a conductor.

The volcanic displays a strong foliated fabric throughout. Significant carbonate veining primarily parallel to the foliation and the presence, m several places, of pervasive carbonatization imparts a distinctive white, marbled look to the unit. The alteration tends to discolour the dark green volcanic to a paler, buffish colour. Only one section from 117.2 to 169.2 m carried little or no veining otherwise there is a consistent 10-2096 flooding of this material in the hole. Pyrite and pyrrhotite concentrations, exclusive of the conductive section, were low except for several isolated intervals of up to 3 m which contained up to 10 or 1596 sulphide. No arsenopyrite was observed. The best section of ankerite alteration occurred from 189.7 to 201.0 m. The heaviest section of veining occurred at the bottom of the hole at 201.0 to 207.0 m. The strongest fabric - a shear banding was located in the 169.5 to 189.7 interval.


0.0 - 31.531.5 - 65.565.5 - 77.7

77.7 - 104.8

104.8 - 117.2

117.2 - 128.2

128.2 - 169.5

169.5

189.7

201.0

207.0

189.7

201.0

207.0

casingbasalt, 1096 qtz-carb v, 596 qtz v, strong fabricbasalt, weakly carbonatized groundmass,strong foliationsulphide zone in basalt, lG-15% qtz/qtz-carb v,1096 py, 5-896 po (596 smsv o.a.), weakcarbonatizationbasalt, strong fabric, 5-896 qtz-carb v, 596 disspo. py108.1 - 109.1: 109& po, 596 pybasalt, strong fabric, chloritic121.6 - 125.0: chlorite-rich, 10-1596 po, py,some qvbasalt, strong fabric, 596 smsv, po, py as thin 136.1-136.8:lenses 0.041 ppm Au139.5 - 142.0: 1096 diss po 136.1-141.0:

0.4996 Zn 150.1-151.7: 915 ppm Zn

basalt, strong fabric, chloritic, 209& qtz/qtz- carb str, shear bandedbasalt, moderately carbonatized, 10-1596 qtz-carb str194.7 - 194.8: qv, 196 po, tr cpybasalt, strong fabric, chloritic, 1096 diss po, py,2596 qtz-carb strend of hole

(17)

The basalts in this hole display the most sustained interval of moderate to strong deformation seen in the 1990 drilling program. The intensity of deformation in the 169.5- 189.7 interval has been sufficient to produce shear banding in the rock. Locally pervasive ankerite alteration and quartz-carbonate veining serve to accentuate this fabric.

Assay results were low with only one gold assay marginally above normal background concentrations - 41 ppb at 136.1 to 136.8 m. Arsenic was also low with the highest being 16 ppm. A slightly anomalous zinc assay of Q.51% across 1.3 m came from two contiguous samples starting at 136.1 m.

FUTURE WORK

A detailed budget for 1991 work has not yet been finalized, however it is planned to continue diamond drilling on the Mikwam property. Exact drill site locations have not yet been finalized.

(18)

REFERENCES

Cooper, P., 1990

Data Review and Exploration Proposal, Mikwam Property, Noranda Exploration Company Ltd. (internal report)

Lacroix, S., Simard, A., Pilote, P. and Dube, L. (1990)

Regional Geologic Elements and Mineral Resources of the Harricana-Turgeon Belt, Abitibi of NW Quebec in C.I.M.M. Spec. Vol. 43, May, 1990

Corstorphine, W. (January, 1991)

Report on 1990 Mikwam Diamond Drilling - Noseworthy and Bradette Townships, Ontario for Noranda Exploration Company Limited (NPL), Pamour Exploration and Freewest Resources Inc., Larder Lake Mining Division, District of Cochrane (internal report)

Established 1928

dwastiKa Laboratories lA Division of As&ayers Corporation Ltd. f OCT g joan

Assaying - Consulting - Representation. NORANDA i

Geochemical Analysis Certificate

compuy: NORANDA EXPL. CO. LTD.Project; 287Alta: P. COOPER

OT-0576-RG1

D-e: SEP-26-90Copy l. P.O.BOX 1205, TIMMINS, ONT. P4N 7JS

2. FAXTO26S-9572

We hereby certify the following Geochemical Analysis of 42 CORE samples submitted SEP-21-90 by WAYNE CORSTORPHINE.

Sanople Number90301 90302 90303 90304 9030590306 90307 90308 90309 9031090311 90312 90313 90314 9031590316 90317 90318 90319 9032090321 90322 90323 903249040190402 90403 90404 90405 90406

Au Au check As ppb ppb ppm

1 10 17 34 1411 1

101 71

14 14 17

7

73 1

27 10

110 106

Certified by

Cu ppm37 122 58 40 3971 48 27 50 2474 18 40 22 4139 35 30 37 2451 28 61 303957 29 75 36 190

AT

Zn ppm202 \ 100 249 162 128143 235 230 142 7885 121 349 244104 J394 157 292 136 304105 1 107 173 110 t242 ]164 73

361 374 3490 ,

411

-

> MK-90-1

> MK-90-2

G. Lebel l Manager

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705)642-3244. FAX (705)642-3300

Established 1928

A Division of Assayers Corporation Ltd.

Assaying - Consulting - Representation


Page 2 of 2

OT-0576-RG1

Company: NORJProject: 287

VNDA EXPL. CO. LTD. Da*. SEP-ZD-90Copy 1 . P.O.BOX 1205, TIMMINS, ONT. P4N 7JS

Ann: P. COOPER

We hereby certij submitted SEP-2

SampleNumber904079040890409904109041190412904139041490415904169041790418

y the following Geochemical Analysis .1-90 by WAYNE CORSTORPfflNE.

Au Au checkPPb ppb

3114

1247586 79515162

14121

1

2. FAXT026S-9S72

of 42 CORE samples

As Cuppm ppm

314351242

1171632202411601283044

Znppm

3200 ^6844

120631

2890 l M K. Q 0-22520 ' MK 90 2

359635109233130 J

Certified by.

G. Lebel l Manager


1928


Assaying-Consulting-Representation

Geochemical Analsis Certcate

Company:Project:Attt:

NORANDA EXPL. CO. LTD.TAD

SEP-26-90Copy l. P.O.BOX 1205, TIMMINS. ONT. P4N 7JS

2. FAX TO 20-9572

We hereby certify the following Geochemical Analysis of 25 CORE samples submitted SEP-24-90 by .

MK-90-1

Sample Nunfcer5801 5802 5803 5804 580586881 86882 86883 86884 8688586886 86887 86888 86889 8689086891 86892 86893 86894 8689586896 86897 86898 86899 86900

Au As ppb ppm

1 17 14

34/27 714 1

27 17 1010 27

1 51

11 1

10 1

3/11 11 7 1

j

PCertified by.

O. Lebel 7 Manager


j

f

j Established 1928

juauuiaiuij cs "-~A Division of Assayere Corporation Ltd.

Assaying- Consulting - Representatio:

Assay Certificate

'^CT 11 1990n

NORANDA EXPL. CO. LTD. Dtte: OCT-05-90Project: TAD Cbpy 1 . P.O.BOX 1205, TIMMINS, ONT. P4N 7J5 Ann: 287 2 - FAXT026S-9572

We hereby certify the following Assay of 45 CORE samples submitted SEP-27-90 by .

Sample Au Au Au check Au check As Number g/tonne oz/ton g/tonne oz/ton ppm90325 90326 90327 90328 9032990330 90331 90332 903429041990420 90421 90422 90423 9042490425 90426 90427 90428 9042990430 90431 90432 90433 9043490435 90436 90437 90438 90439

0.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.010.010.01 0.01 0.01 0.01 0.010.01 0.33 0.18 0.53 0.160.04 0.44 0.36 0.24 0.120.06 0.08 0.01 0.06 0.18

.001

.001 0.01 .001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.010

.005

.015 0.41 .012

.005

.001

.013

.011 0.27 .008

.007

.004

.002

.002

.001

.002

.005 0.26 .008

7 s 11 9 6 22 1

10 ,

\ MK-90-1

51 ^ 6 21

12 7

10 14 52

13 14 3

146

1211 )

t MK-90-2

Certified by

G. Lebel l Manager

P.O. Box 10, Swastika, Ontario POK TO Telephone (705)642-3244. FAX (705)642-8300

l Established 1928

o w a s UK aA Division of Assayera Corporation Ltd.


Assay Certificate

Page 2 of 2

OT-0599-RA1

Company: NUKJProject: TADAnn:

We hereby certi)submitted SEP-S

SampleNumber904409044190442904439044490445904469044790448904499045090451904529045390454

UNDA bAJTL,. IAJ. L li). otto: VA;IHD-WCopy i . P.O.BOX 1205, TIMMINS, ONT. P4N 7J5

2. FAXT026S-9572

V the following Assay of 45 CORE samples17-90 by.

Aug/tonne

0.080.050.030.010.010.010.030.040.030.080.020.050.010.040.12

Au Au checkoz/ton g/tonne

.002

.001

.001

.001

.001

.001

.001

.001

.001

.002 0.11

.001

.001

.001

.001

.004 0.11

Au check Asoz/ton ppm

10 -i1

CI<l132

*:l58

.003 1413161411

.003 15 ;

* MK-90-2

Certified by.

O. Lebel 7 Manager


-C

p

k Established 1928


Assaying - Consulting - Representationli 1990

NOR/.N7 "-ORATICJJ

Assay Certificate OT-0600-RA1

Company: NORjProject: TADAnn: ^g^.

We hereby cenijsubmitted SEP-:

SampleNumber904559045690457904589045990460904619046290463904649046590466904679046890469904709047190472904739047490475904769047790478904799048090481904829048390484

\NDA EXPL. CO. L

y the following Assayr?-90by.

Aug/tonne

0.090.130.100.010.090.110.200.080.070.010.020.010.210.080.010.010.010.030.010.010.010.020.010.010.010.010.010.010.010.01

TD.

of SI CORE samples

Au Au checkoz/ton g/tonne

.003

.004

.003

.001

.003

.003 0.14

.006

.002

.002

.001

.001

.001

.006 0.15

.002

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.01

.001

.001

.001

.001

.001

.001

Dele: OCT-Q5-90Cbpy 1. P.O.BOX 1205. TIMMINS, ONT.P4N7J5

2. FAX TO 26*4572


14 ^16119

.004 41499122

.004 1 CI

11222 J1 1

^l ci CI

.001 *a d j

i^i4\ c

f

* MK-90-2,

' MK-90-4

Certified by.

G. Lebel l Manager


^fcsstablished 1928

Assay Certificate



Page 2 of 2

OT-0600-RA1


Company:Project:Ann:

We hereby certify the following Assay of 51 CORE samples submitted SEP-27-90 by.

Dtte:Copy 1. P.O.BOX 1205, TIMMINS, ONT.P4N7J5

2. FAX TO264-9572

Sample Number90485 90486 90487 90488 9048990490 90491 90492 90493 9049490495 90496 90497 90498 9049990500 90501 90502 90503 9050490505

Au g/ tonne

0.01 0.01 0.01 0.01 0.010.07 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01

Au Au check Au check oz/ton g/ tonne oz/ton

.001

.001

.001

.001

.001

.002 0.14 .004

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.01 .001

.001

.001

.001

.001

.001

As ppm

^ 1 1

31

i 1

i

2 184 ,

> MK-90-4

Certified by.

O. Lebel 7 Manager

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244. FAX (705)642-3300

Established 1928



Assay Certificate

NORANDA EXPL. CO. LTD.

*-.-/

OCT ir 1990

CO. LTD.

Dtte: OCT-10-90Project: TAD Copy 1 . P.O.BOX 1205. TIMMINS, ONT. P4N IK Ann: Z&l 2 - FAXTO26ft-9S72

We hereby certify the following Assay of 67 CORE samples submitted OCT-01-90 by .

Sample Au Au Au check Au check As Nunober g/ tonne oz/ton g/tonne oz/ton ppm90333 90334 90335 90336 9033790338 90339 90340 90341 9034390344 90345 90346 90347 9034890349 90350 90351 90352 9035390354 90355 90356 90357 9035890359 90360 90361 90362 90363

0.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.02 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.02 0.01

.001 0.01 .001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.01 .001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.02 .001

.001

15 8 6

10 9

15 IS 10 10 33 8

18 2 MK-90-1

18 18 3

2 4 5 3 11

3 2

Certified by

O. Lebel l Manager


1928



Assay Certificate

NORANDA EXPL. CO. LTD.

Page 2 of 3

OT-0611-RA1

Date: OCT-10-90Project: TAD Copy 1 . P.O.BOX 1205, TIMMINS, ONT. P4N 7J5 Alta: 2. FAXTO26S-9572


Sample Au Au Au check Au check As Number g/tonne oz/ton g/tonne oz/ton ppm90364 90365 90366 90367 9036890369 90370 90371 90372 9037390374 90375 90376 90377 9037890379 90380 90381 90382 9038390384 90385 90386 90387 9038890389 90390 90391 90392 90393

0.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.01

.001

.001

.001

.001

.001

.001

.001

.001 0.01 .001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.01 .001

.001

.001

.001

.001

.001

.001

.001

16 1 8 2 22 j1 '1

1 1

CI1

1

2

16 J

MK-90-1

> MK-90-3

Certified by.

G. Lebel 7 Manager


jLaooraionesA Division of Assayers Corporation Ltd.

wished 1928 Assaying - Consulting - Representation

Page 3 of 3 Assay Certificate OT-0611-RA1

Company: NORANDA EXPL. CO. LTD. Date: OCT-10-90Project: TAD Copy 1. P.O.BOX 1205. TIMMINS, ONT. P4N 7JSAlta: 2. FAX TO 26*9572


Sample Au Au Au check Au check As Nunber g/tonne oz/ton g/tonne oz/ton ppm90394 0.01 .001 290395 0.01 .001 290396 0.01 .001 5 MK-90 390397 0.01 .001 9 M 90~390398 9:9!......:9?L. ?96399""" """""""""6"6r"""66r""""""""""""""""""""6"""""""""*"""90400 0.01 .001 l

3

Pl

Certified^

O. Lebel f Manager


j

f

JSwastiKa Laboratories lP Established 1928

A Division of Assayere Corporation Ltd.

Assaying - Consulting - Representationj?

NOrUNfMD:?1.c?-.TIC

Assay Certificate

NORANDA EXPL. CO. LTD.TADZB?


FWjccfc

OT-0612-RA1

Date: OCT-10-90Copy l. P.O.BOX 1205, TIMMINS. ONT. P4N 7J5

2. FAXT026S-9572

Sample Nonfcer90506 90507 90508 90509 9051090511 90512 90513 90514 9051590516 90517 90518 90519 9052090521 90522 90523 90524 9052590526 90527 90528 90529 9053090531 90532 90533 90534 90535

Au g/ tonne

0.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.01 0.010.01 0.01 0.01 0.04 0.010.01 0.01 0.01 0.01 0.040.03 0.04 0.14 0.15 0.29

Au Au check Au check oz/ton g/ tonne oz/ton

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.01 .001

.001

.001

.001 0.01 .001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.07 .002

.001

.004 0.24 .007

.004

.008

dCertifiedby ^A/ -

As ppm10 14 8 2 61 1 5 6 102 1 2O MK-90-6

1

1

1

8 1 3 1

183

mG. Lebel l Manager


f


[Establish 1928 Assaying - Consulting - Representation

Page 2 of 2

Assay Certificate OT-0612-RA1

NORANDA EXPL. CO. LTD. o** OCT-10-90Project: TAD Copy l- P.O.BOX 1205.TIMMINS.ONT.P4N7J5 Att.: 2. FAXT0268-9572


Saqple Au Au Au check Au check As Nunober g/tonne oz/ton g/tonne oz/ton ppm90536 0.02 .001 129 uK-fto-a90537____________0.28 .008 _____ _____19399610 0.02 .001 0.01 .001 15 MK-90-590611OI U5I 3 uirwn90612_____________0.01 .001__________________^ MK-90-190613 0.02 .001 2 MK-90-5

l

j

l

l

J Certified by_

O. Lebel l Manager

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244 FAX (705)642-3300

swastika Laboratories "~A Division of Assayers Corporation Ltd. j

jCf Assaying - Consulting - Representation,

Assay Certcate

Company: NOKA1NUA EXFL. CO. LTD. Date: OCT-17-90 Project: TAD Copy 1 . P.O. BOX 1205, TIMMINS, ONT. P4N 7JS Attn: P. COOPER *2S? ( 2. FAX TO 268-9572

We hereby certify the following Assay of 29 CORE samples submitted OCT-02-90 by W. CORSTORPfflNE.

Saonple Au Au Au check Au check As Nuoober g/tonne oz/ton g/tonne oz/ton ppm90601 90602 90603 90604 9060590606 90607 90608 906099061490615 90616 90617 90618 90619906209062190622 90623 9062490625 90626 90627 90628 9062990630 90631 90632 90633

0.01 0.01 0.01 0.01 0.010.02 0.01 0.02 0.010.010.01 0.01 0.01 0.01 0.010.010.010.01 0.01 0.010.01 0.01 0.02 0.01 0.010.01 0.01 0.01 0.20

.001

.001

.001

.001

.001

.001

.001

.001

.001

.001 0.01

.001

.001

.001 .001 .001.001.001 0.01.001 .001 .001.001 .001 .001 0.01 .001 .001.001 .001 .001 .006 0.20

^ "i *tt*C1 CI

1 CI CI CI

2.001 14 \

6 171112

1915 )

> MK-90-3

> MK-90-5

.001 ^ MK-90-3^ *| ^

1 Ci

1 .001 *C1

^ CI

^ 1

CI .006 144 ,

* MK-90-7

Certified by^

O. Lebel /Manager

P.O. Box 10, Swastika, Ontario POK1TO . Telephone (705) 642-3244. FAX (705)642-3300

I Established 1928



Certificate OT

Compuy:Project:Attn:

NORANDA EXPL. CO. LTD.TAD287


SampleNuraber905389053990540905419054290543905449054590546905479054890549905509055190552905539055490555905569055790558905599056090561905629056390564905659056690567

Au Au Au checkg/tonne oz/ton g/tonne

0.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.02 .001 0.010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .0010.01 .001 0.010.01 .0010.01 .0010.01 .001 0.010.01 .0010.01 .0010.01 .001

Dtfe: OCT-10-90Copy 1 . P.O. BOX 1205, TIMMINS, ONT. P4N 7J5

2. FAXT026S-9572

MK-90-8


1^l^^l^

288

151516

.001 410

83

414141

241

542

.001 4111

.001 4141

98

Cuppm

12611014511339210472

119254320294590209

4460

14125412377

346425112120

Znppm

244131124160727372188133276240219204213154151172217164198214342176107

Certified by.

G. Lebel l Manager


1928



Assay Certificate

Company:Project:Attn:



Page 2 of 2

OT-0628-RA1

Due: OCT-10-90Copy 1. P.O. BOX 1205, TIMMINS. ONT. P4N 7J5

2. FAXT0268-9S72

MK-90-8

Sample Number90568 90569 90570

Au g/ tonne

0.01 0.01 0.01

Au oz/ton

.001

.001

.001

Au check g 1 tonne

Au check oz/ton

As ppm

6 6 2

Cu ppm187 148

Znppm155 143

j

PCertified fy

G. Lebel l Manager


Established 1928

.' A Division of Assayers Corporation LW.


j

f

Geochemical Analsis Certcate

NORANDA EXPL. CO. LTD.TADProject-

Page l of 2

OT-0630-RG1

Date: OCT-10-90Cbpy 1. P.O. BOX 1205, TIMMINS, ONT.P4N7J5

2. FAX TO 268-9572

W* te/efry cem# the following Geochemical Analysis of 36 CORE samples submitted OCT-04-90 by .

MK-90-8

Sanple Nnfcer90571 90572 90573 90574 9057590576 90577 90578 90579 9058090581 90582 90583 90584 9058590586 90587 90588 90589 9059090591 90592 90593 90594 9059590596 90597 90598 90599 90600

Au ppb

1 1 1

10 11 31 1

41/483 7 10 1 71

14 7 3 141 I 1 3

3/11 1 1

1/1 1

As ppm

4 9 15

1 ^•CI 9 3 118 2 5 6 42 15 15 6 53 ^ ^ •CI 2

•CI 2 3 ^ •Ci

Cu ppm

547142 263 161 418 152190 149 148 44

78 97 90

Zo ppm

6590,3250 243 166 914 10998 876 955 76

163 127 112

Certified by

G. Lebd l Manager

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 64^3244. FAX (705)642-8300

swastiKa LaooratonesA Division of Assayere Corporation Ltd.

' Consulting - RepresentationEstablished 1928Page 2 of 2

Geochemical Analysis Certificate OT-0630-RG1

comply: NORANDA EXPL. CO. LTD. D*e: OCT-10-90Project TAD Cbpy l . P.O. BOX 1205, TIMMINS, ONT. P4N IKAnn: 2. FAX TO 26S-9S72

We hereby certify the following Geochemical Analysis of 36 CORE samples MK-QO-B submitted OCT-04-90 by .

Sample Nmober90670 90671 90672 90673 9067490675

Au ppb

1 11 1 33

As ppm

2 9 2 ^ 3

•c:l

Cu ppm119

173200

Zn ppm88

110108

Certified ty^

G. Lebel l Manager


V.A.JLVV+ a^tf W C/V 4. V+V

A Division of Assayers Corporation Ltd.'A AVWT

established 1928 Assaying - Consulting - RepresentationJCT 49 1990


Company:Project:Ana:

NORANDA EXPL. CO. LTD. Date: OCT-18-90Copy l. P.O.BOX 1205, TIMMINS.ONT. WN 7J5

2. FAX TO 268-9572

WP terety c*rt#y the following Geochemical Analysis of 27 CORE samples submitted OCT-10-90 by .

MK-90-7

Sample Number90634 90635 90636 90637 9063890639 90640 90641 90642 9064390644 90645 90646 90647 9064890649 90650 90651 90652 9065390654 90655 90656 90657 9065890659 90660

Au ppb1/1

7 1 31

14 1 1

17 11

10 1 3

72/791 1 1 1 314 1

7/14 1 117

As ppm11 5 12 6 51

10 4 15 155 15 2 15 144 2 41 84 4 12 3 215 9

Certified by

G. Lebel l Manager


WHQLE.RQCK.SAMPLE.LQCAIiQNS

DRlLL-HQLE-MKr?Q- 1 s

58365837583858395840584158425843584458455846

Meterage

75.492.0 1O8.5 126.3 180.6 192.9 213.8 235.0 241.4 245.5 255.6

DRILL-HOLE-MK;9gr2:

i^!DBii-b!yfDber bi-terage

5812581358145815

BRiLL.HQLE.MKr9Qr3:

582158225823582458255826582758285829583058315832583358345835

71.8103.0152.0

Meterage

66.585.8103.5151.7177.6187.3202.5215.4242.0261.5275.8289.5299.6309.9321.0

DRI LL.bQLE.MKr9Qr4 s

Meterage

5816 ' 74.05817 129.75818 158.65819 182.95820 209.0

DRILL.HQLE.MK-9Qr5:

Meterage

5847 131.55848 155.5

DR I LL

iaffiBie-Nyfnber Meterage

No Whole Rock Samples Taken

Meterage

5849 100.3 j 5850 l 38. 7

DR I LL,HQlsE.MK-90r8 1

tfeterage

68677 59.368678 111.068679 131.668680 164.368681 183.468682 193.9

•l

l

P

l

• f li

SAMPLE \ X SI02 AL203 CAO MGO NA20 K20 FE203 MNO T102 P205 CR203 101 SUM

5*10581158125S135814

58155816581758185819

58205821582258235824

58255826582758285829

58305831583258335834

58355036583758385839

58405841584258435844

584558465847SB4B5849

5850

48.249.457.750.757.6

62.959.257.254.656.0

57.153.654.556.459.0

62.563.356.955.654.4

60.056.655.258.056.9

57.354.755.262.264.5

53.454.469.368.059.9

57.256.869.474.162.1

54.6

12.813.815.613.617.6

14.615.914.815.514.8

16.616.015.916.815.8

15.818.016.615.917.3

15.217.516.415.816.5

18.514.816.115.314.8

16.416.813.913.616.4

15.114.916.312.914.6

16.2

10.210.95.527.415.08

2.646.564.925.897.56

4.156.557.216.255.15

3.743.016.157.056.54

3.964.017.265.946.10

3.436.015.484.813.47

6.994.892.663.944.73

7.386.921.551.234.18

7.06

10.99.332.243.961.07

2.281.862.522.621.62

2.832.401.883.073.85

1.080.512.102.431.28

1.532.952.061.402.32

2.532.431.441.861.86

2.432.721.371.58.1.93

1.362.181.080.641.26

1.66

1.751.813.891.964.30

0.993.782.822.621.94

4.333.251.202.872.70

4.776.843.913.844.81

2.613.882.782.914.58

5.583.585.511.783.64

3.334.093.170.331.93.

2.694.333.343.273.18

3.04

0.290.320.430.272.29

1.690.130.710.772.52

1.240.782.900.700.82

1.221.140.090.240.98

1.480.290.781.300.18

0.620.460.432.111.03

0.490.392.503.713.57

3.081.744.063.680.94

0.98

11.811.96.819.724.00

8.098.068.619.104.72

6.028.366.497.056.80

5.563.278.807.437.27

7.918.116.508.246.90

6.659.899.005.425.08

9.129.252.611.884.04

5.024.892.311.508.01

7.41

0.18 l0.18 '0.150.26 (0.07 (

0.17 10.160.110.130.09 1

0.120.160.11 i0.09 10.07 1

0.160.070.150.140.14

0.150.120.120.230.14

0.110.200.290.17 10.12 t

0.180.160.08 (0.06 l0.10 l

0.10 )0.10 10.04 10.03 10.15

0.18

).98L05l .339.689.74

9.67l .371.281.339.64

1.391.369.70).749.82

.43

.60

.51

.31

.44

.25

.46

.38

.42

.32

.51

.36

.479.849.58

i. 321.449.279.289.45

9.679.679.29J.19.1.01

1.07

0.110.110.250.110.17

0.060.240.210.220.24

0.250.240.130.150.13

0.300.330.310.220.26

0.210.240.220.300.23

0.250.280.300.230.13

0.220.230.090.070.11

0.260.250.08O.OS0.17

0.20

0.110.08

4.010.010.01

4.014.014.014.014.01

4.014.014.014.010.02

4.010.01

4.014.014.01

4.014.014.014.014.01

4.014.014.014.014.01

4.014.010.01

4.014.01

4.014.014.014.014.01

4.01

1.391.315.93

11.65.39

5.772.855.396.088.62

5.315.777.234.003.08

2.311.472.233.934.47

4.853.006.934.314.23

3.166.084.004.163.70

4.854.392.936.235.54

6.545.851.621.624.31

7.Z3

98.8100.299.9

100.498.5

100.0100.298.799.098.9

99.498.698.398.298.3

98.999.698.C98.299.C

99.298.399.799.*99.*

99./99.*99.199.(99.(

96.!98.'99.(99.198.1

99.(98.1

100.-.99.!

100.1

99.

XKf U.R.A. SUMS INCLUDE ALL ELEMENTS DETERMINED. Kft SUMMATION, ELEMENTS ARE CALCULATED AS OXIDES

J X-RAY ASSAY LABORATORIES 1885 Lesle Street Don Ms Ontario M3B 3J4 (416)446-6766 Fax (416)445-4162 Th OS-986947Menfcer of the SGS Group (Socitt* Centrale de Surveillance) . "

SAMPLE X PPM RB SR Y Zft NB BA

58105811581258135814

58155816581758185819

58205821582258235824

58255826582758285829

58305831583258335834

58355836583758385839

58405841584258435844

58455846584758185849

5850

18IS272164

52OO182963

3623732123

3637331532

4134205022

3834185335

2222619092

7440906530

46

152146390323378

147293280376440

227177140321287

132205251268295

132339178176298

34720896160310

285371384125274

6721100426341121

201

1919391715

2745373500

1928OO1014

3839182141

1444113624

2444374916

4122OOOOOO

1611OO0013

31

72102182111153

340197168181125

191193105119130

212230232178201

170199178209184

209211244223156

176201122104132

11910211398191

186

2544241800

29112923OO

1918122112

1933241916

2128122712

1115202016

201511OO12

00OOOOH22

11

132144136115640

329146336441920

322204234267171

17827269109229

358128154199104

236140135288198

252131465497529

958503766645194

266

X-RAY ASSAY LABORATORES 1885 Lesle Street Don Mis Ontario M38 3J4 (416)445-6756 Fax (416)445-4162 Tlx 06-986947fenber of the SCS Group (Soclet* Centrale de Surveillance)

If I lSAMPLE \ X

68682

SI02 AL203 CAO MOO *A20 K20 FE203 NNO T102 P205 CR203 LOI SUN

6867768678686796868068681

48.46.48.52.46.

15.113.218.117.312.8

7.8010.17.256.6410.1

5.056.954.505.853.99

2.912.313.763.502.26

0.050.170.570.140.28

11.89.219.338.7613.2

0.220.200.190.150.35

1.010.740.961.080.98

0.070.240.070.070.06

0.020.030.040.024.01

6.70 99.610.6 100.44.47 98.33.69 99.69.65 100.2

55.6 17.2 4.91 3.76 4.10 0.78 7.91 0.18 1.04 0.07 0.02 4.47 100.1

XRF W.R.A. SUMS INCLUDE ALL ELEMENTS DETERMINED. FOR SUMMATION, ELEMENTS ARE CALCULATED AS OXIDES

X-RAY ASSAY LABORATORES 1886 Lesfe Street Don Ms Ontario M3B 8J4 (418)446-0766 Fax (418)446-4162 Hx 08-988947Meofcer of the SGS Group (Socittt Centrale de Surveillance)

l/VI XRF - (MOLE ROCK ANALYSIS 26-NOV-90 REPORT 13898 REFERENCE FILE 0881 PAGE t OT

9t

SAMPLE \ PPM

6867768678686796868068681

RB

25^0321715

SR

177214795331156

Y

2311^0^027

ZR

3873385757

NB

•0016171413

BA

76152466134188

33 123 14 46 18 215

X-RAY ASSAY LABORATORES 1885 Lesfe Street Don Mb Ontario M38 W4 (410445-6766 Fax (418)446-4152 Th 06-986947tenter of the SGS Group (Soclttt Generate de Surveillance)

HI K-30-Z.

/) i k, Q p ut*? ;*

M lApproxlmiti haroVtttt for low grtdt tntUmorphlc

se.

———x—l—-——i—————,——— , 14 l M l K l " l H l l-

s ?5

0?

t-

^W

x

s IK

0

g1- o

? ^

•w

* C*

-D •v. 5 r 1tt

tl tt ^

g•^ ^ ^ ^ ^ ^

•t.

5 4 F.jO, i TiO,

U l M 1 H l 4-1 l M l M

Appnwlnuit hiRlnMs lw low ondi mcumxphlc mlMnioty-

FeO t f 1,0)

- S

M l M K l O M l M

Aamutlmiu hHdnm lor low (nek nKUmxphic mlntnlogy.

** BORSURV **

SURVEY DATA AND CALCULATED CO-ORDINATES (metres)

f"PROPERTY: Mikwam HOLE NO: MK-90-5 GRIDi

DEPTH INCLINATION

DATEi Oct 2, 1990 SURVEY BYl WC INSTRUMENT! acid

ISSB.BBBSBBBBS8BBBSEB

O. 61.

,00.00

123.00183.00244.00305.00309.70

-50.00-48.00-47.00-47.00-45.00-46.00-46.00

BEARING 180.00 180.00 180.00 180.00 180.00 180.00 180.00

EASTINGS NORTHINGS ELEVATION-600.000-600.000-600.000-600.000-600.000-600.000-600.000

-3400.000-3440.020-3481.906-3522.826-3565.200-3607.956-3611.221

0.000-46.037-91.748

-135.630-179.509-223.018-226.399

SUMMARY LITHO LOO PROPERTY i Mikwam HOLE No.i MK-90-3

DEPTH

48.10

70.00

74.60

80.00

9B.20

101.60

116. BO

163.37

167.90

169.70

171.80

178.80

189.40

192.70

193.90

211.50

309. 7O

EASTINGS

-600.00

-600.00

-600.00

-600.00

-600.00

-600.00

-600. OO

-600. 00

-600.00

-600.00

-600.00

-600.00

-600.00

-600.00

-600. OO

-600.00

-600. OO

NORTHINGS

-3431.36

-3446. 10

-3449.21

-3432.86

-3465. 15

-3467.45

-3477.72

-3509.44

-3512.53

-3513.76

-3515.19

-3519.96

-3327.27

-3529.56

-3530.40

-3542.62

-3611.22

ELEVATION

-36.30

-52.67

-56.06

-60.05

-73.46

-75.97

-87. IB

-121.27

-124.59

-125.90

-127.44

-132,56

-140.23

-142.61

-143.47

-156.13

-226.40

1

t* BORSURV **

DRILLED WIDTH

48.10

21.90

4.60

5.40

18.20

3.40

15.20

46.57

4.53

1.80

2.10

7.00

10.60

3.30

1.20

17.60

98. 2O

r ~

CORE AN3LE

none

50.0

60.0

non*

60.0

65.0

60. 0

70.0

non*

70.0

7O.O

70.0

33.0

non*

33.0

none

53.0

~" ~" "" " ' "'~ W '

9Page 1 o* 1

TRUE WIDTH DESCRIPTION

— —— overburden

16.78 4Arg(gf),4Bw

3.98 4Bw,4Arg

———— Brittle fault ion*

15.76 4Gw,4Arg

3. OB 4Arg,gf (407.)

13.16 4Bw,4Arg

43.76 4Ss(arg)

——— Local breccia*, qts

1.69 4Sa,arg

1.97 4Arg(gf)

6.58 43*, wacke

8.68 4S*(cil)

——— mn 'r qv

0.98 48* (Bil)

——— Local breccias,qtz

80.44 4S*(*11)

** curxaucw **ASSAY LOG Page l of lPROPERTY: H i Vi warn )LE No.: MK-90-5

FROM TO WIDTH Au(gXt) As^pm)

65.80 66.65 0.85 0.020 15.000163.30 164.50 1.20 0.020 2.000189.40 190.40 1.00 0.010 14.000190.40 191.40 1.00 0.010 6.000192.20 192.70 0.50 0.010 17.000193.90 194.40 0.50 0.010 11.000209.30 210.30 1.00 0.010 12.000210.30 211.60 1.30 0.010 191.000217.20 218.20 1.00 0.010 5.000

** BORSURV **


ROPERTY: Mikwam HOLE NO: MK-90-6 GRID:

DATEi Oct 2, 1990 SURVEY BY l SH INSTRUMENT: acid

DEPTH 0.00

60.00 120.00 180.00 240.00 297.00

INCLINATION-50.00-51.00-51.00-50.00-48.00-47.00

BEARING EASTINGS180.00 400.000180.00 400.000180.00 400.000180.00 400.000180.00 400.000180.00 400.000

NORTHINGS-3044.000-3082.165-3119.924-3158.089-3197.452-3235.961

ELEVATION 0.000

-46.297-92.926

-139.224-184.506-226.531

SUMMARY UITHQ LOO PROPERTYi Mlkwam HOLE No.l MK-90-6

** BORBURV **P*g* l

DEPTH

32.30

37. 1O

37.20

42.60

42.70

52.50

52.60

55.60

55.95

60.90

61.20

68.30

68.50

70.90

71. 2O

97.80

98.00

106.50

110.00

155.55

155.70

160.50

171.60

171.90

181.60

EASTINGS

400.00

400.00

400.00

400.OO

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.00

400.OO

400.00

400.00

400.00

400.00

400.00

400.00

400.OO

NORTHINGS

-3064.55

-3O67.60

-3067.66

-3071.10

-3071.16

-3077.39

-3077.46

-3079.37

-3079.59

-3082.73

-3082.92

-3087.39

-3087.51

-3089.02

-3089.21

-3105.95

-3106.08

-3111.43

-3113.63

-3142.54

-3142.63

-3145.69

-3182.75

-3182.94

-3139.14

ELEVATION

-24.92

-28.63

-28.70

-32.87

-32.95

-40.51

-40.59

-42.90

-43.17

-47.00

-47.23

-52.75

-52.90

-54.77

-55.00

-75.67

-75.83

-82.43

-65.15

-120.36

-120.47

-124.18

-132,74

-132.97

-140.43

DRILLED WIDTH

32.30

4.80

0.10

5.40

0.10

9.80

0.10

3.00

0.35

4.95

0.30

7.10

0.20

2.40

O.3O

26.60

0.20

B. SO

3.50

45.55

O. 15

4.80

11.10

0.30

9.70

CORE ANGLE TRUE WIDTH DESCRIPTION

nona ———— overburden

63.0 4.35 4ArgX4Gw

none ———— qv, mn'r car b, mar, 3X py

63.O 4.89 4ArgX4Gw

nona -———— qv, mn'r carb,mer, S'/i py

65.0 8.8B 4ArgX4Qw

none ——— qv, mn'r car b, mar, 5X py

65.0 2.72 4ArgX4Bw

nona ———— qv, 27. po,py

65.0 4.49 4ArgX4Bw

nona ——— qtx, mil, IX py

65.0 6.43 4ArgX4Gw

none ———— qv, mn'r carb,*er, B7. py,po

65.0 2.18 4ArgX4Qw

nan* ———— qv, mn'r carb,mar, 8X py,po

65.0 24.11 4ArgX4Gw

nona —-—- qti, 4X py,po

65.0 7.70 4ArgX4Bw

none ———— g*'c arg, 5X qc vtr'g

65.0 41.28 4ArgX4Qw

non* ——-— qv, g'f'c arg, IX po

65.0 4.35 4ArgX4Gw

60.0 9.61 4Gw(4Arg,8*)

nona ———- qv, tr py

60.0 8.40 4Qw(4Arg,S*)

SUMMARY LITHO LOS PROPERTYi Mikwam HOLE No.l MK-90-6

** BORBURV **Pag* 2 of 2

DEPTH

201.50

233.20

236.00

248.10

248. 2O

250.00

250.10

255.40

260.00

262.70

288. 00

297.00 V- PYtP

EASTINGS

400.00

400.00

400. 00

400.00

400. OO

400.00

400.00

400.00

400.00

400.00

400.00

400.00

NORTHINGS

-3172. 19

-3192.99

-3194.83

-3202.92

-3202.99

-3204.21

-3204.28

-3207.86

-3210.96

-3212.79

-3229.88

-3235.96

ELEVATION

-155.45

-179.37

-181.49

-190.48

-190.55

-191.83

-191.95

-195.86

-199.25

-201.24

-219.90

-226.53

DRILLED WIDTH

19.90

31.70

2.80

12.10

0. 1O

1.80

0.10

5.30

4.60

2.70

25.30

9.00

CORE ANGLE

60.0

55.0

non*

55. 0

non*

5S.O

non*

53.0

10.0

10. 0

10.0

55.0

TRUE WIDTH

17.23

25.97

9.91

1.47

4.34

0.80

0.47

4.39

7.37

DESCRIPTION

4Arg(gf ), (4Bw,4Sv)

4Bw(4Arg,4Ss)

I55C gr**n mudcton*

40w(4Arg,43*)

qv, ffln'r carb, tr py,po

40w(4Arg,4S*)

qv, mn'r carb, tr py,po

4Gw(4Arg,48s)

•hvar zone, 4Bw

main shear, 5-15X po

•hear zone, 43w

4Gw{4Arg,4Sm) , chl, vheared, 15-20X q-c,

** **

ASSAY LOB PROPERTY: Mikwam

DLE No.: MK-90-6

Page l of l

FROM TO WIDTH Au(g7t) Aa(ppm)

36.7042.4051.8055.5060.9070.2070.8074.6097.60106.90120.80155.40159.30171.50187.50199.90214.90247.90249.90259.40259.90261.40262.50288.00289.20290.00290.90291.80292.80293.60294.80296.00

37.6543.1O52.8056. 1061.4070.6071.4075.2098.10107.90121.60155.90160.00172.10188. 10200.30215.40248. 3O250. 30259.90261.40262.50263.00289.20290.00290.90291.80292.80293.60294.80296.00297.00

O. 950.701.000.600.500.40O. 600. 60O. 501.000.800.500.70O. 600. 600.400.500.400.40O. 501.501.100. 501.200. 800. 90O. 901.000. 801.201.201.00

0.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0400.010O. 0100.0100.0100.0100.0400.0300.0400.1400.1500.2900.0200.280

10.00014.0008.0002.0006.0001.0001.0005.0006.00010.0002.0001.0002.000TRACE1.0001.000TRACETRACE1.000TRACETRACETRACETRACETRACETRACE8.0001.0003.0001.000

183.000129.000193.000

i Ot l** BORSURV **


PROPERTY: Mikwam DATE: Oct 2, 1990HOLE NO: MK-90-7 SURVEY BY: WCGRID: INSTRUMENT: acid

DEPTH INCLINATION BEARINS EASTINGS NORTHINGS ELEVATION0.00 -60.00 180.00 3912.000 -1895.000 0.000

61.00 -58.00 180.00 3912.000 -1926.417 -52.287123.00 -57.00 180.00 3912.000 -1959.730 -104.577182.00 -56.00 180.00 3912.000 -1992.294 -153.777244.00 -56.00 180.00 3912.000 -2026.964 -205.177355.00 -55.00 180.00 3912.000 -2089.835 -296.655357.20 -55.00 180.00 3912.000 -2091.097 -298.457

f

SUMMARY LITMO LOG PROPER!Yi Mikwam HOLE No.l MK-90-7

** BORSURV **Pag* l oi 2

DEPTH

82.60

120.50

128.00

131.10

133.00

143. OO

144.30

143.70

148.50

159.10

159.85

161.00

161.45

162.05

169.70

324.30

330. 80

331.80

338.50

340.10

344. 10

344.70

348.70

352.00

352.50

EASTINGS

TO 1 *5 f\f\*?7 1 4b * W

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912.00

3912. OO

3912.00

3912.00

3912.00

3912.00

3912.00

TO 4*5 f\f\*JT1 At UU

3912.00

TP l 1? rtrtO 7 1 j; * W

3912. OO

NORTHINBS

— i oTn rt^1 TOO * V*

-1958.39

-1962.49

-1964.20

-1965.25

-1970.77

-1971.49

-1972.26

-1973.80

-1979.65

-1980.07

-1980.70

-1980.95

-1981.28

-1985.51

-2O72.45

-2076. 13

-2076.69

-2080.49

-2081.40

-2083.66

-2084.00

-2086.27

—9npn 1 AAVD0. i H

-2088.42

ELEVATION

-70.50

-102.47

-108.75

-111.33

— 11*? O*}— 1 l 4m *t4.

-121.26

-122.34

-123.51

-125.84

-134.68

-135.31

-136.27

-136.64

-137.14

-143.52

-271.35

-276.71

-277.54

-283.06

-284.38

-287.67

-288.17

-291.46

—•904 1 O*Y*f .119

-294.59

DRILLED WIDTH

no x fiDA* ou

37.90

7.50

3.10

1.90

10.00

1.30

1.40

2.80

10.60

0.75

1. 15

0.45

0.60

7.65

154.60

6.50

1.00

6.70

1.60

4.00

0.60

4.OO

3.30

0.50

CORE ANGLE

none

45.0

20.0

45.0

non*

45.0

20.0

45.0

15.0

45.0

50.0

non*

50.0

60.0

50.0

50.0

50.0

35. 0

50.0

30.0

45.0

non*

45. 0

none

45.0

TRUE WIDTH

26.60

2.57

2.19

7.07

0.44

0.9?

0.72

7.50

0.57

0.34

0.52

5.86

118.43

4.98

0.57

5.13

0.80

2.83

2.83

0.35

DESCRIPTION

overburden

2D,t

•hear z on*, 10V. qc v, 1-2X p y

2D,t

wk bx, 5V. py

2D,t

•haar z on*

2D,t

•hear son*

2D,t

2Dt, (gf)

B55C mev p y

2D,t,gf

eer

2D,t,gf

4Arg

4Arg,gf

20V. qtz, shear, IV. py

4Arg,gf

50V. qtz, mhwar, 1-2X py

4Arg,g*

5-8X. qv, mh*ar, 3X py

4Arg,gf

•hear (contort.)

4Arg,g*

SUMMARY LITHO LOO PROPERTYl Mikw.m HOLE No.! MK-90-7

** BORBURV **P*Q* 2 o* 2

DEPTH EASTINGS NORTHINOS ELEVATION DRILLED WIDTH CORE ANGLE

357.20 3912.00 -2091.10 -298.46 4.70 non*


4Arg,M*ck

ASSAY LOG PROPERTY!

IDLE No. iiMikwam MK-90-7

Page l of l

FROM TO WIDTH Au(gXt) As(ppm)

102.30109.60115.60125.10126.00131.00132.00143.00143.60145.50146.50159.80170.80188.50190.00191.50204.50206.00214.10231.10239.60240.30243.20244.00263.30265.20266.20280.90297.00299.80305. 60307.60330.80337.00338.20340.20341.40342.00344.10

102.80110.10116.10126.00127.10132. OO133.10143.60144.30146.50148.20161.00171.80190.00191.50193.00206.00207. 2O214.60231. SO240.30241.40244.00245.50264.00266.20267.20281.40298.00300.80306. SO308.30331.80338.20340.20341.40342. OO343.00344.80

0.500.500.500.901.101.001. 100.600.701.001.701.201.001.501.501.501.501.200.500.700.701.100.801.500.701.001.000.501.001.001.200.701.001.202.001.200.601.000.70

0.0100.0100.0100.0100.0100.020O. 0100.0100.0100.0100.0100.2000.0010.0070.0010.0030.0010.0140.0010.0010.0170.0010.0010.0100.0010.0010.0070.0010.0030.0720.0010.0010.0010.0070.0010.0030.0140.0010.001

TRACETRACE1.000.TRACE1.000TRACETRACETRACETRACETRACE1.000

144.00011.0005.00012.0006.0005.0001.000

10.0004.00015.00015.0005.00015.0002.00015.0009.0002.00015.00014.0004.0002.0004.00012.0001.0008.0004.0004.0003.000

Page l of l ** BDRSURV f*


PROPERTY! mikwam DATE: 21/01/91HOLE NO: mk-90-8 SURVEY BY i weGRID: newmont INSTRUMENT! acid

DEPTH INCLINATION BEAR I NO EASTINGS NORTHINGS ELEVATION0.00 -55.00 180.00 -8400.000 1110.000 0.000

60.00 -54.00 180.00 -8400.000 1075.158 -48.847120.00 -51.00 180.00 -8400.000 1038.632 -96.448207.00 -51.00 180.00 -8400.000 983.881 -164.060

SUMMARY LITHO LOG PROPERTYi mikwam HOLE No.i mk-90-8

** BORSURV t*Pag* l of l

DEPTH

*T 1 VflO i * 9V

65.50

77.70

1 DA nnA V*T a O V

carb)

108.10

109. 10

117.20

121.60

125.00

128.20

139.50

142.00

169.50

189.70

194.70

194.80

201.00

•sftT.nft

EASTIN3S

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

-8400.00

—QArtrt AA~O*r VU * VU

-S400.00

-8400. OO

~nAnn.nft

NORTHINGS

1091.71

1071.81

1064.38

1 ri A 7 no1 V"? f m OT

1045.88

1045.27

1040.34

1037.63

1035.49

1033.47

1026.36

1024.79

1007.48

994.77

OQ1 A O'T i . O^

991.56

987.66

QftT Od

ELEVATION

— *5"t AA*wP. O*f

-53.21

-62.89

— RA TQO*T a O TT

-87.01

*.C37 ftft*"O/ B Civ

-94.23

-97.69

-100.33

-102.82

-111.60

-113.55

-134.92

-150.62

-154.50

-154.58

-159.40

-1 AA ft/.

DRILLED WIDTH

31.50

34.00

12.20

27.10

3.30

1.00

8.10

4.40

3 Aft. *fv

3.20

11.30

2.50

27.50

20.20

S j-vrta Uv

0.10

6 *5Aa *V

A, Art

CORE ANQLE

non*

55.0

45.0

non*

45.0

non*

45.0

50. 0

non*

50.0

60.0

non*

60.0

60.0

non*

non*

non*

nnrvn


——— overburden

27.85 IB, f, 10V. qc v, 5V. qv

B. 63 IB, f, carb, tr py.po

———— lOV.py, SV.po, tr cpy, 15V. q, qc v, lB(wk p.

2.33 IB, i 5-8V. qc v, 2V. qv, 5V. di IB po,py

1 ———— 15*4 po,py

5.73 IB,* 5-8V. qc v, 2V. qv, 5V. diBB po.py

3.37 IB.-f.chl

——— chl-rich, 10-15V. po,py, qv

2.45 lB,*,chl

9.79 IB,* 1-2X po,py(5y..mmv)

———— 10y. diBB po

23.82 IB, f 1-2V. po,py(SV.BfliBv)

17.49 lBf,chl 20X q,qc v

——— IB, f wk p*rv. carb, 10-15V. qc Btr

•"— —— — qVf 15t pO| tr cpy

——— - IB,* wk p*rv. carb, 1O-15X qc Btr

— — —— — IB 4 f-Kl 1 riV HiaB nn nu. *3*!V r\r \J

*V bUKbUKV **ASSAY LOG PROPERTY: Mikwam dOLE No.: MK-90-8

Page l of 2

FROM TO WIDTH AtUg/t) As(ppm) Cu(ppm) Zn(ppm)

31.5035.2045.7060.9063.9075.0076. 4077.5078.5079.9080.9081.8082.5084.0084.9085.9087.0088.4089.7090.2091.6093.0094.5096.0097.2098.2099.0099.60100.201O1.60103.00108.00113.60117.20118.70120.2O121.70122.70123.80124.80127.20129.20136.10136.80139.50141.00143.90144.40145.60150.10

33.0036.0046.4061.7065.0076.4077.5078. 5079.9080.9081.8082.5084.0084.9085.9087.0088.4089.7090.2091.6093.0094.5096.0097.2098.2099.0099.60100.20101.60103.00104.80109.00114.60118.70120.20121.70122.70123.80124.80125.70128.20130.30136.80137.40141.00142.00144.40145.60146.10150.80

1.500.800.700.801.101.401.101.001.401.00O. 900.701.500.901 . 001.101.401.300.501.401.401.501.501.201.000.800.600.601.401.401.801.001.001.501.501.501.001.101.000.901.001. 100.700.601.501.000.501.200.500.70

0.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0200.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0010.001O. 0010.0100.0010.0010.0030.0010.0010.0410.0030.0070.0100.0010. 0070.0010.014

1.000TRACETRACETRACETRACE2.0008.0008.00015.00015.00016.0004.00010.0008.0003.000TRACETRACETRACE2.000TRACE5.0004.0002.000TRACE1 . 0001.000TRACETRACE9.0008.0006.0006.0002.0004.0009.00015.0001.000TRACETRACE9.0003.0001.0001.0008.0002.0005.0006.0004.0002.00015.000

N.S.N.S.N.S.N.S.N.S.N.S.N.S.

126.000110.000145.000113.000392.000104.00072.000119.000254.000320.000294.000590.000209.00044.00060.000141.000254.000123.00077.000

346.000425.000112.000120.000187.000148.000

N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.

547.000142.000263.000161.000418.000152.000190.000149.000


244. OOO131.000124.000160. OOO727.000372.000188. OOO133.000276.000240. 000219.000204.000213.000154.000151.000172.000217.000164.000198. OOO214.000342.000176. OOO107.000155.000143.000

N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.

6590. 0003250. 000243. OOO166. OOO914.000109. OOO98.000876.000

ASSAY LOG PROPERTY: Mikwam

OLE No.: MK-90-8

Page 2 of 2

FROM TO WIDTH Au(gXt) As(ppm) Cu(ppm) Zn(ppm)

150.80151.70156.80158.00158.50159.50167.20170.20173.40176.90178.50184.90186.40194.50199.402O1.00202.50204.002O5.50

151.70152.30158.00158.50159.50160.60167.70170.80174.90178.50180.10186.40187.90195.00201.00202.50204.00205.50207.00

0.900.601.200.50l.OO1.100.500.601.501.601.601.501.500.501.601.501.501.501.50

0.0070.0030.0140.0010.0010.0010.003O.O030.0010.0010.0010.0010.0010.0010.0010.0010.0010.0030.003

15.0006.0005.0003.000TRACETRACETRACE2.000TRACE2.0003.000TRACETRACE2.0009.0002.000TRACE3.000TRACE

148.00044.000

M.S.78.00097.00090.000


119.000N.S.N.S.N.S.

173.000200.000

955.00076.000

N.S.163.000127.000112.000


88.000N.S.N.S.N.S.

110.000108.000

SUMMARY LITHO LOG PROPERTYi Mikwam HOLE No.l MK-90-3

t* SORBURV l*Pag* t of 2

DEPTH

46.30

77.30

78.20

86.90

120.70

121.90

130.78

130.92

142.00

145.50

160.60

161.10

163.30

163.80

167.50

169.50

173.00

183.60

4 OO 1 f\l D T m i V

196.90

199.90

203.00

208.00

209.30

212.10

EASTINGS

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550. OO

-2550. 00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

—2550. 00

-2550.00

-2550.00

-2550.00

-2550.00

-2550. OO

-2550.00

NORTHINGS

-3516. 14

-3516.75

-3522.68

-3545.73

-3546.55

-3552.66

-3552.76

-3560.38

-3562. 79

-3573. 19

-3573.53

-3575.04

-3575.39

-3577.94

-3579.31

-3581.72

-3589.02

-3598.26

-3600.34

-3602.50

-3605.97

-3606.87

-3608.82

ELEVATION

-57.96

-58.62

-64.98

-89.70

-90.58

-97.02

-97.13

-105.16

-107.70

-118.66

— 1 1 Q ft")AIT. V4

-120.61

•"120 1 98

-123.66

-125. 11

-127.65

-135.34

-144.90

-147.06

-149.29

-152.89

-153.82

-155.84

DRILLED WIDTH

46.30

31.00

0.90

8.70

33.80

1.20

8.88

0 1 At i "f

11.08

3.50

15.10

0.50

2.20

0. 50

3.70

2.00

3.50

10.60

5.50

7.80

3.00

3.10

5.00

1.30

2.80

CORE ANGLE

none

50.0

35.0

55.0

50.0

45.0

50.0

none

50.0

none

50.0

none

50.0

none

50.0

none

50. 0

50.0

none

50.0

55.0

55.0

SS.O

25.0

55.0

TRUE WIDTH

23.75

0.52

7.13

25.89

0.85

6.80

8.49

11.57

1.69

2.83

2.68

8. 12

5.98

2.46

2.54

4.10

0.55

2.29

DESCRIPTION

overburden

2A,f

py zone, 20V.*mBV-hdi m* py, 2A,t

2DXA,t - *t. fol'd

2DXA,f

•hear cone 2D/A, t , 1O-15V. dies py

2DXA,t fol'd

qv, tr py

2DXA,t fol'd

•t. fol'd - shear

2DXA,t fol'd

qv, tr py

2DXA,t fol'd

qv, tr py

2DXA,t fol'd

wk. ank, bio, feld. phen.

2DXA,t fol'd

2D,f

5X qv, tr py

2D,f

2D,lt 157. dl**-*mmv py/po

2A,t

2D,t,lt, qv 15X loc, 10-20V. py

•hear, 10 /C py

2D,t,lt, qv 15V. loc, 10-20X py

** BORBURV t*SUMMARY LITHO LOG PROPERTYi Mikwam HOLE No.i MK-90-3

Pag* 2

DEPTH

231.60

241. 10

244.80

250. 10

254.81

OKA. Irt256. 2O

27O.70

272.70

279.60

283.00

305.80

306.60

310.80

312.30

312.80

313.40

321.90

EASTIN8S

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

^.OGCttf") rtft~^O^y * VL*

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

-2550.00

NORTHINGS

-3622.37

-3628.96

-3631.55

-3635.33

-3638.69

— *tA"*O AQOO^T . OD

-."^A^rt rt9oOwV. MA

-3651.45

-3656.37

-3658.80

-3675. O6

-3675.64

-3678.66

-3679.74

-3680. 10

-3680.53

-3686.64

ELEVATION

-169.86

-176.70

-179.34

-183.06

-186.36

-187.33

-197.50

-198.90

-203.74

-206.12

-222.09

-222.65

-225.57

-226.61

-226.96

-227.37

-233.28

DRILLED WIDTH

19.50

9.50

3.70

5.30

4.71

I XQ* O T

14.50

2.00

6.90

3.40

22.80

0. 80

4.20

1.50

0.50

0.60

8.50

CORE ANBLE

50.0

55.0

none

none

non*

none

none

none

non*

50.0

55.0

40.0

55.0

nonv

55.0

non*

55.0


14.94 20, It 5-8V. loc hdi** py

7.78 2D,lt 20V. •mmv-mmv*,dlm*-*tr py

——— 2D,m*v,5'X.qv,tr py

———— 2D,2Dlt, 5-1SX py

——— -fault mnr qv, 10-20X py

———— 2D,bx 5-10X qv

———— 2D

———— 2D,bx

•••.w—* *?rk—— *-— -* 41)

2.60 2D, It 107. di**-mtr py/po

IB. 68 2D

0.51 105C qv. tr py

3.44 2D

———— 30-40V. qv, 3-5V. py

0. 41 2D

——— qV( 20 X *tr py

6.96 2D

ASSAY LOG PROPERTY: Mikwam JLE No.: MK-90-3

**

Page l of l

FROM TO WIDTH Au(gXt) As(ppm)

52.8053.3076.60108.40109.90119.60120.70121.90160.30163.30164.80182.60185.80189.00195.20196.70198.70202.80204.40206.30208.30209.30210.80212.10214. 10216.10229. 10231.60233.60235.60237.60239.60245.60248.30250.00270. 7 '0285. 10305.80310.80312.30313.80319.90

53.3055.3077.60109.901 1 1 . 30120.70121.90122.40161.30164.80165.30183.70186.30189.50196.70198.70200.00203.30206.30208.30209.30210.80212. 10214. 10216. 10218.10230. 10233.60235.60237.60239.60241.10246.40249.00251.80272.40285. 90306.60312.30313.80315.00320.60

0.502.001.001.501.401. 101.200.501.001.500.501.100.500.501.502.001.300.501.902.001.001.501.302.002.002.001.002.002.002.002.001.500.800.701.801.700.800.801.501.501.200.70

0.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0200.0100.0200.010

1.0001.000TRACETRACETRACEl.OOO1 . 000TRACETRACETRACETRACE1.000TRACETRACETRACE2.0001.0001.0001.000TRACE1.0001.0001.0006.0002.0002.0001.0005.0009.0009.0006.0001.000TRACETRACETRACETRACETRACE1.000TRACETRACETRACE2.000

l UT

** BORSURV **


'ROPERTY: Mikwam DATE: Oct 2, 1990HOLE NOs MK-90-4 SURVEY BYi SHGRID: INSTRUMENT: acid

DEPTH INCLINATION BEARING EASTINGS NORTHINGS ELEVATIONO.00 -50.00 180.00 -1900.000 -3208.000 0.000

12O.OO -48.00 180.00 -1900.000 -3286.727 -90.565180.00 -46.00 180.00 -1900.000 -3327.647 -134.446223.20 -46.00 180.00 -1900.000 -3357.656 -165.522

SUMMARY LITHO LOB PftOPERTYl Mikw*m HOLE No.l MK-90-4

DEPTH

56. 10

76.30

77.00

B2.60

82.80

84.30

84.90

90.30

90.80

96.20

96.60

102. 10

102.30

113.40

122.00

139.80

137.70

138.90

139.13

145.70

145.90

146.10

146.30

134.00

171.50

EASTINGS

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900. OO

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

NORTHINGS

-3244.80

-3258. 19

-3258.52

-3262. 19

-3262.32

-3263.31

-3263. 70

-3267.24

-3267.57

-3271. li

-3271.38

-3274.98

-3275.11

-3282.40

-3288.09

-3297.30

-3298. 80

-3299.62

-3299.79

-3304.25

-3304.39

-3304.53

-3304.66

-3309.92

-3321.85

ELEVATION

-42. 34

-57.74

-58. 11

-62.34

-62.49

-63.62

-64.07

-68. IS

-68.53

-72.60

-72.90

-77.06

-77.21

-85.58

-92.03

-102.12

-103.51

-104.39

-104.37

-109.36

-109.81

-109.65

-109.80

-115.43

-128.23

*t BORBURV **

DRILLED WIDTH

56.10

20.40

0. 50

5.60

0.20

1.50

0.60

5.40

0.50

5.40

0.40

5.50

0.20

11.10

8.60

13.80

1.90

1.20

0.25

6.55

0.20

0.20

0.20

7.70

17.50

CORE AN8LE

non*

50.0

non*

30.0

non*

50.0

non*

50.0

non*

50.0

non*

50.0

non*

50.0

40.0

50.0

non*

50.0

non*

50.0

non*

50.0

non*

50.0

50.0

Pag* 1 of 2


15.63 2A/D

———— sil* 'd, IV. py

4.29 2A/D

——— qv

. 1.15 2A/D

———— qv, tr py

4.14 2A/D

——— qv, tr py

4.14 2A/D

——— qv, tr py

4.21 2A/D

——— qv, IV. py

8.50 2A/D

5.53 23X carb mtrg, tr py, 4ol

10.57 2A/D

———— 60X qv, tr py

0.92 2A/D

——— qv

5.02 2A/D

——— qv

0. 15 2AXD

——— qv

5.90 2A/D

13.41 2D/A

SUMMARY LITHO LOB PROPERTYi Mikwam HOLE No.l MK-90-4

t* BDR3URV **Peg* 2

DEPTH

178.30

183. 10

184.20

194.60

200.00

201.OO

OA-? Ort^\J f . AW

210.30

210.40

210.70

213. 20

214.20

223.00

223.20

EASTINGS

-1900.00

-1900. OO

-1900.00

-1900.00

-1900.00

-19OO.OO

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

NORTHINGS

-3326.49

-3329.80

-3330.56

-3337.79

— TTA1 HA^ J*t A . 3*f

-3342.23

-3346.54

-3348.70

-3348.76

-3348.97

-3350.71

-3351.40

-3357.52

-3357.66

ELEVATION

-133.20

-136.68

-137.47

-144.95

— 1 AO O^I f D. Dw

-149.55

-154.01

-156.24

-156.31

-156.53

-158.33

-159.05

-165.38

-168.52

DRILLED WIDTH

6.80

4. BO

1.10

10.40

5 Aft. tv

1.00

6 *5Am 4\.'

3.10

0.10

0.30

2tffi.DO

1.00

8 Oft9 OV

0.20

CORE ANGLE

SO.O

50. 0

non*

50.0

non*

50.0

non*

50.0

non*

50.0

none

50.0

norm

50.0

TRUE WIDTH

5.21

3.68

7.97

0.77

2.37

0.23

0.77

0.1S

DESCRIPTION

•hvar zone, wk carb/vvr, 5"/. di** py, mn' r

2D/A

bx, 20'X carb/mn'r qti, tr py/po

2D/A

wk shear z on*, wk c*rbXa*r, 3'/. di**-*trg

2D/A

w k -mod m*g, lO'X. di**-*trg py, S-BX. qc v

2D/A

qv, 2X py, 5X po

2D/A

wk *h*ar zone, 5-1 0V. qc v, 1O/C di** py

2D/A

10X di**-*trg py, Z'/, po

2D/A

ASSAY LOG PRQPERTV: Mi kwarn HOLE No. l MK-90-4

Page l of l

FROM TO WIDTH Aufg/t) As(ppm)

76.4082.6084.3090.0095.70101.401 1 1 . 60135.20136.20137.30138.40145.60163.50165.40171.40172.40175.20176. 10178.30197.70200.50202.00203.50205.00205.80207.20210.00210.70212.20213.70215.20216.70

77. 1083.4085.0091.0096.60102.40112.70136.20137.30138.40139.40146.70164.50166.30172.40173.40176.10176.90178.80198.70202.00203.50205. 00205. 80207.20208.50210.70212.20213.70215.20216.70217.60

0.700.800.701.000.901.001.101.001.101.101.001.101.000.901.001.000.900.800.501.001.501.501.500.801.401.300.701.501.501.501.500.90

0.0100.0100.0200.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0700.0100.0100.0100.010O.O100.0100.0100.0100.0100.0100.0100.0100.0100.0100.010

1.000TRACETRACETRACETRACETRACE1.000TRACETRACETRACETRACETRACEl.OOOTRACETRACETRACE3.0001.000TRACETRACETRACE1.000TRACETRACETRACETRACE1.000TRACETRACE2.00018.0004.000

** BORSURV **


:OPERTY: Mikwam DATEi Oct 2, 1990HOLE NO: MK-90-1 SURVEY BY l WCGRID: INSTRUMENT! acid

DEPTH INCLINATION BEARING EASTINGS NORTHINGS ELEVATIONO.OO -50.00 180.00 -2550.000 -3625.000 0.000

61.00 -48.00 180.00 -2550.000 -3665.020 -46.037122.00 -48.00 180.00 -2550.000 -3705.837 -91.369183.OO -47.00 180.00 -2550.000 -3747.048 -136.343244.00 -46.00 180.00 -2550.000 -3789.037 -180.591285.30 -46.00 180.00 -2550.000 -3817.727 -210.300

** BORSURV t*SUMMARY LITHO LOQ PROPERTYi Mikwam HOLE No.l MK-90-1

Pag*

DEPTH

73.15

77.30

8O.6O

90.70

112.60

120.30

133.70

144.20

177.30

196.70

203.40

232.90

242.30

285.30

EASTINGS

-2530.00

-2550.00

-233O.OO

— •StA flfl^tJOU* W

-2530.00

-2550.00

-2550.00

-2550.00

-2530.00

-2530.00

-2550. 00

-2530.00

-2550.00

-2550.00

NORTHINGS

-3673. 13

-3675.93

-3678. 13

— tARA ftQOODH . DT

-3699.55

-3704.70

-3713.74

-3720.83

-3743.20

-3756.48

-3761.09

-3781.40

-3787.87

-3817.73

ELEVATION

-33. O7

-58. 15

-6O.6O

— AP 1 1OD. l 1

-84.38

-90. 1 1

-100.00

-107.74

-132.14

-146.28

-151.14

-172.54

-179.36

-210.30

DRILLED WIDTH

73.13

4.13

3.3O

10.10

21.90

7.70

13.40

10.50

33.10

19.40

6.70

29.50

9.40

43.OO

CORE ANGLE

none

non*

60.0

none

60.0

nona

60.0

non*

60.0

35.0

60.0

60.0

30.0

50.0

TRUE WIDTH

2.B6

18.97

11.60

28.67

15.89

3.80

25.55

7.20

32.94

DESCRIPTION

overburden

2A

2D,lt,py (po)

30V. *m*v py(po)

2D, lt,py *po)

35V. smvv py(po)

2D, lt,py (po)

60X mmmv-mBV py(po)

2D,lt,py(po)

2 A, -f

4Arg,g*

4SB/4BN

3t , mmr

7q*P,d*citlc

** BORSURV **ASSAY LOG PROPERTY: Mikwam HOLE No.: MK-90-1

Page l oi 2

FROM

75.5078.0078.7081.0082.2084.0085.0087.0088.0090.0091.0092.0094.0095.0097.0098.0099.92101.46102.90104.46105.46106.46108.74110.42112.60113.60115.00116.00117.00118.80120.44122.00123.00124.50125.50127.91128.98129.90130.90131.90133.57135.50136.50137.50138.50139.50141.00142.50144.00145.50

TO

76.5078.6081.0082.2084.0085.0087.0088.0090.0091.0092.0094.0095.0097.0098.0099.92101.46102.90104.46105.46106.46108.50110.42112.60113.60115.00116.00117.00118.80120.44122.00123.00124.50125.50127.77128.98129.90130.90131.90133.57135.50136.50137.50138.50139.50141.00142.50144.00145.50147.00

l, l, l,

WIDTH

1.00 0.60 2.30 .20 .80 .00

2.00 1.00 2.00 1.00 1.00 2.00 1.00 2.00 1.00 1.92 1.54 1.44 1.56 1.00 1.00 2.04 1.68 2.18 1.00 1.40 1.00 1.00 1.80 1.64 1.56 1.00 1.50 1.00 2.27 1.07 0.92 1.00 1.00 1.67 .93 ,OO ,OO .00 .00 .50 .50

1.5O 1.50 1.50

' SE S S SI B SI S

i(gXt)

0.0010.0100.0140.0340.0010.0140.0270.0010.0170.0010.0010.0100.0100.0100.0010.0270.0010.0510.0010.0070.0010.0010.0010.0100.0140.0010.0140.0010.0030.0010.0010.0010.0010.0070.0070.0010.0010.001O.OO10.0170.0140.0010.0340.0070.0070.0030.001O.O010.0010.010

As(ppm)

TRACE12.000TRACETRACE5.00033.0006.OOO15.0001 1 . 0001 1 . 0002.0001.0003.000TRACE5.000

1 1 . 0009.00012.00014.00082.OOO3.0001.0005.0006.000

66.0001 1 . 000

110.00066.00034.0006.0005.0001.000TRACE18.000TRACETRACE14.00029.00055.00025.00012.00018.00040.00088.00015.00066.OOO18.00010.0004.00010.000

Cu(ppm)

37.000122.000

N.S.58.000

N.S.40.000

N.S.39.000

N.S.71.00048.000

N.S.27.000

N.S.50.000

N.S.N.S.N.S.N.S.

24.00074.000

N.S.N.S.N.S.

18.000N.S.

40.00022.000

N.S.N.S.N.S.

41.000N.S.

39.000N.S.N.S.N.S.

35.00030.000

N.S.N.S.

37.000N.S.

24.000N.S.

51.00028.00061.OOO30.OOO

N.S.

Zn(ppm)

202.000100.000

N.S.249.000

N.S.162.000

N.S.128.000-

N.S.143.000235.000

N.S.230.000

N.S.142.000

N.S.N.S.N.S.N.S.

78.00085.000

N.S.N.S.N.S.

121.000N.S.

349.000244.000

N.S.N.S.N.S.

104.000N.S.

394.000N.S.N.S.N.S.

157.000292.000

N.S.N.S.

136.00ON.S.

304.000N.S.

105.000107.000173.000110.000

N.S.

** BORSURV **ASSAY LOG PROPERTY: Mikwam

JLE Ns.: MK-90-1

Page 2 of 2

FROM TO WIDTH Au(gXt) As(ppm) Cu(ppm) Zn(ppm)

147.00143.50ISO. 00151.50153.00154.50156.00157.50153.20153.50159.5016O.50162.00163.50165.00166.50163.00169.50171.00172.50174.0017^.30176.80179.25183.70184.70185.70189.8019-0.80191.80193.5019S.OO2O9.7O21O.2021O.80217.7023O.50231.35232.45233.45235.0026-4. 2O277.00283.002B4.00

148.50150.00151.50153.00154.50156.00157.50158.20158.50159.50160.50162.00163.50165.00166.50168.00169.50171.00172.50174.00175.30176.80177.80179.75184.70185.70186.70190.80191.80193.50195.00196.80210.20210.80211.30218.20231.35232.45233.45235.00235.50265.70277.60284.00285.30

1.501.501.501.501.501.501.500.700.301.001.001.501.501.501.501.501.501.501.501.501.301.50l.OO0.501.001.00l.OO1.001.001.701.501.800.500.600.500.50O.B51.101.001.550.501.500.601.001.3O

0.0100.0100.0100.0100.0100.0100.0100.0100.0100.0200.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0100.0200.0100.0100.0100.0100.0100.0100.0100.010

10.0009.00015.00015.00010.0003.0003.00010.0008.00018.00015.0008.0006.0007.000

1 1 . 0009.0006.0002.0002.0001.000TRACE2.000TRACETRACE18.00018.0003.000TRACE2.0004.0005.0003.0001.0001.000TRACETRACE3.0002. 00016.OOO8.0002.0003.000TRACE2.0002.000

N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.

N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.

tl*

t

** BORSURV **

SURVEY DATA AND CALCULATED CO-ORDINATES (metre*)

DPERTYs Mikwam DATEi Oct 2, 1990HOLE NO: MK-90-2 SURVEY BYl SHGRID: INSTRUMENT! acid

DEPTH INCLINATION BEARING EASTINGS NORTHINGS ELEVATION0.00 -50.00 180.00 -1900.000 -3400.000 O.QOO

, 60.00 -54.00 180.00 -1900.000 -3436.940 -47.281j 120.00 -53.00 180.00 -1900.000 -3472.629 -95.5121 180.00 -54.00 180.00 -1900.000 -3508.318 -143.743

240.00 -53.00 180.00 -1900.000 -3544.008 -191.9751 300.OO -53.00 180.00 -1900.000 -3580.117 -239.893i 325.00 -53.00 180.00 -1900.000 -3595.162 -259.859

SUMMARY LITHO LOB PROPERTYi Mikwam HOLE No.l MK-90-2

** BOR8URV t*Pag* l t,

DEPTH

46.30

63.50

66.20

75.70

86.40

87.10

no x***iO"* ov

93.50

OO Af\"O m *rW

107.00

119.00

125.00

179.60

203.70

204.90

216.50

223.40

229.40

238.00

252. OO

265.00

272.40

277.00

*?Q*5 QSVfd^rn OV

290.80

EASTINGS

-1900.00

mm t ttf\f\ /S^l1 YUU . UU

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900. OO

-1900.00

-1900.00

-1900.00

-1900. OO

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-1900.00

-190O.OO

NORTHINGS

-3428.51

— XA^CO f\*2O*? O TT m V*

-3440.63

-3446.28

-3452.64

-3453.06

— T A*; A ^tO*?O*r * 33

-3456.87

-3459.78

-3464.90

-3472.03

-3475.60

-3508. 08

-3522.42

-3523. 13

-3530.03

-3534.13

-3537.70

-3542.82

-3551.23

-3559.05

-3563.51

-3566.27

-3569.77

-3574.58

ELEVATION

••TA JIQntfO* fO

-50.09

-52. 26

-59.90

-68.50

-69.07

-71.07

—•y A 01/•l m Jt~i

v7O 1 ^/O* 1 O

-85.06

-94.71

-99. 53

— 1 AX 49i to* *? *

-162.79

— 1 AT "7 A"* lOOa /O

-173.08

-178.63

-183.45

-190.37

-201.56

-21 1 . 94

-217.85

-221.52

— f?^*A 1 A4^O* 1O

-232.55

DRILLED WIDTH

46. 3O

17.20

2.70

9 OCA* tJV

10.70

0.70

2 **rt* 3V

3.90

4 OA* TT V

8.60

12.00

6.00

54.60

24.10

1 *?i"i1 . &V

11.60

6.90

6.00

8.60

14.00

13.00

7.40

4.60

S D 1*1. BO

8.00

CORE ANGLE

non*

non*

50.0

non*

60.0

non*

non*

non*

non*

60.0

non*

60.0

non*

60.0

non*

60.0

20.0

45.0

85.0

60. 0

60.0

60.0

50.0

non*

50.0


p ———— ov*rburd*n

———— 2, t, 1 1

2.07 4Arg,2t

———— 2, t, It

9.27 2t,4Arg(g*)

———— 4Arg(gf)

——— qv 5X py

———— 4Arg(gf)

———— 4Arg(gf),48w

7.45 4Qw

———— chl'c, loc Bil

5.20 4Gw

———— 5y. q-c *it'n(35X),lX py

20.87 4Gw

——— q-rich, 3Xpy, I'/.po

10. OS 4Gw

2.36 5IF-70y.qtz*cht,3Xlam.mt,lSy.py,po

4.24 4QM

7.04 5IF-60y.qtz-cht,30y.pyXpo,10y.mt l*m.

12.12 5IF-50Xqtz-cht,30Xchl mmd, ISXpy/po.SXmt :

11.26 3IF-50Xcht-qtz,40Xchl **d, 13Xmt lam. ,2'X.p'

6.41 5IF-30Xcht-qtz,45Xchl •*d,20XpyXpo,5Xflit :

3.52 4Gw(g*),15Xq-c *tr, lO-lSXpy/po

——— 5Xq-c,X3w

6.13 4G*(gf ), 15Xq-c *tr, 10-lSXpy/po

SUMMARY LITHO LOS PROPERTYi Mikw*m HOLE No.i MK-90-2

•rtt BOR8URV **

Pag*

DEPTH EASTIN8S NORTHIN83 ELEVATION DRILLED WIDTH CORE ANSLE TRUE WIDTH

292.85 -1900.00 -3575.81 -234.18 2.05 non* ————

298.00 -1900.00 -3578.91 -238.30 5.15 50.0 3.95

307.10 -1900.00 -3584.39 -245.56 9.10 20.0 3.11

313.00 -1900.00 -3587.94 -250.28 5.90 nanm ———

325.00 -1900.00 -3395.16 -259.86 12.00 20.0 4.10

DESCRIPTION

two qv, 1-SV.po/py

4Qw (gf) , 15Xq-c *tr, 10-lSV.py/po

4Qw,4Arg(g-f),3-5V. diva py/po

4Gw,4Arg(gf),3-5X die* py/po

** ourvaurw **ASSAY LOBPROPERTY: Mi k warn^OLE No. : MK-90-2

FROM

64.0569.1073.0577.0078.5085.6086.3087.1088.0088.9089.6090.6091.6092.6095.0096.401O9.40112.30199.902O3.70217.00218.00219.00222.40229.40230.70232.00233.50235. 00236.50238.00239.50241.00242.50244.00245.50247.00248.50250.00251.50253.00254.50256.00257.50259.00260.50262.00263.50265.00266.50

i^*~-— **— ••MV*-

TO

64.7569. 7073.9078.1079.3086.3087.1088.0088.9089.6090.6091.6092.6093.5096. 0097.40110.40113.30200. 60204.50218.00219.00220.00223.40230. 70232.00233.50235.00236.50238. 00239.50241.00242.50244.00245.50247.00248.50250.00251.50253.00254.50256. 00257.50259.00260. 50262.00263.50265.00266.50268.00

Page l of 2

WIDTH Au(gXt)

0.70 0.60 0.85 1.10 0.80 0.70 0.80 0.90 0.90 0.70 1.00 1.00 1.00 0.90 l. 00 1.00 1.00 1.00 0.70 0.80 1.00 1.00 1.00 1.00 1.30 1.30 1.501.50,5050

1.501.501.505050505050

1.501.501.501.501.501.501.501.50,50 .50 .50

1.50

0.0010.0010.0010.0270.010O. 1100.0310.0140.0010.0240.0750.0860.0510.0510.0620.1410.0210.0010.0100.0100.0100.0100.0100.0100.0100.3300.1800.530O. 1600.0400.4400.3600.2400.1200.0600.0800.0100.0600.1800.0800.0500.0300.0100.0100.0100.0300.0400.0300.0800.020

IzaSBBSB

s (ppm)

TRACE2.0001.000TRACE5.0001.0009.0001.000TRACETRACE8.000TRACETRACETRACETRACE15.000TRACETRACE5.0001.0006.0002.0001.000TRACE12.0007.00010.00014.0005.0002.00013.00014.0003.00014.0006.000TRACETRACE12.0001 1 . 00010.0001.000TRACETRACE13.0002.000TRACE5.0008.00014.00013.000

IBBSSBSaiSSS

Cu(ppm)

39.00057.00029.00075.00036.000190.000314.00035.00012.00042.OOO117.000163.000220.000241.OOO160.000128.00030. 00044.000N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.

SBSB3S88SBBB

Zn (ppm)

242. 000164.00073.000

361.000374.000

3490.0003200.000

68.00044.000120.000631.000

2890.0002520.000359.000635.000"109.000233.000130.000

N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.

ASSAY LOG PROPERTY! Mikwam

3LE No.: MK-90-2

**Page 2 of 2

FROM

268.00269.50271.00272.35273.05273.70274.80275.80277.00278.30279.80282.80283.60284.50286.60287.80289.00290.00290.80292.00293.00309.50319.00

TO

269.50271.00272.35273.05273.70274.80275.80277.00278.30279.80280.80283.60284.50285.80287.80289.00290.00290.80292.00293.00294.50311.00320.50

WIDTH AuCg/t)

1.501.501.350.700.65

, 10,00,20

l,l,l1.301.501.000.800.901.301.201.201.000.801.201.001.501.501.50

0.0500.0100.0400.1200.0900.1300.1000.0100.0900.1100.2000.0800.0700.0100.0200.0100.2100.0800.0100.0100.0100.0300.010

is(ppm)

16.00014.0001 1 . 00015.00014.0006.0001.0001.0009.0004.00014.0009.0009.0001.0002.0002.0001 . 000TRACE1.0001.0002.0002.0002.000

Cu(ppm)

N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.N.S.

Zn(ppm)

N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S. N.S.

f

** BORSURV **


Mi k warn HOLE NO: MK-90-3 GRID:

DATEi Oct 2, 1990 SURVEY BY: WC INSTRUMENTS acid

ssasssssiasBSBSssascssssssBssssBaiSBsecEissE

DEPTH 0.0061.00 123.00 183.00 244.00 305.OO 321.90

INCLINATION-50.00-48.00-46.00-47.00-45.0O-44.00-44.00

BEARING 180.00 180.00 180.00 180.00 180.00 180.00 180.00

EASTINGS-2550.000-2550.000-2550.000-2550.000-2550.000-2550.000-2550.000

NORTHINGS-3465.000-3505.020-3547.303-3588.605-3630.979-3674.487-3686.644

ELEVATION 0.000

-46.037-91.381-134.904-178.783-221.539-233.279

LATITUDE . 36.258

DEPARTURE 25. SOW

ELEVATION

NORANDA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOG

SurfaceT*(l

Depth Dip Magnetic Bearing

Corrected Besrlng

Projecl No. 287

Property MIKwam

DIP AT COLLAR-50'

____ BPARIMf. G. S. 180*

TOTAL DEPTH 285.3m CORE SIZE BQ 1 7/16

CORE STORAGE Timmins—-——-———.—N.———-—Testing stratigraphy up-ice from

REMARKS MOV-84-27 and major BM conductor.

-AB"

1ft 1m-46'-

NTS 32E/5 ____ TWP. Noseworthy cieim NO JtfiJ

Otu tuned Sept.. 1 5 t 1990 Sept. IB

Contractor Norex Drilling

togged by Mayne CoratorphiJIB.

Depth 81 Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

0.0-73.19

73.18-77.3

INTERMEDIATE VOLCANIC

77.3-177.3

INTERKEDIAT! TO FEL8XC PYROCLASTIC/ SULPHIDE ZONE

Casing, bedrock at 72.On, many boulders.

Very fine grained, medium green to grey green colour. Massive to coarsely foliated or with lensoid banding (diffuse). Pro bably flow rook although no features to suggest it.

Very fine grained, light grey in colour throughout. Groundmass generally has massive appearance but weak to moderate fabric evident upon breakage, very uniform in colour, texture and apparent composition Moderately hard to hard. No free quarts discardable as phenocryst*. Freshly broken surface has sericitic sheen under hand lens (uhl). cored surface suggests fragmental origin, fragment sice variable from few am to 4cm. In all instances monolithic and fragment supported. Distinct matrix only as dark, possibly weakly graphitic material very minor, or pyrite ± pyrrhotite. Probably daoitio.

7*.0*71.B Quartz veining, 401 irre gular form. Fine grained carbonate in groundmass - HCL reaction.

Very minor quartz veining ^l*. Heavy sulphides of pyrite and pyrrhotite. Concentration variable between 101 and 501 with some semi-massive intervals. No other recognizable altera tion.

No sulphides apparent in volcanic unit. Quartz vein SI pyrite in places.

Overall 20-251 pyrite and pyrrhotite.

MR at 75.4m Initial .4m felsic volca but badly br up, pyritic Core angles deg. at 76.7 (foil.). (58

Sulphide pro primary envi ment accept! felsic depoe rather than secondary. I latter, soon after deposi of volcanic material. So sections hav near cherty look.


DIAMOND DRILL CORE LOG m* ™-Sheet No.

MK-90-1

Property

Depth 81 Lithology Description (colour, grein (li*, texture, structure, etc.) Alteration Mlnerellution Remarks

All fragment fonts tend to be flattened but much of the coarser structured sections have irregular breccia-like textures - very irregular shapes usually with sulphide (pyrite ± pyrrhotite) matrix. Dominant sulphide content after 78.10m. Very heavy pyrite -f less pyrrhotite persisting through* out section (ID-50% sulphide). Core angles 55 deg. at 78.0m, lapilli foliation.78.1-78.s TWO semi-massive pyrite bands 4cm and I6cm in width, minor white quartz and beige carbonate. Contacts relatively sharp.

78.5-80.6 Felsic volcanic with lot stringer and heavily disseminated pyrite. Structure to felsic is not clearly fragmental-diffuse. only SI matrix ? as thin filament-like stringers.

80.6-90.3 Felsic fragmental with heavy, fine grained semi-massive pyrite forming matrix to the volcanic to SOI in places, average 25-301. Note whitish calcite associated within more massive pyrite accumulation, about lot carbonate locally but overall only 1-21. Core angle at 89.5, 60 deg. - wispy volcanic fragments.90.3-90.7 (751).

Smsv-msv pyrrhotite and pyrite

No significant alteration noted. Minor fine grained calcite.

451 smsv pyrite bands.

101 heavily disse minated to stringer pyrite matrix.

301 smsv pyrite matrix, minor pyrrhotite (1-31).

Pyrite ± pyri tite mineralii is largely cor able to fabrj 60 deg. to o. especially w) more abundani

601 pyrrhotite and 151 pyrite.


DIAMOND DRILL CORE LOG Project No. 287

Shot No ————3——OF.

Hoi* No. UK-90-1

Property Mikwam

Depth 8. Lithology Detcriptton (colour, grain ilia, texture, structure, etc.) Alteration Mineralization Remarki

90.7-97.s Felsic fragmental - tightly packed, homogeneous, massive overall appearance. 5-81 fine stringer pyrite as matrix.97.5-105.4 increasing pyrite, ID-15% Crude banding 60 deg. to c.a. Heavy pyrite over last meter.

IPS.4-109.2 Pyrrhotite bearing section. Also pale green chlorite bearing silicate interlayering in irregular wispy fashion, S-10%.

107.7-108.91 section.

More Massively felsia

109.2-112.6 151 pyrite -f lesser pyrrhotite (S-5%). still moderately to distinctly layered in appearance, 60 deg. at 111.0.112.6-120.3 Heavy sulphide zona. 35| combined pyrite and pyrrhotite (901 vs 101), At 113.0, first notable appearance of dark wispy areas of blackish grey chlorite? associated with sulphide matrix to felsic pyroclastic flow material. Chloritic component constitutes only 3-St of section but is local in occurrence and up to S-10% over narrow (20-3Ocm), widths.

92.7-99.0 several *:lcm quartz veins, white.

5-8\ pyrite through out section.

None of note. Rare whitish veinlet of quartz, in more smsv to msv pyrite cones gangue to the pyrite is pale calcite (HCL reaction eg at 113.4m.

Pyrrhotite content 10-151 thin, semi- massive, irregular laminae.

lG-12% pyrite, 3-51 pyrrhotite.

351 pyrite and pyrrhotite (90/10).

WR at 92m (St

2-31 pyrrhot: pyrite dissemJ in fine grail felsic ground Sample is hon eous, massive lacks fragmei look.

WR at 108.5m. (5838).


DIAMOND DRILL CORE LOG "o,*.**Sheet No. ———4 rtf

Hole No. ————MC-M-I

Depth 8. Lithology Description (colour, grain size, texture, structure, ttc.) Alteration Mineralization Remark*

120.3-124.BS lot pyrite) and 31 pyrrhotite). Some short section* up to 201 over lOom. Very laminated but with irregular slightly contorted structure. Light grey silicate (felsic tuff??), dark grey sericitic material, other various shades of grey forming finely laminated to jumbled, irregular sequence to which the sulphides act as matrix. Banding scale is typically lam to l or 2 cm but very irregular and contorted. Some of the very pale-near white masses are fine grained quartz (chert??), very hard in many places. Core angle 55 deg. at 123.4m, quasi banding.

l24.85-i2S.is MSV pyrrhotite and lesser pyrite and irregular white chert/quartz masses up to 2 cm across. Non bedded. Pyrite phase floats in pyrrhotite.12s.is-129.,p More homogeneous felsic pyroclastic, heavily disseminated pyrite and pyrrhotite blebs, occasional smsv, fine grained, pyrite pyrrhotite interval usually O-4 cm, S-10% sulphide overall.

129.9-131.9 increased proportion of pyrite and lesser pyrrhotite as matrix to coarsely structured felsic pyroclastic.

131.9-133.7 As 125.15-129.9.

701 pyrrhotite and pyrite (50/50)

S-10% pyrrhotite and pyrite.

15t pyrite and pyrrhotite.

S-10% pyrite and pyrrhotite.

NX at 126.3m fine grained fairly inhomo geneous felsi fragmental. (5839)


DIAMOND DRILL CORE LOG Project No.

Property -

287ShMl No.

Hole No. -

-OF-

MK-90-1

Mikwam

Depth 6 Lithology Description (colour. grain size, texture, structure, etc.) Alteration Mineralization Remarks

^.33.7-14^.2 Heavy sulphide zone - cherty •imilar to 112.6-120.3. Felsio fragmental component le** recognizable (virtually absent). Dominated by *m*v pyrite, *ome spherules and chert - latter form distinct laminae with pyrite.

144.2-146.5 Less vol. looking component-io-h.5% dark, chloritic material with finer laminae of tuff or sediment. Characterized by darker colour overall and fine kink-folded lamina tion (*:icm scale). Distinct volcanic component reappears intermittently after 145.3.

146.5-160.e Distinct felsic pyroclastic section heavily mineralized with 15-201 matrix pyrite and minor pyrrhotite. Fragments are matrix supported and range up to 6cm in cross section. Occasional section more homogeneous and massive in structure, usually *:1 meter in thickness (eg 156.7m). Cor* angle at 1SS.S l is 60 deg. - foliated (attitude of fragments]).

154.0-157.5 Sulphide component falls off to lot. Fragmental nature of volcanic still evident.

157.5-160.8 AS 146.5*154.0. Core angle at 159.1, 60 deg. - fabric/fragments.

116.S7 Quartz vein l-2cm vide. 35 deg. to o.a., minor pyrrhotite.

188.39 QuartE vein 2.Son vide, 30 deg. to o.a.

60-701 pyrite, minor pyrrhotite (ot) overall but heavy pyrrhotite 143.5- 144.3 (301).

pyrrhotite. Pyrrho tite lot of total sulphide.

20t smsv pyrite, minor pyrrhotite.

10-20t pyrit*

lot stringer pyrite, minor pyrrhotite.20t smsv pyrite in in unit, minor pyrrhotite; no notable sulphides in quartz vein.


DIAMOND DRILL CORE LOG t**.* -illProperty

Sheet No. ———fi

Hoi* No. MK

-OF-

Depth ft Lithology Description (colour, grain site, texture, structure, etc.) Alteration MinereDution Remerks

160..8-164. q sulphide)* down to 101 similar to 154.0-157.5. Fragmental appear* nore tightly packed, fragmental nature lees distinct.

164.9-170.1 Gradual increase in fine grained smsv pyrite patches and bands. Pyrrhotite content 5-101 of total sulphide which averages 10-151. Distinct, uniform structure-laminated but not clearly a bedding-type form with discrete beds.

Core angles: 70 deg. 9 166.0m80 deg. 0 167.5m80 deg. e 167.8m

Crude laminae Crude laminae Crude laminae

Felsic fragments are a medium to pale grey. They assume a more laminated structure relative to the sulphides. Sul. component relative fragment structure is very even and uniform. Pale whitish calcite finely distributed (51) in sulphide areas. Sulphide acts as matrix to the volcanic fragments.

1(0.1 3cm wide quartz vein 70 deg. to o.a.

161.4 3cm quartz vein 30 deg. to o.a.

163.0 lorn quartt vein 65 deg. to o.a., coarse pyrrhotite and pyrite at margins.

Hone of note.

Quarts vein contains incorporated pyrite from host rook.

Minor pyrrhotite at margins.

ID-15% pyrite ± pyrrhotitei pyrrho tite 5-101 of total sulphides.


DIAMOND DRILL CORE LOG Project No. 287Sheet No.

Hoi* No. -MK-90-1

Property Mikwam

Depth a. Ulhology Description (colour, grain tin, texture, structure, ttc.) Alteration Minerelitetlon Remerki

170.1-177.3 Continued decrease in sulphide content with this interval carrying only 5-10* pyrrhotite ± pyrite (pyrite 20-251 of total sulphide). Volcanic phase nore tightly welded, in places has nore finely laminated, bedded look. Other sections continue to have irregular look due to the presence of sul. with short stringer type matrix character (Iron wide slivers t blebs),Occasional section, up to 10-l5cm with 20-401 pyrrhotite as fine grained, sns laminae. Also, one interval at 169.9m. Similar to mineralization style in 170.1- 176.2 interval. Core anglest 60 deg. at 170.0m - foliation/laminae. 60 deg. at 173.4m - foliation/laminae.

175.3-175.8l mass.

Irregular quarts vein

176.21 20cm, grey-white quartz vein.

176.45-177.41 Several narrow grey- white quartz veinlets in l-2cm width range. Attitudes vary-some are conformable, at least two cross cut the fabric at 40 and 60 deg. respectively.

Quartz vein(ing)- irregular masses of quartz, grey white colour.

Quartz vein.

Several quartz veinlets.

S-10% pyrrhotite ± pyrite; pyrite 20-2St of total sulphide. Note pyrrhotite more dominant.

Zn S blebs in low angle (20 deg.) oaloite/quartz veinlet at 169.6m and at 171.om. Blebs are up to 3mm long by width of veinlet 2-3mm.

Sulphides-marginal to quarts-related more to host volcanic.

No sulphide other than those related to hosting lithology.



ShM! No.

Hoi* No. - mc-90-1

Properly Mikwam

Depth It Uthology Detcrlptlon (colour, grain tin, texture, •truclure, etc.) Alteration Mlnerellntion Remerkt

177.3-1*6.7

INTERMEDIATEVOLCANICFLO*

Lower contact at 177.3 is arbitrary due to gradational change in rook type. Change i* from a pale medivun grey, sulphidic, aphanitic to very fine grained felsic pyroclastic (welded? or pyroclastic flow) to a nore intermediate tuff.

Fine grained, medium greenish grey colour. Generally massive groundmass but some sections display an overall coarse fabric. Characterized by prominent amount of very irregular quartz and quartz carbonate veining and masses of same-estimate lQ-15% of section. Veining does not appear to be mineralized. Unit probably of andesitio composition.

Core anglest 40-70 deg. throughout - not well defined as unit is largely without prominent fabric - flow material (?). Lower oontaot indistinct over .4 meters.

ID-15% quartz, quartz-carbonate veining, very irregular in distri bution and attitudes. No related hydro thermal alteration to host rock.

188.12-189.7 vein.

Quartz

1*4.41-1*4.7 Several narrow quartz veins.1*9.6-194.ft 30-351irregular grey white quartz-quartz/oarbonate vein material. Very irregular attitudes.

Andesite contains occasional small patch of pyrrhotite and pyrite.

WR e 180.6m.(5840)WR 8 192.9m.(5841)

Trace pyrite, pyrrhotite.Trace pyrite, pyrrhotite.Trace pyrite, pyrrhotite.


DIAMOND DRILL CORE LOG Project No, 267

Sheet No.

Hoi* No. MK-90-1

Properly ttikvan

Depth d Lithology Description (colour, grain tlie, texture, tlructure, etc.) Alteritlon Mlnerellutlon Remerk*

19*.7-203.4

GRAPHITIC ARQXXiLXTE

203.4-238.9

METASXLT- STOmS-WACKB

Dark grey to black, indistinct bed* but finely laminated. Distinct parting parallel to lamination fabric. Core angle; 60 deg. at 199.7. Consider to be locally conductive, very weakly so a* overall graphite component weak except for 297.2-297.7 which ha* good graphite development.

Several quarts vein*, grey white colour and of barren appearance. No hydrothermal alteration associated with veining.

Lower contact i* gradational into medium to light grey siltstone-waoke*. contact arbitrary.

1*7.4 Quart* vein at 40 deg., 2om wide.

209.9 6cm quartz vein, 60 deg.201.19 6cm quartc vein, 80 deg.

201.as 7cm quartz vein, 60 deg.

St irregular, wispy pyrite a* laminae lenses, matrix stringers etc.

Trace only pyrite/ pyrite in all veinlets.

Fine to very fine grained, medium grey colour. Coarsely bedded, individual beds range up to 10 or 15cm. Bedding fairly indistinct in detail but evident on gross scale. Homogeneous lithotype. Texture of groundmass tends to be massive. Rare green mud intercalation of irregular outline (eg) at 210.2 next to quartz vein mass. Moderately hard, no clasts or phenocryst*. In places has fine fabric but not prominent overall. Core angle: 60 deg at 213.4, bedding.


DIAMOND DRILL CORE LOG pro,.c,No.?jiProperty -

Sheet No, ——10 ft

Hoi* No. MK-SO-1

Depth 6 Lithology Description (colour, greln size, texture, atructure. etc.) Alteration Mineralization Remarks

232.9-242.3

FBLSIC TOFF(SERICITESCHIST)

Several grey white quartz veins with barren look. No associated hydrothermal alteration.

206.7-207.1 Moderately deformed interval with graphitic bands. Chevron-type folds. Occasional lithic clast Inn of dark graphitic sediment.

224.33-226.4 Crackle fracture patternin siltstone-wacke. Dark fracture.filling.230.3-232.9 Finely bedded, graphitic argillite, dark grey to black. Core angles variable 50-70 deg., average 60 deg. at 230.6m.

Cored surface very light grey, sericitic. In area of quartz veins, irregular foliation about veins and very sericitic. Strong, schistose cleavage fabric. Core angles consistently 50 deg. to o.a. (eg) at 239.6m. Minor disseminated pyrite K: 1mm blebs locally.

2X0.24-2X0.7 Grey- white quartz vein.

218.010cm.

Quartz vein,

23X.35-23X.C2 Quartzvein, glassy grey/ white 40 deg. to c.a.

832.18-892.4* Quartzvein, glassy grey/ white 30 deg. to o.a

232.9-233.4 Quartzvein as above, very irregular outline.

233.87-233.8 Quartzvein as above.

233.9-834.8 3 narrow quartz vein occurr ences as above.

Nil to trace pyrite/pyrrhotite.


WR at 213.8 clean siltst wacke. (5842

No visible sulphides.

As above.

X-3% pyrite as matrix to frac tured quartz.

No visible sulphides.

No sulphides.

WR at 235.0(5843)

WR at 241.4.(5844)

NORANDA EXPLORATION COMPANY LIMITED Shot No. OF-

DIAMOND DRILL CORE LOG w*. .287 MK-90-1

Property Mikvam

Depth ft Lithology Description (colour, greln site, texture, structure, etc.) Alteration Mlnereliietlon Remarks

242.3-265.3

XNTERXBDXATB TO XA7ZC QUARTZ- 7BLD8PAR PORPHYRY

Fresh surface, pal* grey, very Cine grained. Moderately magnetic due to pyrrhotite content. Distinctly laainated in most bedded sections (l en scale). Lower contact sharp 50 deg. to o.a. Mafic below does not show evidence of chilling but is moderately foliated.

Dark green groundmass, in places weak pinkish red oast from feldspar phenoorysts or fine feldspathic accumulations of small grained site. Cored surface displays distinct l-2mm sited bluish quartz phenocrysts 1-31. Outlines are subrounded to rounded. Persistent through out, but somewhat variable in concentration. Feldspar are more variable in occurrence and sire, sice range is Klmm to 5mm, averaging about 2-3mm generally without crystal form. Average concentration is 5-81 where developed. Colour is generally pale greyish white but in place* may take on pinkish oast (hematite?). Texture varies from massive to foliated but in much of unit there is a fabric usually at 40-60 deg. eg 60 deg. 259.5. Unit is moderately magnetic, caused by fine grained magnetite.

264.2-26^6 QuartE vein, irregular, barren appearance. Several short 2-3cm intervals with faint pinkish cast, possibly hematite alteration in groundmass.

No hydrothermal alteration effects.

Estimate a-3% disseminated pyrrhotite locally.

Very minor, narrow quarts veinlet, 1-31 randomly occurring through unit.

X-5% disseminated pyrite.

WR at 245.5 WR at 255.6 - 10-15 feldspe phenocrysts.


DIAMOND DRILL CORE LOGSheet No.

28?Project No.

Properly .—.i

12

MK-90-1

.OF-

Depth V Lithology Description (colour, grein size, texture, Mructure, etc.) Alteration Mineralization Remarkt

285.3

277.0-277.6 QuartE vein 30 deg. to o.a.* irregular. Texture of porphyry i* finer over last 1.5m.

END OF HOLE

34. DOS NORANDA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOGProject No 287

Sheet No. -J——— O

itoi-iL. MK-90-2

ELEVATION Surface M*en*tlc Bwlng

CorrtcMd Boring

DIP AT COLLAR

TOTAL DEPTH -

52"

.Om

Timmins

- BEARING

CORE SIZE

6.8. 60m 54 0 Property Mikwam

120m 53"

1 7/16'180m 54" NTS. 32B/5 TWP. noseworthy

240m 53300m 53"

REMARKS

Test up-ice stratigraphy from MOV-tTb-11 major BM conductor.__ ———

Sept. 16. 1990 completed Sept. 20.

Connector Morex Drilling——————.————.-

Logged by s - Harding

Depth li Llihology Oetcrlptlon (colour, grain tin, uxtur*. itruciuri, tlc.) Alurctlon Mlnerallutlon Remark*

0.0-46.3

46.3-63.5

XOTBRKBDIAT1 VOLCANIC

Casing

Medium to dark grey, fine to very fine grained with occasional fragments. Various interbedded units of pyroclastics, lapilli tuffs and tuffs. Upper 3m, pyroclastic (flow)? - fine grained with some coarser fragments, possibly graded bedding.

49.3-S9.B interbedded tuff and lapilli tuff. Tuff, very fine grained, hard, some quartz fracture zones up to 15cm. Lapilli tuffi lapilli up to 2mm, weak fabric, moderately hard.

59.8-63.s Pyroclastic?, weak to moderately strong fabric. Fragments vary in size from a few mm to 4cm, have been flattened in same direction as fabric. Clast supported in most parts. Possible minor interbedded sediments near lower contact. Whole zone contains s-10% water seams with strong limonitio staining. Weak to moderately magnetic due to pyrrhotite.

S-10% limonite staining due to water seams. No quartz veins, fracture zones filled with quartz. Weak pervasive carbonate alteration.

21 pyrrhotite, fine grained disseminated. li pyrite, fine graine disseminated with slightly larger concentration along fractures.

Similar to n in top part i

l hole 11, wit) notably less sulphide mim alization. Possibly dac otherwise andesitio.

MR % 55.1-55 (5812)



Property Mikwam

Sheet No.

Hoi* No ..

-OF-

-MK-90-2..

Depth k Lithology Description (colour, grain tilt, texture, •tructure, etc.) Alteration Mineralization Remark*

(3.5-66.2

INTBRBBDDED JUMILLITE/

vonr

66.2-75.7

INTBRXBDIXTB VOLCANIC

Fine to very fine grained, medium to dark grey to black (argillite). Lapilli tuff, intermediate, lapilli sice up to 2mn. Moderate fabric parallel to bedding argillite/occasionally subparallel. Moderately magnetic. 21 limonite staining.Argillite - 35-401 of cone. Occurs in beds, .5cm - 15cm vide. Minor graphite in some beds. Bedding SO deg. to o.a. Beds are moderately soft. Weakly magnetic.

Lapilli tuff with interbedded tuffs, medium grey, lapilli size up to 2mm. Intermediate composition.

67.7-72 t Q More felsic tuffaceous interbeds. 101 limonite staining. ^5t quartz patches along fractures, weakly magnetic.

69.5-69.7 Quartz filled fracture cone with 21 fine grained disseminated pyrite.

69.7-70,6, strong limonite staining, broken core.

73.1S-73.S Quartt/minor carbonate cone with 21 fine grained disseminated pyrite.73.6-73.85 Quartc/minor carbonate fracture cone with strong limonite staining.

21 limonite staining due to water seams.

1-2% limonite staining along water seams.

101 limonite staining.

li fine grained, disseminated pyrrhotite in lapilli. 2t fine grained pyrite along water seams with limonite.

2\ fine grained pyrite in very narrow stringers parallel bedding, l* dissemin ated py and po along bedding planes.

2t fine grained disseminated pyrrho- ite. Ik fine grained disseminated pyrite.

WR at 71.75-71.9.(5813)


DIAMOND DRILL CORE LOGSheet No. .OF-

Project No. 287

Property .

MK-90-2

Depth d lithology

75.7-66.4

INTERBEDDEDTUnr/ORAPHX-TIO AROXUiXT

Description (colour, grain size, texture, itructure, tlc.)

Mediua grey to dark grey and black aeargillite increases downhole. Tuffcomponent of intermediate composition

75.7-78.2 Tuff with ^* argillite!l 31 limonite staining. Weak tomoderate fabric. 21 quartz/carbonatepatches.

78.2-86.4 50* tuff and 50* ^raphltieargillite. 51 quartz/carbonate blebsand stringers in the tuff followingthe fabric - 11 pyrite with some. 10*limonite staining occurring alongnarrow water seams, not as pervasiveas in above units. Hon magnetic.Argillite bands frequently have indistinctcontacts. Argillite increases downholeto 801.

80.3-84.5: Core very broken up, smallpieces.

51 crosscutting quartB/oarbonate veinletsnear bottom contact.

84.6: Bedding 60 deg. to c. a.

Alteration

31 limonitestaining.

101 limonitestaining.

Mineralization

5-101 fine graineddisseminated andeuhedral pyriteoccurring In patchesup to 5cm and alongfabric/bedding planes.5* fine graineddisseminated pyritein tuff.St fine graineddisseminated pyritein narrow stringersand blebs alongbedding planes inthe argillite, thoughsome does occur alongthe fabric in thetuff. Odd stringercrosscuts bedding.

Pyrite increases to10-151 near bottomcontact as argilliteincreases.

Remark*


DIAMOND DRILL CORE LOG Project No. .

Property —

287ShMl No.

Hot* No.

.OF —

MK-90-2

Mikwam

Deptht, Lithology Description (colour, grain size, texture, ttructure, etc.) Alteration Mineralization Remarks

86.4-93.5

GRAPHITIC AROILLITB

•3.5-98.4

INTERBEDDED GRAPHITIC ARGILLXTB/ GRBYWACKB

Gradational upper contact, minor tuffaceous fragments, dark grey to black. Fine grained, 101 quartz/minor carbonate blebs (up to ion) and veinlets parallel to bedding. 151 pyrite. Core broken up into snail pieces throughout this unit, this unit.

87.1-89.6 Milky quartz vein. SI f.g., disseminated, euhedral pyrite in blebs near upper contact and one 3cm patch in centre of vein, occurs as blebs and disseminations in lower 60 cm of vein. Trace pyrite in rest of vein. Quartz vein broken up in places. Argillite moderate to strongly graphitic below quartz vein. Some larger quartz/ carbonate areas up to 4cm across below quartz vein.

Dark grey to green to black, fine grained. Unit divided into zones of predominantly argillite, or greywacke. 151 quartz/ carbonate blebs and veinlets with the argillite and 31 with the greywacke. Argillite beds are moderately contorted, show no preferred orientation. Very weak fuohsite/chlorite? in one 10cm section of greywacke. Increasing greywacke down section.

No limonite staining.

151 fine grained disseminated pyrite occurring in blebs up to 2cm and as stringers. Usually found with quartz/ carbonate. Some massive patches up to 2.Sem. Pyrite mostly parallel to bedding.

51 pyrite in quartz vein, patch occurrence trace in remainder.

15-2Ot fine grained pyrite (disseminated and euhedral) in the argillite. Occurs as semimassive patches up to lcm or as smallei blebs and stringers. Follows the contorted bedding. 21 fine grained pyrrhotite is found within the larger patches of pyrite.


DIAMOND DRILL CORE LOG Project No. ...287,

Property .

Sheet No.

Hole No. .

.OF —

MK-90-2

Depth li Lithology Description (colour, grain (It*, texture, *tructure, etc.) Alteretlon Mineralization Remark*

98.4-216.5

ORBYWACXB

Light grey-green to medium grey, fine grained. Massive with weak fabric in some places. Pale green chlorite evident in some sections. Minor sections up to 10cm of a coarser material possibly a result of graded bedding. 2 1 quart t grains up to 5mm, random distribution. 3-5t lithic fragments up to 3om. 5t quarts/carbonate veinlets and blebs up to 3cm, randomly orientated.

2 1 leucoxene?

lorn patch of fuohsitic? material.

1Q7.Q-iifrn p Rook btoones slightly nor* ohloritiEsd, darker grey green. More siliceous, J.5% quartz/carbonate veins/patches up to 6cm with 31 pyrite. 31 quartz stringers, again random orientation.

2-31 pervasive carbonate alteration. Weak chloritic alteration.

Weak to moderate chlorite alteration.

2-31 fine grained disseminated pyrite in greywacke, also 1mm bleb* in areas of quartz/carbonate blebs. Pyrite increases as argillite component increases.

2\ fine grained disseminated pyrite, some occurring in blebs/ragged stringers, no preferred orienta tion. Some occurs with quartz/carbonate Odd small areas with up to 51 pyrite. Starting at 103.5, It fine grained pyrrhotite, minor blebs of pyrrho tite up to 4mm. Starting at 116.3, trace pyrrhotite.

WR 9 102.9-103.1. (5814)


DIAMOND DRILL CORE LOG Project No. 287.

Sheet No. ———fi———OF —

Hole No. MK-QQ-2

Proptrty Mikwam

Depth*, Lithology Description (colour, grain tilt, texture, structure, etc.) Alteration Mineralization Remark*

109 . 4-110 . 5 i Silicified zone with chert?, possibly a vein but contacts not distinct, sons sediments in con*. 2% pyrite, ^* pyrrhotite.

119.0-12S.O Less chlorite, back to predominantly grey colour. Massive texture, 51 quartz/carbonate blebs, stringers. No quartz grains.

125.0-179.6 Pale grey/green with patches of dark grey, some lighter areas where greywacke has been bleached? Still massive but some areas show a weak fabric. 35-401 quartz/carbonate as small blebs (3mm) , veinlets/veins up to loom, or in siliceous patches. Some veins show a preferred orientation, but the majority are randomly oriented and ragged. Non magnetic.

125. 0-125. 6 i 901 quartz/carbonate patch, no sulphide mineralization.

144.2-l50.lt Decrease in quartz/ carbonate to I5t. Slightly more chloritic.

154.0-154.9, 155. 4-156. 3 1 Silicified sections of 90t quartz/minor carbonate, trace pyrite.

Weak pervasive carbonate alteration.

51 pervasive carbonate alteration. Trace chlorite.

Starting at 122.0 *:tt pyrite.

fine grained disseminated pyrite.

WR i 152.0-152.2. (5815)

143.0-179.4 tt fine grained pyrite, as l-2mm blebs, with only trace finely disseminated pyrite.

^fl^^UMtf


DIAMOND DRILL CORE LOG Project No 287————

Properly Mlkit*m

Shot No.

Hoi* No. -

JZ__ Of-:

MTC-QO-7

Depth 81 Lithology Description (colour, griin size, texture, •tructure, etc.) Alteration MlnereliMtlon Remerk*

161.0-162.3, 165.0-166.41 Sectionswith coarser grain sit*, weak to moderate bedding? 60 deg. to o.a. at 161.5. Fragments up to 4on elongated with the bedding, lot quartz/carbonate blebs up to 2cm, generally follow the bedding. Tr. py.

179.6-191.7 coarser grained thanabove. More chloritic, resultingin a medium grey green oolour. Smallinterbeds of finer material. 101 quartz/carbonate veins up to Son thick and asstringers.

183.1-183.6: Quartz/carbonate zone with it pyrite.

186.0-186.31 Silicified With31 pyrite, 51 pyrrhotite.

191.7-208.s Returns to finer grained greywacke with odd coarser bed. Decrease in ohl content, weak to moderately developed fabric. 10-151 quartz/minor carbonate veins (up to 7cm), stringers, and patches most of which are oriented with the fabric. Veins contain 31 pyrite, It pyrrhotite. Starting 197.0, it leucoxene.

Weak carbonate alteration. Weak to moderate chlorite alteration.

Weak chlorite alteration.

at quirti/Minor oarbonit* 3m with 15t disseminated

aoo.i-200,71veins up to 7cmpyrite in blebs, trace pyrrhotite.

It fine grained pyrite in blebs up to 5mm or in slightly larger concentration.

ISC.0-191.7 3t fine grained pyrite, 3t pyrrhotite ooourrim mainly as local concentrations.

191.7-194.S Itdisseminated pyrite.

194.2-208.5 3-5t disseminated and subhedral pyrite in stringers and blebs. It pyrrhotite. Most mineralization occurs with quarts/carbonate,


DIAMOND DRILL CORE LOG Project No. 287She*! No.

Hole No..

8 .OF —

KK-90-2

Property Mikwan

Depth 81 Lithology Description (colour, greln alia, texture, ttructure, etc.) Alteration Mineralization Remark*

216.5-223.4

SILICEOUS IRON

203.7-204.4, 204.6-204.91 Large zones of predominantly quarts; 31 pyrite, li pyrrhotite.

55 deg. to o.a. at 207.7 - quarts vein.208.5-216.5 coarse grained greywacke. Fabric is 50 deg. to o.a. in top portion and flattens out to 20 deg. at lower contact with iron formation. 101 quartz/carbonate veins/ blebs with generally the same orientation as the fabric. Larger quartz veins contain 5* pyrite, 2k pyrrhotite. Overall fabric becomes more contorted closer to the lower contact.

White to dark grey, 701 quartz with minor amounts of carbonate, sugary chert, and interbedded greywacke. Quartz occurs mainly as blebs up to 3om with minor larger patches. Fabric is contorted and generally runs from 20 deg. to parallel to o.a. Variably magnetic from weak to moderately strong. 31 irregular, contorted magnetite bands up to lcm in width.

3t disseminated pyrite, It disse minated pyrrhotite. Most mineralization occurs with quartz veins.

S-10% fine grained pyrite in blebs up to lorn with odd medium grained euhedral pyrite. 6* fine grained pyrrhotite occurring in ragged stringers along the fabric and in lorn blebs. Mineralization predominantly found with quartz.



Hoi* No.

.OF —

HK-90-2

Mikwaa

Depth tt Lithology Description (colour, grdn tlte, texture, structure, etc.) Attention MlnerellMtion Rtmerki

223.4-229.4

QREYWACn

229.4-272.4

CHERTY/ CHLORITIC OXZDB IROM FORMATION

Medium grey-green, fine to slightly coarser grained. Weak to moderate fabric. Fabric varies from 20 deg. to c.a. at upper contact to 55 deg. at lover contact. ^\ quartz/carbonate veinlets and patches. Variably magnetic from weak to moderately strong at lower contact.

Weakly chloritic.

Colour variable from white/cream to green to dark green/black.229.4-238.0 similar to above iron formation. 601 qtz with ainor amounts of carbonate and sugary chert. Remainder is moderately chloritic sediments with minor amounts of greywacke. Moderate to strongly magnetic. 101 Magnetite bands up to acm. Fabric generally weak du* to predominance of quartz but strong in areas of magnetite bands - 55 deg. to c.a. at 231.0m. Quartz fomrs silicified zones made up of connected quartz blebs up to 3cm in size, edges of blebs usually marked by mineralization.

Moderate chloritic alteration in sediments.

31 pyrite found mainly in quartz veins.

227. t l cm vein of pyrite. 51 fine grained disseminated pyrrhotite in the greywacke with 2t pyrrhotite blebs with quartz veins.

10-151 pyrite-ooours mainly as fin* grained blebs and veinlets up to 2mm with some euhedral cubes up to 3mm. 151 fine grained pyrrhotite as blebs stringers and disse minations along fabric Mineralization is predominantly in quart! rich sections, and foi: ows the fabric in the sediments.


DIAMOND DRILL CORE LOG 287ProjKI No. .

property Hikwam

ShMt No.

Hoi* No. -

10 -OF —

MK-90-2

Depth tt Lithology Description (colour, grain *lze, texture, structure, etc.) Alteration Mineralization Remarks

23B.O-2S2.0 Decrease in quartz to 401, still in patches, with minor crosscutting quartz/carbonate veinlets. Remaining 601 is predominantly dark green chloritic sediment with 20t creamy chert. Sediment shows a generally strong fabric and is slightly contorted in areas of quartz. Fabric orientation varies from 50-80 deg. to c.a. S-8% magnetite bands up to 3cm wide found with the sediments and chert. Chert primarily in bands, up to 8cm wide with odd irregular blebs in quartE.

245.4-245.8t l.Som quartE/carbonate vein parallel to o.a. with no mineralization.250.6-251.5, 251.7-252.01 QuartE patches with 301 fine grained pyrrhotite in blebs up to 3cm, 101 pyrite in blebs and disse minations, minor chloritic sediments.

252.0-265.0 There is a decrease in quarts to 151 and an increase in chert and chloriti sediments, some coarser sed. presence. Band are more distinct and larger, some up to 20cm. lQ-15% magnetite bands, average size 3cm, some up to loom. Fabric of magnetic bands and chloritic sediments varies but average is 60 deg. to o.a., strong fabric very little contortion.

257.7-258.1, 258.2-258.65, 258.9-259.21Quartc veins with 401 pyrrhotite, 101 pyrite with most in massive patches up to Sem.

Moderate to strong chloritic alteration in sediments.

3Strong chloritic component to the sediments.

10-151 pyrite occurs predominantly in stringers/veinlets up to 5mm wide or in semi-massive patches. 2t fine grained . disseminated pyrite in the sediments. 15-201 pyrrhotite, mainly found in semi- massive patches up to 3cm or in veinlets/ stringers surrounding quartE patches. All sulphide mineralizatioi occurs mainly in association with the quartz.

1-2* pyrite/pyrrhotite stringers crosscutting sediments.



She*! No

Hoi* No. ,

11 .or-MX-90-2

Property — Mikwam

Depth li Lithology Description (colour, grein (In, texture, structure, etc.) Attention Minerillzetlon Remark*

265.0-272.4 Quartz increases to 25%. Chert and magnetite bands decrease to St. Weak to moderate fabric. Increase in sulphide mineralization.

872.4-298.0

GRAPHITIC AROILLITB

Dark grey to black with white quartz veins, fine grained. Minor interbedded greywacke. 151 quartz veins and irregular patches, max. size 3cm, no large quartz patches as in iron formation. Weak to moderate folia tion usually outlined by sulphides SO deg. to o.a. at 280.0m. Moderate to strongly graphitic.

Heavy pyrrhotite, pyrite locally throughout unit.

277.0-282.B Decrease in quartz to 51, smaller veinlets up to 4mm in size. More greywacke, coarser sediments.

Up to 401 pyrrhotite, lot pyrite in qtz-rich patches, lot disse minated pyrrhotite/ pyrite with minor blebs/stringer* in the sediments.

266.* 5mm vein of pyrite with 101 pyrrhotite.

269.0-269.3, 269.4- 269.9 Almost massive pyrrhotite with 20t pyrite with quartz.

251 pyrrhotite in irregular blebs and stringers or in massive patches up to 5cm. 15t pyrite in stringers or blebs up to 5mm and with the pyrrhotite. Mineralization is predominantly in the argillite with only st in quartz veins.

Starting at 279.5 pyrite becomes the dominant sulphide.


DIAMOND DRILL CORE LOGShMlNo. -OF —

Projtct No. 287 MK-90-2

Property

Depth d Lithology Description (colour, grain site, texture, structure, etc.) Alteration Mineralization Remarks

282.8-293.0 Quartz increases to 201 in veins and blebs up to 15cm, sharp contacts, random orientation, ^1 sulphides with veina and irregular quartz masses. Total pyrite, pyrrhotite contact 15-201

291.8-291.9: Large quartz vein? with 51 pyrrhotite, 31 pyrite, minor amount of graphitic material.

291.65-292.65s Quartz vein, 11 pyrite.

298.0-325.0

INTBRBBDDBD ORBYWAOXB/ GRAPHITIC AROILLITK

293.0-298.0 Predominantly graphitic argillite with 20t greywacke. ^1 quartz veinlets, moderate to strongly magnetic. Weak to moderately graphitic. Estimate 151 pyrrhotite, pyrite overall.

398.0-307.1 Medium to dark grey, sol greywacke to fine to coarser grained, sol argillite, weakly magnetic, weakly graphitic, li quartz veinlets. Weak fabric, slightly contorted in places.300.9-30l.25: 2cm quartz bleb parallel to o.a. with li pyrite.

isi pyrite disse minated in argillite or in ragged stringers and blebs up to 3cm. 51 pyrrhotite in small ^cm blebs and string ers. 51 sulphides associated with quartz

280.2-880.4 Massive pyrite with round blebi up to 6mm in fine grained pyrite.

289.S-290.8 151pyrite, 101 pyrrhotite in argillite, pyrrho tite is in a 10cm massive patch with 51 pyrite.293.0-8*8.0 101 pyrite, both disse minated and in blebs up to 5mm, 51 fine grained disseminated pyrrhotite.

pyrite in grey wacke. 3-51 fine grained disseminated pyrite and pyrrhotite in argillite.


DIAMOND DRILL CORE LOG Project No.287

Sheet No.

Hole No.

13 -OF —

MK-90-2

ProperlyMikwam

Depth 4 Lithology Description (colour, grain •lie, texture, atructure, •le.) Alteration Mineralization Remark*

325.0

307.1-313.0 Dominantly argillite with only minor interbedded greywacke. 101 quartz veinlets and stringers. Fabric variable, parallel to o.a. in many places.

313.0-325.0 501 greywacke, 501 argillite. 101 quartz veinlets/stringers mainly in argillite. Weak fabric, varies from 30 deg. to parallel to o.a. Weakly magnetic.

END OF HOLE

S-5% fine grained disseminated pyrite and small 5mm blebs. *:il disseminated pyrrhotite.

51 disseminated pyrite and in tiny stringers, 11 pyrrhotite.

LATITUDE . 34.65S NORANDA EXPLORATION COMPANY LIMITED


Projtct No. 287,

Surface-50"

TOTAL DEPTH 321 .9m

GS 180"

BQ 1 7/16"

Ten Depth

film

Dip

,4ft*

Magnetic Bearing

Corrected Bearing

..45*183m -47"

REMARKS

Timmina Core Storage—-——-—. Testing up-ice bedrock stratigraphy from RG Holes 84-26 and 27.

?44ffl in*n

ii. -ii*

NTS —311/5-——— TWP. noseworthy ciaimNo. Jb63

SePt. 19. 1990 eamalmtma SftPt. 22.

Norax Drillin Zitd.

Pane CoratorhineDepth tt Lithology Description (colour, greln size, texture, itructure, etc.) Alteration Mineralization Remarks

0.0-46.3

46.3-77.0

INTBRHBDIATB VOLCANIC FLOWS(8) (ANDB8XTE)

Casing, bedrock at 45. 7m.

Fine grained, medium grey green, foliated groundmass. Andesite flow(s), occasional white ovals up to 6-8mm of quartzfoaloite-possibly amygdules. Massive overall structure, no bedding or laminae. 31 fine white quartz-oaloite stringers cutting core at various angles. Moderately fractured, occasional weak water seam. Core anglesi SO deg. at 48.On, 50 deg. at 67.5m.

Numerous white quartz veins of barren appearance.

B3.3-B5.3 501white glassy quartz veining, irregular outline.

as* a 10 on quartz vein as above.

84.8 10 en quartz vein as above.

Nil to trace sulphide.



66.Sm Whole rook (sample; 5821.



Project No. 267 MK-90-3-OF-

Properly Mikwam

Depth 8. Lithology Description (colour, grain *lie, texture, structure, etc.) Alteration Mineralization Remark*

77.0-78.2

80LPHIDB 20HB

78.8-86.9

INTERMEDIATE TOW (DACXTI AMDBfZTI)

86.9-120.7

INTERMEDIATE FLOW(S) (DACITE- AHDE8ITB)

56.8-59.4 section with 20 deg. cor* angle in foliation. Good amygdule development at 71.5m. Many massive textured sections, unit i* homogeneous. Lower contact marked by semi-massive pyrite mass at 25 deg. to c.a.

Initial 20 cm is smsv pyrite grading into weakly pyritio diffusely layered tuff of medium green to green-grey colours. Core angles: 35 deg. at 78.1m. Lower contact indistinct, somewhat interlaminated.

Fine grained, grey green to green colour. Strongly foliated, probably a weak shear structure 55 deg. to o.a. S\ fine grained oaloite as grains and streaks parallel to fabric-pale, white grey colour. Lower contact gradational,

Medium green to dark green. Similar to 46.3-77.0. Foliated, rare msv appearing section.

Core angles: 50 deg. at 91.345 deg. at 94.060 deg. at 97.240 deg. at 103.9

foliation foliation foliation foliation

No notable hydro thermal alteration. Minor oaloite in groundmass.

No significant sulphide occurrences.

Scattered quartzose laminae-sparse. 2 narrow 5cm quartzveins.

20t total pyrite-smsv to heavily disseminate* conformable wisps.

Nil to trace sulphides.

May be foliai flows due to shear stress*8*.8m Whole sample 5822

Some seotiont could be tufa aoeous but ne clear oontad between tuff and flow mate

109.9m Whole sample 5823


DIAMOND DRILL CORE LOGShxt No. -OF-

ProjtCI No. 287 HOI* NO——MK-90-3

Property Mikwan

Depth d Lithology Description (colour. gr*ln tit*, texture, structure, etc.) Alteration MinereliMtton Remark*

120.7-121.9

8HBAR BOMB

121.9-173.0

INTBRXBDIATB VOLCANIC (T07P?) (DACITB- ANDBSXTB)

Minor calcite as grain* in groundmass andesite. Minor quartz-caloite veinlets parallel to fabric. Width few mm up to 2can. 31 disseminated pyrite crystals 97.0-97.4 in strongly foliated section. In places rock approaches chloritic schist. Several quartz vein occurrences.

120.* 8 on quarts-carbonate with trace pyrite. Lower contact structured, defined by development of shear fabric.

Strong schistose fabric 45 deg. to c.a. small fragments of volcanic floating in fine grained pyrite-oaloite matrix. Sections quasi-banded (-clem scale). Dark blackish green coloured silicate with pyritio laminae (l-2mm) and matrix. Lower contact distinct 30 deg. to o.a. Following unit still well foliated, medium green grading into darker green volcanic. Consider this unit (120.7) as similar to 78.2-86.9.

Similar to more foliated sections of 86.9-120.7. Medium to dark green, well foliated. Strong schistose cleavage, producing lustrous surface. Fabric is 40 deg. to o.a. at 127.0m. Some suggestion in the foliated texture of small fragments particularly between 136.0 and 152.Om.

108.4-111.3 Number of narrow, glassy white quartz veins conformable to irregular in attitude

Weak calcite in pyritio matrix.

SI fine grained calcite streaked through groundmass in wispy fashion.

130.88 14cm quartz vein, irregular outline, glassy white quartz.

No significant sulphides with quartt-oarbonate veinlets.


10-15t pyrite.

Trace fine grained disseminated pyrite.


181.7m Whol rook sample 5824.



Project No.

Property -

MK-90-3

Depth A Lithology Description (colour, grain *ize, texture, structure, etc) Alteretlon Mineralization Remark*

142.0-145.5 Section displaying very strong fabric. Son* suggestion of possible snail lapilli olasts but may only be function of shear deformation. Attitude 35 deg. to c.a.

Other core angles: 50 deg.40 deg. SO deg. 35 deg.

6 130.4 foliation e 136.4 foliation 6 140.2 foliation 9 149.1 foliation

156.9-160. q Homogeneous section lacking tuffaceous look. Still with overall fabric, but not pronounced. Some suggestion of amygdules.160.6-161.1,fabric.

Quarts vein, conformable to

161.1-163.a Foliated to schistose volcanic as 121.9-142.0.163.3-163.8 Quartz vein masses as 160.6.

163.B-167.S Foliated as 161.1.

165.0-165.31 Three narrow quartB veins similar to 160.6 etc. Conformable to fabric which is highly schistose in vein section.

167.s-169.B Xnhomogeneous section, palercolour, weakly formed brownish streaksdue to fine mica. Pale buff- white feldspar

Weak carbonate alteration. Pervasive through groundmass.




^^^^^*MMM*


DIAMOND DRILL CORE LOG-OF.

Projicl No. ,

Property —

287 Holt No. MK-90-

MikwarnDtpth li Lithology Dttcrlptlon (colour, gr*ln ilit, Uxlurt. itruelurt, *lc.) Alteration Mlrwdlutlon rUmtrkt

173.0-196.9

TBL8IC VOLCAKIC F LOW (8)

phenocryst* occurring in localized Banner. Strong foliated fabric. Contact* indistinct -appear to be gradational alteration cone, no veining, no clear oarbonatitation. Core angle 40 deg. at 168.0.

169.5-173.0 Return to intermediate tuff as 163.8m. Lover contact distinct, but greyish green in first 3-4n of next unit suggests clearly homogeneous felsic section may start about 176.3n. Breccia texture in felsic at 173.9 .4n wide.

Very fine grained, near aphanitic. Medium grey grading locally into greenish grey sections of -elm. Some pale crosscutting fractures with alteration halos. Generally massive structure but some areas display a foliated fabric. Quartz phenoorysts noted only at 177.6m. Quite hard, difficult to mark.

Occasional 2-3cm quartz veins-glassy white, of barren appearance.

Stains moderately well for ankerite.

Scattered quartzveins,At 182.751 lOca,irregular qtz 70deg. to o.a.

183.6, 2 cm glassy white quartz vein at SO deg.

lt6.o, 2 cm quartz vein as above, 40 deg. to o.a.

Nil sulphides. Rook stainin- blue do not ) intense hydrc mally alter* appearance (usually a b colour).

S\ very fine grained disseminated po. Unit weakly magnetic throughout.

Trace pyrite only. Nil to trace pyrite/ pyrrhotite.



Initial 4m o: unit appears contain some intermediate (greenish) volcanic tufMR t 177.6m5825MR f 187.3m5826



Hole No -

.Of.

MK-90-3

Property Mikwam

Depth 4. Lithology Detcrlptlon (colour, grain size, texture, ttructure, tlc.) Alteration Mineralization Remarks

Cor* angless 55 deg. at 185.5 45 deg. at 190.5 60 deg. at 191.5 55 deg. at 195.6

60 deg. at 196.2

(foliation) (foliation) (foliation) (internalcontact) (internalcontact)

Some short intervals contain lensoid structures which may be compacted lapilli but these are exception* to the normal dense, near structureless, massive texture.i9S.s-i9S.a pyritio matrix, S-10% as thin, conformable stringers.

196.0-196.7 sol andesite interbeds with felsic, not clearly bedded-possible mixing. Green to grey shading. Lower contact sharp at 50 deg. to o.a.

186.2, 2 cm quartz vein as above, 35 deg. to o.a.

189.1, 3 cm quartz vein at 50 deg. to o.a.

Nil to tracepyrite/pyrrhotite.

Nil to trace pyrite/pyrrhot ite.'

101 pyrite as thin, msv, fine grained pyrite stringers.


DIAMOND DRILL CORE LOG a*-*,-2iiProperty .

Sheet No. ——2———OF.

Hole No. MK-90-3

Depth tt Lithology Description (colour, grain ill*, texture, structure, etc.) Alteration Mlrwfllutlon ((•marks

1*6.9-199.9

80LPHIDBZONZ/FBL8ICPYROCLASTIC(LAPILLITOW)-PYRITI(DACITE)

Similar to pyroclastic encountered in MK-90-01 below 77.3m. Characterised by distinctly fragmental appearance with heavily disseminated to msv fine grained pyrite matrix. Fragment to matrix ratio variable from 951 SI to 601 fragment vs

; 401 pyrite over 10-20 cm interval*. Fragments imbreooiated at 50 deg. to 60 deg. to o.a. Sice is variable from 2 cm thick down to l cm and less in length. Packing is generally moderately open to tightly packed and clast supported. More tightly packed sections become welded in appearance and over some widths have more homogeneous texture.

Fragmental is very fine grained to aphanitic in groundmass texture. Colour varies from buffish grey in case of larger olasts to medium grey in general. Unit displays well defined fabric averaging 45 deg. (SO deg. at top to 40 deg. at bottom). Lower contact distinct over several cm.

199.9-203.0

IHTBRMEDIATB VOLCANIC TOT: '(ANDB8ITB)

Foliated, very fine grained, medium green, lustrous sheen on broken surface. Texture is somewhat variable - lensoidal in places on small scale. No distinct bedding structures. Core angles: 55-60 deg., 40 deg. near lower contact (all foliation). Lower contact at quartz vein.

Non readily identi fied. Possibly very weak ankerite but staining is question able.

151 pyrite ± pyrrho tite overall. Range s-40% over specific intervals.

Non readily identified.

aoa.5 whoii rook sample 5827.


DIAMOND DRILL CORE LOGSheet No. -OF-

Prolecl No. 287 MK-90-3

Properly Mikwan

Depth 6 Lithology Description (colour, grain die, texture, structure, etc.) Alteration Mineralization Remark*

203.0-204.4

FELSIC VOLCANIC (DACITE- ANDBSITB)

204.4-204.7

SULPHIDE 20N! FELSIC PYRO- DA8XTIO(LAPILLI TUFF)-PYRITE!(DACITE)

204.7-210.15

IHTERXIXBD FELSIC TOFF IMTBRK8DIATB MUD OR TOFF (DACITE, ANDEBXTB)

Very fine grained, near aphanitic, grey tuff (possibly foliated flow unit). similar to 173.0-196.9. Appears nixed with chloritic, green sediment in placas- quasi laminated in fine scale. Streaky, laminated fabric. Lower contact distinct over 1-3 cm.

As portions of 196.9-199.9 which have pyrite-rich matrix. Clasts are elongate producing thin quasi~bands and distinct isolated fragment forms. Core angles 50 deg. to o.a. Lower contact gradational interlayering.

Faint, diffuse intermixing of grey siliceous tuff wisps and grey-green tuff or sediment. Several quarts vein occurrences, strong shear fabric develops from 208.0 to 209.3. Centre of shear is 208.9m at 35 deg. to o.a Finely laminated grey volcanic tuff and green intermediate mud/tuff.

No readily observed alteration, some localized next fractures.

No recognizablehydrothermalalteration.

209. (-20*.3 Quartz vein masses in highly contorted host. App roximately 15-201 vein material.

206.*, 2cm white-grey vein 35 deg. to o.a.

107.1, Son irregular quartz vein mass.

151 smsv pyrite.

Irregular stringer pyrite and smsv clots with qtz vein zone and sheared volcanic associated with vein. Estimate 101 pyrite overall.




DIAMOND DRILL CORE LOGSheet No. .OF-

HO** NO

MikwaaDepth 6 Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

210.13-210.i

FBLSIC LAPILLI TOW -PYRITIC

210.8-321.9

nSLSXC VOLCANIC PYROCLASTIC (DACZfI)

Similar to 204.4-204.7 in appearance. Foli. 60 deg. to o.a. Lower contact defined by sulphide content. Volcanic i* the cane.

210.B-21S.2 Sane daoitio rook type as above unit. Grey, very fine grained to aphanitic groundmass, very hard. Similar to 173.0-196.9 where "fragmental" appearance is not in evidence.

Core anglest 60 deg. at 212.5 50 deg. at 215.2

21S.2-231.6 Uniform section, occasional sulphidio section as at 217*6-216.1, 10-151 pyrite. Section is weakly porphyritic with small, scattered, white feldspar phenoorysts of anhedral outline. Section is distinctly monolithic, pyroclastic with matrix a little lighter and weakly calcitic. Rare quartz phenocryst. Core angles 50 deg. to o.a. at 216.5 - clast fabric, scattered pyrite throughout section.

207.5-207.95 Several l-2cm grey-white qtr veinlets conformable at 35 to 50 deg. to c.a.

S11.a 2cm quartB vein, msv pyrite-net- like form.

215.55 2cm quartz vein 50 deg. to o.a.

205.7-209.} In shear tone 101 conformable laminae of pyrite.

201 smsv pyrite matrix, fine grained.

lot pyrite associated with vein.

au. 1-215.aScattered intervals with heavily disse minated to smsv pyrite up to 20-2St in sections up to 20cm wide.

815.2-231.6 S-8% pyrite as local, heavy dissemination scattered through section parallel to fabric.

Nil to trace pyrite.

Unit can be defined as 2: to 210.15-wi various sulp -rich sectio

WR at 215.4m 5828


DIAMOND DRILL CORE LOGShot No 15 OF.

Projwt No. 287 MK-90-3

Property Nikwa

Depth d Lithology Description (colour, grain tin, texture, structure, etc.) Alteration Mineralization Remark*

Core angles: SO deg. at 224.5m. 50 deg. at 228.2m.

817.0 loom quartz vein SO deg. to o.a.219.S-220.9 Severalquartz veinlets Ion to Son SO deg. to o.a.

229.4 25cm vide white quartz vein. Dark fracture line*, contact.

33l.*-a4i.i sulphide rich section. Medium grey felsic volcanic fragments variably supported by fine grained pyritic matrix. Fragments are irregular and ragged to band-like. Where defined, dimensions are in order of Klom thick to several cm thick. Minor occurrences of white quartz as veinlets or irregular masses. None particularly noteworthy in appearance. Hell defined fabric to fragmental, core anglesi

50 deg. at 231.960 deg. at 233.960 deg. at 236.850 deg. at 239.9

241.1-244.a Decreased pyrite content; uniform, medium grey, SI glassy white . quartz veinlets, some fracture and breccia infilling by fine grained quartz. Most veinlets concordant to fabric.244.8-24S.1 increased pyrite as matrix to distinctly fragmental accumulation.

SI quartz veinlets.



Minor pyrite stringer in quartz of upper

201 smsv to msv and disseminated to stringer pyrite in felsic pyroclastic.


10-151 pyrite.

WJR at 242.0 5829

t*'

NORANOA EXPLORATION COMPANY LIMITED

DIAMOND DRILL CORE LOG 0*1*.*-J!LSheet No

Hoi* No -

11 -OF

MK-90-:

Property

Depth ft Lithology Description (colour, grain tize, texture, structure, etc.) Alteration Mineralization Remark*

245.1-250.1 weakly mineralised felsic volcanic. Irregular coarse fabric of tightly packed pyroclastic flow or possibly felsic volcanic flow.

250.1-254.81 Core badly broken up- probable fault structure or highly fractured cone. Contains several quartz vein and pyritio intervals of 5-20om width. Unbroken core length* carry fine fracture and light coloured calcite filaments.254.81-256.2 Grades out of fault into coarsely fractured and broken felsic which in turn grades into brecciated contact rook over the last meter - good breccia texture. Breccia has open texture where coarse, angular olasts have finer textured fragments in very fine, ground mass matrix.256.2-270.7 Uniform section of grey felsic volcanic, foliated to massive texture.270.7-272.7 Breccia interval. Coarse darkened olasts of volcanic supported in places by quartz-calcite mineralisation. Volcanic is darker in colour than usual- possibly altered to a degree.

245.7-246.2 Quartzvein with 101 pyrite infill to brecciated sections of quartz.

Fine calcite filaments.

51 scattered pyrite as local concentration! and disseminations.lot msv pyrite fracture and breccia infill.

Nil related to active fracture tone. Contained quartz veins carry 10-201 pyrite as matrix to fragmental vein material.

5-101 quartz veining of irregular outline contorted about volcanic fragments.

No notable alter ation. Minor calcite in groundmass.No significant or notable hydrothermal alteration.

1-31 disseminated pyrite throughout some lcm masses.

No significant sulphides.

WR at 261.5 5830



StMMt No.

Hole No -

12 .orMK-90-:

Property MikwamDepth tt Lithology Description (colour, grain *lze, texture, itructure, etc.) Alteration Mineralization Remarks

272.7-279.6 Massive textured felsio- weak foliate fabric in places but general appearance of flow. No distinct contacts. Uniform, fine grained groundmass. Some ragged wisps and small lens-like blebs of pale calcite. Contacts gradational.

279.6-283.0 Paler grey colour, more fragmental appearance, weak pyrite/ pyrrhotite matrix developed only in some sections. Core angles 50 deg. Reverts to usual medium grey colour after 1.5m.

283.0-312.3 Weakly mineralized felsic pyroclastic. Fragmental nature question able. Possibly welded or tight flow deposit. Same as previous sections where clearly fragmental origin is not clear. Core angles 50 deg. to o.a. Quite uniform overall, possibly flow rook as little evidence of fragmental textures. Medium grey, fine grained, massive to foliated structure.

305.8-306.6; Several quartz veinlets 30-45 deg. to o.a.

310.8-312.3i Irregular mass of quartz vein material.

Non except white quartz-oaloite masses of irregular distribution and shape.

885.1-289.9 White quartz vein.

lot quartz vein material.

30-401 quartz vein material.

Nil to tracepyrite/pyrrhotite.

101 disseminated to stringer pyrite and pyrrhotite- variably distributed some pyrrhotite-rich intervals some pyritio. Discontinuous wispy type infilling or tight matrix like form.


WR at 275.8 msv section Possible fl( 5831

WR 289.55832WR 299.65833

Trace to It scattered pyrite.3-5t pyrite as small stringers and breccia matrix.

WR 309.0. 5834


DIAMOND DRILL CORE LOG Project No..

Properly —

287Sheet No.

Hole No. -

13 • Of

HK-90-

Mikwam

Depth gi Lithology Description (colour, grain lire, texture, structure, etc.) Alteration Minerelliatlon Remark*

321.9

312.3-31S.O Mor* heavily mineralised with pyrite. Section has pyrite) supported fragmental look in places especially 314.4 to 314.9. Still medium grey volcanic.

315.0-321.9 Uniform, more massive structured felsic volcanic as 283.0-312.3. Continues uniformly to end of hole.

END OF HOLE

318.8-319.4Irregular quarts- white colour, mixed with volcanic. 201 stringer pyrite.

320.3 20 cm (true) white quartz vein 20 to c.a.

Average 101 pyrite most of it localized in vicinity of quartz veining centred at 313.1.

HR 321.0. 5835

LATITUDE . 32.088

DEPARTURE

ELEVATION .

19.00W


DIAMOND DRILL CORE LOG

Surface

DIP AT COLLAR-50 0

BEARING 160

Ted Depth

120m

Dip

-48"

Magnetic Corrected Bearing Bearing

Project No.

Property tH twain

Sheet No. —l——— OF

Hole No. MK-90-*

180m

TOTAL DEPTH 223.2m CORE8(2E BQ 1 7/16*

Timmins————^—————^—— Testing up-ice stratigraphy from

REMARKS ____ ——— RG holes 85-11 and 84-25. 26. Sanded at 223.2m

32B/S TVUP noseworthy ciaimNoL6Ja:

Date atarted Sept. 20 f 1990 completed Sept. 24, :

Contractor More* prilling

Logged by 8. HardingDepth 4 Lithology Deacrlption (colour, grain alze, texture, atruclure, etc.) Alteration Mineralization Remarks

0.0-56.1

56.1-61.0

61.0-154.0

XNTBRKBDIAT; i VOLCANIC(AHDE8XTB- DACZTB)

Casing

Ground core, recovery 51.

Medium grey-green to dark grey-green. Fine to slightly coarser grained. Mostly massive with various well foliated sections Unit made up various tuffs and inter bedded flows (coarser). Contacts are predominantly gradational. 10-151 quartz/ carbonate veinlets, veins, and blebs. Most are oriented with the foliation but some are crosscutting. Average size 3-4nm, veins average 1-2 OB. Foliation 45 deg. to o.a. at 82.0m. Weakly magnetic.

76.5-77.0 siliceous tone, predominant quartz with 201 volcanic material, 11 pyrite.

82.6-122.0 Rock is mainly well foliated. Increase in quartz to 25-301 with vein size increasing to a maximum of 35 cm. Some contacts are weak and there is volcanic mixed in with the quartz. Foliation varies from 30-45 deg. to o.a.

Minor pervasive carbonate alteration

fine grained disseminated pyrite. Trace in some quartz veins.

HR at 74.0 (5816)

Possible weak serioi alteration in some intensely foliated sections.


DIAMOND DRILL CORE LOG Project No. , 287Sheet No.

Holt No. -

.OF_

MK-90-4

Property Nikwan

Depth tt Lithology Description (colour, grain sit*, texture, structure, etc.) Alteration Mineralization Remarks

82.6-82.8: Quartz vein with St tourmaline/black quartt?

84.0-84.3: Coarse fragments up to - 2cm, very siliceous.

84.3-84.9, 90.3-90.8, 96.2-96.6l Large quartz veins/cones, trace pyrite in soae, weak carbonate.

102.1-102.3: Quartz vein with 2t black tourmaline, 11 pyrite in volcanic at contacts.

Most veins have *:U black quartz/ tourmaline(?). starting at 104.0 increase in carbonate stringers to lot.

ill.6-112.21 Section of elongate volcanic fragments?, 151 quartz/carbonate blebs up to 2 on, 21 pyrite, traoe pyrrhotite.

113.4-122.Ot Dark grey, no quartz veins, 2St carbonate/ainor quartz stringers and some blebs. Still well foliated 45-50 deg. to o.a. at 119.5m.

122.o-i54.fl Medium green/trrey, rook is more tuffaceous. Moderately foliated in places. 5t quartz veins, maximum size 3ciu, *:it pyrite. S-10% quartz/ carbonate stringers and veinlets most oriented with foliation but odd one is crosscutting. 50 deg. to o.a. at 132.3m.

Carbonate stringers are feathery, possibly a breccia?

Very weak pervasive carbonate alteration.

pyrite, traoe pyrrhotite in volcanic.

Trace pyrite.

pyrite in quartz veins. Traoe disse minated pyrite in rock.

WR at129.6-129.8. (5817)


DIAMOND DRILL CORE LOG Project No. 287Shot No. 3 nr

Hoi* No. MK-90-4

Property .-. -

Depth tt Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

154.0-823.a

FELSIC TO INTERMEDIATE VOLCANIC (DACITE- ANDBBITB)

135.8-137.7: 60t quarts veins/ patches. Trace pyrite, <l% tourmaline?

138.9-139.15, 145.7-145.9, 146.1-146.3s Quarts veins/patches, trace pyrite insome.

Volcanics gradually become more felsic, not sharp contact. Light to medium grey, weak to moderate foliation in plaoes- 50 deg. to c.a. at 162.Sm. 10-151 quartz/ carbonate stringers/veinlets and small patches, most are randomly oriented. Only a few quartz veins, up to 4 cm. 21 black tourmaline? in quarte. Weakly magnetic.

171.5-178.3 shear con*, weakly sheared in upper and lover zones. Strongly sheared in the centre, schistose appearance. Shears 50 deg. to c.a., some contorted. Upper contact gradational, lower contact sharp.

173.5-174.3: Core very broken, rock weak. 151 quartz/carbonate stringers and veins both parallel and crosscutting shears.

173.2-173.3: Quartz vein, 31 pyrite 2*: tourmaline.

Weak to moderate carbonate alteration.

Minor sericite alteration on shear planes. Weak pervasive carbonate alteration.

fine grained disseminated pyrite. ^\ fine grained disseminated pyrrho- tit. Most sulphides found in quartz veins.

St disseminated pyrite pyrite with a few narrow stringers. 2-31 with quartz- mostly along contacts.

WR at158.55-158.7(5818)


DIAMOND DRILL CORE LOG Projtct No.

Property -

287Sheet No.

Holt No. -

-OF-

MK-90-4

Mikwam

Depth 8. Lithology Description (colour, greln *lie, texture, ilructure, etc.) Alteration Mlnerellntlon Rama rk*

178.3-194.6 Felsic flows, medium grey, fine grained with cone snail 2mm lapilli*? Generally na**ive with weak foliation in a few places. Some slightly coarser cone*, gradational contacts. Weakly to moderately magnetic, 101 quartz/carbonate veins and patches average site 6mn, random orientation

178.4-178.7: Quartz cone, 21 tourmaline?, 3-51 pyrite/pyrrhotite.

183.1-184.21 Dark grey, 20t carbonate/ minor quartz stringers, feathery. Possibly a breccia zone. Trace pyrite/ pyrrhotite.

194.6-200.6 weakly sheared zone, rook is light green-grey. ist carbonate/quartz stringer* and veinlet* mostly oriented with shears. Shear* 50 deg. to c.a. at 195.5. Weakly to moderately magnetic, St quartz ble m up to 2cm.

200.6-207.2 Felsic volcanic with possible graphitic cherty interbanded material. Rock is dark grey, weak to moderate foliation, varies from 30-50 deg. to o.a. S-8% quartz/carbonate stringers/veinlet* randomly oriented, It pyrite. Weakly to moderately magnetic, darker area* more magnetic.

207.2-223.2 Rhyolite-Rhyodacite, light grey, fine grained. Weak to moderately foliated 50 deg. to o.a. 3t quartz/ carbonate stringers.

Weak pervasive carbonate alteration,

Weak sericite alteration giving •hear plane* a sheen. Weak pervasive carbonate alteration.


3t pyrite-disseminated and in stringer*. 3-St disseminated pyrrho tite, some mineraliza tion occur* with larger quartz vein*.

WR at182.85-183.0(5819)

3t fine grained pyrite, disseminated and in minor vtringer* trace pyrrhotite.

8-lOt disseminated pyrite in stringers and semi-massive patches up to 5mm. it occur* with the larger quartz veinlet*, Stringer* predominate- follow foliation.

3-5t pyrite predom inant in stringers, It with quartz.

WR at 208.9- 209.0 (5820)


DIAMOND DRILL CORE LOG IVo(*ct No ——?.?J?——

She*! No.

Holt No -

-OF-

MK-90-4

Property NikwaaDepth 6 Lithology Description (colour, grain (In, texture, structure, etc.) Alteration Mineralization Remarks

210.3-210.4: Quartz vein?, 21 pyrite, 51 pyrrhotite.

210.7-213.2: Possibly weak shear zone. S-10% quartz/carbonate patches, veinlets.

223.2 END OF HOLE

Hole abandoned due to sanding - bottom plugged, oenent failed.

101 disseainated pyrite in rook and with quartz. Patches up to lcm which have been recryst. to font 3mm "grain*" of disseminated pyrite. It disseminated pyrrhotite.

214.2-223.2disseminated pyrite in stringers/veinlets up to lorn. 31 disse minated pyrrhotite.


DIAMOND DRILL CORE LOGShMI No .OF.

Project No. 287——

Property Mlkwai

Hoi* No. MK-90-5

Depth i Lithology Description (colour, grain tit*, texture, atruclur*, etc.) Alteration Mineralization Remark*

70.0-116.8

OREYWXCKB t INTERBEDDED AROXU.ITB

Occasional white quartz or quartz- carbonate veinlet. These are not uncommon, widths over which they occur are variable as they can occur individually or in groups

Numerous sections of broken core and areas exhibiting water sean effects and leaching.

Light to medium grey, fine grained grey wacke and darker grey argillite. Little graphitic argillite. 90t greywacke, well banded sequence.

Core angles: 60 deg. at 70.in bedding 60 deg. at 79.7m bedding 60 deg. at 88.4m bedding

Wacke beds variable, massive looking, separated by vague, darker argillite laminae.

74.6-80.0 Fault zone? badly broken and leached core.

•S.8-6*.68 Humorous white quartz veinlets, 5-6mm wide- irregular to sharply defined-worm like appearance.

•0.2 20 cm section with thin quarts veinlets. white colour, 101 of interval, irregular.92.8vein.

15 cm quartz

5* scattered pyrite masses and stringers.

Nil sulphides observed.




Hoi* No.

——— OF

MK-90-5

Property Mikwan

Depth d lithology Description (colour, grain ill*, texture, •tructure, etc.) Alteration Mlnerellietion Remark*

116.8-169.7

AROILLACBOU0 SILTSTONE

98.2-101.6 401 black, graphitic argillite interbeds. Several white chert laminae <l en thick.

Trace to 2t pyrite.

101.3-101.6: chert.

Core angles:

White to greyish white

70 deg. at 98.3m 60 deg. at 101.4m Average 65 deg.

101.6-116.8 Continuous section of greywacke, with occasional dark graphitic laminae and pale chert accumulation, (eg) 108.41 10 cm pale whitish grey chert banded 50 deg. to o.a. Unit grades gradually into darker blackish grey argillaceous siltstone.

Dark blackish grey, very fine grained near aphanitic. Lacks any distinct bedding structure due largely to uniformity of grain site. Strong schistosity despite appearance, in places a faint lamination discernable. Occasional irregular white quartz vein concentration over 5-20 en wide. Very clean looking section. Core angles: 70 deg. at 135.0. Only occasional internal bedding contact. Occasional black epiclastic fragment 1mm in sire. Rock is quite hard. Only occa sional quartz as matrix to brecciated siltstone - crackle type.

MR 131.5

Nil sulphides in vein intervals.

WR 155.5


DIAMOND DRILL CORE LOG Project No. 287ShwlNo. ———S————OF.

Holt No MK-90-S

Property Mikwam

Depth 81 Lithology Dctcription (colour, grain tlzt, texture, structure, etc.) Alteration Mlnereliietlon Remerki

169.7-171.8

GRAPHITIC AROILLITB

171.8-176.a

8XZ.T8TONE- WACKB

No indication of alteration, very, very uniform unit. Very dark grey to black fresh surface, cored surface medium to light grey.

163.37-164-4 Brittle crackle breccia- coarse fragmentation. Grey white quartz matrix 15-201 of section.

165.8-166.3 Same as 163.37-164.4,breccia with quartz matrix.

167.6-167.9 Same as 163.37-164.4, breccia with lot quartz matrix. Lower contact interbanded, core angles 090 deg.

Black, fine grained, finely laminated graphitic argillite with faintly greyish thin greywacke laminae lorn or so thick, in small amounts (51).

Some boundinaged chert beds about l cm thick. Core angles average 70 deg. Moderately developed fabric - foliation schistosity. Lower contact gradational.

Very cherty in places. Very similar to 116.8-169.7. Fine grained, medium to dark grey. Fine schistosity in less cherty sectio all changes are gradational but distinct contacts are not uncommon. Fine, siltstone- sandstone beds separated and sometimes mixed with grey-green muddy siltstone.

No visible sulphides in breccia matrix.

As above.

No hydrothermal alteration. No structural deformation.

No alteration.i-

Oocasional short interval carrying 5-8t pyrite/pyrrhotite Fine disseminated pyrrhotite throughout 1-31.

No significant sulphides.



Property -

287Shott No.

Hot* No. -

-2___OF

MK-90-f

Mikwan

Depth d Lithology Deicrlptlon (colour, grain fin, texture, structure, etc.) Alteration Mineralisation Remark!

176.8-309.7

CHERTY8ILT8TONE-WXCKE

Section is quite uniform but at 172.6- 172.9 a chert section borders a green chlorite mud bed which is nonmagnetic. Bedding contorted, upper contact 70 deg.

Non conductive, similar to 171.8-178.8. Very hard in some sections. Very fine, dark grey to dominantly black. Cherty in places, no real change in appearance between cherty sections and softer siltstone. Occasional laminae of greyish wacke.

Core angle: variable between 75 deg. in upper part to 50 deg., average 55 deg.

Despite massive look the siltstone has a well developed schistose fabric at 65 deg.

189.4-191.4 Section containing grey- white quartz.

192.2-192.7 Several lcm grey white quartz veinlets discordant to local (35 deg.) bedding but at 55 deg.193.9-194.2brittle.

Quartz filled breocia-

209.3-210.2 Breccia matrix quartz.

211.0-211.5 Breccia matrix quartz.

No alteration. No significant sulphides.




Nil to trace pyrite.Nil to trace pyrite.


DIAMOND DRILL CORE LOG Project No. .287

Properly

Sh**t No.

Hoi* No. -

.OF-

Depth 6 Lithology Description (colour, grain (li*, texture, structure, etc.) Alteration Minerelizetion Remerkt

909.7

Occasional fine laminae l-3nun, sometimes irregular and contorted, of pyrrhotite ± pyrite. Core angle at 230.0m, 75 deg. Overall veining by grey-white quartz is less than 31. No change to end of hole. Very hard throughout.

END OF HOLE

LATITUDE . 30.44S NORANDA EXPLORATION COMPANY LIMITED

DRILL CORE 287Surface

DIP AT COLLAR

TOTAL DEPTH .

-50*BEARING .

60mDip

-51"M*gn*lle •••ring

Corrcettd Btirlng

120m -SI*

297.0m CORE SIZE BQ 180m -50*

Project No.

Property -

32B/5

240m -48

RPUABKR

Timmins—.————^—^——————Tested gap in stratigraphy up-ice from RG 84-20.

297 -47 e

- TWP. Noseworthy

D.t.ittrttd Sap*-- 24, 1990 compltltd Sept 26.

L6 L6

Contractor

Logged by -

Morov Drilling

HardingDepth S

LitholOBV Description (colour, grain lite, texture, structure, etc.) Alteration Mineralization Remarks

0.0-32.3

32.3-160.5

INTERBEDDEDJUMILLITE/ORBYWACKB

Casing

Medium to dark grey, fine grained. Contains 151 interbedded greywacke in bands from l cm to ^Ocm. Weak to moderately bedded/foliated - 65 deg. to o.a. 31 quartz veins, up to 7cm- contain minor carbonate, 1-21 pyrite, lot ragged quartz/carbonate veinlets/ stringers, random orientation. Weak to moderately magnetic in places. Argillite contains fine laminations in places.

37 .1-37.2. 42 r 6-42.7. 52.5-52.6 Quartzveins with minor carbonate, 2-31 sericite, up to St pyrite.

Starting at 56.0, decrease in quartz/ carbonate stringers/veinlets to St.

55.6-5S.95 Quartz vein, 20t lintonite staining, It pyrite, ^t pyrrhotite.60.9-61.2 Quartz and silicified sediment*, st limmonite staining, minor sericite, it pyrite.

Very weak pervasive carbonate alteration 3-51 limonite staining along water seams.

5\ disseminated pyrite in ragged stringers and blebs in sediments. 21 pyrite in quartz veins.

2\ disseminated pyrrhotite in sediments.

Starting at 68.0, - no limonite staining


DIAMOND DRILL CORE LOG ProitOI No

Property -

2B7

Hikvan

Sh**l No

Holt No .

*____OF.

HK-90-6

Depthg. lithology Description (colour, grain *lze, texture, etructure, etc.) Alteration Mineralization Remarkt

68.3-68.5. 70.9-71.2 Quartz veins, minor sericite, carbonate. 51 pyrrhotite in blebs up to 3sun, 3t pyrite in smaller blebs and disseminations.71.2-106.5 Increase in greywacke to 25-301. No quartz veins, 51 quartz/ carbonate stringers and patches. Well foliated, contorted in places -60 deg. to c.a., moderately magnetic.

90.5-97.0? 60t greywacke.

97.8-98.0: Quartz patch, 31 pyrite, li pyrrhotite.

106.5-iio.Q Predominantly graphitic argillite, core is broken for SOt of section. St quartz/carbonate stringers, crosscutting bedding.iio.Q-129.4 sot argillite, 501 greywacke. Moderately to strongly foliated/bedding 60 deg. to o.a. to parallel o.a. in one section. 101 quartz/carbonate stringers and small veins up to l cm. Some large quartz patches up to 20 cm, 1-2t pyrite. Quartz/carbonate stringers/ veins parallel to foliation/bedding.

Starting at 71.0 increase in pyrite to et, 3t pyrrhotite.

lot disseminated pyriti in stringers and blebs up to 4mm.

St disseminated pyrite in small beds up to 3mm and in ragged stringers.


DIAMOND DRILL CORE LOGSheet No. -OF

Project No.

Property

287 Hoi* No. MK-90-6

Depth 6 Lithology Detcription (colour, grain tin, texture, ttrueture, etc.) Alteration Mineralization Remark*

160.5-181.*

OR2YWACXB/KINO*INTERBEDDEDAROILLITB,SILTSTONE

181.6-201.5

AROXLLITH/MINORINTERBEDDEDGREYWACKE,SILTSTONE

129.4-160.s Predominantly argillite with 15-201 interbedded greywacke, ainor patches of very fine grained siltstone. Most sections are massive or finely laminated. 51 quartt/ carbonate stringers/veinlets. Argillite weakly to moderately graphitic in places, weak to moderately magnetic. 3-51 contorted quartz/carbonate patches up to 5 cm wide found in siltstone zones. Increasing greywacke down hole.

155.55-155.7: Quartz vein with 51 graphitic argillite, It pyrrhotite.

*:10I argillite, siltstone, generally massive, weakly foliated in places 60 deg. to o.a. 5t quartz/carbonate stringers mostly crosscutting foliation/bedding. Weakly magnetic in places.

171.6-171.9 Quartz vein, trace pyrite.

Very weak pervasive carbonate alteration in places.

greywacke and siltstone. Argillite- weakly to moderately graphitic in places. 5-101 quartz/carbonate stringers/patches.

193.2-194.0. up.

195.0-197.5 Core is broken

•ell disseminated pyrite. It pyrrhotite in stringers usually with quartz/carbonate veinlets up to 3mm.Starting at 158.0 - St pyrite.

2-3t disseminated pyrite with odd stringer.

3t pyrite in narrow blebs. Found mainly in argillite or with some quartz patches.



Properly

287

Sheet No.

Hoi* No. -

-l___OF-

MK-90-6

Mikwan

Depth Si Lithology Description (colour, grain site, texture, structure, etc.) Alteration Minersllutlon Remarks

297.0

262.6-262.71 At the bottom of strongly sheared zone, 151 disseminated pyrrhotite, strongly chloritic.

262.7-28B.O Weakly sheared sediments. Low angle shears, causing bedding to flatten out, bedding varies from 60-30 deg. to o.a. ^1 chert patches up to 10 en.

288.0-297.0 Weakly sheared, strongly chloritic? sediments. Dark grey-dark green, bedding contorted in most places. Shears are low angle. 15-201 quartz/ carbonate veins/patches up to 10 cm.

END OF HOLE

Strong chlorite? alteration.

3t disseminated pyrite It disseminated pyrrhotite.

31 disseminated pyrite/ pyrrhotite in sedimenti 151,pyrrhotite, 5t pyrite in quartz veins and in areas of contorted sediments.

NORANOA EXPLORATION COMPANY UMITED

DIAMOND DRILL CORE LOG Protect No. -——287.

Sheet No. *

Hoi* No. W-90-6

Property Mikwam

Depth ft lithology Description (colour, grain ilie, texture, itructure, etc.) Alteration Mineralization Remarks

201.5-297.0

ORE WACKE/MIKORINTERBEDDEDAROILLITE/SILTSTONE

Medium to dark grey, 15t interbedded argillite/siltstone. 101 quartz/carbonate stringer/patches. Weak foliation - 55 deg. to o.a. Increasing siltstone downhole, at 230.0, 201 siltstone.

225.S Load cast - greywacke sinking into finer grained siltstone, tops are up hole (north).

233.2-236.0 151 dark green (chloritic) mudstone, including one 40 on section.

241.0-242.7 Coarser greywacke, with 20t quartz/carbonate stringers and veinlets.

248.1-248.2. 250.0-250.1 Quartz veins, minor carbonate, trace pyrite/pyrrhotite.

255.4-286.0 shear cone, upper and lower zones are weakly to moderately sheared. Shears vary from 60 deg. to o.a. to almost paralle to o.a. near the centre. I0-15t quartz/carbonate stringers/veinlets.

259.5-259.71pyrrhotite.

Quartz vein with St

260.0-262.7: Intensely sheared sediments, shears are 10 deg. to c.a. to parallel to c.a. SI quartz/carbonate veinlets parallel shears.

Weak to moderate chloritic alteration in mudstone.

Weakly chloritic.

Weak pervasive carbonate alteration. Weak chloritic alteration in well sheared parts.

•ell disseminated pyrite.

Starting at 233.0, It pyrite predominant with quartz/carbonate veinlets.

It disseminated pyrite, it disse minated pyrrhotite.

262.6-262.7 15tdisseminated pyrrhotite.

LATITUDE . 18.95S

39.12B


DIAMOND DRILL CORE LOO

ELEVATION Surf***

DIP AT COLLAR -60"

TOTAL DEPTH 317-9m

Till

61m

Mapnelle Corr*citd Boring Staring

58 0 ProperlyHJW..., MifcWam

i**0 123m 57 e

7/16*182m

NTS..32B/5 Noseworthy

56244m 56355m 55e

ott. tttrud Sept 26, 199Q

Drilling Ltd

Seot 30.

REMARKSTested A-8 stratigraphy 400m NE - tnn p^r^lto) from discovery A~~8 hole Logged by W. Corstorphine

Depth 6 Lithology Description (colour, grain slie, texture, structure, etc.) Alteration Mineralization Remarks

0.0-82.3

82.9-82.6

82.6-159.1

GREY INTER MEDIATE TOT! (DACITE)

Casing, later reamed to 91.4m to prevent sanding.

Boulder?, differs considerably from rock below it - fresher, unweathered, higher grade. Biotite-hornblende - feldspar rock ± quartz. Strong foliation by hornblende and biotite in more massively textured feldspathic ± quartz groundmass of grey colour. Fine grained groundmass, hornblende is dark green t of coarser grain size. Distinct outlines of elongated, slightly paler olasts containing less hornblende/biotite. Fragments matrix supported and up to 7 or 8 mm in thick ness by up to 4 cm in length. Foliation 40 deg. to o.a.

82.6-84.1 1.2 m of ground core, 201 recovery. Fragments highly bleached and weathered. Appearance same as84.1-90.5.

Mon recognized. Nil observed.


DIAMOND DRILL CORE LOGShwlNo

Project No. 267 HOU No... .*K-9P-.7

Properly Mikwe

Depth tt Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remark!

84.1-90.s Pal* buff, leached, limonite stained fracture surfaces, rusty pits locally. Fine grained, strongly foliated to near schistose fabric 35 deg. to c.a. Fabric defined by darker lines which suggest irregular matrix of tightly packed, strongly foliated fragmental - not regular as in bedding. However, unit may be same as below.

Ankerite stain indicates pervasive carbonate alteration, throughout groundmass Rook does not however have obvious outward sign of same.

Nil to trace disseminated pyrite. Non readily in evidence. A few sulphide specks here and there in groundmass.

84.1-87.2: recovery.

2.1 m ground core, 301

87.2-90.21 2.1m ground core, 301 recovery. Core is very badly broken up.

90.5-159.1 orey, intermediate tuff. Groundmass is very fine to aphanitic. Colour various shades of grey, generally medium to dark grey. No greenish oast. No distinct bedding structure, only a very strong schistose fabric of very finely laminated structure. Like a fine mylonite, overall a vague streaky type of fabric. Some ragged laminae structures of wispy form. One section resembles a fresher form of 84.1-90.5, of medium hardness.

90.5-99.5t Core badly broken up.

Core angle consistently 30-35 deg.

As above. As above.


DIAMOND DRILL CORE LOGSheet No t*r

Prelect No.

Properly —

287 MK-90-7

Mikwam

Depth 8, Lithology Description (colour, grain size, texlurt, structure, etc.) Alteration Mineralization Remarks

White calcite-rich veinlets and discontinuous micro veinlets are scattered throughout some sections of unit in up to 81 concentration. Most occur as conformable veinlets and laminae. Sections have whitish grey colour.

Numerous concordant, white quartz- carbonate stringers have comminuted texture of granular host floating in veinlets.

120.5-128.0: Shear Zone - Gradual change, paler, whitish grey, calcite/ quartE bearing section, numerous micro- laminae stringers throughout 101. schistose fabric more prominent due largely to white quartz-oaloite laminae and stringers. Strong deformation banding and cleavage develops between 125.1-127.2.

Calcite veinlets and streaks.

10215 4 cm true quartz vein, concordant.

Grey-white quartz vein at 109.9m - 10cm true, conformable. Cut by caloite-rioh veinlets which here are discordant.

U.S.* Several l-2cm grey-white quartz veinlet concordant attitude.

Nil sulphides noted with white oaloite- rioh veinlets and stringers.

Nil sulphides associated with vein.

As above.

WR 100.3: 3 pyrite-local fine grained oonoentratio good specime (5849)

No observable sulphide.

1-21 fine pyrite grains.



ShMtNo. . nt

Hoi* No. MK-90-7

Property MikwamDepth d Lithology Description (colour, grain *!ze, texture, atructure. etc.) Alteration Mineralization Remark!

Centre of shear tone i* 126.0, banding rotates from 50 to 20 deg. at centre of cone.

Sporadic pyrite concentrations of 101 over 2-15 en; commencing about 131.1m.131.1-133.0: A number (7) of pyrite occurrences averaging 10-201 fine to medium grained py. each in heavy disse minated to smsv concentrations. Does not appear related to shear structure as rock is not strongly sheared but some indications of coarse structural deformation - partially fragmented, sulphide cone appears primary.135.7: l cm brecciated quartz vein, white quartz/carbonate (fine grained) matrix to grey white quartz vein fragments. Attitude 20 deg., numerous smaller veinlets for .5m either side of larger vein.

143.0-144.31 Shear cone 10-30 deg. to o.a. Two quartz vein occurrences and lesser veinlets at 143.0 and 144.0. Both low angle, conformable to shear.

186.0 several l cm quartz veins following 20 deg. Shear fabric - quartz is fractured and boudinaged.

Nil to trace sulphides in quartz veins. White natrix is grey, fractured quartz is as in other stringers of calcite-quartz,

191.0-1)9.0 51pyrite in local concentrations of S-20% fine to medium grained pyrite over 2 to 15 cm.

1)5.0-130.2quartz veining 20 deg. to o.a

Nil to trace pyrite only.

MR 136.7 Grey tuff stains blue but doesn't look altered(5850)


DIAMOND DRILL CORE LOG Project No. ——2A2

Property

Shmt No.

Hot* No. -

-OF-

mc-on-7

Depth d Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remark*

159.1-159.85

GRAPHITIC IOTBWCBDXATB ORBV TOFF

159.85-161.O

XA88ZVB VYRXTB BOMB

145.7-148.5: Shear cone, 10-20 deg. to o.a. Quartt vein occurrences at 146.0 parallel to o.a. and at 147.6 20 deg. to c.a. plus lesser thin 1-2 mn laminae - like quarts.

147.8-148.1: gouge.

Lithology sane throughout - grey tuff to 159.1. Core angles typically between 35 and 55 deg., average 45 deg. Lower contact totally gradational over a few on with the appearanoe of slightly darker grey tuff caused by weak graphite component. Occasional pyritio lens 5-81 pyrite in each.

Slight darkening due to mixing of graphitic component. Fine grained, strong fabric producing schistose parting. Still observe sone of original structure - tuffaceous. Fabric slightly contorted average 40 deg. to c.a. Lower contact sharp 50 deg. to o.a.

Massive, fine grained to coarse, recrystallized ion pyrite. Sone dark tuff or sediment nixed in centre of zone, strongly foliated. Pyrite lacks distinct banding structure but has crude layering of sorts. Lower contact distinct, ninor intercalation over loon.

Trace only sulphides.

Weak ankerite as previous unit.

in Sporadic pyrite lenses and disse minations < 2mm thick. Average

overall.

851 pyrite.


DIAMOND DRILL CORE LOG Projcci No. 267

ShMt No.

Hoi* No. -

—5——OF.

MK-90-7

property MikwamDepth 8. Lithology Description (colour, grain alie, texture, structure, etc.) Alteration Mineralization Remark*

161.0-169.7

ORATHITIC XNTBRXKDXATB QRZY T01T

169.7-357.2

GRAPHITIC AROXUiXTB

As 159.1-159.85. Strong fabric after sulphide rone for 0.5m.

161.45-162.05 Paler grey , uniform section, very homogeneous felsic? tuff. Fabric 50 deg. Almost sericite schist, contacts gradational. Unit has more laminated structure with s-10% darker grey to black laminae regularly interbedded with grey tuff. Dominant fabric/banding 60 deg. to c.a. Lower contact gradational.

Dark grey to black with lighter grey sections, fine texture. Mainly non- conductive argillite of black colour.

169.7-172.0 Finely laminated, rippled 60 deg. to o.a. Locally concentrated pyrite laminae and irregular lenses 1-2 mm thick.

172.0-179.4 sol lighter grey argillite interbedded with graphitic variety. Core badly broken in places.

174.3-178.611 Several gouge seotions and seotions of rubbly core.

179.4-192.9 Black, weakly conductive? graphitic argillite. 5* white quartz ± calcite, very fine stringers 1mm.

180.3-181.0: Gouge and rubbly core.

No distinct alteration.

No evidence of alteration.

11 disseminated pyrite as small 1mm blebs.

Minor pyrite concen trations up to St average ^t overall.

St locally concent rated pyrite.

SI disseminated pyrite.


DIAMOND DRILL CORE LOG Project No. .

Property —

287Sheet No.

Hoi* No. -

-OF.

MK-90-7

MikwamDepthg. Lithology Description (colour, grain six*, texture, *Uucture, etc.) Alteration Mineralization Remark!

192.9-198.2 Gray argillite, tending towards greywacke) - occasional black lithic clast l-2mm in sice.

Coarsely to moderately bedded, medium to dark grey beds l to 30 cm thick. Core angles 45 deg., sharp contacts in most places. Upper contact sharp with graphitic sediments; lower contact is distinct, somewhat gradational over last* DID*

198.2-207.1 Black to dark grey graphitic argillite similar to 179.4-192.9. Some greyish, argillite-waoke beds from 203.0- 204.3.

204.3-207.3: Black graphitic argillite.

At 206.5: centre of soft gouge (loom) in narrow shear/fault between about 206.2-206.7 - gradational margins.

Minor white-grey quartz/carbonate veinlets Klom thick generally conformable to fabric. Can occur in lot concentrations over short, ^5m intervals. Carbonate staining show evidence of both calcite and some ankerite in veinlets and in the groundmass of the argillite. Stains are of moderate to weak intensity.

Calcite ankerite.

S-8% coarse pyrite splotches throughout unit, unusual form, reorystalliced form- radiating crystal lines from dense core of pyrite.


DIAMOND DRILL CORE LOG Prolect No, .

Property —

287

Sheet No.

Hoi* No. -

-OF-

MikwamDepth i Lithology Description (colour, grain size, texture, etructure, etc.) Alteretion Mineralization Remark*

207.1-214.8 Variably banded argillite- vaoke. Similar to 192.9-198.2. Upper contact interlaminated over .5m. Core anglest 50 deg. at 207.5.

Darker, graphitic sections occur at: 209.20-209.70 212.14-212.40

Lower contact arbitrary with development of graphitic component.

At 214.2: 2 cm quarts veinlet, minor oalcite/ankerite.

214.8-248.2 Major section of uniform- graphitic sediment similar to 179.4- 192.9 etc.

At 223.2: 6 cm vein of pinkish white calcite with open space pyrite crystal growth, also 2mm msv pyrite vein (discontinuous). Pyrite content of calcite vein is 15-201.

Core angles: 50 deg.

At 228.6: Several l cm quartz/carbonate veinlets.

At 231.3: 3 cm quartz/carbonate veinlet.

At 231.58: Banded quartz/carbonate veinlets - small.

At 232.6: l cm quartz/carbonate veinlet.

1-21 grey-white quartz veinlets with traces of beige ankerite.

Usual S-10% white quartz/carbonate veinlets usually conformable, often deformed and wrinkled. Moderate quantities of blue staining ankerite with most quart!/ carbonate veins.

Weak carbonate content.



Minor occurrences of of coarse, reorystall- ized pyrite similar to that in graphitic section above. Mo direct sulphide with quartz veinlets.

Nil to trace associated pyrite.

3-St coarse, disseminated pyrite. No direct association with quartz/carbonate veinlets.

Nil to trace associated pyrite.Nil to trace associated pyrite.

Nil to trace associated pyrite.



Property

287ShMtNo. ——i

Hoi* No, -

-OF-

MK-90-7

Depth g, Lithology Description (colour, grain slie, texture, structure, etc.) Alteration Mineralization Rama rita

At 233.4: 3 cm quartz/carbonate veinlet.

At 239.8: Low angle fabric, parallel to c.a. broken up, narrow quarte veinlet, covers .4m.

At 240.85: 20 cm of contorted quartz veinlet material in carbonate bearing section, conformable.

At 243.46: l cm quartz vein, conformable.

At 243.7: Quartz vein, 3 cm pinching.

At 244.9: 30 cm section with a number of l cm quartz veinlets (5).

Lower contact gradational.248.2-249.4 Continuous section of grey argillite - wacke.249.4-2S7.2 Finely laminated argillite and graphitic argillite. Finely folded -rippled structure, core angles average 50 deg. Lower contact gradational.

257.2-307.6 Black to dark grey graphitic argillite as 198.2-207.1 etc. Periodic white-grey quartz veinlets 2 to 3 meter intervals.

Weak ankerite associated with quartz veinlets.

51 pyrite.

1-2\ pyrite.

Trace pyrite.

Trace pyrite.

Trace to it pyrite.

SI grey white quartz (carbonate) veinlets, conformable. No significant indicatio of carbonatization possibly trace amounts.

Trace to 11 pyrite only.


DIAMOND DRILL CORE LOGSheet No. 10 -OF —

Project No. 287 Hoi. No. MK-90-7

Property MikwamDepth tt Lithology Description (colour, grain site, texture, structure, etc.) Alteretion Minereliietion Remerks

At 263.7i 40 cm section of conformable quarts veinlets 30 deg. to c.a.

At 266.6: 50 cm quartz veining (151) conformable to irregular. Unit is uniform but a little inhomogeneous in appearance due to local contortions of bedding. Occasional grey or section •elm which changes back to black graphitic sediment.

At 281.li Grey white quartz, irregular breccia type structure.

At 284.1: Two, l cm quartz veinlets.299.8-300.7: Increased concentrations of thin quarts laminae, and some beige carbonate? Several 2cm and one 5cm quartz vein.

Core angle at 302.0m, 55 deg.

305.6-306.8: 15\ quartz vein material. 307.6-309.0 Grey argillite section.

307.6-308.15: I5t quartz veinlet material.

309.0-319.8 Black graphitic sediment Core angles 50 deg. average. Some small scale fold structures.

319.8-321.1 Grey argillite wacke massive, little evidence of bedding.

Trace ankerite.

Trace ankerite with veins.

Nil ankerite.

Minor calcite. Minor ankerite.

Minor calcite.

Minor calcite.

Nil to trace pyrite only.

Trace to 11 pyrite with some of the quartz.

Nil sulphides.

Nil sulphides.SI disseminated pyrite as heavy disseminated laminae and blotches.

Nil to trace

sulphide. Nil to trace sulphide.

Local pyrite splashes 1-2t.


DIAMOND DRILL CORE LOG *****^-I&L-Shot No. 11———OF.

Hoi* No. HK-90-7

Property

Depth 4 Lithology Description (colour, grain tile, texture, structure, etc.) Alteration Minerdiution Remerkt

321.1-324.3 interbedded black argillite and grey argillite - wacke. Doninantly argillite - wacke 751.

324.3-352.? Dooinantly black to dark grey argillite, similar to previous sections of such rook. Variably bedded; in places fine laminae - generally contorted and in other short sections, nore massively bedded.

Usually where quartz±caloite,*ankerite occurs there is stronger deformation with bordering sediments exhibiting a stronger fabric and shear bandingi These occurrences are generally isolated with intervening sections showing some contorted bedding but not penetrative shear fabric. Attitudes are variable but average 40-50 deg.

330.8-331.8s 201 quartz in shear structure. Minor disseminated pyrite. Quartz is not sharply defined as a vein - tends to be a contorted mass or stringer. Core angles variable, 30-50 deg.

336.5-338.5t Section of graphitic sediment marginal to widest interval of silicified (quartz bearing) shear in hole. Sediment is locally well laminated, possibly due to shear but in general does not look strongly sheared. Several 2 cm quarts veins of irregular definition. Lower contact with silicified shear sharp at 30 deg.

Minor ankerite? peripheral to more central quartz mass.

Minor ankerite suggested by staining solution.

11 pyrite.

11 pyrite.



Project No. - 287 MK-90-7

Properly MikwaDepth 6 Lithology Deacriptlon (colour, grain vita, texture, structure, etc.) Alteration Mineralization Ramarka

338.5-340.1 Medium grey colour, shear banded to "jumbled" looking mass of contorted quartz (upper .5m). Greenish black interlaminar with the quartz. Estimate 501 quartz component. Shear banding is 30 deg. to o.a. at centre but increasing to 40 and SO deg. away from centre.340.1-341.4 Graphitic sediment with strong fabric. Initial 340.2-340.8 graphitic gouge with some quartz material.

341.4-342.0 A short section similar to 338.5-340.1 with central quartz. Core of 12 cm thickness. Core angles 40-50 deg. Bordering sediment has schistose fabric.

342.0-3B7.2 Laminated, graphitic sediments and Interbedded argillite-waoke.

344.1-344.7s Graphitic section with S-8t thin, contorted quartz veinlets.344.7-347.91 Variably bedded graphitic sediment, locally contorted.

347.9-348.7: Massive argillite-wacke bed.

348.7-352.5J Contorted graphitic argillite. Fault gouge, broken up core at 342.1 for 20 cm.

Moderate to minor ankerite (blue stain). Ho sugges tion of calcite.

l-2t disseminated pyrite.

Minor ankerite (blue stain).

It pyrite.

51 pyrite.

Minor ankerite associated with interval.

St disseminated pyrite.


DIAMOND DRILL CORE LOG Project No. ——282

Property

Sheet No. 13——— of.

Hoi* No. MK-90-7

Depth ft Lithology Description (colour, grain ilze, texture, structure, etc.) Alteration Minerellzetion Remerki

357.2

352.5-357.2 j Mor* argillaceous-vaoke component than graphitic. Still irregularly banded and contorted on small soale - small recumbent folds, jumbled appearance. Fabric is not as schistose as in more graphitic or sheared sections.

END OF HOLE

LATITUDE . 11.ION

DEPARTURE 84. POW

ELEVATION Surface


DIAMOND DRILL CORE LOGProject No. 287

Sheet No ———— O

MK-90-B

DIP AT COLLAR-55' BEARING. 180* GS

Test Depth

60mDip

-54*

Magnetic Corrected Bearing Bearing Property Mikwam

120m. -si*

TOTAL DEPTH 207.0m rnnr Rae 1 7/16" BQ

NTS.. "B/12 Noseworthy cliimNo L63J

CORE STORAGE—TiBaains______________ ____ ____ ____ ———— Casing left in-making water. To teat___ ———— ____ ————

REMARKS BM.conductor and boat ntrntigraphy for Casa B type Au mineralization.

Sept. 28, 1990 eompl.lw, Sept. 30.

corrector Morex Drilling Ltd.——————

Logged by 8 * Harding ____________Depth ft Lithology Description (colour, grein die, texture, structure, etc.) Alteration Mineralization Remarks

0.0-31.5

31.5-77.7

XA7IC VOLCANICS

Casing

Interbedded flows, medium grey/green-green. Fine grained with various coarser sections. Moderate to well foliated 55 deg. to o.a., some parts 40 deg. to o.a. Some sections appear massive but are actually well foliated. Weakly magnetic with small ^20cm) sections strongly magnetic. 10*; quarts/carbonate stringers and veinlets, most oriented with foliation but a few are crosscutting. St quartz veins, max. size 10 cm, some have 31 pyrrhotite, 21 pyrite. Odd ragged vein of almost pure carbonate.

Trace pyrite in rook.


Trace pyrite in rock. Up to 3i pyrrhotite in some 30cm sections. Up to 31 pyrrhotite, 21 pyrite in some of the larger quartz veins.

57.0-57.3 fragments,

Predominant lapilli sized well foliated.

65.S-77.7 weak ankerite alteration causing the rook to change to a light beige-grey colour, with some silicified sections.

Weak pervasive ankerite alteration.

Trace pyrite/ pyrrhotite usually found with quartz.

HR 59.3 (68677)

61.0-61.2, 64.2-64.4: trace sulphide.

Quartz veins,


DIAMOND DRILL CORE LOGShot No.

Project No. . 287 HOI* NO. MK-90-8

Property Mikvam

Depth tt Lithology Description (colour, grain tin, texture, structure, ate.) Alteration Mineralization Remarks

77.7-104.t

XAMO VOLCANIC BDLPHIDB ZONB

Rook i* the same a* above unit. A bit less ankerite) alteration, rook i* predominant grey-green colour. Moderate to well foliated - varies fron 45-30 deg. 10-151 quartz veins, quartz/carbonate veinlets. Moderate to strongly magnetic, decreases down section. Below 91.5, slight decrease in large quartz patches and veins.

Weak pervasive ankerite alteration decreases down seotioni

101 disseminated pyrrhotite, S-8% disseminated pyrite, 31 cpy. Sulphides are found throughout the zone with larger concentration found in areas of quartz patches/veins. St of zone consists of semi-massive sulphide sections up to 20cm with pyrite as the predominant sulphide. Pyrrhotite is found mainly in the volcanics with lesser amounts in quartz areas. Cpy is found only in areas of quartz and the larger core of sulphide.

Below 91.5, there is a slight decrease in sulphides. There is less pyrrhotite in the host rook, sulphides come more into specific zones.



Hole No. -

.or.

MK-90-1

Property Hikwam

Depth 8. Lithology Detcription (colour, grain tlze, texture, structure, etc.) Alteration Mineralization Remarks

104.8-117.8

MATIC VOLCANIC

117.2-128.2

KA7ICVOLCANIC,(CHLORITIC)

Upper section i* predominantly a coarse flow, possibly porphyritic?, appear aassive but is well foliated. Rest of the section is similar to above units. Moderate to well foliated - 40-50 deg. to c.a. Only S-8% quartz/carbonate stringers and snail blebs. 21 quarts veins with trace sulphides. Bottom section weakly chloritic. Weakly magnetic in a few sections.108.1-109.1 section similar to that of sulphide cone with 151 sulphides.

Green to dark green as chlorite increases Volcanic flow with strong chlorite alteration. lS-20% quartz/carbonate veins, blebs and stringers, mostly oriented with foliation. Moderate to well foliated - 50 deg. to c.a., weak to moderately magnetic.121.6-125.0 Rook is strongly chloritic, dark green. Increase in number and size of quartz veins.

Weakly chloritic at base of unit.

Moderate to strongly chloritic. Weak ankerite alteration in some veins.

Strong chlorite •Iteration.

S-5% disseminated pyrrhotite, 1-21 disseminated pyrite.

ice. 1-10*. X lot pyrrhotite, 51 pyrite, l* cpy.

WR 111.0 (68678)

St disseminated pyrrhotite, a-5% disseminated pyrite. Sulphides found predominantly in areas of quartz/ carbonate stringers.B-10% pyrrhotite, 3-51 pyrite. Only trace sulphides in quartz veins.

187.3-128.2 Four 2cm massive patches of pyrrhotite.



Hoi* No. -

-OF.

MK-90

Property MikwamDepth ft Lithology Description (colour, grain alia, texture, •tructura. etc.) Alteration Mineralization Rama rka

12*.2-1*9.ft

MAFIC VOLCANIC

169.5-169.7

MAFICVOLCANIC,(CHLORITIC)

Interbedded fin* to coarser flow*. Moderate to well foliated/ 60 de?, to o.a. 101 quartz/carbonate veinlets/ stringers, 11 pink carbonate in some veinlets. 51 brown mica in some sections, usually with pyrrhotite or along quartz veins.

Starting at 149.0 - 51 quartz veins, only minor stringers.

14S.B-HS.9 Quartz vein with 101 pyrrhotite, trace cpy.

Weakly ohloritio in a few Dittoes. Weak pervasive ankerite in a few places.

162.0-169.s Rook contains 301 dark green chloritic? blebs (up to 3mm) giving it a porphyritic look. Also contains 51 carbonate blebs up to l ea. SI quartz veins up to 6 en, trace sulphides in some.

Unit is similar to previous chlorite zone. Green to dark green, moderate to well foliated 50-70 deg. to o.a. 201 quartz veins and blebs, up to 3cm, quartz/ carbonate stringers.

1-21 pyrrhotite/ pyrite in rook. SI semi-massive patches up to 10cm of 151 pyrrhotite, 51 pyrite, 11 cpy in argillite?

199.5-142.0 8-101disseminatedpyrrhotite.

142.0-15t.O 51 patches up to 15cm of 101 pyrrhotite, 31 pyrite, Kll cpy with quartz. SI disseminated pyrrho tite in some parts of the section.

1-21 disseminated pyrrhotite. ^* pyrrhotite/pyrite in some quartz veins.

Up to 51 pyrrhotite in places. Up to 31 pyrite with the pyrrhotite.

WR 131.6 (68679)

WR 164.3(68680)

WR 183.4 (68681)


DIAMOND DRILL CORE LOGOF -

Project No. . 287 Hoi* No. MK-QO-fl

Property MikwamDepth tt Lithology Description (colour, grain size, texture, structure, etc.) Alteration Mineralization Remarks

189.7-201.0

MAFIC VOLCANIC

201.0-207.0

MAFICVOLCANIC,(CHLORITIC)

207.0

Grey to grey/green, similar to other units but has undergone weak ankerite alteration. lQ-15% quartz/carbonate stringers with a few veins. Gradational upper and lower contacts narked by increasing chlorite as chlorite rones are approached.

194.7-194.8 Quartz vein with l* pyrrhotite, trace cpy.

Similar to above chlorite cone with increase to 251 quartz/carbonate veins and stringers.

Weak chlorite alteration in upper and lower zones. Weak pervasive ankerite alteration.

S-5% disseminated pyrrhotite, it disseminated pyrite.

WR 193.9 (68682)

Weak to moderate ankerite alteration in some areas and veins. Strong chlorite alteration.

S-8% disseminated pyrrhotite, i-2% disseminated pyrite. Odd patches up to 5 cm wide with lot pyrrhotite, 31 opy, 11 pyrite.

END OF HOLE

32E12SE0814 63.6823 NOSEWORTHY 020

GEOPHYSICAL REPORTON THE

MIKWAM PROJECT, NOSEWORTHY TOWNSHIPFOR

NORANDA EXPLORATION COMPANY LTD.

l

J

Prepared By:J.C. Grant, GET, FGACExsics Exploration Ltd.February,

32E12SE80M 63.6023 NOSEWORTHY 0S0C

tJ

TABLE OF CONTENTS

i

Page

INTRODUCTION . . . . ... . . . . . . . . . . . . . . . . . . . . . . . . . . . . t . . . . . . l

PERSONNEL......................................... . . . 2

LOCATION AND ACCESS............... . . . . . . . . . . . . . . . . . . . 2

CLAIM STATUS......................................... 3

GEOPHYSICAL PROGRAM.................................. 3

SURVEY RESULTS....................................... 6

RECOMMENDATIONS AND CONCLUSIONS...................... 8

CERTIFICATION

IP PSEUDO-SECTIONS

J

LIST OF FIGURES

Figure l - Location Map Figure 2 - Property Location

Appendix A

Appendix B

APPENDICES

EDA IP-4 Time Domain Receiver Huntec 2.5 kva Transmitter Metal Factor Calculation Chart

INTRODUCTION

j This report will deal with the results of an Induced

Polarization (IP) Survey, which was completed over an existing

grid located in Noseworthy Township, Larder Lake Mining Division

in Northwestern, Ontario. Refer to Figure l and 2 of this

report.

Exsics Exploration Ltd of Timmins was contracted by Noranda

Exploration Company Limited to perform this survey during the

J month of December 1990.

-i The purpose of the survey was to test several lines of a

Jfe much larger grid that had been surveyed before with conventional

l EM techniques.

A broad anomalous zone had been suggested from this past

j survey and due to a suspected target of highly disseminated

sulphides, it was thought that the IP Survey would better define

and possibly separate more conductive zones within this wide

j response.

It was hoped that the IP Survey would outline geological

structures favourable for gold deposition.

J

J

tJ - l -

i PERSONNELi

i The people directly involved with the program and collection

of the field data were as follows:

Richard Mathieu.......IP Operator.......Timmins, Ontario

Paul Edwards..........Helper............Timmins, Ontario

Pierre Mail let........Helper............Timmins, Ontario

Denis Maillet.........Helper............Timmins, Ontario

All of the work was carried out under the supervision of J.

J C. Grant.

LOCATION AND ACCESS

The Mikwarn Property is situated in the northeast section of

i Noseworthy Township, Larder Lake Mining Division, District of

Cochrane. It is situated approximately 56 km northeast of the

Town of Cochrane just west of the Bradette - Noseworthy Township

l Line in northeastern Noseworthy Township. Refer to Figure 2 of

this report.

Access to the property was by helicopter from the end of the

, Tomlinson Road which terminates just to the north-northeast of1 J Payntouk Lake. The crew and gear was slung in from this point.i

tJ - 2 -

r

J

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J

CLAIM STATUS

Since this current project was done on a select group of

lines which are part of a much larger grid, the status of the

property will not be discussed in this report. It was also not

evident as to which claims or part of claims have been covered by

this current program.

GEOPHYSICAL PROGRAM

An Induced Polarization Survey was conducted over a select

f number of test lines on the Mikwam Property. These test lines

were completed over a broad area of finely disseminated sulphides

with the hopes of better defining the zone and or locating

parallel structures.

The following is a brief description of the survey conducted

and the parameters used:

Induced Polarization Survey:

The IP method involved applying a current across two

electrodes in a pulse manner, ie, 2 seconds on, 2 seconds off. A

second "dipole" or electrode pair, measures the residual

potential, or voltage between them after the voltage is shut off

or during the 2 second off cycle. The potential is recorded at

j - 3 -

f

different times after shut off. If, for example, there is

sulphide mineralization within the measured dipoles, they will be

polarized or charges set-up in the sulphide particles. This

polarization gives the zone a capacitor effect/ thereby blocking

the current decay, giving a higher chargeability reading.

h typical signature for many gold showings would be a

chargeability high, resistivity high and magnetic low. This is

characteristic of a mineralized, highly altered carbonitized

and/or silicified zone.

However, this is by no means the only geological setting for

gold deposition, therefore, ever IP profile should be looked at

individually and correlated with all other geological and

geophysical data.

The electrode array used for this survey was the pole-dipole

array, using the following parameters:

Method - Time Domain

Electrode Array - Pole - Dipole

"A" spacing - 50 meters

Pulse Duration - 2 seconds on, 2 seconds off

j - 4 -

Delay Time - 500 ms

Integration Time - 420 ms

i Receiver - EDA IP-4

Transmitter - Huntec 2.5 kw

Data Presentation - Individual Line Pseudo-Sections (In Report)

Pole - Dipole Array:

In this array, one current electrode, (CI) was placed at

infinity for the entire survey, while a second current electrode

J (C2) and 4 potential electrodes (P1-P4) are moved down the line

uj in unison. In this case, the "a" spacing or distance between

reach dipole was set at 50 meters. For an Ns l reading, the

closest current and potential electrodes were 50 meters apart.

The C2 dipole remains in the same place, while all the potential

j dipole 2-4 are read. This set up is then moved 50 meters and

i read again.

The IP chargeability readings have been filtered by two

different filter methods "A" and "B" as described in Appendix B.

These filters average the values in a triangle form which takes

J into account the "Pant Leg Effect".

Filtered values can be found on the top edge of each pseudo-1

J section.

l

J - 5 -

SURVEY RESULTS

j It should be stated here that originally an "a" spacing of

l 25 meters was tried but did not appear to reach bedrock in

' certain areas. The survey was then completed with Ha"-50m and on

j reviewing the results, the zone appears much better on NS 4

suggesting considerable overburden depths in places,

j L5200ME;

There is a chargeability high of 23 - 24MS between 1450MS

J and 1575M8 on the south flank of a moderate resistivity high. A

H second very weak or deep zone may be showing between 1700 6

^^ 1800M8 over a resistivity low which may suggest the presence of

j minor sulphides.

The feature at 1450MS to 1575MS seems to be the more

J predominant or shallower structure.

L5100ME:

j There is a chargeability high of 23MS on the south flank of

a moderate resistivity high. The second zone is situated between'1y 1875MS and 1975MS with a chargeability high of 12MS associated

O with a moderate resistivity high suggesting a target at depth 1 with minimal sulphides.

- 6 -

L4200ME:

This line shows a narrowing of the main feature with

chargeability highs of 28 to 31 MS on the south flank of a

moderate resistivity high.

CONCLUSIONS S RECOMMENDATIONS

Generally the IP results has proven the existence of two

zones on the survey grid. The main feature is relatively

consistent, appears to be situated between 15050MS and 1700MS and

strikes across the entire survey area. The weaker zone may

f represent a stringer type response striking southwest off of the

main zone originating between lines 4600ME and 4700ME. This zone

is somewhat weaker than the main zone and may be plunging to the

J southwest.

A follow-up program should consist of diamond drilling

especially in the areas of L4600 and 4700ME where the zone is

j broader. Should the drill results prove interesting then further

drilling would be warranted along strike.

,a

J J J

J

Respect

John

- 8 -

L5000ME:

Again the main zone is evident between 1575MS and 1650MS

with chargeability highs of 23MS. The second feature between

1875M8 and 1950MS appears to be strengthening to 20M8

chargeability highs with a moderate low resistivity.

L4500ME/L4800ME:

These two lines show the main feature shifting slightly to

the south with the chargeabilities increasing slightly to 25MS

again on the south flank of a moderate resistivity high.

The second response on these two lines appear to be shifting

slightly to the north with a moderate increase in chargeabilities

of 23 to 24MS. Both of these highs are associated with moderate

resisitivity lows.

L4700ME:

The IP results show that the two features may be merging

together at depth. The profiles is quite broad with an increase

in chargeabilities to 32MS in the area of the main zone. There

j is a slight resistivity low associated with the northern feature

suggesting sulphides.

J L4600ME to L4300ME:

i These lines generally show one broad feature with a

chargeability high of 35 - 36MS over a moderate resistivity low

i

3 suggesting sulphides are present.

- 7 -

f

CERTIFICATE OF QUALIFICATIONS

I, John Charles Grant do hereby certify:

1. that I am a geophysicist and reside at Lot 2 Martineau Avenue, Kamiskotia Lake, Timmins, Ontario.

2. that I am a Fellow of the Geological Association of Canada.

3. that I am a member of the Certified Engineering Technologist Association.

4. that I graduated from Cambrian College of Applied Arts and Technology, Sudbury Campus in 1975 with an Honour's diploma in Geology Technology.

5. that I have practised my profession continuously for 13 years.

6. that my report on the MIKWAM PROJECT, NOSEWORTHYTOWNSHIP for NORANDA EXPLORATION CO. LTD, is based on work carried out under my supervision.

4. I hold no specific or special interest in the described property. I have been retained as a Consulting Geophysicist for "the property".

Dated this 18th day of February, 1991 at Timmins, Ontario

jJohn C. Grant, C.E.T., F.G.A.C.

J

J

J

APPENDIX A

f

J

J

iiiiiiiiiiiimimimMifiHMiiiiiimimiim

Major Benefits* Six Dipoles Simultaneously Measured* Ten Windows Available

* Choice of Arithmetic or Logarithmic Window Width* Programmable Arithmetic Window Width* High Input Voltage* Weighs Only 8.5 kg.* User Friendly

kW

• l

TransmittersDESCRIPTIONThe HUNTEC M-4 7.5 and 2.5 kW Induced Polarization transmitters are designed for time domain, frequency domain (PFE) and complex resistivity applications. The units convert primary 400 Hz ac power from an engine- alternator set lo a regulated de output current, set by the operator. Current regulation eliminates output waveform distortion due to electrode polarization effects. It is achieved in the transmitter by varying the alternator field currents. Tne transmitters are equipped with dummy loads to smooth out generator load variations. :

fftllli HUNTEC/SYSTEMSJ'Vg'vi'-X'li'"-:^

FEATURES* Solid-state switching for long life and

precise timing.

* Open circuit during the "off" time ensures no counter current flow.

* Resistance measurement for load matching.

Precision crystal controlled timing.

* Failsafe operation protects against short-circuit and overvoltage.

Automatic regulation of output current eliminates errors due to changing polarization potential and load resistance.

APPENDIX B

f

j

j

t \ 4 t N^ t——. It II hM. 4 few l t l f l k—— l t l

Filtered Value Plot Point

N-4

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- 16.5

4 1103,3

FRASER FILTER METHOD BDOUBLE WEIGHTED llf N

Filtered Value Plot Point

[(39X2) * (28+30*31) * (29+17+21) "] * 8

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METAL FACTOR CALCULATION

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Elactrod* Array : POLE - DIPOLE

Moflo s TIME DOMAINReceiver ; EDA IP-1 Tr*n*mitter : HUNTEC 2.5 KW Pulie Tims i 2 Sec on 2 Sec o** Clunjejbili f, Window Plotted : H3 D*lay Time i 500 me Integration Time i 420 m*

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Date o* Survey i 18/1/91

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Date of Survey : 20Xt'9i

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-200

-300

-400

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1O P* lwo*o ic Iwndif fer*ntiated)

Sedimentary Rock* 1OL* LiMNlton* i OS* S*nd*t0ne

t Proterotoic (uodif ferentiated)

VI Intrusive Hock* *wi Volcanic and todi**r.tary Mock*

t Diabave Dyke* 1*11 *9**)

™

7 F*l*ic lntru*iv* Rock* l undi f f er *n t latea j

7ft Apia t* 7* ^egmetit* 78 Gram t* 7f fm l *ic Dyke7S Byenit* 7q^ Quart! Porphyry 7Ba Oranodlorite 7fF F*lOaear Porphyry 7Tj Trondjnewit* 7qfP Quar H -fm J d*p*r- Porphyry

6 Malic Intrusive Mock* (yndl f f *r*nt l*t*O l

*D Dior j t* 60 Gabbro W* *nortKo*it* 6U Ultramafic

5 Ch*"ical fl*t***(Si**rit*r r Roc** (u"di '^*r*nti*t*d i

5cht Ch*rt SIF Iron F gr** t ion [ unai f f *r*r( i *t*0 )

31Fo Quid* P*tiv* (**q"*t*t*i 31F* Sulehltfv F*ci** (pvi po ) 3IFj J**p*r tCh*rt^ 51IF kndcd Iron F crm* 1 1 or

*Chl Chlorit*-r ich Iron For**tion 5Ot Braphit*

4 Cl**tlC n*t***di*i*rit*i'y Rock* ( vJfnS,i M *r*n 1 1* t*J J

4Ca ConglOM*r*t**0 Ou*rtlit* 4flw Bc*yw*C k B 4ATQ Af 9! Ill t* 4S* S*"**too*4ft tiltvton* *Scn tchj.t 4V volcanic (w* f le , tuf+l

3 F*Lmic M*t*volc*nic flacky l undl f **r *n t LatvO )

3R RhyolLt* 3Rd Rhyodaclt*

2D D*C 1 1* 2* Andvtit*

1 n*fit n^tavoleamc Roc** (undif f*r*nti*t*d)

IB la** It lit Iron T ho J*i it* It* n*gn**iu* T no l*i it*

lu UltramaficIK KOAAtlit*

D*ftcr ipt lv* ftObr*viat ion*

apn aphanitic •09 aoglOM*rat* **y anyQOal Oldal tM 0*dO*d Dnd b*^d*d eg caar**-gr4iri*c] fi flow *-b. flow br*cci* fg fine-grained fol foliated gr graphitic hy riy* loc l **t 1C la* la*in*t*d tap l*BtlliIt lapilli tuff MVV *aft*iv* •g **dlu*~gr*in*d pi pi l lowed pel pyoc l ait ic *M*V •*Ai****iv* t tu*f v vvticular *ch *cfii*t

AI t*f*ation

alb a l bi t i t* *^* anker 1 1* bl bleached carb carbortat ited ept epidote K potatvlc •*r **ficit* *ll *1 1 iclf leat ion S

Illllllllllllllllllllllll

WR 68

WR 666*1 y

WR 68*82 y

ta.9t i. *h. IK-W-i ^^"".

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WR 6*478 *^ * V

/\f—————— - — : —————————

WR 68679^ y f*-f.Y "\ Asec y

x,xss". s

-

WR 5828 * WHOLE ROCK SAMPLE

NOTE: SCALE OF AU ASSAYS EXAGGERATED TO

o

\.

SHOW SAMPLE INTERVALS

x o oOJ

z o o n

d400U

0

-400

z o o•*-

:

-100

-aoo

-300

'

1

PROJECT 287 MIKUAM

SECTIQSCALE:

DDH No

Assay Scale :

NORANDA E

N 8400W1/1000 l

: HK-qO-8

Au i c m -- .1 0 g X 4, !

i

XPLORATION~ *" .- . . . . . .

32E12SE0014 63.6B23 NOSEWORTHY

* ', ^# ^

* S \

Ch*rtIron9 ir o 0*14*MF* CulBKltf* FM!** (pv. P*) SIFJM1F ian^M lr*n Far M 11 on

*chl CM*rlt*-ricn Iron

*it tlIt4*eh tchivt4V Volcanic (**fic, luff)

A*tavOlCfi*C Nock* (unflif**r*ntl*t*0)

Rhyollt*

PROJECT : 287 MIKUAM

SECTION 2550WSCALE: 1/1000

WR 5626 9 WHOLE ROCK SAMPLE

DDH No : MK-90-1 andNOTE: SCALE OF AU ASSAYS EXAGGERATED TO SHOW SAMPLE INTERVALS

Assay Scale : Au 1cm ^ .10 g/t

ank ankerit*carb c*rbonatita4K potassic•t) •Uteitieaton NORANDA EXPLORATION

32E12SEaei4 63.6023 NOSEWORTHY S30 - 4702.3

en o o(Dro

CO O O

COoO IDto

en o o in ro

oo

COo o to

COo o t\j f)

I900U 1K-90-2 IK-90-4 1900W '

-100

-200

utotr*

C13

:

1O Pal*otoic

S*di**it lOLtt L i l OS* S*nd*ton*

Prot*roi 0ie (onfllf f*r*nt l At*d l

WR

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00

r 4 SJRfr * **A ^L \ -v.K. ..l, ',. S^ V -

-200*I Int'ottiv* Hock* 'V/S Volcanic and S*t)i**n

C

E

B Diab*** DyK W* 1*11

ARCHEAN

F*lttic lntru*iv* Rock* i undi't**'-*ntiai*d J

7A Aplit* 7P Pvgmatlt* 7G Br*nit* 7f F*l*i

\.** "-

v V x*fJ **l *'r ^ JS "v x x7qP Ou*rtl PorpMyry

Qr*nadiari t* TfP P*ld*p*r Porphyryt* 7g*P O"j*r- 1 1 -F* l dtpf Porphyry

Rock* ( jnfli

V''A. '

-300 I.

bD Diorjt b G Gabbro

Ch*i*ic a l H* t •••diner- 1 ary ROC k* t

3cht Cn*rtSIF Iron Formation l unflif'*'-*rti*t*fli

31Fo OM tO* F*Cl*tt I m*q^*'. i ' * '5[F* Sulp^id* Faci** 'Pi, TO'^lf j Jatp*' icno't ;^B IF BmntjBd I run F or 11* t l L)''

*C^1 Cr'lOrJta-ri^h IrQf ^OfT4tlO^

5G* Gr *prii t*

Cl**tit n*t a^wdim^ntary Roc k k u na j t ' *^

.sMB.O l .-

ithB-e *fc

-10C40 Ouartflt4Gv* Q'*yMacli

4Arg flrgi lilt4S* Sana* t o^*St Sil t*tan*Sc h ^rhi*i*V Volcanic FI**1C,

f* i tt i c "i*t*-oli:*n t

S" 5Rd

[ T ']"2D 2A

l c *^' j c ROL k* i o^d i

-400

IBt I ran Thol*i i t IB* n*gn**iu

1U Ul t r •(••f icl* *0"*t l i t*

*pha"l t J C*gg lo**' at*

la*

C D* r ft* gr a in*d

l"* -gr ain*d aphi tic

bnd baodvd

*-b" t low b'*c c i*'ol roli*twofly "y* i oc l a*t i clap lapilli^———


MOTE: SCALE OF AU ASSAYS EXAGGERATED TO SHOW SAMPLE INTERVALS

mglv Ma*miv* l DI llow*d

32E12SE93M 63.6023 NOSEWORTHY 240

to

l Byrocla*t1C

A l t*ration

• l D *lbitit*

•pi *pidot*•*r t*ricl1*Chl CMorjtll

c ircxxiiti t*d

PROJECT : 287 MIKWAM

SECTION 1900WSCALE: 1/1000

DDH No : MK-90 P and

Assay Scale : Au 1cm O g/t

NORANDA EXPLORATON

COo ofs.

oso oIO

03o o in n

m oo

(Oo oto ooOJfj

wo o(Oo o oK)

600U IK-90-5 600U

-100

-200

-300

-400

309.70 a. W-90-fi

32E12SE9014 63.6023 NOSEWORTHY 250

\

KOLOGICM- i f f

f f *r*nt i*t*d )

Tntru*iv* Mock ft*V/! Volcanic and 3*dln*" tary Rock*

DlafcaM Dy k** (*11 ag*k )

ARCHEAN

CTD F*i*ic Intruviv

7A Ap l i t *78 Gr in 1 1*7S Sy*oit*73a BrarXJdior 1 1*

TronO J H** l t*

7gP

can":

Mafic I

l f * Bf^n 1 1 * t*

P*gm* tit*F* l mieQuartz PorphyryF*la*p*r PorphyryOu*'~tl-F*la*p*r Porphyry

66Dior i t* Gabbro Anort ho* 1 1*

U n0j f0*lfl* F*ci** (M*

51** Sulphlcl* F ac i** ipy, po) SIF J J^ftpvr (ci-*' l ) 3BIF B*nd*d Iron Corm* t lOfi Chlor l t•-^lc^ Iron fo

t*''y Rock* t f *r*nti*t*d )

4Cg*Q Quar11 i t*

4Arg Argjl l 11*4S* Sand*tOA**8t Sllt*ton**Bch Schtvt*V Volcanic !**fit, tuff)

*OC k * ( uflfl l f

M* f ic "*t*volc*nic Rock* l ono j f **r

lit Iron T ho l*i 1 1*10* M*gn**iuM TnolVJlt*

1U UltrMMficL K *0*a CiitB

*ph av^ianitic agg agglow*rat* bd

fi flowf l ri*-qr agrcorii t ic

TT•gpelt•eh

Upilll tuff *waiu*-gr*m pyroc)**tic tuff

Dnd bAndvd

f-Du f lo- brecciafol foliatedhy hyaloclavticlap Upllll

•Ib *lbiti t*b l ei**cn*d•pi *pidot*

pi pt llon*d *M*V ••Mima**!

ank ank*r^t*carb carbonati(*gK pot•••le• 11 tlUcif lcation

chl crilon t i f at Lori

100 j

MOTE: SCALE OF AU ASSAYS EXAGGERATED TO

HOC

SHOW SAMPLE INTERVALS -400

-300

PROJECT 287 NIKUA M...J

SECTION 600USCALE: 1/1000

DDH No MK-90-5

Assay Scale : 1cm ~ .10 g/t

NORANDA EXPLORATION6023,

COo oIN.ro

COo otoTO

COo o inrO

COo oCOo o wro

COo oCMK)

COooCOoo oKl

400E ^-90-6 400E

-100

-200

3 f*rent J* l*d )

totf*i**ntar y ftoek* 10L* L in** t on*

-too

-300

-300

-400

COoom

fi Intruvtv* Woefc*W/s Volcanic and Sedfmntary lock*

Oiaba** Dyke* [all aq**)

ARC Hi AN

f*l*ic Intrusive Rock.* l uno l M*r*nt l at*d l

7A70787047Tj

AC H t* Oranite Syenite 9ranodLOf"l t* Trondjh**! t*

7P 7F 7qP

Feltic Dy** Duartt ôrflhyry F*ia*par Porphyry Quar tI-F*ld*P*r ^

L7QfP

Ma* ir lnfu*ive Hock* i undi f f *r*nt lated l

•D Dtor 11*

frA Anor4tJ

5 ROCKS

Iror. F or** t J or lundl f f *r*ntl ttVtf l D- id* F*tl*t i**9n*tii*) Solphld* F*ci** [py, pol

(ch*rt iIrort Forw^tiOn

CMorite-rJcft lô" fo*-**tion58*

' C.*1 —— T ' — 1

n(J 1 f f *-f *n t 1

COAQlorne* -300

— 1 ——— 13C

CI

TT"• O*) 4Ar fl•S*• St48eh Schist 4V Volcanic

T* t b ic. r** t a vo) C arii c Ri

W flhyollte Wd Rnyodac 11*

[nt*rm*diat* M*t*volt

20 Dac11* 2* Ano**it*

tu'fl

i * '*r*r. t j,*t BO ;

c floc k ^ t urvdl 1 t*r*.n t 4 *t*0 )

Hafic Mwtavolc

11 Ba*a11lit Iron IB* naqnwi

1U Ultra-aîc IK Kooatitt*

D**cr ipt i v* AoCr*v tat ion*

Hock* lunfli f f *r*rtt l*t*0 i PROJECT 287 MIKWAM

•p*•44 bd eg fifa. gr la*

aphanitic*OTlo**i-*t*bcddvx)coar**-gr-aLnflDofln*-qrain*d fraptMtlcIwkinatM

fol hy

TT-

•gKlt

UpLlli Wv n*Mi Pi

a*yflO*loida) bandvc

iIOM breccia foilat*a hyaloclactic ^•gilli NOTE: SCALE OF AU ASSAYS EXAGGERATED TO SHOW SAMPLE INTERVALS

la*tlctuff

Alteration

alb albititebl bleacrtax)•pi epidoteMT **riclt*cM chlori tiiatlon

an h an K *^ 1 1*carb careonat n*dK pot a** i cmil ultei 'lcatlor.

SECTION 400SCALE: 1/1000

DDH No : MK-90-6

Assay Scale : 1cm ~ .10 g/t

NORANDA EXPLORATION4,2,

32E12SE0K14 63.5023 NOSEWORTHY 260

o oK) OJ

COoo c\j f*J

V)o o

COo ooCVI

COo o enCOo oCO

COoo

3912E 1K-90-7 39jj?e i

-100

-200

-300

32E12SE0C14 63.6023 NOSEWORTHY

GEH-OGIC*. LEI* UK

[uno.

lOLft L l (Wit or,. IDS* S*nd*tan*

9V/S volcanic and S*di**ntar^

Ditbaft* Dyk*t f*ll ag*cl

ABCHtAN

F*lnc Intr im Mocks tundiff*r*nt;

rf P*o*ai

7GO Qr*nodiori t* 7T j T rond j h*Kii t*

Intr u*iv

Di or i t*

F*l* ic Dy*BOu*r 11 Porphyry T*ld*p*r Porphyry Quart I-F•)d*D*r ^orphyc

l f f •r*fit l

i**r,t*f-y Roc k m f

ChartIron Forimtion l undi f f ar*^ t i d tad ) 51Fo 0x10* F*Cl** liagnvtitCJ

Sulphid* Faci** Ipy, po j

5B1F Banded Iron Formation CMort t*-rtcfi J'Qn Formation

SO f Graphl t*

Clastic H*ta**dlM*nta-'y Rock* ( unfli f f *r*ntiat*4 l

at*


NOTE: SCALE OF AU ASSAYS EXAGGERATED TO SHOW SAMPLE INTERVALS

00

-200

-300

-400

*OQo*rttIt*Gw Gr*v**ac k4Or g Arg i l l i 'L45* 5a"d*ton* St Si l tmtor,4Se r, ScM*t

['" T5 i F* l 4 ic "l*t a,o] i

L .JJB3flar" T

L .1ZD D*CltB 2A And** 1 1*

LI] Roc

l B Ba*al llit Ironli* n*gn*kium Tnol*lit*

1U Ul tr*(ft.f 1C i* tom*t i i t*

Dr*c r i p 1 1 v* AOf *v l at ion*

• pu *pft*n11 liagg Od

f ln*~gr*i grAphitic

ond bandvd

t-b" 'lo* brace i*fol foll*t*d•IY hyaloc l atticlap lapilli_____

PROJECT 287

IT

pel pyroc l**t ict luff•c " me hi* t

Al t*r*ti(Xi

bl•pi *pidot***r **fit it*C hi cMoritnation

pt oi.iioM*a• ••v ••ffi M***L

carb carbonatn*d

*ll *ille if leat ion gO CM CM

SECTION 391?ESCALE: l 71 100

DDH No : MK-90-7

Assay Scale : 1cm - .10 g 71

NORANDA EXPLORATION

Submitted by: Paul Coad, Senior Project Geologist, …Senior Project Geologist, Regional Exploration...

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Transcript of Submitted by: Paul Coad, Senior Project Geologist, …Senior Project Geologist, Regional Exploration...