NTS 42 C/3 WAWA AREA ONTARIO · 2017-01-17 · 42c03nw0015 2 16555 abbie lake 010 a logistical and...

42C03NW0015 2 16555 ABBIE LAKE 010

A LOGISTICAL AND INTERPRETIVE REPORT

ON

SPECTRAL IP AND RESISTIVITY

SURVEYS

CONDUCTED ON THE

ABBIE LAKE PROJECT

NTS 42 C/3

WAWA AREA

ONTARIO

2* 165 55

JVXLtd.

A LOGISTICAL AND INTERPRETIVE REPORTON

SPECTRAL IP AND RESISTIVITY SURVEYSCONDUCTED ON THE

ABBIE LAKE PROJECTWAWA AREA

ONTARIO

For:

Freewest Resources Canada Inc.800 Rene Levesque Blvd. W Ste. 1525 Montreal, Quebec H3B 1X9

Attention: Mac Watson Tel: (514) 878-3551 Fax:(514)878-4427

Freewest Resources Canada Inc.855 Field Street Thunder Bay, Ontario P7B 6B6

Attention: Don Hoy Tel: (807) 346-0777

By:

JVXLtd.60 West Wilmot St, Unit #22 Richmond Hill, Ontario L4B 1M6Contact: Blaine Webster Tel: (905) 731-0972 Fax:(905)731-9312 JVX Ref: 9603 March, 1996

J VX 42C03NWOO15 2 16555 ABBIE LAKE 01OC

TABLE OF CONTENTS

1 INTRODUCTION™__...™..........™..........™....——.......™....................."....————.............™.....™.........-4

1.1 GENERAL...................................................................................................................1.2 PURPOSE.....................................................................................................................................5

2 DATA ACQUISITION.......——.......""——..———..———............™......................™.™....™™....-.-.--.---6

2.1 SURVEY SPECIFICATIONS ..................................................................................................................62.2 GRID SPECIFICATIONS ...................................................................."".....""..................... -... --- 62.3 PRODUCTION SUMMARY..................................................................................................--..-..---------------?2.4PERSONNEL..............................................................................................................................------72.5FELDINSTTIUMENTATION....................................................................................................................8

3 DATA PROCESSING.........——...........™™—.....™™.........................™.........™-.—.........™..".————9

3.1 IPAhJDRESISTrVITY..................................................................................-..................................--.-"

4 INTERPRETATION METHODOLOGY ........™....................................................................................""" 11

4.1 IP AND RESISTIVITY ..............................................................................................-............................. 11

5 DISCUSSION OF RESULTS........"".".""....-..™.™.........".".""""""........""""™™....."".-...-..""""-". 13

6 RECOMMENDATIONS..™......™"."..™™——™———.....™..............™......™..————......................™. 13

J VX

FIGURES

Figure l: Location Map

Figure 2: Grid Map

TABLES

Table l: Specifications for the IP/Resistivity Survey

Table 2: Summary for IP/Resistivity Survey (3=25 m )

APPENDICES

Appendix A: Background to the Geophysical Methods

Appendix B: Plates

J VX

PLATES

Black and White Line Plots :

Plate l: Chargeability Contours, n^2, Scale l :2500

Plate 2: Resistivity Contours, n=2, Scale l :2500

Plate 3: Compilation Map, Scale l :2500

Plate 4: Stacked IP Pseudosections; MX Chargeability and Apparent Resistivity, L.500W to L. 100W Scale 1:2500

Plate 4a: Stacked IP Pseudosections; Spectral M and Tau, L.SOOWtoL.lOOW Scale 1:2500

Plate 5: Stacked IP Pseudosections; MX Chargeability and Apparent Resistivity, L.O to L.400E, Scale 1:2500

Plate 5a: Stacked IP Pseudosections; Spectral M and Tau, L.OtoL.400E, Scale 1:2500

Plate 6: Stacked IP Pseudosections; MX Chargeability and Apparent Resistivity, L.500E to L.I 100E, Scale 1:2500

Plate 6a: Stacked IP Pseudosections; Spectral M and Tau, L.500E to L.I l GOE, Scale l :2500

J VX_________________

Colour Plots (in 2 reports only):

Plate I: Chargeability Contours, n=2, Scale l :2500

Plate D: Resistivity Contours, n=2, Scalel :2500

Plate ffl: Staked Chargeability Pseudosections, Scale l :2500

Plate IV: Stacked Resistivity Pseudosections, Scale l :2500

Note: l set of individual colour pseudosections in l report only

J VX

INTRODUCTION

1.1 GENERAL

JVX Ltd. conducted time-domain spectral induced polarization (IP) and resistivity surveys from February 25 to March?, 1996, on behalf of Freewest Resources Canada Inc. The survey was located on the Abbie Lake property located approximately 35km from the junction of the trans Canada highway and about 10km east of the Magnicon Mill in central Ontario (N.T.S. 42 C/3). The property is accessible by permanent road from the Trans Canada Highway.

The work was performed on claim number 1189076 which contains 16 units.

1.2 PURPOSE

The purpose of this survey was to map locate gold bearing disseminated sulphides on the property and to improve the geologic understanding of the property.

J VX

2 DATA ACQUISITION

2.1 SURVEY SPECIFICATIONS

Table l : Specifications for the IP/Resistivity Survey

LR/Resistivity

Transmitter

Receiver

Array Type

Transmit Cycle Time

Receive Cycle Time

Number of Potential Electrode Pairs

Electrode Spacing (a spacing)

Number of Lines Surveyed

Survey Coverage

Scintrex TSQ3/3.0 kW

ScintrexIPR-12

Pole-Dipole

2sec

2 sec

8

25m

17 lines

7425 metres

2.2 GRID SPECIFICATIONS

The survey grid, located on the Abbie Lake Property, Wawa -Mishibishu area of central Ontario, is shown in Figure 2.

Abbie Property

LOCATION MAPFREEWEST RESOURCES INC.

ABBIE LAKE PROJECTWawa Area. Ontario

NTS 42 C/3

GROUND GEOPHYSICAL SURVEYtoo 00 o

Surveyed by JVX Ltd. February 1996

N

HFMLO GOLD GROLT \

W9076 •

FREEWEST CLAIM G ROl'F

GRID MAPFREEWEST RESOURCES INC.

ABBIE LAKE PROJECTWawa Area, Ontario

N.T.S. 42 C/3

GROUND GEOPHYSICAL SURVEYScale l : 33,333 (approx.)

Surveyed by JVX Ltd. February 1996

Figure 2

J VX

2.3 PRODUCTION SUMMARY

Total IP coverage was 7425 metres. The following table lists the survey coverage in detail:

Line

500 W400 W300 W200 W100 W0100 E200 E300 E400 E500 E600 E700 E800 E900 E1000 E1100 E

From (stn)00000000000000000

To (stn)475 N475 N475 N475 N475 N475 N475 N475 N475 N450 N425 N425 N400 N375 N375 N350 N350 N

Distance (metres)475.0475.0475.0475.0475.0475.0475.0475.0475.0450.0425.0425.0400.0375.0375.0350.0350.0

TOTAL 7425.0

2.4 PERSONNEL

Ted Lang (Geophysical Party Chief):Mr. Lang operated the Scintrex IPR-12 receiver and was responsible for data quality and theday-to-day operation and direction of the survey.

Henry Odwar (Geophysicist):Mr. Odwar operated the transmitter and helped process the data.

Three field assistants were also engaged by JVX.

Andrew Hwang (Geophysicist):Mr. Hwang processed the data, prepared the plots, and is responsible for the data storage.

J VX

Dagmar Piska (Draftsperson):Ms. Piska carried out all manual drafting, and assembled and bound the report.

Vaso Lymberis (Draftsperson):Ms. Lymberis assisted Ms. Piska with manual drafting and assembly of the report.

Blaine Webster (President JVX Ltd.):Mr. Webster provided overall supervision of the survey, interpreted the data and wrote thereport.

2.5 FIELD INSTRUMENTATION

JVX supplied the geophysical instruments described below. Additional information about the geophysical methods may be found in Appendix A.

2.5.1 IP. TransmitterThe Scintrex IPC-7/2.5 kW Time Domain Transmitter powered by an eight-horsepower motor generator was used. The transmitter generates square wave current output with a period of 4, 8, or 16 seconds. A digital multimeter in series with the transmitter was used to measure the magnitude of the current output.

2.5.2 1. P. ReceiverThe Scintrex IPR-12 Time Domain Receiver was used. This unit samples the voltage decay curve as measured by the potential electrodes at ten points in time. Readings were repeated until they converge to within a tolerance level, and the data were stored in solid-state memory.

J VX

3 DATA PROCESSINGAfter being transferred to a field computer at the end of each survey day, the data were examined, corrected, and organized by the instrument operator. The results were plotted on the following printers:

- STAR NX-80 colour dot-matrix printer* EPSON FX-80 dot-matrix printer

These plots were used to monitor progress and data quality, and to make an initial interpretation. Thus survey parameters and design were altered when necessary.

The data were sent by courier to the head office of JVX in Richmond Hill, Ontario. They were processed and results were plotted on the following printers as was necessary:

. HEWLETT PACKARD DESIGNJET 750C 36 inch colour plotter* NICOLET ZETA 36 inch pen plotter. TEKTRONIX COLORQUICK ink jet printer* FUJITSU DL2400 colour dot-matrix printer* TEXAS INSTRUMENTS MicroLaser Pro 600 Laser printer

The processing procedure is outlined below.

3.1 IP AND RESISTIVITY

Steps l and 2 were performed both in the field and in the head office. Steps 3 and 4 were performed at the head office.

1) The GEOPAKIPSECT Package was used to generate colour pseudosections of chargeability and resistivity data.

2) JVX software was also used to perform spectral analysis of the time-domain data. This step was crucial to maximizing the information that can be obtained from IP data. This software analyses the shape of the I.P. decay curve, giving information about:

(a) the grain size (indicated by the parameter T),(b) the uniformity of the grain size (indicated by c), and(c) the magnitude of the chargeable source (indicated by M-IP).

(Please see Appendix A for more information about spectral analysis.)

JVX

3) The pseudosections from 2 above were aligned in AUTOCAD, then plotted. Since chargeability values are quite low over this grid, none are presented in this report.

4) Contoured plan maps of both chargeability and resistivity data from one dipole were produced using JVX in-house software and the GEOPAK or GEOSOFT Line Processing Package. Additional drafting on these maps was done manually or through AUTOCAD.

JVX

4 INTERPRETATION METHODOLOGYJVX uses its many years of experience in geophysical interpretation to extract the most accurate information from the data. The procedures involved are simplified for the sake of clarity. The SPECTRAL data was extensively used to further define the grain size (fine or coarse grained). The high chargeability amplitude associated with the iron formation made it difficult to select drill targets on chargeability alone therefore IP anomalies with fine grained SPECTRAL responses were given a high priority for drilling.

4.1 IP AND RESISTIVITY

The IP and resistivity data were interpreted using the following procedure:

l ) Chargeability anomalies were picked on the pseudosections and classified using the following scheme as a guide:

Very Strong (^ 30 mV/V) and well defined

____ Strong (20 to 30 mV/V) and well defined

_ _ Moderate ( l O to 20 mV/V) and well defined

- . - Weak (5 to 10 mV/V) and well defined

- - - - - - Very Weak (3 to 5 mV/V) and poorly defined

x x x x Extremely Weak ^3 mV/V) and very poorly defined

The peak of the anomaly provides a qualitative indication of the depth to the top of the anomalous source and the location of the centre of the body. Where possible, the location and dipole number of the peak are written beside the anomaly bar.

2) The SPECTRAL characteristics of the anomalies were examined. The peak value of M- IP is noted, and r was classified according to the following scheme:

L Long ( ^ .00 sec )

M Medium ( l .0 to 8.0 sec )

S S/iorf^l.Osec)

44,

J VX

3) Resistivity anomalies were picked on the pseudosections and classified using the following scheme as a guide:

no symbol VH(n) Very High (? 30, 000 Qm) highly silicified

no symbol H(II) High ^ l O 000 Om) probably silicified

no symbol WH(w) Weak High ^ l O 000 Qm) relative increase comparedto surrounding material

SL(n) Strong Low — strong decrease in resistivity

~ ~ ~ ML(n) Medium Low — medium decrease in resistivity

WL(w) Weak Low — weak resistivity decrease relative to surroundingmaterial,

where n is the dipole number at which the anomaly peak is located.

4) The anomalies from steps l to 3 were marked on the Compilation Map.

5) Resistivity anomalies on the Compilation Map were joined into conductive and resistivezones.

6) Zones of high chargeability were interpreted based on resistivity and geometric information.

7) The chargeability anomalies were further prioritized employing the SPECTRAL parameters paying particular attention to the relative amplitude of the MTP response and the length of the time constant.

8) The IP and Resistivity data was reviewed on the compilation map with ancillary geologic and geochemical data.

J VX

5 DISCUSSION OF RESULTSThe IP anomalies are shown on the compilation map and on stacked pseudosections.

6 RECOMMENDATIONSThe IP anomalies on the compilation map should be examined geologically and geochemically.

If there are any questions with regard to the conducting of the survey or the interpretation of the data, please call the undersigned at JVX Ltd.

Respectfully submitted,

JVX Ltd.

Blaine Webster, B.Sc. President

APPENDIX A

Background

to the

Geophysical Methods

J VX

INDUCED POLARIZATION AND RESISTIVITY

l THE IP EFFECT

The induced polarization (IP) phenomenon is primarily caused by:

1) electrical polarization at the boundary between the rock or soil and the pore fluids, and

2) electrical polarization at the boundary between metallic minerals (particularly sulphides) within pores and the pore fluids.

This polarization occurs when a current is applied across these boundaries. Its magnitude can be measured in two ways:

1) in the frequency domain (also known as phase IP), in which the applied current is sinusoidal, or

2) in the time domain, in which the applied current is a modified square wave.

JVX conducts IP surveys in the time domain because spectral analysis, a powerful interpretive tool, can only be performed in the time domain.

Generally, the current is transmitted as a modified square wave with a period of eight seconds (two seconds positive, two seconds off, two seconds negative, two seconds off). The voltage measured in the ground will have the form shown in figure IP-1. The IP effect is manifested as a roughly exponential voltage decay after the current is turned off, similar to the relaxation effect of a discharging capacitor. The IP receiver samples this voltage decay curve at a number of points.

The SCINTREXIPR-11 receiver repeats and averages the following measurements until they converge:

Vp The primary voltage (the steady-state amplitude of the voltage while the current is being transmitted).

IP-1

J VX

SP The self-potential (the steady state voltage when no current is being transmitted).

mO to m9 The chargeabilities (measures of the IP effect at different times along the decay voltage curve Vs(t)).

Each chargeability value (mO to m9) is the ratio of the average secondary voltage over a time window to the primary voltage. Mathematically, this is given by:

r*-m = 1000 l Vs(t) dt

VP(VU J t,

wherem = chargeability (in mV/V)

Vs(t) = secondary voltage (i.e. the voltage decay) Vp = primary voltage t, = beginning of time window ta = end of time window

The IPR-11 uses the ten time windows, also known as time slices, listed in table IP-1 and shown in figure IP-2. Unless otherwise stated, the term chargeability refers to the eighth time window (m7).

IP-2

Vp

coSP

Vs(t)

Figure IP-1 : The I.R. Waveform

J VX

SLICE

mO

ml

m2

m3

m4

m5

m6

-;tfft :v- V - -•-•-.-.Kf.^^-^.f'jf^.-:.-:--

m8

m9

DURATION (msec)

30

30

30

30

180

180

180

36O -;^1;

360

360

FROM (msec)

30

60

90

120

15O

330

510

^690liS - : .- .. -. . z -:-,\ \.-X.-- -.--..:-

1050

1410

TO (msec)

60

90

120

150

330

510

690

lofpijj1410

1770

MIDPOINT (msec)

45

75

105

135

240

420

6OO

1*; :^ :J1230

1590

Table IP-1 : Time slices recorded by the IPR-11 receiver

Nominal total receive lime 0.2.1.2.4 sec

Window Width

IPR- It ftvsienr Windows

Figure IP-2 : IP effect decay curve with IPR-11 time slices

IP-4

J VX

2 SPECTRAL ANALYSIS

With the ability to sample the decay curve at a number of points, the shape of the decay curve can be analysed. This gives important information about the characteristics of the source.

Spectral analysis utilises the Cole-Cole model of the IP effect (Pelton et al.. 1978). This model uses the following four parameters (described in Johnson, 1984) to calculate a theoretical IP decay curve:

pa Resistivity (Sim)This quantity is described in detail later in this appendix.

M-IP Chargeability Amplitude (mV/V)This quantity is related to the volume percent of the chargeable source, although there is no simple quantitative relationship.

t Time Constant (seconds)The time constant is related to the grain size of the source. A short time constant (0.01 to 0.3 s) indicates a fine-grained source. A long time constant (30 to 100 s) indicates a coarse-grained, interconnected, or massive source.

c Exponent (dimensionless)A high value (e.g. 0.5) indicates that the grain size is uniform. A low value (e.g. 0.1) indicates that there is a mixture of grain sizes.

Conventional chargeability is a combination of these spectral parameters. A change in any one parameter will produce a change in the apparent chargeability. In the absence of spectral analysis, such changes are always ascribed to a change in the volume percent of the chargeable source, even though the cause may be a shiftfromjine-grained to coarse- grained material.

JVX has developed a software package called SOFT n which determines the spectral parameters by comparing the measured decay curve with a library of model curves. The quality of the fit is given as a root-mean-square difference (expressed as a percentage). A low value (e.g. l *J6) indicates high quality data of medium to high amplitude. A high value (e.g. greater than 10 *J6) indicates poor quality or low amplitude data. If the fit is greater than 5 *J6, the spectral parameters are considered to be of poor quality, and therefore are usually discarded.

IP-5

J VX

3 ARRAY CONFIGURATION

As mentioned above, a current must be flowing through the ground in order for the IP effect to occur. This current is applied using two electrodes, which are called C l and C2. and the voltage decay is measured using two potential electrodes, PI and P2. The distance separating PI and P2 is known as the a-spacing, or o, and generally remains constant during the survey.

The three most common electrode array configurations are:

1) GradientC l and C2 are located at an "infinite" distance (i.e. very far) from the grid, with one on each side. The potential electrodes move throughout the grid.

2) Dipole-DipoleC l and C2 are separated by a distance of o, and move along with the potential electrodes.

3) Pole-DipolcC2 is located at "infinity". CI moves along with the potential electrodesthroughout the grid.

The gradient array allows for fast reconnaissance surveys. However, no depth information is obtained (described below), and the resolution is much lower because all of the ground between CI and C2 is energised. Furthermore, the current will be channelled through conductive zones, which could result in inaccurate chargeability and resistivity values. Thus, great care must be used when using a gradient array.

In JVJC experience, the pole-dipole array is superior to the dipole-dipole array. Since C2 is located at an infinite distance, a greater volume of ground is energised. This results in better depth penetration (i.e. higher quality data), and is particularly important in the presence of thick and/or conductive overburden. However, the pole-dipole array does not have the disadvantages of the gradient array. Since C l is located near the potential electrodes, depth information is obtained (see below), and resolution is high.

4 A-SPACING AND NUMBER OF DIPOLES

The resolution of the data depends on o, the electrode spacing. The smaller a is, the greater the resolution. However, the depth of penetration Is also smaller. A larger a results in greater depth, but less resolution. Thus, both factors must be considered when selecting the electrode spacing.

The standard pole-dipole array is shown in figure IP-2. Seven potential electrodes are used to measure the voltage simultaneously across six electrode pairs (P1-P2, P2-P3. P3-

IP-6

J VX

P4, etc.). Each pair is labelled using an integer, o. where na is the distance between the first potential electrode and the nearest current electrode.

The depth of investigation is greater when the potential electrode pair is farther from the current electrode (i.e. larger n). However, a greater separation distance also results in greater signal attenuation, limiting the number of dipoles which could be used effectively.

5 RESISTIVITY

The DC apparent resistivity (pa) is a measure of the bulk electrical resistivity of the subsurface. Electricity flows primarily through the groundwater within fractures and pore spaces. Therefore, fault zones can be detected as low resistivity zones. However, sulphide minerals, some oxides, and graphite are also good conductors and so produce low resistivity zones. The current flow is electronic in these minerals rather than electrolytic as it is in groundwater. Sometimes, the geometry of the low resistivity zone can distinguish between a fault zone and a mineral source. In other cases, additional geological information is needed. Silicates, the most common rock forming minerals, are very poor conductors of electricity, producing high resistivity zones.

The resistivity is measured simultaneously with the IP data. For a homogeneous and isotropic subsurface, it is given by the following formula:

wherepa = apparent resistivity (Qm)

Vp = primary voltage (measured while current is on) (mV) k s k-factor (m)

The k-factor is an array-dependant component. For a pole-dipole array, it is given by:

k = 27m(n*l)a

wheren = dipole multiple (dimensionless) a = electrode separation (m)

Although the assumption of a homogeneous and isotropic earth is unrealistic, the calculated value of pa can be used qualitatively to map changes in rock type (even to identify the rock type in some cases), and to map low resistivity fault zones.

IP-7

J VX

References

Johnson, I.M. Spectral I.P. Parameters as Determined through Time Domain Measurements, pp. 1993-2003 Geophysics 49. 1984

Johnson, I.M., B. Webster, R Mathews. and S. McMullan Time Domain Spectral IP Results from Three Gold Deposits in Northern Saskatchewan. The Canadian Mining and Metallurgical Bulletin, Feb. 1989

Pelton. W.H., S.H. Ward. RG. Hallof, W.P. Sill, P.H.Nelson Mineral Discrimination and Removal of Inductive Coupling with Multifrequency IP. pp. 588-609, Geophysics 43, 1978

IP-8

APPENDIX B

Plates

flPR-lS-96 09:33 FRffl-EST RESOURCES CflNflOfi

•i k. li: ^hl.tl i: 5'' Ml M Mi REG S S MARIE

TEL: 907-346-0778

TEl :05i-l56935

P:02

P IJWi

Ministry ofNorthern Developmentand Mines

Ontario

Report of Work Conducted After Recording Claim

Mining A*

.!W90DO.

Paraonal iftto'maUon cotactvd on ihl* lot m i. owajnod und*r mo Minority Of ir* Mining Aa. TN* information lil D* uaad tor cormpondanca. Ouastioni tooui thii mirror* nrrniirt rm d'wanrt m rtw PmvlnrW MMMOTY Uftino l mm MnMry rt rinnrwn nmrimnmni nnd Mmn. Feunn Flogr. i tt CMM Sun:. fcKtoory, Ontario. PIC MS. Mlaplwna (70S) 670-72*4

instructions: - Please type or print and submit m du*"-"- Refer to the Mining Act and Regulat

Recorder.- A separata copy of thia form must b- Technical reports and maps must ex- A sketch, showing th* claims the we

165 55

42C03NW0015 2 16555 ABBIE LAKE 900

Wgrfc

WanTO.

37&ZFrpm:

Work Performed (Cnech One Work Omup Oily)Work

Oeotectinlcsl Survey

RECEIVEDType

Phytlcal Work. Including OrtlNng MINING LANDS BRANCH .--iRenabOnaiiori

AuthoUedVUOfV SECTION 18 ONLY —. ^ .Assays

Aselgnmwit from Reserve

Total Assessment Work Claimed on the Attached Statement of Costa S ^.

Note: Trie Minister may reject for assessment work credit al or part of the assessment wont submitted if the recorded holder cannot verify expenditures claimed In the statement of costa within 30 days of a requeet for verification

and Survey Company Who Performed ttw Wo/fc (Give Name and Address Of Author of Report)Name Address

60 Oin( to'.nwl W,

t sch*dt4* If n*cs*sary)

Certtflcatlon of Beneficial Intereet * See Note No. 1 on reverse side

l eorriV iMt d ** *n* *** wwrm DM pvrtomwd. UM ctakn* covered In M* wort xH*x*)*nm*i*lBtK*niiKfO*M*i'*ii*i**oMMuo4*i 11*..W. Vmt*.** by Ih* cuirww r^cortfod

i*Certtflcadon of Work Report

l RMtlfy thill l hmn H prwnri frnrmlMlQa tt fh* Itrm aat form m mt Work ropot. nixing portormod mo Mont or na compMHon and nnanod rtporr b toua.

MM* *urMf nATtr

c*rnyin(tort* Ac..

DiE

dent to, CFor oniee Uee Only

Tot*! Pan

f S r

RECEIVED

, APR 1 5 1996 pM"s* '-f .VlJ.2.3.4.5.1

i

769 P03 00 -00 00:00

ffiH

ln i

i! S l

Cradta you an daiming hi into rapon may ba cut back, in ordar to mWmtoa fha advwa* cfhxa of aucfi dalatiom. piaaaa indteata from which daima you wlafilo prtortw tt* ovation gf cradto. Piaaaa mark (^) on* of tha following:1. O CradHt ar* to b* out bacfc ataninfl wfm ma dahl RMad (tat, wortdnfl2. Q Cradta ar* to b* cut oacfc aquafty ovar al otaima contaJnad In thb raport of wort.3. O Cradto ar* to ba ci* oaok aa priorlxM on th* aoaonad appamttc.

In ma awm that you hava not apaefflad your ehttte* of priority, option ona wM o* bnptomantad.

tHJHfXUOfbtnajlrirt toHr** an*imrrnnrnVtitraoafm.optionaorxnunti.mamorandgaaofao^oomofito.eta..whhraapaet lo Hw mining ctafma.

it wont naa Man pwwmwd on pataMM or land, pta

tJonmr*or fMtttf tontf it tftff ttvnt DM mvfc ww

•5S5T

Ontarioana Mint*

Mininarodu DtvMoppemem du Notd el dM mines

769 P04 J

W ' 80 00:00

des coats aux fins du crtdlt devaluation

Mining Act/LoJ Mf tea mint*

Penon*) Information Mtecwo1 on rtrii term la obtained under the auDwrky Of the Mining Act Tnj| IfltBrfMdOn rt tM iSWrt Hi mnMtln t record and ongoing, stalu* of tfte mmbig cttl*i(*). OueeOone aoout 1MB oo*l*chon ehovld be dUacvd to *e Provlndel Manager. Mlflhg* Land*. Mnttry ol Nonftoni Development end Mlnee. 40 ROOT. iW Cedar Street. Sudbury. Ontario P3i 6A5. telephone (70S) 670-7284,

Le* ren*e4gn*menit* pareanntt* comnu* dan* la pr**Kiw l* U Ut 4M U* ••A-* ** Mivhuni i terur a f

formula tor

dee eoreertuiu mWere*. Adrtntr tout* queakon n/r la oafleoe oe ce rtoMkjnemtnla tu chtl provlnoW dM tatntnt Nnien. mWatir* d OtvwjppMfWM du Nocd et dtt Mine*. 1S*. rue Cedar. 4* ftagt. Sudbur (OmartO) P3t *AS. ItMphont (70S) 170-7194.

i. uuvct coftta/CoOto dtrectf

Type

WogeaSeUioa

conttootar*end CoAtuTfanrt't Pee* Orolt.de rentrapronotfr e* d* 1*4.^^1- eoAaea

Supaaaauted TournHuiea unaiea*

•ouuMoni VtonMt Laotttonde•maalAflklItVVAaM/MMJ

nAAAJHJVaVMiuvnuiyuun

Labour Makwd'oouvr*FMd SuptfvMan SuunnWon sur It terra*

TVP* IftuwIU^

f.p. *.*Mf

T*te

TIT*

AfMUH

ManMrt

S.*o

/S, 5(3

Total Oiract Coat* Total daa ooOts dlraota

Tou* ToWgtobJl

/t2f3

rt.*fc

7 irunrart rottt/CoQtc** Note: Wntn claiming Aehibtitanon wort mdirea oettt are not

aNowrabie aa MMwntm work. Kogr it mmMuêment dot trtvwn de rehtbikMton. le* cootl Indbteu no tent pa* admieeltlM en MM quo iravaugr ftvaluaten.

Tnmpoit

ModoM Ladêak II IIJÎ^

NomHurtot

MlbMOBMMtl

Armir*Montan!

TnmH Total glob*i

Sub Total of Indkvct Coata Total partial daa eotta Mirveta

attr than JO* of Otratt Coets) ada*tibit (n-enaaam pet 10 W de*

ToW Veto* ol to(Te*l *l Btrtct MM ABnroV*

Vrieur ItWe du

NMO- The recorded hoMor -a bo roaMO* it wo*V tiownOJH* tit^.^J .. dM MM*mtM( a* MM wKMA W J.r * uf * .-m**wl k* mlRuBthm U MrtVitlnn ir nnr mtoo. tho Utnlatai May M|iil (M UUUM^.4 --.k al or p*t of m* asMcarftant *om tubmiaad.

Nw4* : U KuUv wirvgh)n4 eon wu oe vermtr tea oepentat oemaodtes tfan i* praatnt Mtl des ooos nant le* X )ounj sulvant urt* demand* t ei Hw. St l* J.IILA*! uW |Mi Mmnueo. * mmun* peui r*)*ter KX. OU une p*H* dM Wwvmu* d'Avduatton pnUeniM.

CXaeounta

1 . Work filed within two yea* of completion li dalmad at 1 0Ofc of tho obowo Total Ualu* tf A*Mi*.w*.U

Ramlsn pourdtpAt

1. LM tnvaiH dtpotm dan* IN oeux ant tuWant Itw aohovtmeni tout iHinuguniw* wu-notavaiouf totatflsuememuir**ducttc* Jfr/Mualo

2. WofktilodtNw. fogrortlv*ytar*antTeo(nplationitci*lm*dal 50*A of tttv above; Total Vakia of AsMtamont CrooU S** calculations boWw.

rot*l vaw* M AJIHIHUK OetV

OJO

2.aont romboursa* 4 SO H de la valour toiato du credit d'ovaluabo iunnanttonfit. Votr hw aim* rinx**n

M 0.10

CeitfflCltlon Yiftlvlrro fttniffiwnt nf

l horaby certify:that rho amount* tnown ara as aoounto aa possible- and (nasa eoata

tn *a aaaamatKylH* ru,u.l wl Wwik

Affectation do I'dtot ala* aadta

J*utaste par la praaania:qua (aa montanla indlquaa aont la ptua anct possible at qua ea (llVlrWm nrfl M mdO-H W* iftartiinr Irr tmrui d'OxluoK*. sur m terrains moiquas oana la •ormglf M rweort da travsn cHnini

Etou-atUreda(ttuair* rvigmr*. r*ertt*nuit. MMI oceuot MII n

)a iuh

lo maKa this certification. a faira cone an**tattoo.

fegnwurt

B1IIOM-) , (onou'l

OntarioMinistry of Ministere du Geoscience Assessment OfficeNorthern Development Developpement du Nord 9 33 Ramsey Lake Roadand,Mines et des Mines 6^h pioor

Sudbury, Ontario P3E 6B5

Telephone: (705) 670-5853 Fax: (705) 670-5863

July 5, 1996 Our File: 2.16555Transaction #: W9650.00022

Mining RecorderMinistry of Northern Development 6 Mines60 Church StreetSault Ste. Marie, OntarioP6A 3H3

Dear Ms. Lessard:

SUBJECT: APPROVAL OF ASSESSMENT WORK CREDIT ON MINING LAND, CLAIM TB.1189076 IN THE ABBIE LAKE AREA

The revisions outlined in the Notice dated June 27, 1996, have been corrected. Accordingly, assessment work credit has been approved as outlined on the Declaration of Assessment Work Form accompanying this submission. The credit has been approved under Section 14, Geophysics (IP) of the Assessment Work Regulation.

The approval date is July 3, 1996.

If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5858.

Yours Sincerely, ORIGINAL SIGNED BY:

Ron C. GashinskiSenior Manager, Mining Lands SectionMines and Minerals Division

^LBJ/CC

cc: Resident Geologist /Assessment Files Library Sault Ste. Marie, Ontario Sudbury, Ontario

jw i li' 1-"

toQ) -1s

UJ

L-j1

UJCQ;DO

10 Q)

01 l

OL

REFERENCES

DOCUMENT NO.

MINMO CLAIMS f TC AAlLWAVAMpftJQMTOfWAY ,ftjrtuw

SSM

I06I979 JI06I980 |I06I9BI

OAIOIMAi SHOHELMI

*8M S SSM 1062181 Nns9|76 1062175 |O62I441 S* 1061293

OF CMMM LANDS

LCfNCS Of OCCUPATION .- OftDfft MICOUNCIL fttKAVATKM CANdLLEO SAND A OftAVtL

FOR STATUS.

G-23861224638 Ofti mmmm NNIWT* M ^**ML* r*r*MTC0 MIMNI f* ***VMtIB M *IN*MAt f*t*frff( *r ftM

ACT. HA* **i*. M/v M*. Me M vwflnc t-X^A rAREAS WITHDRAWN PROM OIIPOtlTlONO^XT- i , ' ^^ y

224636 i XI224637 fl M.ftX). - MINING ftfOHTS ONLY

. - SURFACE KIOMT5 ONLY

M.* S. - MINING AND SUM AC* ftfOHTS1224639,

r ISSUESSM j S^iv l SSM ' SSM

992123 j 992124 199626Z 996261 99626O

j— — __

5262 996261 '

sri. - i

i SSM T~SSM l SSM i 991618 l-991617 9916161

SSM \ j SSM 992127 , 992128 '996266 1996267V 996288 '

'-———— >--J

SCALE: 1 INCH - 40 CHAINSLEGARD

FOR'STATUS

SSM i S&M

1 asieee ooicc?

SEE PI/AN-- G-

ABBIE LAKEM. N. R. ADMINISTRATIVE DISTRICT

WAWA

MINING

SAULT STE MARIEUNO TITLES/ REGISTRY DIVISION

THUNDER BAY

Ministry ofNaturalResources

Ministry ofNorthern Developmentand Mines

G-3762

42C03NW0015 2 16555 ABBIE LAKE 200

LO Q) -1 01

iCD

UJ

CD OD

l/Q-sO

i

Ut

8s

U

8 8 8 8M

8

Claim Block 1I89O76

400 N

300 N

200 N

42C03NW0015 2 16555 ABBIE LAKE

400 N

300 N

200 N

100N 100N

210

1* *

2.165 55

FREEWEST RESOURCES CANADA INC.

ABBIE LAKE PROPERTYWAWA AREA, ONTARIO

______N.T.S. 42 C/3^——-

CHARGEABILITY CONTOURS (NN2)CONTOUR INTERVALS' 1.0 mV/V

POLE-DIPOLE ARRAY (a^ CHARGEABILITY MX ( 310- 1050 ms)

SURVEYED BY JVX LTD. USING SCINTREX IPR-12 Rx : TSQ-3X3.0kW Tx

MARCH 1996

50 50

METRES

100 150

PLOTTED BYA.H.

MARCH 1996SCALE 1:2500 PLATE 1

JVX REF NO 9603

400 N

300 N

200 N

100N

t*8 8

w8

42C03NW0015 2 16555 ABBIE LAKE 220

8 8 8M8 8 8

m

w8

Ol

8 8OB

8ID

8m 8

m

400 N

300 N

200 N

100N

165 5 5

FREEWEST RESOURCES CANADA INC.ABBIE LAKE PROPERTY

WAWA AREA, ONTARIO ______N.T.S. 42 C/3______

RESISTIVITY CONTOURS (N*CONTOUR INTERVALS: 500 A 2000 OHM.M

POLE-DIPOLE ARRAY (a-25M)

SURVEYED BY JVX LTD. USING SCINTREX IPR-12 Rx : TSQ-373.0kW Tx

MARCH 1996

50 50se*

METRES

100 150

PLOTTED BYA.H.


JVX REF NO 9603

w8

400 N

300 N

200 N

100N

Very Strong

Strong

LEGEND

WH(2) - Weak High Resistivity n-2 H(1) - High Resistivity, n=1 VH(2) - Very High Resistivity, n-2

l Strong Resistivity Low

Tun*

Weak l

M-IP(mVV) 517 . L j ( onstant (Long,Medium or Short) ' |

Very Weak

Extremely Weak

CHARGEABILITY ANOMALY

8

Weak Resistivity Low

Very Weak Resistivity Low

RESISTIVITY ANOMALY

l42C03NW0015 2 16555 ABBIE LAKE 230

400 N

300 N

200 N

100 N

LEGEND

IP-1

- -7*7 r/•7*71^7- '' l/ RH-ia

•Chargeability Zone

Wide Anomaly with two centers

•Resistivity High

* 16 5 5 S

COMPILATION MAP

FREEWEST RESOURCES CANADA INC.

ABBIE LAKE PROPERTYWAWA AREA, ONTARIO

______N.T.S. 42 C/3——^—

CHARGEABILITY CONTOURS (N=2)CONTOUR INTERVALS 1.0 mV/V

POLE-DIPOLE ARRAY (c^ CHARGEABILITY MX ( 310- 1050 ms)

SURVEYED BY JVX LTD. USING SCINTREX IPR-12 Rx : TSQ-J/Z.OkW Tx

MARCH 1996

50 50

METRES

100 150

PLOTTED BYA.M.


JVX REF NC

LINE : 500 W

INDUCED POLRRIZRTION SURVEY

POLE-DIPOLE flRRflY

. . —DfPTH POINT

N z 1. 2. 3. 4. ..."H" SPHCING = 25.0 METRES

FREEWEST RESOURCES INC

RBBIE LflKE

WflWfl RREfi. ONT.DflTE : MflRCH 1996 REF : 9603

SCRLE - l i 2500

JVX LTD.

RESISTIVITY

MX CHO.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

| IQpN ,12SN f 1 5pN t 175N t 20pN . 225N t 25pN | 275N , 30pN 32SN , 35pN t 375N | 40pN | 42SN' ' " ' ' ' ~'~ "

. . , -, - . .

20 . W /O/

10

7K l .9K 4v2K 5.1K^3.2K 2.8K.

2-6K 2. OK 3. OK 3. IK 3.4jt^b.

2K 2.6N l77lN7.6K 2.81? K2K

2.8K/.7K l -5KN2.3K /5-6K

OK 1/.7K l -9K l -4/ V.1K

2.3K l -8K 1.9JC3.2K

5.6KRESISTIVITY

N:l

N:2

N:3

N:4

N:5

N:6

-r/*-/ r/9-/' z/*-/"75.N l OPN 1 25N . 1 5QN . 1 75N . 20QN 225N . 25QN . 275N . 30PN 325N 375N 400N 425N 450N 47

15

LINE : 400 W


POLE-DIPOLE RRRRY

Nfl . K

DEPTH''POINT

N - 1 . 2. 3. 4. ... •R- SPRCING : 25-0 METRES


RBBIE LRKE

WRWR RREfl, ONT.DflTE : MflRCH 1996 REF : 9603

SCRLE r T: 2500

JVX LTD.

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:fa

N:2

N:3

N:4

N:5

N:6

ON N t 1 25N ( ISpN t 1 75N t N | 25pN ^7^ t 30pN | 325N t 375N t 40pN

782.0

O l.OK l

J5.0 382.0 324.0 286.0 793.0 952.0 l-5K l .2K 4^JK 2-OK 3.OK 2.3K V 1-^K 5.8H

.0960.0789.0616.0 l -7K l .7K l .6K 1.1K 2.2K 2.9K 2.4K 2.6K 2-2K 2.4K

li.O 1-6K l . -IK^t^TK 2. 7 K 2-l^K l .4K ^-T^K/T^a* 2-8K 2.5K 2.8K 2.8K

- U I -1 r\ y/fxK^ A. B AK -j r 3fl 3 . 8 K 2 - l "K 2 - 4 K A * o K l .6 K 2 * 9K 2*3K 3- 3K

1.4K l .yK/^Tgpr^&iTK 5.2KJ 2-7K 3-2K 1/8K 1.8K^.2K 3.2K 3.3K

.3K 2 .JtfK Z.QK fUTeR^T^K 3T-4K 4-OK 2.3K l-8K Z .\K 2 -6K 3-7K

RESISTIVITYN:l

N:2

N:3

N:4

N:5

N:6

175N 20N 225N 25N 30N 325N 35N 375N 40N 425N

12

13

13.8

LINE : 300 W


POLE-DIPOLE flRRflY

N - 1 . 2. 3. 4. ... "R" SPRCING - 25.0 METRES


RBBIE LflKE

WRWR RRER. ONT.DflTE : MflRCH 1996 REF : 9603

SCRLE - 1 : 2500JVX LTD-

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

3N t 125N t ISDN t 175N | 20pN 22SN , 25pN ,275N [ 30pN . 325N , 35pN [ 3*75N | 40pN 425N ,45pN | 475N.i;1""^,-'- iol fa? o 'v ' h'-T H'^V RESISTIVITY

686

1.0K325.0 2..3JS l-4K 3.7K 1.51693.0, 3.01*17.0 l .9K

1.5K 1.2K l.Otf 4-rWJ 3. 1K\1 .iX^^Hl /-2K l .2K N:2

.OK 2.9K 2.2Kx^XO^/!-**--r;5K N:3

3.3K N:4

2.1(681.0 l ./(//pfttl^T'.ChL 4.0K N:5—v //7 *—-*S/6K /^8Kl l .1(666.0/ /7AOKx^.lK 6.2K N:6

I P- J 7*2 IP- Z q35pN t 375N t 40pN t 425N

CHO.

LINE : 200 W


POLE-DIPOLE flRRflY

ocrTM*roiMT

N r I ' g- 3- *- - - - __ 25T5 M ETRES


RBBIE LRKE

WRWR RREfl, ONT.DflTE : MflRCH 1996 REF : 9603

SCRLE r 1: 2500JVX LTD-

RESISTIVITYON N tIQpN |125N tISpN | 17pN |20pN , 225N , 25pN ,275N t30pN t325N | 35pN , 375N |40pN 425N ,45pN t 47pN

N: l

N:2

Ni3

N:4

N:5

N:6

18

312

-O 187.0 372.0:

276.0x*fTl(616

^1.4K 1.1*/' 1 -4K 1-2(67

.OK 1-21647

1-5K913-0

273

HI5T1-3K I-4JJ 2-3J624-0 368-0 ^2.0(613.0 2.7K

T-fr^ 2\JJ^ l -6K

8K 2.7K /s^^. l "

2(659-0/^S?ru o l \

5.2K

O 367.0XV7.iK~7.0K 6-9K

RESISTIVITY N:l

N:2

N:3

N:4

N:5

N:6

MX CHG.

JTP-fJN JOpN J25N

IP-2. IP- IP'3175N

4.6 4.7 4.4 ^5-2l,. T-ji H' tot

^25pN .275N 30PN 325N 35QN 37SN 400N' -l m.* * ' l. * **t . .L * i- ^.'i . .' . f * *

T-.^S^H-Sl^ "7,0. 5-3

N:2

N:3

N:4

N:5

N:6

CHG.

3.0

N:2

N:3

N:4

N:5

N:6

LINE : 100 W


POLE-DIPOLE flRRflY

fl.

DEPTN'VoiNT

N r 1. 2. 3. 4. ... R" SPRCING - 25.0 METRES


RBBIE LRKE

WRWfl RREfl. ONT.DOTE : MORCH 1996 REF : 9603

SCRLE r 1: 2500JVX LTD-

RESISTIVITY

MX CHG.

l

N:2

N:3

N:4

N:5

N:6

N:l

N:2

N:3

N:4

N:5

N:6

2.165 55175N ^ODN t225N ^5pN

Unes 500 w - 100 W

ON SON 225N "

30 lN ^2^ t 35pN (375 ~~~~

MX CHG.

N:5

N:6

PLATE 4Scintrex IPR-12 Rx

42C03NW0015 2 16555 ABBIE LAKE 240

K

LINE : 500 W

INDUCED POLRRIZFITIONSURVEY

POLE-DIPOLE flRRRY

H/) .a

--0, ^* x *

oerTM^poiNT N - 1 . 2. 3. 4. ...

"R" SPflCING : 25-0 METRES

FREEWEST RESOURCES INC-

flBBIE LRKE WflWfl flREfl, ONT.

DRTE : MRRCH 1996 REF : 9603

SCflLE - 1 : 2500

JVX LTD-

SPECTRAL MN:l

N:2

N:3

N:4

N:5

N:6

TRU(X 10') N:l

N:2

N:3

N:4

N:5

N:6

Op t 25,N ( 50^ t 75,N ÔpN t!25N t ISpN (175N ÔpN 225N 2SpN 275N 30pN 325N 35pN 375N 40pN 425N 45pN 475NSPECTRflL M

83.1 70.7^51/0268.7 279.3 164.6 153.9 123.6 105.7 196.6 91,. 8 68.3 86-9,127.7117.6201.7202.4255^,4198.4192.7 Nil

79.5/1^X^8.9(260.2^30.8 W~v5 128.2 125.2 140.V^.-3 66 .5 1MT?~725 .9 114.6 16y.7 240.3 252^5 2 20.5 258.0 N:2

169.5 2^9.5 230.5 223.1 239-4 llS4.6\130.1 121 .2 97~7 88.1^6^*^32.6120-6160^1220.3213.7241-9250.7 N:3

227.0 229.2 204.1 226.4 18^.7 158\ 116.5 128-9 Wj^'ljiiUjaWl . 4 1 26 . 1 1 6CX3 2)^\9 1^/7^7.4246.4 N:4

223. 1 207.9 213.0 Larf.O 174 .5 1315.9 142-7 1 09 .72^-r5) 1 48)5 133-1 \ Kg\\ 2 23.4 179 .7 ZrtfTs 215.4 N:5

204.1 214.0 \fh.2 1 67.0 143/0 115.5 165^T538^3 1^6. 0/137. 2 18^1 22^0 18^3 200/3 202-4 N:6

ON 25.N 5QN 75.N 10QN 125N 150N 175N 20QN 225N 25QN 275N 30QN 325N 35QN 375N 40pN 425N 45pN 475N1- — i —— i- — i —— 1 — -*- ••T-.-t p— — i — -f-- i f t p- — i —— p —— i —— p —— i —— f —— , —— p —— i —— p —— i —— f ' —— r —— i —— F —— i —— F —— i —— p —— i —— F —— ' —— TTflU

15.6 J7-8500.0 1 .UK 2. OK 2-OK, 4. OK ?.OK 2.QK ^6-01^50 .0 15-fi -1 2.0(^50-0 2 -OK 2. OK ,4 .OK 1 -OK 1 -OK N:l

7.8250.0500.0 KDK 2\OK X.OI^XKOK-— i^0l| (^^^^^W25 .0 f / l !X2-OtC^ .0 lloK 2 .OKî-0K—2-X)K 1 .OK N:2

250.0 500.0 500.0 SOOTD) VjlK--1^jBKiOO .0 VjaP-ffT^)] .3 xl/^^^ckp.O l.*fK 2 . Ot6Qj*Ttr5TJTJ7IT-^l -OK N:3

500-0 250-0 500.0 /2-OK 1^0(600-0250-0 1-^^1.3 ®.2 /7 .WsÔ lXm^2.0K?StKO 125 .0 1 -OK N:4

250.0250.0 iV^WemTTo 500-0 250.0 1 .9 13^6 ^?1 /2.0I60/.0 1.^/^0)6^0^0 62.5250.0 N:5

250.0500.0250.0250.0250.0 31.3 Ss,9^^.1 1 JoK 1 .BK 1 .BfK 2VQ4eSlKt) 250 .0 62.5 N:6

LINE : 400 W

INDUCED POLRRIZflTION SURVEY

POLE-DIPOLE flRRRY

NO fl

-î [^DfPTH HPOINT

N z 1. 2. 3. 4. . .. "R" SPOCING - 25-0 METRES


flBBIE LflKE

WflWfl flREfl. ONT.ORTE : MHRCH 1996 REF : 96D3

SCflLE :: 1 : 2500

JVX LTD-

SPECTRRL M N:lN:2

N:3

N:4

N:5

N:6

TflU

(X K)') N:l

N:2

N:3

N :4

N:5

N : 6

ON i 2^ t 5CJN t 7^ ( IQpN 4125N | ISpN f 175N f20pN 225N 25pN 27^N 30pN 325N 35pN 375N 40pN 425N 45pN 47^NSPECTRflL M

69-9102,2 76.2142.7184.5152-5 88-2 68.7 56.9 36.8 62.9 76.2 96.6172-1225.6186.2162-9152.7398.0524.0 N:l

99.4 W+Hrg^fSOxfln 82-5 Zee-HSlsV 4 \69.2 52.3^X8.3^74.6 82 .6 103^4106 .7 iTTrT*.^^ .0^02 .4 L*^.5,jjW^Z 3TT:S N :2

114.6152/7174.3216.218^.110013 66.6 sWfl 85.4 91 . nyfa .Q 1 12 .9 1 1 1 .2 1 44\S DS~8 12M.3^yf7l 340 . 4 N:3

151 ^5 172-6 198.S-HrfT7 1?7.5 9\.8 70-1 88.2 98 -Kl21 -5 1 15 .9 1 21 -2 1 38 -6L89 -5i3*MXMX^4 ^15 -5 N:4

169.8 197.8 170-8 1*4.6 131-9 9vl-jJJ)jU5-Hm-Yl25 .7 116-2 121.2 143-7^^3.5/01 -9yM!r2 293-8 N:5

189-1 170-9 1/19.4 110-2 104-4 122-9 116-0 126-8 117-5 131-6 149 .9^67 -5 H 6- 7 2^.8- 4 287-9 N:6

ON 25.N 5QN 75.N 10pN 125N 1 5pN 175N 20pN 225N 25PN 275N 30PN 325N 35PN 375N 40PN 425N 4SPN 475KTflU

62-5 15-6 15.6 500-050^0^ ^P-OK J 1,- 3 1-0 1.9 7 .8 1 25 .p , t ^.01690 -^ v4xLOK 4 fQKy f J^y/Ji-% 4^P// ij^lRl l 6 ' OK N !I

31.3 ft.6 5^^/^mOp^^^^l^l .3 7.8 62 .5 25jMT^.oSoeÔ 2^^^^S\l^^^^K^Vo|t^-^ YÔK N:2

15.6 SiJ'^SoVTO^ffÔ^SO^STW.O^^.S 62 .5 250^0 500^.0 500 -0 250-0/1 ^ jt^^^^^^^/^-^'^-^^ N :3

500 -0 2STj7(f250 -0 250-0 250 -0 900/00^-0 25(Ko 5JX5 -0 500 -0 250 -0/Z5 J///) "^^^Pl^HjmHTO^ \-OK N :4

250-01^5.0125.0125.0 31 T^fibn .7S250^0 5((6 .0 500 .02^0 .0 2SQ^^^Q^l^:^T^^^^S^fJ ^-Q N :5

125.0 62-5 62-5 125-0 250. Q 300 .0^50-0 \00-0 2/5)0-0 1^5. 1 //^^KfWHl/^2^5-^50 -0 5(KfÔ N:6

LINE : 300 W

INDUCED POLflRIZflTION SURVEY

POLE-DIPOLE flRRRY

MR , fl.

"î r^\ /'

OEfTM'l'rOIHT

N - 1 . 2. 3. 4, ... "fl" SPRC1NG - 25.0 METRES


flBBIE LflKE WflWfl flREfl. ONT.

DflTE : MRRCH 1996 REF : 9603

SCflLE r 1: 2500JVX LTD.

SPECTRRL MN: 1

N:2

N:3

N:4

N:5

N:6

TflU (x 10 3) N :1

N:2

N:3

N:4

N:5

N:6

ON ( 2^N t 5(|N ( 7^N ( 10pN p 125N ( ISpN f 175N f 20pN 225N 25pN 275N 30pN 325N 35pN ( 375N 40pN 425N 45pN 475NSPECTRflL M

66-9 79-5^41-1 91 -8 1,89.6 93 .8 55.1 34^.4 50 .fl 4H.8 77.1 91.6 93.4 91-7 98.7 78.8 75 .jj. 16J7 .0 232 .5 370 .4 N:l

83-8 1/0.2 112.7 L8^. 8 1M.1 W). 5 * \^tf(j^!yW-P B 1 - J 103^rTl3 .9 108 .6 105 .7\ 93 . 1 /T32 . 1 Ipe^T^Tl .8 Z83 .5 N:2

112.0 116.5 1JB3. 8 171 .9\ 25. 9) 54^ 58^^^^X90 .6 \pft. \ 1 23.6 132-3 110.8 100V4-^ .7 1/0 .9^34 . 1,^80 .3 N:3

123.8 1^4-1 151 .0-^-2/^5-— -j. 05^2 92-3 Wf9- 9 126.5 151 -8 1 17 . 1 105.2 1^TTT99Â^34 .3-2^1 .8 N:4

183.0 \ *y~*~^??.^//.?! fO Ste- 4 94.6^.4 124.3 125.3 118.3 101 .3 17X-7 200^2240. a/ve. 8 N:5

ISg./i/^'TCT .0 1 î 91 -6 106T5U2-3 126.7 138.9 120.7 104 .8 164/7 198./228.5 2^9.2 N:6

ON 2^N 5qN 7^ 10pN 125N ISpN 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425N 45pN 475NTflU

31-3 31-3 1-0 3-9 1 -OK 62-5 .5 .1 -1 31 .31 . 011^.1.0)600 .0 62 .5 125 .0 125 .0 ^W/? 'Qfijfe? 'Av 2' OM N :I

62.5 7.8/ /.g/^w^^s 3-9 -/i /i 62 . y fayffi35^g^y?(. 3 25p^tr?^Tjra ^^^^^^^* 2"^0 N :215.6 V. 8 5^ .Jj^^y •l NVJ> <V-:l 3 1 .3/^Ôffi^KO 2*1*0 .^^.8250/0 250^0/1 ;J^^^^^ 25^- 0 N :3

7 . 8 SfDOÔ// . 1 ( .1 .0 U3 62 .V^ÔjewKo 250. 0/ 3.9 125.0 125-0 ;^PY*lîP/" 2^* 0 N :4

500-TS /.\J^^.\ - 0 ^8^7.8^YÔCW^05I(6T]) /5- 6 125.0 25^) ^ jmfr^jjffl'l'^ '.Q N :5

.1 1-0 -0 -D 15-6 25D-W5flÔ 250.0 /7-8 125-0 125-0 - l/^Î^Û^ZSÔ N:6

LINE : 200 W


POLE-DIPOLE RRRRY

Nfl .B

-^1 fîDtrTH'VoiMt

N - l. 9. 1. i. ^. , .

"fl" SPflCINO r 25.0 METRES

FREEWEST RESOURCES INC.


DRTE : MRRCH 1996 REF : 9603

SCflLE r 1: 2500

JVX LTD.

SPECTRRL MN:l

N:2

N:3

N:4

N:5

N:6

TflU

(X 10 3) Nil

N:2

N:3

N:4

N:5

N:6

ON 2^ 5t)N 7^ 10pN 125N ( 15pN t 175N | 20pN 225N 25pN 275N ( 30pN 325N 35pN ( 375N ( 40pN f 425N 1 45pN ( 47p(SPECTRflL M

70.0 85.4 63.7 85-6 75-3 97. Z 34.7 41.0 38.9 29-2 57.7 90.6^97^5 97.5 89-2 51-3000.0104.3142.6192.5 N:l

93.9 78.2 87.0 93.0 32TO--54 . 2 46. 4 48.5 41 .3/72^6 97^140.6 SB. 1 flT^h 5 5 . 9 Vutto^^l54x5^93 .2 N:2

84.7 105^rmrX) 45/6 47.^ ei .3 4\.6 46-X88.71J16^2^7F^8.1^flf5.a-V4.3 ÎjJ/iTeQ^ 60^6 199.7 N:3

108-0 115 -J/jJêySfTis 8-9 73-2 ^9-^93-^18.5 1 35- VnTO- 1 109.8/62.7 71.013^6^5-8210^6 N:4

lig.o'/a) 6^8-9 66-0 62.8 84-2 95-^^6-0138.4104-9109.4/64.6^^^^6x^177.7208^8 N:5

-0 7,8^3 76-7 66-3 69 -4 104x^123 -8 126 .5 1 1 5 -5 1 13 -2 /63 -6/ -0 I4fl -/193 -5 2TT^9 N:6

ON 2^ 5QN 7^ ,10pN 125N ( ISpN f 175N f 20pN 225N 25pN 275N ( 30pN 32pN ( 35pN ( 375N 40pN 425N 45pN | 47^NTflU

62.5 15.6125-0 31-3125-0 -1 31-3 31-3 15.6 31 -3 500 .0500 .0 15 .6 15-6125-0 62-5 .0 -3 .3 2-0 N:l

15.6 62.5125-0125.0 31.3 7.8 31.3 15 -6 /W .3 yQfjT^mlz.S 1 25 .0 31-325^1 -0 ^-r-3-J— 3 .5 N:2

62.5 62.5125-0 7.8 62-5 15.6 31-3 31.350^0500^^^9125.0 62-5 62-5 - 15*tfPT\ ^3 O .5 N:3

125.0125.0 15.6 62.5 62.5 3 .9 31 .3^5^ SOOJJ/^5 2jj0-r8 62.5 62-5 -15/0^0^50.8^ -3 N:4

250.-8 .0 62. S 62.5 31-3 Kg 5/6^0 2(51^0^52^5 25^^5 .0 *8?.5 ?2^f. 0^00 .05DTT: 0 N:5

-0 31.3 31.3 62.5 15 .6 250f.O 900 .0\125 .0 125 .0 125 -C(V^^^\N .0 5(10^.250 •O'SOO .0 N:6

LINE : 100 W


POLE-DIPOLE RRRRY

m . H ,

-HDj ^

DtPTH*rOIMT

N - \ , 2. 3 . 4. ... "fl" SPflCING z 25.0 METRES


flBBIE LflKE

WflWfl flREfl. ONT.DRTE : MRRCH 1996 REF : 9603

SCflLE :: 1: 2500

JVX LTD-

SPECTRflL M N:l

N:2

N:3

N:4

N:5

N:6

TflU

(x 10 3) N :1N:2

N:3

N:4

N:5

N:6

Hiiiinii

2.165 3d 'ON 25N SON 75N 10pN 125N t ISpN ( 175N 20pN 225N 25pN 275N 30pN 325N ( 35pN 1 375N 40pN 1 4 25N 1 4 5pN i 47fN

SPECTRflL M 79.8 61-0 4^2,73.3100-7 5 1 . 8 yUflj^î' 9 6 3 ' 8 86 ' 4 S 6 ' 1 8 9 ' 2 9 0 ' 3 8 4 ' 6 9 5 ' 2 67 .7 34 .8^ 87 .8^07 .3 178 .8 N--1

72-3 60.1 86.6H14^5 ST^^S^^sa^K 71 .2 90.2 73.4 91.5 99.9 88.2 93.7 91.3 45^104^8^27.3^^3^8 N:2

74.8 92-1/T6.4 /45X7 .0^1^^74.2 95.6 99;3-MT75To5T5 jbs .0 87.3 91-8 67 . 1 10^/7 1 34 . 3X91 . 7 N:3

99-7 \G2- 2/^63 -B/ -0 72^ 85-9 97-1^85^0124.2121.6 99 J5 88.6 79-0 56-21^5^4140^^96.5 N:4

106.4r69.oX -0 76^3 84 . 1 lOJ^flfToe .9 126 .9 134 .6 1 19 .5^r.4 82.8 71 .6 1^4 l^rTTl99 -0 N:5

.0 .0 90^9 92-5/^35^6 113.6 134.4 137.3 123. 67^ÎTNB7. 7 95.^^30-9159/2210^1 N:6

Lines 500 w - 1 00 W

ON 25N 5QN 75.N 10PN 12?N 15PN 175N 20PN 225N 25PN 275N 30PN 325N 35PN 375N 40PN 425N 45QN 47JN

15-6 62.5250-0 62.5 1-9500-0 -0 -1 .3 -1 -3 ^0 -5 -1 -5 ^ 1.0 ,1 .3 2-0 N:l

62.5 23t5J3 l/K.Q l .tf*)31-3 -1 *— r .3 .3 2-0 -1 1-0 .5 r^^ - 3 - 5 ^r o -3 - 5 N:2 X \ V r^* — " lo ( J

62.525^9 1.9 7.8 ^jOt25.0 .3 .3 .5 .1 1.0 -5 - ^\^P 4 ' 0 -L^-S -5 N:3

125.0 7.8 UE^ .0125.0125.0 ' 3 p\' 5 - 1 ! - Q ' 5 - 5 - 3 ' 3 - 1 ' 3 ' 5 N :4 7.8 l.jS ft) 125.025^7b~250^j) \*^~ 91 .5 -1 1.0 .3 .1 .1 .3 .5 N:5

.0 1 .0/31.3125.0 7.8125.0 \f . 5 .5 rvB, .3/^0 l -3 .1 .5 N:6

imnn42C03NW0015 2 16555 ABBIE LAKE 250

LINE : O E


POLE-DIPOLE flRRRY

N - 1 . 2. 3. 4.

"fl" SPRCING ^ 25.0 METRES

FREEWEST RESOURCES INCflBBIE LflKE

WflWfl flREfl, ONT.DflTE : MflRCH 1996 REF : 9603

SCflLE r l: 2500JVX LTD-

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

ON 3QpN t 325N t 35pN t 375N ,40pN t 42SN

l .6K 2.1K 4.8K 2.8K 2. IK 5.4685.0 1,9K 2-5K

.4K l .K 3.OK 3. IK 3.2Ki8ri.O

RESISTIVITY

3.4K 4-2K N:l

N:2

N:3

3K 1/rflK 3. 3K

" O* i*0"

2.SK 2.2K A-9W3S.0714.0 /3.3K/ 4.5K 4.^K 2-5K

Z.2K 3-5Ki24TQ7Q5.0 /-SK 4 *fijt 3rSK 3-5K

5.2KN3.0K 3.4m*Tl-O 957.0 Z'.SK 3.2K 3-6K 3.2K

N:4

N:5

N:6

IP-!ON

MX CHG.175N 200N 225N 250N 275N 300N 325N 35QN 375N 40QN

*-^~—— —— *. '••i.. —H^-^^m-J^,^ —— —— *- —— — ——. *———^ ^J———l —— —— —— ——'-H——* ~~J-~. ~, ^ ——'

LINE : 100 E


POLE-DIPOLE flRRRY

DEPTH POINT

N - 1 . 2. 3. 4. ... fl" SPRCINO - 2 5.0 METRES


WflWfl flREfl. ONT.DflTE : MflRCH 1996 REF : 9603

SCflLE r 1: 2500JVX LTD-

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

Ni5

N:6

. 25.N . 5QN . 75.N . IPPN . 125N . ISpN . 175N . 20pN . 225N . 25PN . 275N , 30PN . 325N . 35QN . 375N . 40QN . 425N .45PN . 475H' 1 —————— ——— ——— ——— ——— ——— ——— ——— ———^""^

3.3K 1-6K. 2.7K 3.9K 2.9K

2.8K 2.9K 3.1

'.0&-2-2K 3.7,

.3K \.7KA2.8K^5.

2.6KV-W2K 3^6*^2

.8K 3.3K 2.IK 2.9K 5-6K

3.SK 3.IK 2.4K 3.2K

3.OK 3.2K 3.2K 2.7K

IK 3.4K 3.3K 3.7K 3.5K

2K 3.9K 3-8K 4.IK

14.. .6K 3.IK 3.OK .K5rTN2.5K 2.7K4.8K 4-5K

RESISTIVITY N:l

N:2

N:3

N:4

N:5

N:6

I''-N i crnKi 1 Tcrid iJUN i fpn N t27pN | 30pN t325N |350N t 375N , 40pN t 425N

MX CHO, N:l

N:2

N:3

N:4

N:5

N:6

LINE : 200 E


POLE-DIPOLE RRRRY

fl.

DEPTH*POINT

N - 1 . 2. 3. 4. ...

R" SPRCING - 25.0 METRES

FREEWEST RESOURCES INCRBBIE LflKE


SCflLE ^ 1: 2500JVX LTD.

RESISTIVITY

MX CHO.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

0(t 5CJN N .125N [ ISDN f 175N ^OpN ,225N | 25pN t 275N f 30DN ^SN t 35pN t 375N t 40pN | 425N , 45pN t475

VHW ' ' ' ' ' ' n'-V ' ~ "'~~ -~ ~c'

15

14

O- L (X; M '

2.OK 3.OK 1..9J*48.0 ^ \ - 3r613\0 441 .0 593.0

OK 2.5K IXjrtftta.O M.IK 1.

3.7K \ fjM\fyfi 692.0KuOK l .2K l .5K

K 2.8Jr^5yj660.0632.0888vO

3.1IG^.O 627.0 582.0 577.0/ 1.

9(6*0.0 814.0 538.0560.0 /1.3K/3.

^RESISTIVITY

N:2

N:3

N:4

N:5

N:6

IP'1

Oft N 75N 100N 125N ISDN 175N

, B MX CHO, ? o i ri -It , 3-5 N:l

N:2

N:3

N:4

N:5

N:6

LINE : 300 E


POLE-DIPOLE RRRRY

DEPTH POINT

N - 1. 2. 3. 4, ...

fl" SPRCING z 25-0 METRES


WflWfl flREfl* ONT.DflTE : MflRCH 1996 REF : 9603

SCflLE - 1 : 2500JVX LTD.

RESISTIVITY

MX CHG.

N:2

N'3

N:4

N:5

N:6

t 275N ^OPN t325N 35pN , 37^N , 40pNN t 175N | 200N t 22SN | 25 ---"~

I P-t r r-2.

8."4

RESISTIVITY

N:2

N:3

N:4

N:5

N:6

- 3"--2f1X CHO.

LINE : 400 E


POLE-DIPOLE RRRRY

fl.

V DEPTH POINT

N - 1 . 2. 3. 4. ...

fl" SPRCING - 25-0 METRES



SCflLE - l : 2500JVX LTD.

RESISTIVITY

MX CHG.

N:l

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

2.165 55ON 25.N . 5QN . 75.N fO()N 125N 15PN 175N 20QN . 225N 25QN 275N 30PN 325N,. 35pN . 375N .40QN 425N .45QNM ' *wv vih 1 v^.\ 1 WA v^,\r ,U'/—••'•-tl ^V : - 1 --— ''Kiv -o—p—^"^

22,.2k

33.3K 2

28

25

33

27

37

IP-ZON

Lines O - 400 E

6-0 4-0 4-5 3-9 4.8 5

.3 5.7 5-6 sk I2.7

PLATE 5

Scintrw IPR-12 Rx

42C03NW0015 2 16555 ABBIE LAKE 260

LINE : 0 E


POLE-DIPOLE flRRRY

na. .i ,

-^ [^\ t

*v'OfPTN POUT

N r 1. 2. 3. 4. ... •fl" SPflCING - 25.0 METRES


flBBIE LflKE

WRWfl flREfl', ONT.DflTE : MHRCH 1996 REF : 9603

SCflLE :: 1: 2500

JVX LTD-

SPECTRflL MN:l

N:2

N:3

N:4

N:5

N:6

TRU

(xlO-3) N !lN:2

N:3

N:4

N:5

N:6

ON j 25,N ( 5qN t 75,N ( 10pN ] 125N ( ISpN ( 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425N 45pN 475NSPECTRflL M

54.3 57.1 lOT^Jj 60.7 76.9 73 .4 -76 .6 72 .7 100,8 180 .9 123 .9 1 12 .5 1 17 .9 1 19 .7 129-0 03.2 9 1-0 77.9109-4128.5 N:l

66.3 92-7 86.2 89.8 60. B/ -W^fr^2 97.//122 - 8T53.1 1 29 .6 1 1 1 .9 136 .8 106 -0 127 .8 109T3TOS^7 86 -2^32 .9 N:2

90.6 86.5 94.2 63-7 63~r4— 1 .0 98^^124 .2 11 1 .6 130 .0 1 17 . 1 135 .4 9Q^STOTH5132 .0 1 1 1 .6 109 .7 122-8 N:3

92-2 97.6 69.7100-0 93.9108^4125.9113.4119.0122.8142.9 84/9 (^To^t^V-S 126 .0 1 16 .8 140.4 N:4

101-3 73-6y^T5^97.6jW.8 133-1 116.0 126. 1 127.1 142.2 94 ,^-4^8~rS^\^l.O)l^5 -9 129 -2 147 .2 N:5

79.8 f - 0 KTO.a/UJg.O 129.S^x"7DNl^9.4 144.7 136.3 VTs~?S \ /~7DM3.2 /5-TS3~^3 129-4 156^.7 N:6

ON 2^N 5(|N 7^N 10pN 125N ISpN 17SN 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425N 45pN 475NTRU

31.3 15-6 1,0 15-6250-0 31 -3.^8 ' ^ffi - 0 1 \OK N4^0r^ 2 .OM500 .0 1 .01600 -0 250 -0 125 -0 250 -0 250 -0 J .OK 1 -OK N:l

31.3 7-8^.8125.0 1 5 ' •^^gg^BtfrvJ 1 . OieoV^C^-Z-flK 1/0(250.0500.0500.0 62.5250.0125.0 (2.QH 1 .OK N:2

15-6 31.3125-0 7 J^ffl^^WmW^ 1 -01600. 0500. O^DITO 500.0 250.0 500-0 250-0 1 -ON25 -0 250 -0"-~4..0K N:3

31-3125-0 7 -XvêSSPre^SO.O 500-0500-0250.0 250.0250.0 125.0 .0250-0250.0250-0500-0 N:4S J f~~^125-0 7 .je dJ 125.0 500.0 250.0 500.0 125.0 125.0 250.0 62.5 15 - b-*— Q O 125 .0 500 .0 500 .0 Ni5

7.8/ .0125.0250.0500.0 .0250-0 31.3250.0 .5^- — v.0 250 -0 125 -0 250 -0 1 .OK N:6

LINE : 100 E

INDUCED POLflRIZRTION SURVEY

POLE-DIPOLE RRRRY

HI) -, B"0] r^l*\ y'v

DCPTH POINT

N - 1 . 2. 3. 4. ... "fl" SPflCING r 25.0 METRES


RBBIE RLKE WRWR RREfl. ONT.

DflTE : MRRCH 1996 ÊF : 9603

SCflLE - 1 : 2500

JVX LTD.

SPECTRRL M N:l

N:2

N:3

N:4

N:5

N:6

TflU

(x ia3) N :1N:2

N:3

N:4

N:5

N:6

ON 25^ t SqN t 75^ ( 10pN ( 125N t ISpN r 17J5N E20pN (225N (25pN 275N , 30DN 325N ( 35pN ( 375N ( 40pN ( 425N 45pN 475NSPECTRRL M

59.2 64.0 66.0100.0 99.8107.1113-5,88.1 79.4103.6148.1 94.3 96.8 63.5 96.5 85.7 82.8 57-1 66.0 80.4 N:l

69.6 83.8 9 9,^110.7 112 .5^54-^8^69. 2 84 .6LK^6 1 15 .4 1 12 .8 g1^^ 78 .6 1)^51247^709^*7 75-2 83.8 91.8 N:2

87.7 19,4^1 120.4 106.ST ^TO^— ..0^03.S-rTl . 1 114.2 108.6 105.3 122-9 129-2 135.7 124.9 fl2.0 88-4 95.2 N:3

117.1116.2102^^63^ \^ lira. IT118. 5 110.1 114.1 99^109 .9 154^8-4^.5 1 34 .6 1 42 . 7^2^-5 /T24^7 N:4

145.0 \ QQ,AS^Q . (^— 0.0\?4.0 120.6 113-1 lOS-STOT-S 153^ 170 -^J^ -3 ^Trf^SB^^ma -7 N:5

109. r f . 0r lo i0tTT\ .Vah?.4 124.0 109.4 138.5 UT. e iBz./XxSîVaX /o" —— :o N:6

ON 25^ 5(]N T^N 10pN 125N ISpN 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425N 45pN 47SNTflU

62-5125-0125-0 7.8^5-6250-0250.0 -.1^2 .5 500 -0 1.0(^50-0500.0 62-5 31-3125-0125.0 31-3 62.5 31-3 Nil

125.0 62.5 31.3 15-6250-0 1-OK62-5 62 .5 250 .0 ?SO .0 500 .0 250 .0 500 .0 125 .0 62-5125.0125-0 62-5 15.6 N:2

62.5 31.3 15.6250.0 -0 -0 62-5500.0250-0250-0250.0 1 5 .6 250 -0 125 -0 125 .0 250 .0 1 25 .0 15.6 N:3

15-6 31.3250.0 15 -6/^0 p2 .5 500 .0 1 .ON 25 .0 500 .0 125 .0 62.5 1 .OW25 .{L^^9 250 .0 3.9 N:4 7.8250.0 .O/ôO ^Jo 1 25-0 250.0 250-0 125-0 250.0 125.0 31. 3250. oC —— JL 0?. 8 125-0 N:5

62-5 -O/ Jo 62-5 .0250-0125-0250.0 15.6250-0125.0 -O//^^^ -\) \ -0 N:6

LINE : 200 E


POLE-DIPOLE flRRRY

Nfl fl .

-^1 f^l

otPTH*poiNT N - 1 . 2. 3. 4. ...

"R" SPflCING H 25-0 METRES


flBBIE LflKE

WflWfl flREfl. ONT.OflTE : MRRCH 1996 REF : 9603

SCflLE - 1 : 2500

JVX LTD.

SPECTRRL M N:l

N:2

N:3

N:4

N:5

N:6

TRU

(xlO 5) N :1N:2

N:3

N:4

N:5

N:6

0(*) , 2^ 5qN , 7^ 10pN 125N 15pN | 17pN 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 1 4 2pN 1 4 5pN 47^NSPECTRflL M

63.4 74.1 85.9 82.610^5^90.5 82-7 93-2 68.1 50.1106.1123-9 80-1 46-8 60-0 30-3 33.8 18.9 41-6,58.6 N:l

78-8 81.5 77.7 87.0 85-1 86-0 97.1 92-0 81 .3 120^3 105 .8 109 \ 50^4/^W 9—^4 . 1 31-2 29-7 52x4^81-3 N:2

99. 8 89.6 75.4 73.5 93.5 98.3^0575^91.^26.8 97.8110.3^/^0 5\-5 \7.6 38-2 41.2 SX5 92.8 N:3

91.8 95.8 87.3 94.9 91.01oJ.6 9^^130.8 122 -8 16b..4^JJ6 .6\^ .0 ^.Q\6.Q 43.7/6^0 93.6 Ns4

88.7 77.0 93.2 88 .0 10^6 1 10 .9 1 32 - 1 1 44 .7 ("rrDr^TTTNB^ .3^74^3 56 .2Xv-56-rff72 -9 102 -6 N:5

86.8 106-^7-^67.5 L85^9 112.4 117.1 133-4 16*-.6V\ \0 \. 0X78.9 /^To^\96 . 6 95.51-J4T.2 N:6

ONj 2^ 50N 7^ 10pN 125N 15pN 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425N 45pN 41fNTflU

125-0 31.3,3-9 3-9 -5 .5250-0 15-6 7^.8 125 -D 500 -O 500 -O 500 -O 125 .0 1,9 62 f5128 -OK 3,9 7.8 31-3 N:li / —— r/ vv^^^y/j y62-5 15:6, 7.8 1.9 U8250.0 31-3 62-5 31-3125-0500-0 LO(C50.0 62 .5 3T.3 l^^^âiJs (S 31 -3 N:2

S5-8 /7-8 7.8 3.9^125.0 31.3 31.3250.0 62.5 62-5500.0 .0125.0250-0 1 .OrK^3^9^3Jj^ 3 1 ' 3 N :3

7.8 3.9 Ida'125. 0 62.5 62 -5 125 -0 125 .(3125^0 (fTo^)25 . of~*\) 5 00 .OUOK 15 .6 62-5 62-5 N:4

3-8 15x^250.0125.0 62.5 62.5125.0 ^^LQBs^*t) ^ 8?-p5-5^0.0 (j?.0(yi5.6 62.5 62-5 N:5

13-B 125.0 62-5 62.5 62 .5 500 .0 125 .^/^^V\\-D 10 X?Trj|^ .0 1-9 31.3 62-5 N:6

LINE : 300 E


POLE-DIPOLE RRRRY

w . c ,-HD-| r®-i

"vOEPTH POINT

————— - ———————— N * 1. g. 3, 4. ... ————————————————————————

"fl" SPflCING - 25.0 METRES


flBBIE LflKE

WflWfl flREfl. ONT.DRTE : MflRCH 1996 REF : 9603

SCflLE = 1: 2500JVX LTD-

SPECTRRL M N:l

N:2

N:3

N:4

N:5

N:6

TflU

(xlO-3) N !lN:2

N:3

N:4

N:5

N:6

ON 2^ S^N 7^N 10pN 125N 15pN 175N 20pN 225N 25pN 275N 30pN 325N 35pN , 375N 40pN 42p 45pN 47^NSPECTRflL M

86.9 80.5 65.6 74.0 73.5 .0120.2 95,6 50,6 30.0 57 .5 113 -5 57 .7 41.9 30-9 29.5 21-^J 1 -O 22 -9^ 80 .2 N:l

80.0 79.1 80.5 91.0 75 -8^^ 15*^8 VB - 0(^0^0^ WQ-I SSO . 9 69. 4^38. 6 50 2 1 ^tfB^g^Wl^f09 . 1 N:2

85.2 94.7KL2-A 88.p^3T2 "\ (7-2^6105.8 74 .6 L2^.0 S^.7 85.4 64 .8 \40 .s( 90 -3V \2 :^^^4^15^7 N:3

90-9 bn-0 g^/HW-S 186-0^ J)83-6 82-91^1.5 86.5 88.4 80-6 68-3^3^1 -0 55^116^0 NM

124.8 132-5 17^.9 191 .9 /42/rT^^^ 80-0^26-8 93^5 90-5 88-2 83-5 56 -VjM-8 64^4 1 2^0 N:5

149-2 145. 2S.49.4xf06. 6 123-6 131-3 90".2105Ta 86.9 84.6 71.1 97.6 74-212^-2 N:6

ON 25N SON 75N 10pN ^SN^SpN 175N 20pN 225N 25pN 275N ( 30pN 325N ( 35pN j 37pN 1 40pN ( 425N ( 45pN ( *1^NTflU

31.3 31-3 62.5 62-5 15.6 -0 15.6 1.0500.0 -1125-0500-0500.0 62-5500-0 1-9 3,9 48-0 4 .p .1 N:l

62.5 31.3 62-5 31-3500.0 .1250.0 15.6250-0250-0250.0250.0500.0 1 g 2^^^^ o "^ - 0 N :2

31-3 31.3 31.3500.0 3-9 15-6 .1*250-0250-0250.0250.0125.0 31 -3 ^-V^^^^j) ' 0 N' 3

62-5 31-3500-0 7 -8 f~^^ *1 \2*i - 0 250 .0 250 .0 250 .0 250 .0 31.3 62-5 S*w5*Hx .1 N:4

15.6 31-3 15-6 */. 1 ^5-6 125.0 1 -0(C50 .0 250 -0 125 .0 125 -0 62.5 -1125-0 62-5 N:5

15-6 62-5 /2 y-B — -1 250-0500.0 62-5250.0250-0250-0 .1 62.5125.0 N:6

LINE : 400 E


POLE-DIPOLE flRRRY

mi fl

— Oi rGh

OKPTIt*POINT

N r 1 . 2. 3. 4. ... "fl" SPflCING - 25.0 METRES


flBBIE LflKE

WflWfl flREfl. ONT.OflTE : MflRCH 1996 REF : 9603

SCflLE - 1 : 2500

JVX LTD.

SPECTRRL M N:l

N:2

N:3

N:4

N:5

N:6

TflU

(xlO-3) N !lN:2

N:3

N:4

N:5

N:6

UUIIHIHI

2* 165 5 SON 25N 5qN 7^ 10pN 125N ISpN 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425N 45pN

SPECTRflL M 81.4 54.8 69-3 60-5 87.2 96-5 90-2 78.0 53.6 58-9 4^5^ 69-0 81.6 49.7 19.9 26.5 26.7 26.6 -0 N:l

64.9 70.7 70.3 99^2-ltfTrrnTTvJ 87.3 30rT9~^8.7 51.9 80.0 81.4 83.6 34.2 28-8 28.7 36-5 -0 N:2

82-8 78-311^7115-2123-5 93.7 2^-7yD8v3 64.9 83-4 84.9 82.9 58.9\41.4 32-0 40-lX7T"-7 N:3

90.1 W^5 128.9 134-5 103-7 71 -3 77-2 59-8 91-7 86-7 83-7 70-3 63.3X4.5 42-8/82.0 N:4

139-6138-6146-1110.2 (90.6 87.2 62.6 87.8 96-8 90-7 74-8 77.0 64 .9 55-r5rX87 .7 N:5

149-2 ISa^C 118.2 102. VrtJB~^ 64.6 88.8 97.3 91-5 76-8 81.5 75.8 71-813^9 N:6

Lines 0 - 400 E

ON 2^ 5(]N 7^N 10pN 125N 15pN 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 1 40pN ( 425N t45pN1 HU

250-0250-0 62-5 62-5 15-6 15-6125-0125.0500.0 1 .0 500 .0 500 .0 2 .0(600 .0 7.8 7-8 7-8 1 -OK .0 N:l

250.0125.0125.0 15-6 31.3250-0125-0 62-5 15 .6 500 .0 125 .0 500 /fr-—iVOt600 .0 31.^3^.3 1 .OK .0 N:2

125-0125.0 15.6 31-3125-0125-0 7 -8/^/250 -0 125 .0 250 .0 250 .0 500 .0 250 -0 62-5 1 -OK -1 N:3

125.0 31.3 31.3125.0125-0 .f 1 X5125 .0 125 .0 250 .0 250 .0 125 .0 250 .0 250 .CIJ-OK -1 N:4

15-6 31.3125.0125.0 JC l eOM25.0 62-5125.0125-0125.0125.0250.0 ("2.0KI -1 Ni5

31.3125.0125.0 . Y 1 /0250.0 62.5 31.3250.0125.0125.0250.0500.0 .1 N:6 PLATE 53

mm42C03NW0015 2 16555 ABBIE LAKE 270

LINE : 500 E


POLE-DIPOLE flRRflY

DEPTH POINT

N z l . 2. 3. 4. ...

•fl" SPflCING - 25.0 METRES


flBBIE LflKE .... WflWfl flREflp ONT.

DRTE : MflRCH 1996 RtF : 9603

SCflLE r 1: 2500

JVX LTD.

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

ON | 25N | 5DN t 7 5N , I QON | 125N t ISpN t 175N 1200N [ 225N 25pN 275N 30QN 325N 350N 375N 40QN 425NW' Wi, Hvl Hfl\H(i\ m^ VMOHI,'. H it' ' ' *" —' — -t- —'— J - ' ' ' f ' ^ ' j~ ;

.2K7B7^) 257.0 145.0 208.0 172.jy543.0 487.0

4K 1./7M523..0

37

31.4

21 ."5^)29. 6K 2-

692.0825xV^

l . 9K152 .0 539^0 842.0 648^.Q -1 T6ie97 -O l . l K

2K J.VOK767.0 ^-r3W7"5^0 2.SK l .5K 1.4K

13.0850.0 /l.7K 1.4K 3.4K 2.IK 2.OK

6K993\0 522-0 /1-9K l-8K 4-5K 2-7K 2.7K

RESISTIVITYN:l

N:2

N:3

N:4

N:5

N:6

TP- 2ON

8-2 9

CHG.

LINE : 600 E


POLE-DIPOLE flRRflY

N - l . 2. 3. 4. ...•fl" SPRCING - 25.0 METRES


flBBIE LflKE

WflWfl RREfl, ONT.DflTE : MRRCH 1996 REF : 9603

SCflLE r 1: 2500

JVX LTD.

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

ON | 2^N | SON | l ^N ^ OON ^2^ ^SDN ^VSN ^DON ^ZSN 25DN 275N 30DN 32SN 35DN 375N 400N 42SNv^ti lUi Vrt' 1 VH*'' vui' rtii\ HM- ivo') i^.i !,,. ~"^~t'~ ~ ' ' , ' TT* '

UQZSyOieB.O 88 .0 140^-8^419.0 485'.1) 6(

rf39.0 36CKQ^9g^D-afâ?5l.O 723.0 353.

-0418-0314 j0-5?6 . a^T'/SK l 73l**l^p9i*56.or~~ "" ~ -x--- "" - ' - ~ ~~" ~

.0383

A 4.4K

U9-0 485'.TJ 684.0 l -2K

."0723.0353.0 l .5K

992-0

2-7K 2-OK759-0 U4^ i OfJ

.8K 2-8K 1.1K 2-1K

3-8K 1-5K 2-9K

RESISTIVITY N:lN:2

N:3

N:4

N:5

N:6

If- f5tN | 125N t ISpN , 175N ÔpN | 225N t 25pN ÔpN t325N t35pN ^7^ ÔpN t 425N

.1^, f,'

9.9 9 5.4

MX CHG. N:l

N:2

N:3

N:4

Ni5

N:6

LINE : 700 E


POLE-DIPOLE flRRflY

OtPIH*POIMT

N : l . 2. 3. 4. ...

"fl" SPflCING - 25.0 METRES




SCflLE r 1: 2500

JVX LTD.

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

ON N ,225N

30-6K 33. 2K 31 .

N , 35pN 40Np

'50\0 189.0 102.0 120.0J^3.Jff557./) 413.0

383^0 244 .0 21k.-eT42B,XJ~956 .0T497 .0

368.0390^5^22.0780.0 1-61666.0

396.0412X777.0 l .3K 2.6K l .OK

1.8K 3.9K 1.5K

53

345.0 447 vffl90S. O

l.OK 2.2K 5-3K 2-2K393.0397.0

IP- fON N t 275N t 30pN t 325N t 35pN | 37^N 40pN

3.4 l.- 9 1.3 1.3

9.8

RESISTIVITYN:l

N:2

N:3

N:4

N:5

N:6

T .V'M- -i| M X C HG- L,9 2-0 '^2-1 ' N:l

N:2

N:3

N:4

N:5

N:6

LINE : 800 E


POLE-DIPOLE flRRflY

otfiH*roiMi

N - l . 2. 3. 4. ... •H" SPflCING - 25.0 METRES


flBBIE LflKE

WflWfl flREfl* ONT.DflTE : MRRCH 1996 REF : 9603

SCflLE r 1: 2500

JVX LTD.

RESISTIVITY

MX CHG-

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

ON | 25N t 5 QN | 75N | 10QN VUi.'.'mi? I\VM HV,

46-

175N ^DpN t225N t250N t275N t 3 DpN t325N t 35pN'ft

2.;2.7K

5K 1.5(832.0559-0/1.9^65.0 l .7K

.8^25-0885.0/2.6*699.0 2-BK

|^05.0852 :iJX 3-8K753.0 3-5K

3.6K I.IK 4.4K

P"'-,

( f r.

Of! | 25^ | 5(|N | 125N , 175N

5-6 5-0 5.7 5-6

RESISTIVITY

N:2

N:3

N:4

N:5

N:6

pN t225N ^SpN t275N |30pN t325N [ 35pN |375N ~n~j;''' . ....-— -— ; i MX CHG.

N:2

N:3

N:4

N:5

N:6

LINE : 900 E


POLE-DIPOLE flRRflY

DEPTH POINT

N - l . 2. 3. 4. ..- •fl" SPflCING r 25-0 METRES




SCflLE - 1 : 2500JVX LTD-

RESISTIVITY

MX CHG.

N:2

N:3

N :4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

OH 25.N . 5QN . 75.N .10PN.125N.15PN.175N.20PN.225N.25PN.275N.30PN.325N.35PN.375N-- r——^—— ~~~ ' —— ——

16 2K 3

1.2K447.0 1.3K

• 2K572.0 988.0

1.3K 1.5K

.OK 2-5K

3.9K

.7K

RESISTIVITY N:l

N:2

N:3

N:4

N:5

N:6

ON

IP-r250^N^27^N ÔpN . 32^N t 35pN , 375N

VYTIX CHG.

Scintrex IPR-12 RK

LINE : 1000 E


POLE-DIPOLE flRRflY

DEPTH POINT

N - l. 2. 3. 4. ...

•R" SPRCING ^ 25.0 METRES


flBBIE LflKE

WflWfl flREfl* ONT.DflTE : MRRCH 1996 REF : 9603

SCflLE - 1: 2500

JVX LTD.

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

ON t 2^N SqN 7^ t IPpN 125N ^SpN f 175N 20pN ^2^ t25pN t275N t30pN t325N t35pNa o \*i*1

25

N 350N

8.7

RESISTIVITY N:lN:2

Ni3

N:4

N:5

N:6

MX CHG.

N:l

N:2

N:3

N:4

N:5

N:6

LINE : 1100 E


POLE-DIPOLE flRRflY

N - 1. 2. 3. 4. ... •fl" SPflCINO = 25.0 METRES


flBBIE LflKE

WflNfl flREfl, ONT.DflTE : MRRCH 1996 REF : 9603

SCflLE r l: 2500JVX LTD.

RESISTIVITY

MX CHG.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

li 6to-c

N ^2^ 425pN ^75N | 30pN | 325^N t 35J1N

1.6K 1.8K 1.2K735.0

3K 3-4192.0 NOK

85

3.8K /f.UCfe'8.

K . 3(^4 3- O6K ~

K 1.2K

RESISTIVITY

N:l

N:2

N:3

N:4

N:5

N:6

Lines 500 E- II00El IP-1'" IP-1

ON 2^ | SqN t 7^ JOpN ^ZSN f ISpN ^7^ DpN , 22^N ^SpN | 275N | 30pN , 325N , 35pN

5.2

8.8

MX CHG- N:l

N:2

N:3

N:4

N:5

N:6

PLATE 6

Scintrex IPR-12Rx

42C03NW0015 2 16555 ABBIE LAKE 280

LINE : 500 E


POLE-DIPOLE RRRflY

W R .

-- ©^ |^hj

DEPTH*POINT

N ^ 1. 2. 3. 4. ... "fi" SPflCING r 25.0 METRES


flBBIE LflKE

WflWfl flREfl, ONT.DflTF : MRRCH 1996 REF : 9603

SCflLE r 1 : 2500

JVX LTD-

ON ( 2^N ( 5()N t 7 5,N 410pN f125N f15pN , 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425N

SPECTRflL M - SPECTRflL M N:l 70-2 71.5 58.6 76.6 71-3^89.0 79.6 99-0 91.1 44.1 86.6 3D. 5 39.5 32.7 47.2 45-3 39.5 39.0 N:l

N'2 62.0 71.7 B ^BT^BSA . 9 84 .5 U^Pfcs f^V^^^^fi^ y43^T\iJ^tt^^f?rZ^p . S 5 6.0 N:2

N:3 74.2/^3^7 1^^.\1 îTT^SN^-rfe. 7 99 .(tl ^^ 9 45.9 64X1 63 .S^^ê s f.S N :3

N'4 97.1 Xf?.8 l^S^FT\5^3J^rTn 0 4 - 3 l^R^ 6 Sl^&SSwXa^^^^^^&Ô 64.0 Ls^^-.Q N :4

N:5 \ \l-T l?m.\ 12S-1 \^3^ \^.3^^^DA^L^^^ê^^^^^^.3 6 5.3 60^83.5 N:5

N:B 133.7 138.2 W3^8 1 22 ^//'^^ûVVl^flv^V 5 1 sVrSS^Sr^ . 8 69.0 8^4 N:6

ON 25N SON 75N lOON 1 25N 15pN 175N 20QN 225N 25QN 275N 30PN 325N 35QN 375N 400N 425N1 ' 1 ' 1 ' 1 i 1 i f i f i -F- —t- -F —— i —— F —— i —— F — ' —— F — i —— F— -* — F — ' —— F —— ' — -F — i —— F — ' —— fTRU Tflu

(X 10 3) N :1 6 2 ' 5 3 1 ' 3 6 2 ' 5 6 2 - 5 6 2 ' 5 1 5 ' 6 62-5125-0250.0500-0 -1 3-9 7-8 62 .5 . BÔK .1 3.9125.0 N:l N:2 125.0 62.5 62.5125.0 15 .6 1 K - 0 125 .0 250 .0 1 .OK .1 7-8 15 -6 250 .^^^(^^.y 1 ."9 1?5 .0 —— -N:2 —————————————

N:3 62-5 62-5 62.5 15-6 62-5250-0125-0 7-8 -1 T5-6 31 .3 250 •jtfjjpl?fy'jzj*? .X0 1 25 -O N:3

N:4 62.5125-0 15.6 62-5125.0125-0 -2 V^Û—— . 1 250 -^^^^^^9 U^3 1 25 .0 N:4

N:5 125.0 31.3 62-5125.0250.0 1 .^ 5 15.6 3^9*^V . l^^^^^^B 1?5 .0 125 -0 N:5

N:6 31.3 62-5125.0 62-5 .0—15-6 -1 31-3 7.8 ^^^^B 31-3 62.5 N:6

LINE : 600 E

INDUCED POLflRIZRTION SURVEY

POLE-DIPOLE RRRRY

NR ft

--O] ^

DEPTM*rflIMI

N - 1 . 2 . 3 . 4 . . . . "H" SPRCING - 25.0 METRES


flBBIE LflKE

WflWfl flREfl. ONT.DRTE : MflRCH 1996 REF : 9603

SCflLE r 1 : 2500

JVX LTD.

ON 2^N t 5 0,N t 75^ 10pN t125N t15pN (175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425NSPECTRflL M ' SPECTRflL M

N:l 68-8 60-4 70.0 B l -3 8 8 .8 159. 1 91 .0 10?. 1 1 14 . 1 51 .8 27.9 18-5 23.2 52.7 37^J) 51-9 55.8 22-8 Nil

N:2 68.2 70.9 86^2 88 .^^k^8 Lfljtf.4 \tfT.1 1 16 .0 03 . ^JfeQ-Ô^TTr^ 27 .0 4^5 47.9 55 .6fc3T3\ 43 .2 N:2

N:3 87 .T^ge'.jîiM^SwsVl yf6(ÔJÔa-LL9 . 9 ^.1 95^^2*Q^XOUl^2^2 52.5 Sy3tt*.\ 6 7-8 N:3

N:4 106 -1 112-^^-9 12/B.O 129-3 125. 8/ 9X.9 95.4^2X^2^^.2^74.5 ^2jJ,^53^3 71.2 76.8 N:4

N:5 \ 22 .-^]^^ 1/41 .^ML~^rfT^ 1 1 k^tTf3^^^^^^^^^^^8^8 WfT^^d . 3 74-6 N:5

N:6 175.7 154. 7 158-2 129.1 132.8 1 35^1 1 ////Ô V~ -Ô /7S^7 67 .V-3B .7 8J-.7 N:6

ON 2^ 5qN 75^ 10pN 125N ISpN 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pN 425NTflU TRU

/x |Q-3\ N:l 31-3 62-5 62.5 15-6 15-6 1-9 31-3125-0 62-5 31-3 31-3 ,1 3.9 . 1 125 -0 250 -0 ^2 .OK 31 .3 N:l

N:2 250-0125.0 62.5 31.3 3.9 31-3250.0 62.5 .1 15.6 .4, ^3. 9 Wo 1 25 .0 125 .0 125 .0 125 .0 N:2

N:3 62.5 62.5 31-3 7.8 31.3250.0 62.5 X ^t — -^1/1 5. 6 .2125.0 62.5 31.3 62.5 N:3

N:4 62.5 62.5 7.8 31-3250-0 62-5 ./f .1 .1 \6— -2 500 -0 62-Sr-ai -3 62-5 N:4

N:5 62.5 15.6 31.3250-0 31.3 .-T .1 .0 .5 o0250.0 ^^^1*^25-0 N:5

N:6 15.6 31-3125.0125.0 ~/ . 1 .0 .0 ^250.0 62. S7/^^^^. 5 N:6

LINE : 700 E


POLE-DIPOLE flRRflY

NA S

—(Eh rSh

~V''

OePTN POINT

N - \ . 2. 3. 4 . ... "fl" SPRCING - 25-0 METRES


flBBIE LflKE

WflWfl flREfl P ONT.DflTE : MRRCH 1996 REF : 9603

SCflLE - 1 : 2500

JVX LTD.

ON 2^ B^N 75^ | 10pN f 125N g ISpN r 17^N 20pN 225N 25pN 275N 30pN 325N 35pN 375N 40pNSPFCTRHL M SPECTRflL M

11=1 76,2115.8120.7 B5-^3LD6.4 105. 1 1Z3..2 98.81092103^6 45.6 30.9 23 .2 .58 .3 2.2* 5-J3 .9—23-^1 N:l

N:2 94.4 i2oXaîoo.)r"T5*-rs~r?ê-tir5^8 pi .3 ne. e 109. /6s.s\42\i3 4-3/53. e a^fi^BTT s i. 4 N:2N:3 101 .1 106. B U1.8-J35 i.^49TTKl 1 7C^^rTiTk 1 .ax^^T^S /ON^8.J^51 .9 4 1 . 05 8 . \^TC. 5 N:3

Ns4 98-1 1^7.0/f 4^TT6^*8 138. 3 132.3 l>^ JJ^^y^J-JZlôJ'-^^f 6 -2 60,? 72.3 N:4

N:5 133.9 W9.4 ITtfT. 4 I/I 6.8 r3fl-^6-4^.,^^^âr^(^r^5-^92 .5 /^ 38^3 79-5 N:5

N:6 M6.0 1 6/3 15/-4 156-6 ^3^ l^^^\^\ 46^^~^B^\ 87.1 80-2 78-2 N:6

ON 25.N 5QN 75.N lOpN 12?N 15QN 175N 20PN 225N 25QN 275N 30PN 32?N 35pN 375N 40PN

TflU TflU (X JO 3) N :1 1 25 - 0 7.8,^-9 62-5 15-6 62-5 15-6 62-5125.0 15.6500.0 31-3 15-6 -1125.0 31-3500-0 N:]

N:2 31-3 7-8 31-3 7-8 31-3 15-6 62.5500.0 1 5 . 6 x— il6 2 . 5 15.6 1-0250-0125-0 62-5 N:2

N:3 31-3 31.3 7.8 31.3 7.8 62.5250-0 31.3 \.\ /j) 15.6 3*9500.0 62.5 31.3 N:3

N:4 125.0 15.6 31.3 7.8 31-3250-0 7-8 .JJX . l/ 1 . Q Q . 5 250 . 0 1 25 .0 1 25 .0 N:4

N:5 31.3 31.3 7.8 31-3250.0 7.8 JS . 1 O .1 MMD250.0 62-5 62.5 N:5

N:6 62-5 15.6 31-3125.0 3-9 .O/ .0 A .2250-0 31-3250-0 N:6

LINE : 800 E


POLE-DIPOLE RRRfHY

Ml fl

--(Eh KD-i

DEPTH POINT

N - 1 . 2. 3. 4. ... "R" SPRCING r 25.0 METRES


flBBIE LflKE

WflWfl flREfl, ONT.Dfllfc : MflRCH 1996 REF : 9603

SCflLE - 1 : 2500

JVX LTD.

ON t 2^ ( 5(jN 7^ ( 10pN (125N (15pN ( 17pN 20pN 1 2 25N (25pN 275N 30pN 325N , 35pN 375N

SPECTRRL CI SPECTRflL M N:l 141.0 83.1 94 . 1 1 Q 1 -6 1 07 .6 11 1 . 4 L24 -3 95 *4 1 23^6 1 03 -5 1 45^4 85-3 5krL* 5 -y/!/! 7 7 6 ' 6 N :1

N:2 97.4 80.2 101 /l 124^*JQ6.9 1^35.0 1 2 4 :~6-4**-- 3 ekrTsTî-Xj * ^^~-SQ-f^\^4 BS .B N :2

N:3 85.7 9 1 . 4/1 3^5 11 sLz-m^S ! 2 3 ' 6 jx^7^ P 6/1 95 -S^ 1 1 4\^^ .VêO^V^fo/.S N:3

N:4 100.^^^1123.71^1^1217^X^-81/^4^21^2*12^^ Ns4

N:5 132. 1 121 .9 1/1 -^T49 - 0 LTf^T A 2)5^513515^ 4 l^-L3a^9T42A2 \IfftJ Le9r-2 N:5

N:6 128-8 1.8B.O 146-6 1^8-4 1/2-1 ^^^\WaC3M \7rnJ, ill ChS 17/6-7 1*3-6 N:6

ON 2^N 5(jN 7^ 10pN 125N 15pN 175N 20pN 22bN 25pN 27bN 30pN 325N 3bpN 375N

THU TflU (X 10 3) N:l 1.9 31-3 31-3 15-6 15-6 7-8 31-3 62-5 15 -îivjS^SÂ 5 ' 6 6 2 ' 5 3 1 ' 3 - 1 1-OIC50-0 N:l

N:2 15.6125.0 31.3 15.6 31.3 31.3 31 -3 125 .0,/^.ngjg^S 31.3125-0 -1500-0250-0 N:2

N:3 125-0125-0 15-6 31-3 31-3 62-5 62 -5^n|jMf L^.S 7-8 15-6 l-OrC50-0 N:3

N:4 125.0 62.5 31.3 15.6 62 -5^fi2 -^ff*|^^ 15.6 62.5 ^1500-0250.0 N:4

N:5 62.5 62-5 31.3 31.3 S^rS^/.W^^TJ S. 9 .5 .1250-0250.0 N:5/s/^Z^" — \ i// f "A

N:6 62.5 62-5 6 2 . 5 1 2 5 . O^^SN 1 //A 1 31-3 (l Jl 62.5 62-5 N:6t . i*Hh*,i "i li *-* * J , ... -. -. - -foi. —— -'V. 1 - U W-Htj, ,. . . . , . ,... ,. — -m..,,.- ^. -n j,, , .c. , - -, -mf- m-,-

LINE : 900 E


POLE DIPOLE RRRRY

DePTM*P01KT

N - 1 . 2. 3. 4. ... •fi" S PRCING - 25.0 METRES


flBBIE LflKE


SCflLE - 1 : 2500

JVX LTD.

ON 2^ 5^N 7^ 10pN 125N , 15pN t 1 75N 20pN 225N,25pN 275N i 30pN ( 325N t 35pN t 3 75N

SPECTRflL M SPECTRflL M N:l 140.2 195.8^ 84.3 10^-7 121 .7 1 14 .4 86.7 77^4^J^.5J 42 . 1 123 .9 151 .3 91^9 90 .0 V59.6^,87 .7 N:l

N:2 134^H^^3-m^9JjJ^p'l45^1 V\i 94.0 9 0 . l, . JjH'ffl 4 oWt62^5^t^^^^\95 09\ J-StTs N:2

N:3 122-8 M 3.2 13B^6 141^5^8 .V^06^^^9^6^8^t*?-8-4S^ N:3

N:4 145.X4\^^jlp.3 125-7 1 3 3 . 9H3L^^WrV3 7 . 2\g Y^^ 3J6 .^ 151 -2 158-9756^1 N:4

N:5 564/9^^)^2.4 131 .9 \ 33.^m^^^.:::^^^^l^^\AOJ-i-l^B-OOS^.\ N :5

N:6 .t)-t66 ^603^1 - 6 140/6260^5/1^^^^^^ iVj 19. 7 128. 3\ 641-9 N:6

ON 25,N 5CJN 75,N 10pN 125N ISpN 175N 20pN 225N 25pN 275N 30pN 325N 35pN 375N

TflU TflU jx jQ-3x N:l 1-9 -1 62-5 3-9 3-9 3-9 15-6 15-6125.0125-0250.0250.0250.0250.0 1.0IC50.0 N:l

N:2 1-9 15.6 31-3 15-6 3-9 15-6 7-8250.0250-0 62-5125-0250.0250.0500-0250.0 N:2

N:3 31.3 15.6 15-6 7.8 3^—^.8250.0500.0 15 . 6/^l.B 1 25 .0 250 .0 500 .0 250 .0 N:3

N:4 31-3 15.6 31.3 7 .Bf 3*9 250 .0 500 .0 15.6 f .f 3 1 .3 125 -0 250 -0 250 .0 N:4

N:5 .1 7-8 15.6 7^250-0250.0 15.6 Jl ol .0 31.3125.0250.0 N:5

N:6 .0 7.8 15.6250.0250.0250.0 .0 V .9 1 5.6 62.5125.0 N:6

,-

LINE : 1000 E


POLE-DIPOLE RRRflY

, m , B ,--®-i r®-\

OEPTM*POINT

N - 1 . 2 , 3 ,* 4 . . - - "R" SPflCING - 25.0 METRES


flBBIE LflKE


SCflLE - 1 : 2500

JVX LTD.

ON 25N SON 75N 10pN 125N 15pN 17pN 20pN 225N 25pN 275N 30pN 325N ( 35pN

SPECTRflL M SPECTRflL M N:l 149.8 98^2^7-6 61-7 69.4 91.3 75.0,91-7 95.^ 1 07 -4J 34 -322J.6 157 -6 1 21 .7 68.4 N:l

N:2 89 . -B\ 1 22. 7 J 6/. 4/93^^91. 6 98.6 81 .6 104 ?7 l^^TÂ B^^Dji.B UP -B 104 .0 N:2

N:3 105.9 W.6JJ16^1^^TbTr4l 13^Tri^9^3^fl^^ N:3

N:4 89.3/(^7<Tr^9^22\^7.•7^r4^8IIfr^^l/9 Ns4

N:5 121 A 1 38-4 138-7 135 \31^^^îa^(^^^^^1 2Q 4 Jn4a*9 N:5

N:6 140^74T^No/^l63^^3^8^LiBr8^r^Z^^^^ N:6

ON 2^ 5(jN 7^ 10pN 125N ISpN 175N 20pN 225N 25pN 275N 30pN 1 325N { 3 5pN

TflU T flU (X 10"') N :1 ' ' 9 1 5 ' 6 3' 9 I 5 ' 6 3 1 ' 3 3- 9125 ' 0 l 5 ' 6 31.3125.0 31.3 .1500-0 31.3250-0 N:l

N:2 62.5 7.8 62.5 15.6 15.6 15.6 31.3 31.3250-0 62.5 15.6500.0500-0 .5 N:2

N:3 31.3 62-5 31-3 7-8 31-3 7-8 62-5250-0 62.5 1-9500-0250.0 62.5 N:3

N:4 125.0 31.3 31.3 31-3 31-3 31.3250-0 31-3 ^.0500.0500.0 15-6 N:4

N:5 62-5 31.3 31.3 15-6 62.5250-0125.0250.0500.0250.0250.0 N:5

N:6 31.3 62.5 31.3 31.3250.0 62.5 -1250.0250-0500-0 N:6

LINE : 1100 E


POLE-DIPOLt RRRRY

. m . R .

DEPTH POINT

N - 1 . 2. 3. 4. ..-

"R" SPflCING - 25-0 METRES


flBBIE LflKE


SCflLE r 1: 2500

0. 165 55ON 25.N 5QN 75N 100N 125N ISpN 175N 20pN 225N 25pN 275N 30pN 325N 35pN

SPLCTRRL M ' SPECTRflL M N:l 171.1 78.6 64.3 79-6 61.5 80-0 92.1 9^4 1 24, .0,1 60. .9 1.31J^2 .9 1^0^^2^,199-1 N:l

N:2 79-9 W^— 15^6^7 0 . 2 'S8^31JJ8- . 8 'nB-^-il^' ^^ CA^^^49^S^^^*2 . 5 N:2

N:3 79.1 101^8 8 4 . VT0^6^fl7 . QsT33 ^ 5J^9^TT54 . B 20 31.3 Ztfy/^ZT^. 1 25*,7Xl^..9 N:3

N:4 105 .^10lVe-Tl^JJJ^8^39.Xl3*r2) 1 3*~âs20 O^.A^^^4 2 9 3 . 2 2\4 . 1 2 36 - 7 N:4

N:5 97-7 \ 2^^^^^-^4Q-^yfl- 9 1^5/3 1^^^^)^3295.9284.6)260.3 N:5

N:6 124.1)147^4 151 - 7x2Ortkl\36 ^rr72x?^^^294 .2 284.3/260-5 N:6

Lines 500 E- 11 00 E

ON 25N 5QN 75N 10PN 125N 15pN 175N 20pN 22?N 25PN 275N 30pN 325N 35pN

TflU T flU |X jQ-3) N:l -5125-0 62-5 15-6 62-5 62-5 15-6 31-3 1-01-01-9 1,.OK 1 -QK31 .3 -2 N:l

N:2 250-0 62-5 15-6125-0 62-5 15-6 15-6 3-9 1 2 J l l v-tfK 2 -OK— zTf3tN3 1 . 3 N:2

N:3 125.0 31.3 62-5 62.5 15.6 15.6 1-9 1.0^ — / O.OK 2 -oV 2^0K I .OK N:3

N:4 31.3 62-5 62.5 31.3 15.6 1.9 7 .8^— k . 1 /Z .OK 2.0h| ZxOK 1 -OK N:4

N:5 125-0125.0 15.6 31-3 1.9 15-6 ^W/2-OK 2. OK 2VTJK l.OK N:5

N :6 125.0 31.3 31.3 1.0 31-3 1.9 /2.0K 2-OK 2-OK l.OK N:6

PLATE 6a . rriiiiiEiHiiiiiiiiiiEiiiiilfllllU e.,.,.... , nn ^ n

^VXLTO HlllllllllllllllllllI2C03NW0015 2 16555 ABBIE LAKE

NTS 42 C/3 WAWA AREA ONTARIO · 2017-01-17 · 42c03nw0015 2 16555 abbie lake 010 a logistical and...

Documents

Transcript of NTS 42 C/3 WAWA AREA ONTARIO · 2017-01-17 · 42c03nw0015 2 16555 abbie lake 010 a logistical and...