GEOPHYSICS REPORT ON THE BELANGER PROPERTY · GEOPHYSICS REPORT ON THE BELANGER PROPERTY...

$Page 1: GEOPHYSICS REPORT ON THE BELANGER PROPERTY · GEOPHYSICS REPORT ON THE BELANGER PROPERTY NORTHWESTERN ONTARIO FOR 2.17095 CANADIAN ZEOLITE LTD. fib U 4 ^ i \yJ DanPatrie.'-^ Dan Patrie$
52N02SW0011 2.17095 KNOTT010

GEOPHYSICS REPORT

ON THE

BELANGER PROPERTY

NORTHWESTERN ONTARIO

FOR 2.17095CANADIAN ZEOLITE LTD.

fib U 4

i J^ \yDanPatrie.'-^

Dan Patrie Exploration Ltd.

Decembers, 1996

IV

D s R H

52N02SW00112.17095 KNOTT 0 1 OC

TABLE OF CONTENTS

PAGE

INTRODUCTION l

SUMMARY AND RECOMMENDATIONS 2

LOCATION AND ACCESS 3

INSTRUMENTATION AND WORK DONE 3

REGIONAL GEOLOGY 4

PROPERTY GEOLOGY 5

CLAIM DESCRIPTION 5

INTERPRETATION 6

RECOMMENDED EXPLORATION PROGRAM 7

PERSONNEL

REFERENCES

FIGURES

CERTIFICATE OF QUALIFICATION

LETTER OF CONSENT

CHARGEABILITY ANOMALY MAP

BASE MAP

MAG MAP

VLFMAP

DIP ANGLE MAP

INTRODUCTION

Canadian Zeolite Ltd. acquired a group of 3 unpatented mining claims in the Birch-

Confederation lakes metavolcanic-metasedimentary belt that is situated within the western Uchi

Subprovince of the Canadian Shield. A geophysics programme was recommended by the property

owners, and work began in November, 1996.

The property is underlain by a mixed metavolcanic-metasedimentary sequence of the

Birch-Confederation greenstone belt, within the western extension of the Uchi L ake subprovince.

The sequence defines a northeast trending belt of Archean rocks which extends from the

Confederation Lake area to the east to Gullrock lake to the west.

In summary the Belanger Property has shown to have considerable merit and warrants

further exploration work in order to evaluate its potential to host economic precious metal and base

metal mineralization.

Dan Patrie Exploration Ltd. was requested by Canadian Zeolite Ltd. to carry out a limited

programme of line-cutting, mag and induced polarization survey to better define ore potential on

their newly acquired claim group.

The following report summarizes the results of the work carried out during the current

programme and the results obtained.

Respectively submitted,

Daniel F. Patrie

Geology and Geophysics Technologist

Decembers, 1996/A,•Cjfr- l

Page 2

SUMMARY AND RECOMMENDATION

The Belanger property is located in the Patricia Portion of the District of Kenora, Red

Lake Mining Division east of Red Lake, Ontario which consist of 3 unpatented contiguous mining

claims located in Belanger Township.

The writer has been requested by Canadian Zeolite Ltd. to do a geophysics program on

the property. The following report summarizes the available information and recommends further

work to evaluate the economic potential of the property. The writer supervised the work done.

In November, 1996 a mag/VLF, and a 4 level Pole Dipole Induced Polarization survey

was done on a portion of the Belanger grid. A total of 11 kilometres of line-cutting and mag/VLF

and l O kilometres of induced polarization was surveyed. The survey indicated large areas of

chargeabilty anomalies which could host massive sulphides or precious metals.

The following report summarizes the results of the work done during the program.

Since there has been no detailed geological work during this program the interpretation is

speculative.

It is recommended that the following program be carried out on the property to complete

the evaluation.

1. Completion of grid lines spaced 50 metres over the claim group.

2. Geological mapping and prospecting to identify zones of mineralization.

3. Completion of the induced polarization survey.

4. Humus sampling over anomalous areas to better define drill targets.

Following completion of this work and contingent upon the results then additional work

could be considered to further evaluate the economic potential of the property for base metal and

gold mineralization.

Respectively submitted, r s f/' ) .

Daniel F. Patrie .^Cfr^

Geology and Geophysics Technologist.

December3, 1996

MANITOBA / '

XX

LAKC

PROPERTY

55*

ON T ARJO--- --""""^ ——UCHI SUBPROVINCE

QUEBEC

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U.S. A45'

FIGURE l

GENERAL LOCATION MAP

Page 3

LOCATION AND ACCESS

The property is located approximately 75 km east of Red Lake, Ontario (Figure 1) in the

Red Lake Mining Division, District of Kenora.

The claim group lies in Belanger Township. Access to the property is from the town of Ear

Falls up South Bay Mine Road, 65 kms northeast of the town of Ear Falls.

INSTRUMENTATION AND WORK DONE

The pole dipole induced polarization survey was done using an MG-2 motor generator and

a Pheonix transmitter with an EPR 12 Time Domain Receiver made by Scintrex Ltd.

The readings were taken every 25 metres with 4 levels being read and stored in the receiver then

dumped to a computer and plotted in pseudosection with Geosoft software.

A total of 10 kilometres of induced polarizationwas read over the Belanger property grid.

The total field magnetometer and VLF survey was carried out using an EDA OMNI PLUS

magnetometer/VLF unit and an OMNI base station magnetometer. These are total field

magnetometers which measure the magnetic field through the use of proton processional effects

caused by the interactive of a magnetic field with a spin-aligned-rich fluid. An instrument accuracy

precision and resolution of 0.5 nT may be obtained with these instruments under ideal conditions.

Microprocessors contained in these instruments allow for the collection of the readings along with

the time and its position in digital form suitable for transfer to portable computers.

The total magnetic field was measured at 25 metre intervals along all grid lines. The total

field measurements were concurrently recorded at 30 second intervals by the base station

magnetometer which was located on grid. All field measurements were corrected for diurnal

variations of the earth's magnetic field by direct subtraction of the base station readings taken at the

same time.The corrected magnetic data has been plotted, contoured and is presented in the total field

magnetometer plot. The Vlf measurements were also taken with the mag/VLF units. Readings were

taken every 25 metres along grid lines. A total of 11 kilometres were read.The data was plotted and

present in the back of report. All data was stored on diskette in Geosoft files.

Page 4

REGIONAL GEOLOGY

The Birch-Confederation lakes metavolcanic-metasedimentary belt is situated within the

western Uchi Subprovince. Fenwick-1965, Muir-1981 and Thurston-1985 concluded that the belt

comprised of a thick succession of predominantly metavolcanic rocks and minor metasediments

intruded by mafic and felsic bodies.

The belt includes Casummit and Birch Lakes in the north, and Uchi and Slate Lakes in the

south. The belt is composed of mafic, intermediate and felsic metavolcanic flows and pyroclastic

rocks with subordinate metasedimentary rocks. The south and southeastern margin of the belt

consists dominantly of linear units of metavolcanic rocks alternating with thick sequences of clastic

metasediments. Various late, felsic, intermediate and mafic batholiths, plutons, stocks, plugs, dikes

and sills intrude the metavolcanic and metasedimentary rocks. All of the rocks in the belt are inferred

to be Archean in age. Varying degrees and types of alteration such as carbonatization, sericitization

and chlorization are common in the rocks throughout the belt. Large scale folding is common

throughout the Birch-Confederation lakes greenstone belt.

There are over 120 known gold deposits in the Birch-Confederation lakes area, the majority

which consists of structurally controlled, gold-bearing quartz veins hosted by shear and or fracture

zones concentrated in areas of greenschist grade metamorphism. The gold bearing quartz vein system

are associated with deformation zones trending north and northeast at Confederation, Woman and

Uchi lakes. Out of the 3 metavolcanic-metasedimentary cycles in the belt most of the gold deposits

in the area are situated within the Cycle II sequence. Cycle in sequence hosts a number of significant

but sub-economic Cu-Zn base metal deposits and prospects. All of the deposits and prospects are

typical VMS deposits exhibiting Cu-Zn rich massive sulphide mineralization localized along

stratigraphic maine breaks with intensely altered footwall rocks, and unaltered hanging wall

stratigraphy.

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PROPERTY GEOLOGY

The property is situated within the Uchi Mine structural domain which consists of a

dominant east-trending foliation and subordinate northeast-trending foliation which represents a high

strain zone (Fyon and Lane 1985,1986). North and northeast-trending mafic metavolcanic flows are

intercalated with dominantly intermediate to felsic pyroclastic rocks and minor interflow

metasediments.

CLAIM DESCRIPTION

The property consists of 3 unpatented contiguous mining claims all in good standing

located in the Red Lake area of northwestern Ontario, situated in Belanger Township.

Table l

Belanger Property. Red Lake Mining Division

Claim Description

Minin Claim Number of Units

KRL1143537

KRL1184553 02

KRL1184554 12.

TOTAL 1 8 Units

Page 6

INTERPRETATION

There are many good high chargeability anomalies located on most of the lines surveyed

on the Belanger grid, located on all of the 4 levels of induced polarization read and are open at both

ends running off of the grid portion that was surveyed The anomalies run from line 0+00 to 10+00 W.

The first chargeability anomaly is on line 0+00 centred at 2+OOW.

The second anomaly is on line 1+00W centred at 3+OOW.

The third anomaly runs from line 3+OOW to 4+OOW centred at 2+OON running off grid.

The fourth anomaly runs from line 5+00 W to 6+OOW centred at 2+OON running off grid.

The fifth anomaly runs from line 7+OOW to 10+OOW centred at 0+50S running off grid.

The chargeability anomalies extend mostly the length of the and is open at both ends, and is shown

on the chargeabilty map included in back of this report.

The chargeability values for the anomalies are well above background values and are

consistent with metallic mineralization. The bulk resistivity values on some of the anomalies also

correspond to a mineralized target (2000 ohms-m). Background values between 2mV7V and 5mVYV

are caused by electrilytic polarization as opposed to the combination of electrolytic and electrode

polarization in the case of metallic mineralization. The resistivity plots show bulk resistivity

corresponding to bedrock values. Before drilling any of these targets there should an evaluation of

all data from the property to establish a proper drill program.

The magnetic signature of the property is relatively uniform in the range of 59,300 nt. An

elevated magnetic signature trending east-west in the centre of the grid coincides with the induced

polarization survey.

The VLF survey also, showed anomalies in the areas where mag and I.P. anomalies were..

The results of the survey are considered to be encouraging and in view of the potential of

this property and lack of full coverage of this survey, the rest of the claim group be surveyed is

recommended.

Page?

RECOMMENDED EXPLORATION PROGRAM

The following program is recommended to evaluate the property for its potential to host

a base metal and or precious metal deposit.

1. Complete the line cutting as required to provide a control for geological, geochemical and

geophysical work.

2. Geochemical sampling over target areas before drilling to establish better drill targets.

3. Completion of ground magnetometer and VLF survey.

4. Detailed induced polarization over selected areas.

5. Do geological mapping and sampling over all of property.

6. Stripping, trenching and sampling targets with potential interest.

As a result of the encouraging results obtained from the recently completed geophysics

survey, additional exploration on the property has been recommended.

7 , ^^Daniel F. Patrie


Decembers, 1996

PERSONNEL

1. Dan Patrie

Massey, Ontario

2. Brent Patrie

Walford, Ontario

3. Bryan Patrie Spanish, Ontario

4. J.P. Paradis

Massey, Ontario

5. Charles Laundriault Walford, Ontario

6. Tim Kelly

Spanish, Ontario

7. George Savard

Massey, Ontario

8. Arron Andress Massey, Ontario

REFERENCES

1. Atkinson B.T. and Parker J.R. 1992

Gold Occurrences, Prospects and Past-Producing Mines of the Birch-Confederation

Lakes Area.

2. Bruce, E.L., 1928

Gold Deposits of Woman, Narrow and Confederation Lakes, District of Kenora (Patricia Portion); Ontario Department of Mines, Annual Report for 1928. Volume 37, Part 4, 51 p. Accompanied by Map 37h, scale 1: 47 520 or l inch to 3 4 mile.

3. Fyon, A.J., and Lane, L., 1986Assessment of the Gold Potential in the Uchi-Confederation-Woman Lake Area: Preliminary Results, District of Kenora (Patricia Portion); Ontario Geological Survey, Map P. 2989, Mineral Deposit Series - Preliminary Map, scale 1:50 000. Geology 1985.

4. Goodwin, A.M., 1967Volcanic Studies in the Birch-Uchi Lakes Area of Ontario; Ontario Department of Mines MP 6 p.

5. Winter, 1987

Geological report on the Exploration Potential for Gold and Base Metals of the Shabumeni Lake Property, Birch Uchi Lakes area, Ontario for Greenstar Resources Ltd. Revised August 6, 1987, 17 p.

6. Winter, 1988Exploration Programme Update Shabumeni Lake Property, Birch-Uchi Lakes Area Ontario for Greenstar Resources Ltd., 12 p.

7. Winter, L.D.S., 1987

Geological Report on the Exploration Potential for Gold and Base metals of the Shabumeni Lake Property, Birch-Uchi Lakes Area, Ontario for Golden Hope Resource Limited.

CERTIFICATE OF QUALIFICATION

I, Daniel F. Patrie do hereby certify:

1. that I am a geology and geophysics technologist and reside at 190, Hwy. 17 West, Massey, Ontario,

Canada, P.O. Box 45, POP 1PO,

2. that I graduated from Cambrian College of Applied Arts and Technology in 1987 with a Diploma

in Geological Technology with a one-year certificate in Geophysics,

3. that I have practised my profession continuously since that time and prior to that since 1972,1 have

been an active prospector,

4. that this report is based on a personnel review of Provincial, federal and some assessment reports

as well as interpretation of field observations undertaken on the Belanger Property, Belanger

Township, Red Lake Mining Division, Ontario and was present on the property throughout the

whole program,

Daniel F. Patrie


October, 1996

LETTER OF CONSENT

I, Daniel F. Patrie, of Massey, Ontario, do hereby consent to Canadian Zeolite Ltd. using in whole or in part my report on the Belanger Property in a prospectus or statement of material facts or

for filing with government regulatory bodies as is deemed necessary.

Dated at Massey, Ontario, on December 3, 1996 in the District of Sudbury.

Daniel F. Patrie


FM RES XVI XM RES FM

j \ /""^X - ^^^^^t^-^^^^^/S-^.'-N /"-X j'•™- H " ^̂ ^ \^~*^~*~""^~^ X^CX ^^^-I^^^c^^ ' ' i™ -OM'r. n| o t i i i i i i - ' , . i i t i i i i i i i i : i i i i i i j i r i i i i i i i i i i i i i i i t i i i i i , i ( i i i i j i , , , i i i , , , , , , i , | , | ; o lo ' n

Vp+Pl Fnrtnr 6+00 S 5+50 S 5-OOS 4+50 S 4+00 S 3+50 S 3+00 S 2+50 S | 2+005 t 1 +50S 1+OOS 0+50 S 0+00 0*50 N 1+OON 1+50N 2+00 N 2+50 N 3+00 N 3+50 N Mptnl Fnrtor

Filter 0.090 0.060 0.050 0.030 3.040 0.040 0.040 0.060 0.080 0.10 0.11 013 0.090 0.11 0.090 0.11 0.13 0.14 0.12 013 0.13 0,12 0.11 0.060 0.11 0.10 0.17 0.12 0.12 0.14 0.060 0.060 0.15 0.15 0.12 0080 0.070 0.040 0.090 0.070 0.060 Filter

0=1 0.040 0.060 0.030 0.020 0.030 0.040 0.090 0.12 0.15 0.14 0.17 0070 0.11 0.11 0.16 0.16 016 014 0.20 019 0 '3 014 0 D60 017 0.13 033 015 0.16 0.29 0.050 -030 0070 018 015 010 010 J. 050 0.17 0060 0.060 0=1

0 = 2 0020 0030 0,030 0.023 0.11 0.030 0.060 0 C70 010 0.080 012 0090 0.090 0.080 0.080 0.11 0.17 0.15 0090 013 0.12 012 0060 0040 0.12 010 018 0090 0.12 0070 0040 0.33 0060 0 080 Oil 0 OK 0.040 0.030 0.12 0050 0 = 2

0=3 020 00100 3.030 0.030 0020 0.020 0.050 0.060 0060 O.OBO 0.10 010 017 0070 0080 0070 0.14 019 0.12 0080 Oil 015 0.080 0070 0040 0.16 0070 016 O.I; 0.060 0.080 0050 046 0060 0.070 0.11 0050 0030 0.030 010 n-3

0 = 4 0.050 029 00100 0040 0.050 3 03C 0.030 O.C4C 0050 0.050 0.090 0.080 0.17 0.13 0.060 0.0713 0070 012 015 0.10 0.060 013 0.10 0.11 0070 0040 012 0060 016 0.060 0070 0.090 0050 0.37 0050 0070 0070 0.040 0030 0030 0 = 4

Rpcistiviry 6 l(los 'Jt;)OS S"005 4*MS 4tOOS J*MS •WXJ - 2 45CS 2tOCS U50S '*flos 0*MS O400 0™ N l 4floN '*50 N 2+00 N 2+50 N 3*00 S 3*50 N 3pe;ic;tivity- Filter 28K 2211 22K 30K 3'K 29* 25* 16K I2K 9954 8115 6761 12K I2K I5K 13K UK 9438 9883 i32B 8935 8546 10K I6K I3K I2K D635 9901 9575 B2M 8779 4502 6141 5014 5300 9416 I2K 18K 13* 12K UK -iltor nÛnm-m u (Jhm-rri

0=1 I2K UK j m, 34* __ :5K IK i 9458 6812 4381 — 3617 3878 v 13K 7;37^ UK 8292 SS4I 7182 "95 -. 4361 5185 5852 5763 - '2K - 4849 7760 4018 69!3 — H94 2521 - 5505 ...441 . .. 7692 1986 2904 9332 -, 5397 , 1 4K ^- 1800 ^ 11* 111 0=1

0=2 m ^~^m~^ m (w ( ' 'S3 '1 ) 34* Vis* izx"^ TOiTir~so95 \~56so'' 7529X14* —— 14* 15*- :2*N 7972 gt96 ion—. ewT~~ KM 674?'/ m ('"m \^?w fiaT^V w ' TiTj " 6557 ~̂ m~~^ 7 068 ^74^'^ 6197"^" 5098 4719 v nrf*^, i TiT/^lw^Me? \^ 13* 0=2\ \ \-^ \ ^-^-^ \ ( \ S. v^ ~Oy i \ ; \ \ / ^** i s \ ^ --. \\V N\ ~ \ ^^ \ \\\?\ \\\\ r \ ̂ ^ \( ^ y vx&uV^

0 = 3 1474 V 47K v 22K 24K \ 44K 45K 23K . I5K 13* I3K 9341) 7412 5561 . ; IW 1* ' 1* \ 3710 7551 l OK IK 9925 7014 / m ' tt V 24* ,\ 5839 \ W\ '186 95!B '3K 9694 7382 \" 1130 \ 9525 S80I . 4101 l 18* ^ 24K 22K X* 2137 0 = 3 -i"^\ O- \ (~\ \ l \ ~~ ———— ~, ^~^ \ 'A\ ~- \. \ / \ ~~ S "~ \ \\SkAV V ( \ \ A^\\\\\ l \ \ X-) \\ V V \V

0 = 4 7111 1654 * 66K "- ^ '9K ^2* 3* 3W - 26K s IBK I7K N I2K I2K ' 5474 SIM ' 22K - 17K '9K ^ UK 9291 I3K 11* 8838 UK UK !6K 24K X^" 7379 ~ 19* - '848 ' 15* — :3K 9593 6694 ~ 1429 - N 12!O~ 64M 5*02 21K 21K 2IK 0 = 4

. hnr^ pnh j t y 6+OOS 5+50S yOOS 4+50S t 4^05 3'50 S : 3+00 S 2*50 S | 2*OC 5 . HW' IrtCS 0+M , 0+BO 0'5n N 1+OON 1+50 M 2.00 N :*50 N 3KB N 3+50 N rhnrfjpnhility

^y/y Filter 5.2 5.6 6.6 78 16 9.2 91 9.1 8.9 8.4 7.6 7.9 9.6 11 12 13 13 13 12 '1 M 95 9.7 93 9.6 10 12 11 9.8 8.3 5.4 3.3 5 45 4.7 ' 6. J 7 5.1 5.1 6 Filter mV/V

0 = 2 5.5 62 67 83 1.9 91 93 8.2 9 75 6.7 1 1 12 12 13 13 14 13 (93 \ '2 ''0 ^ 84 9 ___ a4 91 l 12 IS 10 8.1 6.BV 26 25 52y 4 'i 82 52 7,1 V 26 X67 0 = 2

0 = 3 2.9 \ 66 7 7.2 S i .6 , - -^0~\ 6.9 8.1 9.6 9 7.3 9.2 x 12 12 12 13 14 12 "~ 9 J 11 " ~"---^L/ '' 9 ' 9 9.3 \ 12 12 Ys 8.3 7.5^-^3.4 5.2 5.4 ^-.4.6 43 1,4 6.5 7 3 \, 22 0=3

n-4 33 *8 74 69 82 9S ^ T '0 9.3 9.1 'II s 9 5 91 91 12 12 13 14 1* 12 ' 9 4 - '2 12 11 12 10 B. 8 M 12 9.8 91 84^-35 53 5 8 x 4 3 * 7 BC E 8 74 0 = 4

Line 0

Pole-Dipole Arraya na a

1 —— CD-i r-®nFilter J 1 1

*

X \^ / ' a ^ 25.0 M

41 * * * tf"plot point

Logarithmic . . q 0 , ^ 7 r l nf\ i l| '•'J.i-ii/.W./.Jl iU...Contours

INTERPRETATION

' Strong increase in polarization accompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity aecrease.

D Poorly defined polarization increase with no resistivity signature.

W Low resistivity feature.

Scale 1 :2500Z5 0 25 50 75 100 125 150

(metres)

CANADIAN ZEOLITEINDUCED POLARIZATION SURVEY

BELANGER GRID INDUCED POLARAZATION

Date: 96/11/06 Interpretation: D. PATRIE and B. PATRIE

DAN PATRIE EXPLORATION LTD.

FM RES XM 0.22-, 32K- 12-

0.11. 16KJ 6.

J

oJ o.

Metal Factor

ResistivityOhm-m

chargeability mv/v

6*005

Filter 0.020 0.030

0=1 0.030

0=2 0020 :'i

0 = 3 O 020 O 020

n-4 0.030 O 020 f

Filter JOK 24K

20K

*K NJ7K JiK

\ M l

Filter 6.' 6.!

0=1 6

0 = 2 6.6

0 = 3 6.5 7 4

0 = 4 48 7 S

XW RES FM1 1 T71C O 99

\^ ''''^--. .— — - ,—- , --''~'' Sc---'''^---, ^ — ~~Z /"^ ^-^ ^ — ̂ -6 hK h011v~--*.'"~~~' Jl." " ---- - s- ~^,^ 2*.^ — ..^.^ r̂—~^/ \^ ••v. '""" i 1

f -'" "~~-,^. ,*-"^" " " — •-— ^^ X "~~" ---------' N^ -^ ~-.--"~~ •"^"•"•—••^ [

'•*50S 5*005 4+50S ( 4+00 S | 3+50 S | 3*00 S | 2*505 ( 2+pC S 1*505 | 1*OOS | 0*505. | 1*00 QW* ! *OJN 1+50 N 2*00 N 2+50 N 3*00 N 3+50 M Mptnt Factor

0.040 0.040 0.040 Q. CM 0.070 0.090 0.090 0.12 0.10 0.090 OJO 0.10 0.090 0.10 0.090 0.090 010 012 0.20 0.14 0.10 0.11 0.13 Oil 010 0.060 0060 0060 0.070 0.14 014 0.080 0 OSO 0.070 0.070 0.070 0.090 0.10 Filter

0.040 0050 0.050 C. 060 0 OBO 0.070 0.060 0.12 0080 0.11 0.11 012 0090 0.11 0090 0.060 O.WO 015 021 0.060 0.060 016 0.20 0080 0010 0080 0090 Oil 013 029 021 0080 0041 0 OK 0.080 0.060 0.11 0.11 0 = 1

020 0.040 0050 0.040 0050 010 0.080 0.060 0.14 0070 0070 013 OJO 0.090 010 0080 0.1! 010 OJO 025 0070 0.050 011 015 010 0 08C 0040 C 060 3050 0080 019 015 0040 0 OK 3080 O.OW 0.070 011 11 = 2

0 OJO 0040 0.050 0040 O.OM 0.090 0.090 0070 0.13 0060 0.080 011 0090 0090 0090 0.080 0.080 0070 012 028 0-060 0050 0080 0.18 012 0 OW 0030 0 C50 0040 0070 016 010 0050 0090 0.070 0.050 0 OSO 0=3

•580 0030 0.040 0040 a. CSC 0080 0.090 027 0080 013 0.060 0070 0.13 0.090 0080 OJO 0060 025 010 0.21 040 0050 0030 0.14 022 0090 0050 0020 3. OSO 0030 3060 0030 012 0060 012 0.060 0.060 0 = 4

VMS 5*00 S 4*50 i 4+00 S 3*50 S 3*00 S 2*50 S 2*00 S | 1*50 S 1.00 S p 0+50 S | 0+00 0+50 N 1+00 N 1+50 N 2*00 N 2+50 N 3+00 N 3+50 N Resistivity

25K 23K 22K 18* 14K UK 7612 7024 IOK I2X I2K "K I2K IOK lil tOK 8880 7320 4944 111 161 I4K UK UK 9165 I4K 14K I3K UK 5665 6107 I2K 16* 121 9625 101 7038 5855 Filter Qh

28* 211 20K^ 14K 9689 ^l?"x 5947 6Z4I ^ I7K 9538 9567 8301 9730 5701 7*55 8178 ,, 6996 4072 - 2170 ^ lw , 12K - 5.128 6041 v!4K 7606 7214 - 4887 3855 — 3762 -- 1556 , 4864 . I5K , 241 . I f* x 6236 - III l 5103 — 5451 0=1\ ^ \ \ — i ^ \ \ f ̂ - " — ' v ' — "- V'^\* —— '-V- NX ) -- ~^/ — ̂s^^n-- — OxN'O \\\M( s ' s i \ \ \16K ) 26K 23K 23K \ 1W 8872 7425 7077 6564 \ '* , —— I5K 69)^/1 'K ' Ik "^^-tST^y IOK ^^^2 -. 6796 __ 6ffiO . 2445 XliK , 2W ^- ™?9 ^ 705J XÎJ 7418' ITiT^-. IOK IOK—. 7241 x' 2197 \ 7366 \ 21K^, ' 1*' /74S1 1 -X 9 339 4316 0 = 2

*~~Za( 26K 22K 22H \ ' 14* 1*^^757) 666B 5M\ . 'K ; IK UK 13K I2K UK 12K 111^9357 ' 8671 3025ÂziK ?8K "N 10K\ 6377 9942 -"^ tx I 25K\; ^9466 j I4K ^ 7071 , 2748 \ \ UK X^ 1 tt 1 8834 IOK 12K \ 6680 n^3

9189 s- 26* 22K 26* 3* ' III 12lN 5609 6694 7157 "'16* 'W J699 :4K IS* 9799 '4K IOK 8417 v 5633 lilt ^ m m -\ 5661 5419 ' '4K 16K ' 51K ^ 12K I2K^ 1888 X 2898 x 5204 1211 ^- 4044 6958~~M45 11 = 4

VMS 5*005 4-50 S 4*005 ,3*S3 S J'OO S :*W S 2*00 S 1*505 IKX15 0(50 S -HOG 0'50 N 1*OON 1*50 N 2*(Xj N 2*50 N 3*00 N 3+50 N rha rqenDi litv

89 9.6 98 J.I 87 1 6 .6 7.8 ].1 98 II 11 II 9.7 9 9.4 67 85 8.1 )3 94 14 10 11 85 7.8 6.5 5.6 5.3 4.6 7,5 8.2 86 B 4 6.8 6.7 5.6 5.6 Filter y /y

10 -10 10 87 J 5 9 i J.S v 7 1 9.3 10 11 97 84 13 7 66 S3 ( : - 4 s 1 ! 6 B f 7 . 12 10 ^ 5 5 58 45 43 47 45. 10 X9 9 9 52 sg 55 59 n- 1 \ \ \ 1 1 ~~~--^ —— ̂ \ "~N ~^\ /" 1 N \ \

66 94\ 1 1 9 8 7* 9 6 1 ^~-* i^ * 9 8 ! 1 " ''9.8 86 83 33 '.5 b8 * M ^. 93 98 \^ H H V. 58 6.3 5.9 x^ 5 5 6 \ 4' 'l\82 93 83 69 63 49 n = 2

8 J.B^ÎO/ 93 B. 3 3.7 7 49 9 C. , " " '2 1! 11 "^-~ 9 f 91 8.1 ,, ' 9 a 1 5 V 12 9 B 8.5 N^ 11 li 1- 66 8 5.2 6 5.3., 4^.3 11 \ 84 7. f 6.9 6 5.4 n-3

J 6 83 S 5 9.8 '0 93 ^- l7 " is^"~ 54 89 9.6 s M 13 13 12 "~10 t 5 ' ^- ,". ^^ 52 ^ "- 8 7 - 12 "94 5 ^ 12 13 s- 7.5 84 6 -"li*' S . 5 0.77 s 11 x- 74 n - 59 6.1 n -H

Line 100 W

Pole-Dipole Arraya no a

- — CD-i r®-iFiltpr 1 1 1

*

t*/* "^ /' a " 2 5 ' 0 M* * * i ""d

plot point

Logarithmic 5 2 3 y 5 Q Contours

INTERPRETATIONB Strong increase in polarization

accompanied by marked decrease in resistivity.

Q Wetl defined increase in polarization without marked resistivity decrease.

Q Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature.

Scale 1:250025 0 25 50 75 100 125 150

(metres)

CANADIAN ZEOLITE INDUCED POLARIZATION SURVEY




FM RES XM XM RES FM

"" "" " ^Nîx^'^^'^^ -^' \ — -^ " h *~.--- \r.-x---.-'' ^ "----j ~-— ' ~ ---... .. - ~ \ i

M-. al f^r,, wos wes wos . j.ss . MOS. .,, wos. 2.ws t* s ,. MBS wos M* WON. ........WON. . ran . 2^N . 2*N u.tol Foc^r

Pesi^tivity 5*OOS 4*MS WCS Jf50S WBS ^MS 2*00 S ( 1*WS 1*03S i 0*50S J*00 0*50 M 1XCN 1+WN 2*00 H 2*50N pe o rt j v ;ty"hm-m rilter OT 1 JI( ) SC IT11 *7* nw JOO i* W m Mil w '* '* '* lw JWt )Ui i* w* UB T9 l* iw '* i* 10 IJK MH UK ftx 77W 73K Filter Ohm-m

n s2 '* ̂ î* "*-i. JJ7* 5^J^"X^M4\ 1*" \ t** '^!?-^?li^ 'S?S "^ Vv^J Wn '"îJ^-^lÎr^x'^^^vAvV*!^" ̂ " XX\ ^-V? ^ ( V * '"' \ ?* \ lfl( *; m7 ~-~JlS! /^l*\ 5671 — 74W ^^2

n-4 HK ^ iW^ (JJ* ^Tjll^ 7110 'an IBD — TJS-'T* J* ^ UK *^ i*J) UOi * ' Z* ffl( W ' 1*^^*fl III) -^ '* *^ 7SO "- HB RID QS 11K^ J*^ l W 1* - —— IB MK ^ ZK n-4

t. . - -. S*O1^ 4**OS WES 3*50 S 5*005 ;*50S 3*00 S '+SQS 1*00 S 0*50 S MD >50 H 1*00 N 1*50 N 2*00 N 2+50 N L. t. -ri

Line 200 W

Pole-Dipole Array a na a

1 — ®n r®-.Filter 1 i j

, , , \ ; ' a - 25.0 w* 4 * 4 ô'

ptot point

Contours • l - 5 ' 2' 3' 5' 7- 5 ' 1 0 --

INTERPRETATION

H Strorc increase in polarization accompanied by marked decrease in resistivity .

t3 Well defined increase in polarization without marked resistivity decrease

d Poorly aefined polarization increase with no resistivity signature.

V Lo* resistivity feature .

Scale 1 ;250025 0 25 50 ?5 100 125 150

(metres.)


BELANGER GRIDINDUCED POLARAZATION

Date: 96/11/11 Interpretation: O.PATRIE and B.PATRIE


FM RES XM 0.18- 21K n 12

l

J

l0.088 11K-) 6.

1

J

1Qj oj 0.

Metal FactorFilter

a-2

n-3

11=4 0

Resistivity

11=3

chorgeabil tymV/V Flller

n-4

/\ -^ /*\ 1 ^rr^^^

^*-^\ ~"^*"" — ̂ — ̂ *^^ **' ^^. ' ^x^

4+50 S 4+CO S 5+50 S 5*00 S 2+50 S 2*00 S 1+50 S 1*00 S 0+50 S

0.11 0.090 0.10 0.090 0.040 0.060 0.050 0,090 0.050 0.070 0.050 0.060 0.080 0.050 0.14 0.11 0.1) 0.10

Q. ID 0.050 5.18 O.Offl 0.040 0.050 0-050 3.060 0-040 0-060 0.050 Q. ODD Q. 070 0.040 0 17 Q. 10 O.OBO 0.091

0.19 0.070 0.050 0.13 0.16 0.020 0.050 C OSO 0.10 O.C60 0.050 0.050 0.050 0.050 0.030 0.16 O.OSO 0.10

020 0 15 0-10 0.040 -O.H 0,040 0030 0-030 0.050 0.13 0.040 0.070 0.040 D. 040 0.040 0.030 0.19 0.11 0.1

4+50 S 4*00 5 3*50 S 3*00 S 2+50 S 2*00 S 1+50 S 1+OQ S 0+50 S

6197 4607 3973 6217 15K 12* 14X 3X9 1 1K WH 12K UK 10K 14* 9203 10K 9197 67(6

4255 ^ 1324 v 5441 y. W -, 5269 9569 -^5™ v^-IS ** 5J42j vi* 6481 ^JJW . 11K -^ 2102 -8295 5685^^4467 -

2409 (^9081" \ 1390 A/ l* ^- 'W ^^ UM ["iS^"1^ J968 \Vl3K ^ S6S7 I4K 8613 _ 9783 C 1 8K \\2US\\ 11K !1K\ 3789

1518 V 3B50\ 9058 "C 1811 — 41 JT J J2K \s 1QK 1 21K yS "4266 ~N IS "K ^ ~~— 14K I2K\ 1* -^1435 \\ IW^) 7924 \

OK ^ 2049 3H4 r'uKrv^ t273 ^'19*^- 32*^" I4K —— H" -^ 406C ^ '2K 10K ^ !9K 14K 12K 'l4K ̂ 31B ;s^- 1ZK ^- 5948

4*50 S 4*00 S 5*50 S 5*00 S 2+50 S 2*00 S 1+50 S 1+00 S 0+50 S

\l\\C /—s ( — \ f ^

\ \ \ \ V ^—— * \ \ \

XM RES FM———— , —— , —— , —— , —— , ———— , —— , —— , —— , ———— , ———— , —— , —— , —— , —— , —— , —— 12 r21K .0.18

~^**jft^J \ , ^^ . . .6 |.11K .0.086s ^ " " ""-v ----- s * i i[ 1

0+00 0*50N 1*CON U50N 2*00 N MMnl F^f + ^r

0.10 G.070 0.16 0.080 0.080 0.060 O.C70 0,060 0,10 0.11 d. 2 Filter

0.13 c.oeo a M O.DS O.CBO 0,020 o.ow O.OBO 0.12 0.12 o. M 71=10 10 0.060 0.14 0.040 0.050 0,050 0.070 Q 060 D.15 0.10 r^2

0080 Q.090 O.OJO 0.13 0.030 0.080 0.050 0.070 O.OM 0.15 n-3

0.080 0.060 0.040 0.29 0.040 0 080 3.060 0.070 0 070 n^4

0+00 ( 0+50 N 1*00 N '+50N 2*00 N RAQistivHv

7572 'JK 9908 1* 18K 19(1 14K 15K 12K 10K 9014 Filter ^L.

7407 N. 12K^^,17W ^^..2* ' "K ^ 2W l '* \W \93* 3735 MIS 0 =1

\ 7944 16K^S 4743 \\2JK J2K IK l* \ 17K\ 8576 1* n-2

4111 -\ XJOK ( 5 1K \\ 5127 \ [ 37K \ 16K 16K -j 13K \ 17K \ 7 405 r^3

i3SS'l 17K 2R^ 273D ^-31K ^- 1W— ~"^14K 12R 12K r^4

OfOO r 0+MN : . 1+CON f . 1+50 N , 2*00 N , rh n rn nnhjlifw

"^\ \ V

\ i ^\ ^^

Line 300 W

Pole-Dipole Array3 na a

' — ®n r®-iFiitpr 1 i 1

* * \ ' t . , \ - ' a ~ Z5 ' 0 h-

plot point

Logarithmic, 2 3

INTERPRETATION

B Strong increase in polarization accompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease ,

O Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature.

Scale 1:250025 0 25 50 75 100 125 150

(metres)



Date: 96/11/11 interpretation: D.PATRIE and B.PATRIE

DAN PATRIE EXPLORATION LTD.Geoson Software ro r f ne Eartn Sciences

FM RES XM XM RES FM 0.30. 29K n 18 ———— , —— , —————— , ———— , —— , ————————— , —— , ——————————— r—, ———— ,——,--, —— , ———— , —— , —— , ———— , —— , —— , ———— , ———— , —————— , —— [—1 —— , —— r—, —— ,— -..-18 r29K .0.30

\^ /f^^^~^^ \

~~^- /*\. /̂ *^~~~~ /' ^0.15. UK.) 9. ^v^ \ '^^'^^^"^^ ' ^~^ - -- - '9 r- UK - 0 ' 15

Mptril FT-tor 4*OOS 3+505 3KD S 2*505 2+005 1*505 p 1*005 0*505 t 0*00 ) 0*50 N 1*00 N 1+50 N Mptnl FnrtnrFilter 0 030 0.050 0.060 0.11 0 (MO O.OBO 0.060 0.10 0.090 0.060 0.14 0-10 0.12 010 0.19 0.16 0.13 011 0.27 0.15 0.12 012 0.15 0.11 Rlter

nil 0.050 0.050 0.23 O.OSO 0.15 0060 0.17 0.17 0.12 0.28 0.090 0.16 0.11 0.37 0.21 0.16 0.17 0.62 5.10 0.080 0,080 0.19 0.10 0=1

ns2 0.020 0.030 0.15 0.040 0.030 0090 0.060 0.11 0.040 0.070 0.13 0090 0.070 0.11 0.20 0.19 0.10 0.10 0.30 0090 0.080 0.13 0.14 0=2

[1=3 0.030 0.0100 0 '5 0.020 0.040 0.020 0.11 0.070 0.040 0.030 0.060 0.20 0.080 0.090 0.090 0.16 O.IO 0.080 0080 D 24 0.11 0.16 0.11 n*O

n-4 5 .050 0030 0.060 3.030 0020 0.030 0.030 0.14 0030 0.030 0.030 0.080 0.16 012 0.060 0.11 0.12 0.080 0.080 0.10 0.27 017 0.12 n^4

Resistivity 'HOOS 3+50S 3*00 S 2*50 S 2+OOS . 1*505 i 1*pOS 0*50 S ; 0*00 | 0+50 \ 1*OON '*50N Resistivity, L Fj|[ er 26K XX IK 1" 1* IX 12K 8007 UK UK B073 7t33 7315 8723 6876 8186 98*3 UK 9015 1* 11K 1ZK IOK !2K filter AU Uhm — m vnm~m

n -\ 1 4K —— . 14*^,. 3157 ,- 9083 ^27!l v 9748 -. 2513 3287 — 2610 ,^^1M9 -j 4754 4958 - 752B x2679 5242 8148 7J8! -^^61^ 333 10K UK . 8921, UK n-1

n s2 39* 'X.2IK'/. 5265 ÎTK —— "TS -O 5787 V 9663 x 3741 //IMI^C 8432 -*. 3482 5786 f m\ 7514 5369 7565 -/l'* 1*\. 666s' \ 13K 14K 12K 1IK [1=2 ^1 \ \fa///^' ~^ s^^ *^ "vJlV/ 1 ^\\\\ \ \ V | --^ / S \XJ \

n^3 22K X 40K//; 3944 Y/ 331 X 21K 24K \V 5059 8650 —— IK 1 22K \x 9223 V 2579 \ 8788 — 9858 —— 10* 74Z2 f I 2K I2K 13K \ 7383 \ 13K 9949 i2K n -3^^JMff^jiin \ ^ \V\U- ^ f - _ —l i \\\\\ \ ^- y \ l V-\f^Jn s4 13K 20K — 7626 -*~' 18K v 37K^- 23K 20K ^^ 4478 ' ' 20K ~~ 'SK s 26K vN 8461 *373 6780 ' 12K 9479 8731 15K 13K '3K ^ 7456 9834 1IK 0=4

rhnrônhiltv 4*005 3+505 . 3-305 Z*W 5 i 2WS | 1*50 S ( 1*005 : 0*505 t 0*00 | 0+50 N 1+OON | 1*50 N i rhnrgpnhilih/, Filter 6 6 1 6.7 7 6 5.6 5.9 b-2 5.7 5.2 5.4 5.6 7.8 8.4 9.8 11 '2 12 16 14 13 13 16 14 niter mV /y

nil 6.5 77 7.2 4.7 43 -, 5.6 \4 2 ^5.6 x 3 4.2 41 8.8 79 9.8 11 O 13- -22 x x!6 6.1 9.3 y 17 i 13 0=1\ ^ \ \ ^- ———— ̂ 1 \ \ \ ' \ ^——————' /

n = 2 62 5.8 7.6 6.7 48 ___ 49 5.9 X 4. 3 \58 5.6\ 4.4 J 6 86 8.4 11 t5 11 13 v ^0 \ M 12 , 16 16 0 = 2

n s3 5.8 5.8 5.9 7.1 7.3 5.8 5.5 6.4\4.4\ 6.7 5.5 57 6.9 9.3 8.9 J 12 '2 10 __ -îN '5 ^"~ 15 — " 16 -^"li" 0=3

1

Line 400 W


—— OH r-OnFiHfir 1 1 1

* x , '

\ / ' 0 = 25.0 M

* * * * ^ 4plot point

Logarithmic ,Oontours

INTERPRETATION

H Strong increase in polarization accompanied by marked decrease in resistivity.

Q Well defined increase in polarization without marked resistivity decrease.

d Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature .

Scale 1:250025 0 25 50 75 100 125 ISO

(metres)



Date: 96/11/11 Interpretation: Q.PATRIE and B.PATRiE

DAN PATRIE EXPLORATION LW.Geosoft Software fir the Earth Sciences

FM KES 0.44,, 31K-

0.22j -6KJ 17.

XM RES FM .33 3 1K ..0.4'

.D LO uO

2+WS 2*OOS I+50S 1+OOS 2*50 N 3+00 N

0.030 Q.OSO O.MO D.ftW 0.11 0,080 0.080 0.060 0.080 0.13 0.15 D. 21 0.2J D.J6 0-18 Q.U 0 35 0.2* 040 0.32 O. 0.33 D.24 0.23 0.29 0.26 0.15 0.11 Filter

0.11 O 040 O.OBO 0.15 0.040 0.060 3.050 3.1! 0.12 0.080 0.050 O 51 O 54 0.47 0.13 0.25 O.il 0.31 0.77 D.J4 0.87 O.tt 0.41 O.ZO O 12 0.16 O JB O.J1 0.090 O 090 n =]

0.040 Q.070 D.0100 0.040 0.14 O 040 0.060 0.050 3.10 0.14 0.070 O.Z1 Q.29 O ZZ O.SB 0.15 0.21 0.17 j.2* O.M O.Z7 0.41 0.32 0.56 fl.tB B.H Q.Z9 Q 35 0.20 O 070 n^2

0.030 0,040 0.0100 0,050 0.23 0.050 0,050 0.040 0.13 0,15 O.Z5 O, W 0,12 O.M 0.60 o.Jt 0.14 2.14 0.16 Q.S 0.16 0.26 O.J7 O.U 0,20 0,20 O,ffi 0.23 0.16 r^3

0.020 C.020 3,040 0.0100 O.OM 3.22 0.0*0 0.040 D.060 0.17 Q.IB 0.17 0.1* Q 10 0.2S O.M 0.12 O.U D.M C.20 3 0.10 D.29 0.36 O 82 O Z! Q.19 Q H 0 .2Z ^ 4

1*00 5 . 0*50 5 0 N 2*00 N

28K IK ZSK 22V IX 14K UK IX MK

4505 -^ 17K~^ 43*4 225* -o^. !8K -UK 1*K

teM 42W 4W JE20 J7SS JK6

. 2B7J — 2084

JOK 41K 2* '

'

— 31M

SJW . 8 7?"^- S6IJ- \MOK \

3656 JM6 245*

1303 — 1137 -^53^ —— -^S^~3009 — XU5 ^JW — 121^,

f ~~ 5004 — 4773 J2Sfi N-^4217 -- 21ZB X 693B M96 6201 '

207S 3114 3916 7671 13K 12K KK 12K 21K Z4K Fi|nn

4786 9to4 15*-^, UK 8583 UK , 22K 22K n-^\\,'^\v \ \ir-att V '* ̂ 1* \ 9MO "^ ™ 3* n-

X 1017 \ I7B *OB1 \ 14* -. 1* 8746 l I 2K \ !2K 0=\ \ x^^v^ — \ i \11S \ 207B ^ J734 J7W ^ 12( 1* ^ 92*6 14K n^

'84! (MzY X~

i*cos 0*50 s

h si 4.9 5.9 x 1.4 3.3 ^ 7 I S J 7.3 72 5.8

1=2 5.5 5.5 6.3 \ J.Z 3.7 \ 7 7 71 i 6.4 7.8

1=3 6.7 5.8 5.9 6.6 \ 3.5 55 79 S Z 59 7.1

1=4 6.; 6.8 7 5 7^-4.1 4 Z 7 Z 58 5.7 7.6

7 73 87 9 B 7 Z 7 6.7 6 5.5 *.9 5.J 5.3 9,5 '6 M 23 Z* ZB 30 26 2* niter

5.2 5.5 7.9 9 - Z.8 5.! 5.1 ^* 1 1.6 * .53 5 7 ^ 14 19 19___. IB __ 17 , JZ 33

S 7.2 9.6 3.) 4.6 J) 6.4 6.2 5.3'——- *! 4fi' 65 MB \ 14 20 B --— 26 27 29

10 11 x 5 6 7 6 s' 9 6' 5 5 2 5 4 -—J 3 * 3 \ u \ a f 27 H f~^\ 29B 7.S 67 5 x G.flO 53 6.1 ^ H \ ZJ - 26 ft ZZ^-

14^ 19 n*1

n=2

chargeabilitymV/V

t Scftwvrtt for i"ê

Filter

Line 500 W

Pole-Dipole Array

plot point

INTERPRETATION

* Strong increase in polarizationaccompanied by marked decrease in resistivity.

Q Well defined increase in polarization without marked resistivity decrease.

Q Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature,

Scale 1:25000 25 50 75 1 00 1 25 1 50



Date: 96/11/11 interpretation: D.PATRIE and B.PATRIE

DAN PAJRIE EXPLORATION LTD.

FM RES XM XM RES FM

0.42- 15K-) 12. ' ————— s /-"' "^ f ^^"^ \ J ̂ ^ - 12 I-' 5K -0 ' 42

i T^\ — "~" -^ "" ^— -

M^tnl Fnrtnr , 3*X S , 2+50 S. , 2+00 S ( . t+50 S , 1+QOS . (WO S . MX) . 0*50 N , HOD N . 1+50 N , 2+00 N ] Z+50N 3+00 N ( M^ql pnrfnr

Filter 0 0* 0' 040 i1 - 030 0- OJO O Q3Q C' ()W -0-0100 O.OW 0.12 0.*3 0.49 0.55 0.4? 0. 30 0.64 0.40 0.52 0.76 0.64 0 54 0.55 0.26 0.26 0.23 0.25 0.14 0.16 Filter

na1 0.040 0.050 0.040 Q.050 0.040 O.WC 0.060 0.070 0.070 0-78 0.72 1.3 0.88 0.17 1.1 0.27 0.36 0.93 1-00 0.64 0 67 Q. 17 0.19 0.12 0.24 0.070 r^1

11=2 0 .050 0.040 0,030 0.020 0.030 0.050 0.050 0.050 3,34 0,72 0,50 0.46 0,14 0.82 0.36 0.30 O.SO 0.72 0.53 11 0.28 0.26 0.18 0.2S G.tJ 0.11 n=2

1-1=3 0.040 0,030 0.020 0.020 0.040 O.Q50 0,040 0.29 0.40 0.37 0.23 0.060 0.58 0.27 0.30 0.79 0,66 0,30 0.66 0.28 0.33 0.17 0.37 0 15 0,19 C. 13 n^3

Pocjjî-Jvi + y 5*® s 2*50 S 24a) 5 1*5Q S 1 4QO S ^ S (W30 : 0*50 N )4CQ N H50 N 2+00 N 2+50 N 3+00 N R Activityn . filter W "'W 24K 2TY. 2* KK IfiK 15K 9810 1230 173B 2466 29Z1 3379 1991 J301 1247 2666 32*4 i6H XX 6 732 6614 7568 7*51 !SK 14K niter p,h

0=1 1W ; UK I4K ——— J4K 15K ^2IK ^ UK 1* 14X^x945—^59 462^^^,588 ^— Z127 v- (SJ7 , , J429 3496 2405 Z21J- J07E 598 .lOK^ 7258 7974- 5425^ tBK n^1

^=2 I4K x IW^^" 74H ^-^ 32K-. 20K X !3K x-ÎSK __ 1* V/1 IM2 655-^ TJlBJ^ 14B3 -^^STra i') 947^/2503 1544 J 2053 2613 5099 j 20ZD 6115 6835 8301/3614 A/1* L 2QK n=2

ns3 17K/^ 27K ' 44K 3K l 14K J 22K Z2K /y l4sT ^740 r 1 755 ^ 2666 /72D4 J 1418 y 3238 J706 .x 2422 2612 4918 2760 ^ M70 4111 ' 9J67 f 4032 /s 1 3K 12R^^- 16K r^3

0=4 26K ^ J9K 42K ^ 19K 19* 2W ^-^1714 849 - 1696 2793 "^ 1* ^ 1798 - J825 *J78 ^14fi v 2733 4430 209J ^ 5271 M45 4717 — 4135 " I'K 11K x — 9382 141; r^4

--hnrqpnhi ty 5+005 2+50 S 2+00 S UK S 1+005 0+50 S 0+00 0+50 N 1+00 N 1+50 N 2+00 N 2+50 N 3+00 N rnnrnprîl'ty

t ^ ^ ~ ~ — ' ^^ \ -^ 7 v/ ^ ^-^" \ f ^ ^^— -^ ^X

f '^ / 1 S \ /^ ——— ̂ ] X --- ——— v. J -- ——— -~-^ Jx-^

Line 600 W


1 — OH r-®-,Flltpr 1 1 1

plot point

^-1,1.5,2,3,5.7.5,10,..

INTERPRETATION

B Strong increase in polarization accompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease.

n Poorly defined polarization increase with no resistivity signature.


Scale 1:250025 0 25 50 75 100 125 150

(metres)

CANADIAN ZEOUTEINDUCED POLARIZATION SURVEY

BELANGER GRID INDUCED POLARAZATiON


DAN PATRIE EXPLORATION LTD.Geosott software for the Earth Sciences

FM RES XM

0.32. Hid 9.7. ' \ -̂-^"~~~-~. , _ ^^^^ ^ -- - -\ ^- ^^--••""""N s^ ^~~~~ ———— ———— — ' ^ —— — *""\ ——— *- *— x*

H| 0' fi l l i 1 1 1 [ 1 t l l 1 i 1 1 : t l l l i 1 i 1 1 1 l i . i l 1 i 1 1 1 l l l

MptH pqr-tnr 1 t5" s ; tais Ot50 s , O"100 î* N , ''f0 N . ' t50 N , 2KC N 2t5c N J*?0 NFilter 0.34 0.56 0.59 0.19 0.15 O.H 0,13 0.19 0.27 0.30 0.31 0.15 0.10 0.060 0.050 0.050 0.070 u.380 0.080 0.080 0.070

0=1 1.X 0.57 0.92 0.20 0.17 0.050 0.040 0.050 0-11 018 0.31 0.060 0.050 0.030 0.040 0.030 0.050 0.080 0.10 0.090

0 = 2 029 14 0.25 0.10 0.19 0.070 0.050 0.20 Q. 24 0.39 0.22 0,080 0.050 0.040 0.030 O.C40 0.10 0.080 0.10 0.060

0=3 045 0.32 0.14 0.14 0.17 0.11 0.21 034 0.38 0.23 0.22 0.080 0.070 0.030 D. 040 0.080 0.080 0.080 0.060 0.070

0=4 0.20 0.19 0.21 0.13 019 0.43 0.35 0.54 0.37 0.23 0.21 0.12 0.050 0.060 O.C50 5080 010 0.060 0.070 0.12

Rp^ktivity 1*50S 1 TOS tt*502 040C ^pN '-W U50N 2*CON 2t50N :MOKQ. Filter *)95 1891 4491 8840 8742 UK 13K I2K 7552 6537 5560 9619 12K I7K 20K 21K 12K 97S5 9605 S976 12K

n-1 4568 4375 -, 1198 , 7799 6197 \ ISK 20K 20K -* I K -, 9209 4963 . y 1* 1* l 21* —— - 2W 24* , 121. S643 7618 8401

///A /////X —— \\ Y\ \ / ^"^ S X l \ \ \ X A~^ -, ' ' '0=2 *407 •rrJB '1 7875 13K \ 7268 \ !4K W/ 6381 — 74!E 4792 6755 NJ2K 15K ~^ 19K f 33* l m iiX 9 799 8024^ 1 1K

0=3 l ]X y 5285 U2K UK. t\X •*^X^' 75B7 5502 " 4530 7039 6393 \12K 12X ( 31K X m/ HK^~"!a 9841 '3K t K

0=4 5566 7116 8508^ UK 7743 "" 4512 4786 3451 6213 6102 6299 - 9193 -M9K —— 15* !2K :IK' 7872 ' I3K 12* 9439

^hqrnprihility K50 S -*00 S ^^ S 0*® ^X N HOO N ( i-50N 2*00 N 2+50 N 3*00 Nv ,v Filter 'l " '4 16 14 13 12 14 17 18 16 12 9,4 6.3 8.5 8.3 7.6 3.1 7.9 7.8 7.9

0 = 2 '3 —— :3 ^20 \ 13 14 9.8 ——— 10 y 16 18 19 15 9.1 7.1 7.4 8.8 6.5 8 7.5 77 6.3

0=3 5 \ 17 16 ^~ 15 14 13^,^16 :9 17 17 J 1 4 9.9 8.9 8.8 8.2 9.3 8.! 8.3 7.2 8 ^ V. _ ^ ***^ ^ —— ~ f ~^---^^ ^ — X s

0=4 11 H IB 14 15 20 17 W ^ 25 ^ 1 4 13 11 ~ 10 8.3 11 x 9.3 7.7 73 9 ^ 12

XM RES FM-19 p23K .0.65

l

.9.7 j.11 K .0.32

1

.0 Lo LO

Metal FactorFilter

11=10=2

0=3

n-4

ResistivityFilter Ohm-m

n=•\ n-2

0=4

chargeabilityFilter mvyy

0=2

0=3

0=4

Line 700 W

Pcle-Dipole Array

1 —— CD-; r®-iFilter 1 1 i

* \ ' '

,**** "\ / '' a = 25 - 0 M* * * * ^

plot point

Logarithmic , . , , - s ? , Contours ]' ' ' b ' ^ ^ 5' 7' 5 ' 1 0 '"

INTERPRETATION* Strong increase in polarization

accompanied by marked decrease in resistivity.

D Weli defined increase in polarization without marked resistivity decrease .

Q Poorly defined polarization increase with no resistivity signature .

T Law resistivity feature .

Scale 1:250025 0 25 50 75 100 125 150

(m e; res)



Date: 96/11/10 Interpretation: D.FATRIEand B.PATRIE

DAN PATRIE EXPLORATION LW.Geosoft Software for tne fcarth

FM RES W ™ R ES FM 0.65.. Z3K 19 ———— , ———— .——r-, ———— r——,—, ———— i i i l ———— , l l l ——————— , ————————— , ———— r— r—, , i i i i i i l i - 19 r23K -0 ' 65

0.32. PK-I 9.7. ' \ .̂^^~~"~~^ -- ^*^L ^-- ^.—— - 9 ' 7 f l1K - 0 ' 32 \ -^ •s.*-'""" N ^-^ "~~ ——— " ———— ~~-— —— - ̂ i -- —1 ^/^-—--~-~~ *-.,. i -

Mf t -i Fnr'-nr '+50S 1+OOS 0+50 S 0+00 3+50 N ( 1+00 N , 1+50 N . 2TO N | 2+50 N 3+p N M etn | Fnrtnr

Filter 0.34 0.56 3.59 0.19 0.16 0.14 0,13 0.19 0.27 0.30 0.31 0,15 0.10 0.060 0.050 0.050 0.070 C. 080 0.080 0.080 0.070 Filter

r^] OJ6 0.57 0.92 0.20 0.17 0.050 0.040 0.050 0.11 0.18 0.31 0.060 0.050 0.030 0.040 0.030 0.050 0.080 0.10 3090 0=1

n-2 0 29 14 0.25 0.10 0.19 0.070 0.050 0.20 0.24 0.39 0.22 0080 0.050 0.040 0.030 0.040 0.10 0.080 0.10 0.060 n =2

n,J 0 .45 0.32 0.14 0.14 0.17 0.11 0.21 0.34 0.38 0.23 0.22 0080 C. 070 0.030 0.040 0.080 0.080 0.080 3060 0.070 0=3

n ,,4 0.20 0.19 0.21 0.13 019 B. 43 0.35 0.54 0.37 0.23 0.21 0.12 O.C50 0.060 0090 0080 0.10 0.060 0.070 0.12 0=4

Reciotiuiry 1'f50 s ; tOOS 0tX s 04flo ^ N 1'tfloN ^x N ^ N , ^ N ^P0 N Rpqktiviivpi| ter 095 3891 4491 6840 8742 11" I3K I2K 7552 6537 5560 9619 12K I7K 20* 2IK 12K 9765 9605 9976 12K Filter Ohm-m

n=^ 4568 4375-, 1198 , 7799 6197 x I5K 20K 2Ct(^ 12^^. 9209 4963 x UK I X , 2 1* -— 2W 24K , ^ 12K . 8643 7618 8401 0=1

n-2 4407 y^83 y 7875^ 'isTV' 7268\ \ ̂IW^ 8581^7(26 4792 6755^^2* 15K -^ 19* /la) 'It! 8336 9799 1024^ UK 0=2

n^ \ W* y yat, ( l2K UK. 1190 •^^^ 7587 5502 — 4530 ' 7039 6393 \!2K 12K 1 M/ I 9K s '.\f~ ~ 1 0K 9341 ' X 1 2K 0=3

n - 4 5566 7116 850!" ^ 1IK 7743 "(512 4786 3451 6213 6102 6299- 9193 ' 19K —— 15K 12K 'K' 7872 ' 13* I2K 9439 0=4

r ^ or , an rîiitv '+50S ' -WS O*505 l*00 5*50N !1)ON , !'?ON , 21* N , 2t,MN , ^P0 *4 rhnrgpnhiliry" ' Filter 13 16 '4 'S '4 13 '2 14 17 18 16 12 9,4 5,3 i. 5 B. 3 7.6 8.1 7.9 7.8 7.9 Filter mV/V

^2 1 3 —— \ l f 2 0 \ '3 14 9.8 __ ^ s It I S 19 15 ^9,1 7,1 74 8.8 3.6 8 7.5 77 6.3 0=2

n ,3 ~^\ l 7 1 6 ^ —— t 5 H tl^'t 1 9 17 17 b 14 9.9 8.9 8.8 82 9.3 8.2 8.3 7.2 8 0=3

n^4 ; l —— H 18 14 15 20 17 18 -^""2!"^ 14 13 n^~ 10 S. 3 - 11 ^ 9.3 7.7 73 9 ^ 1 2 0=4

Line 800 W

Pole-DIpole Array

1 —— CD-1 H2HFilter i 1 i

* \ ' '

*v* \ '' a s 2 5 - 0 M* * * * ~v'

plot point

Logarithmic 1 , 5 2 3 c ? 5 , Q Contours ' ' D ' L ' ' D ' '- 0 ' i u ' ' '

INTERPRETATION

* Strong increcse in polarization accompanied by marked decrease in resistivity.

O VVell defined increase in polarization without markea resistivity aecrease



Scaie 1:250025 0 25 50 75 100 125 150

(metres)




DAN PATRIE EXPLORATION LTD.Geosoft 5o?t*o r- 'or [he Eartn S ciences

FM RES XM XM RES FM0.28-, 24^ 21 —— , ———— , ——————— , —— , —— , —— , —— , —— , —— | ———— , —— , —— , —— , —— , —— , ———— , —— , —— , ———— , —— , —— , —— , —— , —— , —— , ———— , —— , —— , —————— , —— , —— , —— , —— , —— , —— , —— -21 J.24K r0.28

"^^"^^^ ̂ --"'' "**. /^\ ,S*\. "" 1

UpfQJ Factor , '^S 'f15 , , ^r* 5 , "f0 , *P K UfCN , 1*?0 N , 2fON , 2^ N , 31MN , 3l fiON , M otnl FnrtnrFilter 0-'8 D'U 0- 090 O' 090 0- 090 0- 1 ' 0' 13 0- 16 0- 13 0 l()S) 0- [190 0- ow 0- 16 0 lOW 0- 080 0- 070 0- c80 D lt)eD 0 lOW 0- 13 D ils O l ' 9 0- 25 Filter

0=1 0.12 0.11 0070 0.070 010 0.13 0.22 0.15 0090 0.17 0.060 037 0.080 0.090 0050 0 MO 0.080 0.060 0.12 0.13 0.16 0.28 11=1

0 = 2 0.17 0.060 0.060 0.080 0.090 0.10 0 18 0.17 0 11 0.050 0.070 0.090 0.19 0.050 D.OfiO 0.060 0.090 0050 0.10 0.17 0.22 0.24 0=2

0=3 0.23 0.10 0.050 0.090 0.12 010 0.11 015 0.13 0080 0030 0.070 0.060 0.090 0.040 0.090 0080 0.080 3060 013 0.20 0.19 n-3

0=4 0.36 0.18 0.090 0.070 0.16 0.15 0.12 0.13 0.15 0 12 0.060 0040 0050 0.050 0.11 0.060 0 12 0.070 O.OM 0.10 0.12 0 18 11=4

Revstivjty 1*505 1*00 S 0*505 0*00 0+50 K 1 *00 N 1+50 N | 2*00 N Z+50 N 3*00 N 3+50 N Resistivity

n Filter 12* "* "* 'Z*5 "K "* m "K '* "* 1 9K '" 9339 '* 2 :K Z* 1 9K '* m ixl S 1" ss25 39g* Filter Oh

0=1 5446 —.4SB 7695 14* UK IOK 5011 779T/ UK — 6111 , l* s^- 3042 ^s 26K 22K 23K m , U K 12* f 7240 5571 7124 , 2432 0=1

0=2 983l""^ I3K\ 6S54 ^ 9615 15* 12* L 8631 10* 14*' f 24K^~~- 16* 13K\X 38J2 XV SIK^X 25K 21K 15* IK \ 9668 , 55(2 (^4530 4091 n*2

n ^3 t o* f l* 16* \ 6614 S514 15* 1t*\-976f 15* ' MK ( 45* N^ 14* I 4"\\ "78 \\ 5*/ 2 1K 'K m '* ) ™ xlt 6 1 " 0=3

0=4 4907 1 14K 17K 13K- ^ 5155 TW 1 2* 10* 12* N 17* ' 29K 31K ^"" 13* I2K -^ 4078 -- 26K ' 16* 17* 14K IOK ' 6373 7216 0=4

^ hqr:rnh ;i K, 1+50S 1+OOS | 0+KS 0+00 , OS N 1*00 N ; 1*50 N 2+OOK ; 2*S)N ; 3*00 N ; 3*M N p r-hnrrjpnî iKr-ii is 13 8.9 7.7 10 12 14 16 15 14 12 11 9 13 15 14 14 12 10 99 9.5 11 9.1 Filter ,-v A;mV/v .TIV/V

n -9 i7 X76 \ 4 ' 75 f 13 12 16 17 ^*"* 15 12 11 12 ( ~l-l~~~~--. ' 6 19 X 13 14 95 '0 — --9.6 ^ _ -10 9.9 0 = 2 •- \ \ ^ J \ \ ^sxv J ^~~ *\ \ \ V

0 = 3 23 \ 17. \ 7.7 61 10 14 12 '5 19 17 N^ '3 10 — '8.8 pu \ 15 19 Nu 14 9.2 ) 10 12 12 0 = 3 \\'x. \ 1 X/ l\\\ V ^ 1-^-' "-N.

0=4 17 25 x 16 9.6 3.! V 12 14 14 ' 17 20 17 N 12 ' 7.2 6.2' 4.7 x 16 19 x 12 13 99 7.6 x 13 0 = 4

Line 900 W

Pole-L-':;o!e Arraya na a

^ —— Q^ H2HFilter i I i

* x\ * * v\ ' tt4 \^ ^' 0 = 25.0^1

plot point

Logarithmic . 1 r * 7 c, 7 c in

INTERPRETATION

' Strong increase in polarization accompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease.

O Poorly defined polarization increase with no resistivity signature.

1 T Low resistivity feature .

Scale ":250025 0 25 50 75 100 125 150

(metres)



Date: 96/11/1 1 Interpretation: D. PATRIE and B.PATRiE

DAN PATRIE EXPLORATION LTD.Geosort ^cftHare for :ne tartn sciences

FM 3:5 XM

^———— - -^^^^^^

J ^

n , n | n i i i i i i i i i i , i i i i i i i i i i i i i i i i i ; i i i i i i i i i i t

Filter 0.10 0.090 0.090 0.10 0.090 0.080 0.060 0.07D 0.050 0.060 0.080 0.090 0.090 0.13 0.10 0.0/0 0.090 0.090 0.15 0.11 0.060

0=1 0.10 0.080 0.10 0.12 0.080 0.070 0,050 0.090 0040 0.040 0.070 0.090 0.090 0.17 0.090 0.030 0,10 0,040 0.26 0,22

0 = 2 011 0.070 0.10 0,090 0.090 0.060 0.050 0.030 0.060 0.050 0.070 0070 0.11 O.IS O.C60 0.060 0.060 018 0.14 C. 040

0 = 3 0.090 0.080 0070 0.10 0.080 0.070 0,030 0,050 0.080 0.070 0.070 0.10 0.13 010 0.090 0.050 0.23 0.090 0.040 0.050

0 = 4 0.12 0.080 0.11 0.10 014 C. 040 0.050 0.10 0.13 0.060 0.11 0.15 0.080 0.16 1 .070 0.13 0.020 0.040 0.040 0,14

Resistivity 1+505 1+00 S 0+50 S 0+00 t 1*50 N 1+00 N K50 H 2*00 N 2*50 N 3*00 N^. F i'tpr 12K 13K 12K UK 12K '2K I5K 16K 18K 19K 15K 16K 16K UK 13K 18K UK 11K 5595 7844 I3K(JnnH-m

0=1 I2K I2K 10K 8496 13K UK 12K - 7535 - 1JK x^25K j UK ___ 14K 17K , 9165 12K , 26K 9010 '-^^ "72 1 880

0 = 2 12K 15K UK 11K 12K 13K 16K ^~~* 22K ^\ 17K 17K 17K S 22K/ 13K f 8 707 | ^̂ /W^^]WJy- 3503 — 2950 '/UK

0=3 15K 13K I4K IOK 12K '3K f 29K 23K j I2K NlBK *C 21K -""^ 14K 9995 '4K —— 15K I9K J j 3272 4945 'j'-'l*/ m

0=4 11K 13K 9839 9198 T309 ' 23K 25K ' " K X^9088 \ 1BK - IZK -^ 8530 I6K 9319 15K -îOT 3732 ' 12K ' 21K '?033

^ hnrc-jpnbi ; tv 1+50S 1+OOS 0+50S ( 0+00 Ch-50 N 1+00 N : 1 +50 N ( 2+00 N f 2+50 N 3+00 N

, Filter 12 11 H 10 '0 9.1 8.4 86 8.4 11 11 13 14 14 12 " 9.3 7 5.2 5.1 6.6

0=1 12 -^.8.9 9.9 10 - 9.9 S.I 64 6.9 5.2 10 96 12 15 16y 11 ^-^35 9,2 7.7 4.6 42

0 = 2 13 H 10 l 9.8 ( 10 7.6 84 6.8 9.8 94/ 12 1 1 6 15 14 '3 10 8.4 6.2 ) 4 *9

0=3 14 11 1C 10 9.6 9.6 8.1 S 1 1 \**/ '2 1*^—15 13 14 14 j 8.9 7.6^X4.3 4.4 9.2

0=4 14 11 10 ' 9.4 10 8.3 -12 11 12 12 13 13 12 '5 11 ^ 84 ^064 5 8 10

KM RES FM 16 .-21K ..0.17

L

7.9 LICK .0.083

0 LO .0

Metal FactorFilter

0=1

0=2

0=3

0=4

Resistivity ™ er Ohm-rn

0=1

0=2

0=3

0=4

chargeabilityFilter mvyv

0=1

0=2

0=3

0=4

Line 1000 W

Pole-Dfpole Arraya na a

1 — (D-| r®nFilter 1 1 i

* ^ \ x

\N ,''' 0 = 25,0 M

plot point

Logarithmic , i s 2 "5 S 7 S in Contours ' ' ' ' ' ' ' ' '

INTERPRETATION

* Strong increase in polarization accompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease

d Poorly cefined polarization increase with no resistivity signature .

T Lew resistivity feature .

Scale 1:250025 0 25 50 75 100 125 150

(metres)



Date: 96/11/11 interpretation: D. PATRIE and B. PATRIE

DAN PATRIE EXPLORATION LW.

FM RES XM 0.24.. 25K, 12

1

10.12. 13KJ 5.8.

1

J

0. Oj 0-

"~ ——— — ̂ s \ '' ^^C^^^^^~ ^^ "\ ^~..~ W^ -X"-"--" \

. — ' ^— ——— ___ S \-

1*00 S 0*50 S 0*00 0*50 N 1*00 N c 1*50 N 2*00 N 2*50 N 3*00 N 3*50 N

Hiter 0.040 0.050 0.050 0.050 0.050 0.060 0.090 0.080 0.090 0.10 0.20 0.22 0.13 0.10 0.070 0.070 0.080 0.090 0.10 0.13 O.ffi

n -1 0.060 0.050 0.050 0.070 0.070 0.090 0.030 0.10 0.14 0.46 3.42 0.11 0.080 0.030 0-060 0070 011 0.18 O.Z8 0.06

n -2 0 .050 0.050 3.040 0.070 0.040 0.050 0.080 0.060 0.090 3.12 0.20 0.24 0.080 0.080 0-050 0.050 0.11 0.14 3.080 0.050

0=3 00*0 0.040 0.0* 0.060 0.050 0.030 0.050 0.19 0.060 3.060 0.080 0.16 0.14 0.080 0.10 0.050 3070 0.090 0.080 0.020

0=4 0.060 0040 0.040 0070 0.040 0.050 0.040 3.11 0.21 0.060 0.050 C. 12 0.17 0.18 010 D. 12 0.070 0.060 0.080 0.020

Pocjstjv/it" '^ S 0*50S O*00 O*501* "OON '*KN MON i 2*50 ' 1 3 tOON 3f50N

Ohm-m ™er

0-1

0=2

0 = 4

cnargeability mV/V niter

0=1

0=3

0 = 4

tTK I7K I6K 141 141 14K UK 17K UK 9789 7312 SIM 5830 5612 "* -K MI I2K 15* I7K 23K

1* ———^—^ "* 13* 'OK 7450 \OOIC i 9561 5782 , HK1 2655 4090 tffl ^"X , 1 OK .^5300 6072 4394 2482-9040

I8K 19K :7K 11K ( 20K ^13JTV 9333N \I9K \ 82J8 6453 6564^~- 4458 -^ 5495 SJjOv 14K 13K \.7!65 6027 r I IK^: W

17K 20K 2IK 1 1 2K 14*^ 20K 14K\ "5295^'" '* ——— '". 83CB 6799 6988 5770\ 5T) '3K ;1K' —— 11K //SK x "^-——-^ 1 \ \ 1 7 Vv "" 1 s^ A S/ f

3K ^ I7K 19* I4K 13K til v !9K N 8665 5075 I5K 12K ' !39I ^ 5792 6021 7349 5875 -- 'W 15* I4K ' ' 46K

IXWS ^50 S 0*00 0*50 N '*OON i*5C N 2*05 N 2*50 N 3*00 N 3*50 N

7.5 8.2 7.! 7 7.3 7.1 7.7 9.1 9-2 J.I 10 11 7.7 5.9 6.9 ' : ' .9 8.5 9.1 8.S 75

56 62 68 88 78 68 77 33 8.2 x '4 '1 4.4 3.5 x 6.! 1.9 6 6.6 78 5.9 5.6 /""^ 1 \ \ \ -1

8.1 87 61 7.2 7.5 74 7.6 f 1 2 ] 5.4 " \ ' 3 " 1 S 4 1 ' ' 3 B' 7 8- J 8' 2 9' 2 8 !

5.1 8.4 !.8 6.8 6.3 5.1 73 ( 1 2 9.8 6.4 7.8 \ 13 ^9.6 5.5 —— ' i.i 7 .9 8.4 9.9 ^9 3 10

7 6.5 8-3 9-7 5.1 56 77 9.4 '0 x 9.3 63 10 9.9'"'" "li 7.5 69 97 9.4 V 11 '0

XM R ES FM r 12 ^25K ^0.24

l

.5.8 L'3K .0.12

l

l

.0 Lo o

Metal Factor0 Filter

0 0=1

0=2

0=3

n-4

ResistivityFilter Ohm-m

0=1

0=2

0=3

0=4

chargeabilityFilter mvyv

0=3

0=4

Line 1100 W


1 — ©H r~®~iFilter 1 1 i

* \ ' ' x s* * \ '

t t t \ / ' 0 =25.0^/1* * * * ^ '

plot point

Logarithmic, . 5 ? , , Contours '' ' l 3 ' A J' D' ' ^' l 0 "-

INTERPRETATION* Strong increase in polarization

accompanied by markea decrease in resistivity.

O Well defined increase in polarization without marked resistivity decrease



Scale 1:250025 0 25 50 75 100 125 150

i ———————————————————————————— l

(metres)



Date: 96/11/1 1 Interpretation: 0. PATRIE and B. PATRIE

DAN PATRIE EXPLORATION LW.f ft e L ar.n i c/e.ices

FM RES XM XM RES FM

0.10., 7060- 5.6. w^2*^' ]X^ — -— --, ^.-^•'^ ,'----~~. _ --- . .5.6 .7060 f.0.10

——— -- ——— "-"'"'

r, n | n t i , i i i i i i i i i i i i i i i i i i i i . i i i i i i i i i i i j D lo un

Mptn! Fnrtnr , , , ™ S . , 0+5GS , 0+00 , . 0*50 N . 1+00 N. | , 1+50 N, , 2+00 N , 2+50 N ( 3+00 N , W p f n | Fnr+nr

Filter 0,™ 0,040 0.040 0.050 0.060 0.090 0.090 0.13 0.13 0.19 0.13 0.10 0.10 0.090 0.080 0.11 0.11 0.10 0.11 Filter

0=1 0060 0040 0.030 0030 0.030 0.080 0.060 0.17 0.18 0.40 0.18 0.090 0.070 0.080 O.OBO 0.13 0.10 0.080 0=1

0 = 2 0 WO 0,040 0.040 0080 0.070 0.070 012 0.14 0.14 0.18 0.090 0.10 0.090 0.060 0.090 0.14 0.080 013 0=2

0 = 3 0.040 0.050 0040 0.080 0.070 0.15 0 11 0.12 010 0.10 O.t1 0.13 0,070 0.070 0.11 0.10 0,13 0.070 0=3

0 = 4 0.050 0,040 0.10 0.080 010 0.12 0,060 0,10 0,070 0.12 0.17 0,12 0.090 0.11 0.090 0.14 0,080 0,10 0 = 4

pAcjoti"ity UOCS t)*50S "^ 0*50 N | 1+OON 1+50 N J*00 N 2*50 N 3+00 SI P^QJ-j+JvityFilter 9K17 I2K 13K UK 9581 7064 8691 6270 7310 6364 7085 8479 8746 9491 10K 7937 8469 9295 9748 Filter Q ft

0=1 7475 13K - 16K , 14K 13K/ , 5481 t Hl, 4385 4570 2277 , 5397 10K 91B6 7944^. 9992 .5666 6947 7845 0=1

n-2 IW H* 1 4K C WI8 6590 961) ^ 5544 6247 7149^ 4655 8691 7886 9295 13K 8492 6483 IOK 7286 0=2

0=3 UK 12K C~15K ) 7122 1DK f 4875 afiT" 8262 9410^ 6939^ 7484 7373 1 14X IOK 9454 9213 3472 f 1 4K 0=3S/ } f J : 1 f *\ \ \ \ S J

0=4 UK I2K — 5802 ' IOK ' 6203 6694 S008 8925 I3K^ 5530 6018 8717 10K 7991 10* 8638 -^ 13K 8758 0=4

rhnrgonhilitw , 'f S , 5*50 S p 0+00 ( 0+50 N | . 1+OON ^ 1 +50 N , 2*00 N | 2'WN , 3*00 N rhnrrj^nhility

v ,v Filter 4,5 5.1 5.1 5.3 5.2 6 7,2 77 8.6 8.5 8.6 8.6 8.1 S. J 3.3 8.4 8.9 3.8 10 Filter mV/V

0=2 4.3 4 a! 5.7 \ 4.5 48 71 66 B. 9 97 8.3 8.1 8 8.3 8 1 .2 S . 8 8.3 9.6 0=2

0 = 3 4.2 f 5. Z 5 .4 5.4 7.1 7.3 9 9.6 9 6,7 8.3 9.6 9.4 7.4 9 9 ./It ^'-5 0=3

ns4 52 5.3 5.7 8.3 5 73 5.1 8.5 8.7 6.8 9.9 10 1 92 8.8 3.2 ^ 12 10 9 0=4

Line 1 200 W


- —— CD-i HSHFiltfir 1 i 1

*

***** X\ y a ^ 25.0 M

plot point

Logarithmic . 1^9^^7510 Contours ' ' ' ' ' ' ' ' '

INTERPRETATION

M Strong increase m polarization accompanied by marked decrease in resistivity .

U Well defined increase in polarization without marked resistivity decrease .


V Low resistivity feature .

Scale 1:250025 0 25 50 75 100 125 150r - - ——— i

(metres)



Date: 96/1 1/11 Interpretation: D.ÂTRIE and B. PATRIE

DAN PATRIE EXPLORATION LTD.Geosc!' software tor the Lcnh ~-aences

Personal informatio 1- Mining Act, the info Questions about t 933 Ramsey Lake

Instructions:

Ministry ofNorthern Developmentand M ines ,

Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.O. 1990

52N02SW0011 2.17095 KNOTT

type or prim in inK.

Transaction Number (office use)

Assessment Files Research Imaging

900

nd 66(3) of the Mining Act. Under section 8 of the it work and correspond with the mining land holder. )f Northern Development and Mines, 6th Floor,

ft* 17095m, use form 0240.

1. Recorded holder(s) (Attach a list if necessary)Name Client Number

Address Telephone Number

Re. JFax Number

Name

A.Client Number

Address Telephone Number

i/,Fax Number

2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.

r-^nXaeotechnical: prospecting, surveys,l—I assays and work under section 18 (regs) D Physical: drilling, stripping,

trenching and associated assays | | Rehabilitation

Work Type

li t ,/r J J - (rt C/tS C e- Ci f P 'fa ' 2#f7 #1

Dates Work i t, o/ -r Jc~ j, of Performed Rom f /f T& To '^ /f 7 P

Day Month Year Day Month YearGlobal Positioning System Data (if available) Township/Area /J.rrrl6 iyffiK,

f? j si ~^ n* .J k t A'/VcTZL. . U c. 1*3 fs T (i t^r T&P

M or G-Plan Numfcpr '

G. 31 (J 2- / G- /z 07

Office UseCommodity

Total S Value of 4^//^ /o^- 03 Work Claimed /O 7 /oO-

NTS Reference /r TV/ -

Mining Division A/V ^t-/^-^

Resident Geologist Q j , District f\fj[ J-ti/JL^

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)Name

Address

RECEIAddress

—————————————————————————————— ———— ;~ F B S 4Name i ^ ^

Address MINING LANDS

l PC

VED

BRANCH !

Telephone Number

Fax NumberV- 2 t /3f- ês-*

Telephone Number

Fax Number

Telephone Number

Fax Number

4. Certification by Recorded Holder or Agent

l, [Jrfn/e.1 l - _____ , do hereby certify that l have personal knowledge of the facts set(Print Name)

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.

Signature of Recorded Holders* Agent

erfi

Date

Fax Number 7Agenjj s Address

TTTelephone Number

0241 (02/96)

TEL:507 727 3553 P, 003FEB.-m?|TUE) 11:16 MINING-RECORDER--R I,

- - - . - . .VHH J-^ y|

6. Work to b* rvcardad wui attributed. Work can only be SAslgnaci to cJaJma that wt conllguoui (adjoining) to thi mining land wt*c* work ma performed, at tha Uma work was p*rterm*d. A nap ihovring tha contiguous link must accompany this form. - - .

Mining CUUn Humbw. Or H work wu don* on other •flffWo mining Unc, *how In tait caluftitt Ihe towan numb* lrxstofti*d W) th* Dl*)m nip.

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18 ha

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Column TOUto

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cblm W dhw rriJng tind.

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0

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r sr/ rvf/O T&Q '

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mining CitJlu.

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BtAk. V^y* ol work u hi tS*Mbut*4 H l tUKr* dtl*.

S 2,825

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^.,

.

-4-

, do henecy certrfy thet IM abov* work crecilU are under17 (1) ol tho Astussmeni Work Reflul

the claim where the work was done.6/96 for Malgnrnsnllo ctntljuoua claims Or far sppltoeion lo

6. Instruction* fur cutting back t k thit *ro not ipproved.

Some ol the crwJUs clahTwd In this declaration may b* cut baex, PleaM cneck. i ^ ) In tha boxw below to show htmyou wish to prioritize the deletion of cratfts;

Q"""l. CrarJlU are to be cut bseX Irorn ttw B*nk first. Wlcrwad by uprJon 2 or 3 or 4 es Indlcamd. Q 2. Credits ara to tm cut back starting with tha claims listed la! t, wortdnfl backwards; or CZK"3. Credlls ara to ba cut beck equally over an claims listed trt l his declaration; or D 4. Crftdlls ara to ba cut bask M prtorlrjzad Oft the attached 6f pendx or us teHov/s (describe):

200 'd

Note: H you haw not Indlcatwl how your oradlls era W be dueled, crwlla wll Do cut bock from the BanX first, by option number ZII n*c4*4ary.

FEB 0 4 1997 TeW

N3JI-A001039/ONINIW (3(ll)i6,8l-'83d

Ontario Ministry ofNorthern Developmentand MJtvss

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal information collected on this form is obtained under the authority of subsection 6(1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, the information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to the Chief Mining Recorder, Ministry of^lorthernDevfllQprnjejit Mines, 6th Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

Work Type

X t rt e. (-tj Iff/I at

M*o /^/-\7 r .

L IS? rtu'Ce. ci 1 0/4* 1 2* r/fr

Units of WorkDepending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

/l Jr( /n sneistLS

/l /?, in /x e. fs* e. S

/O /C t /f) SHrêf

Associated Costs (e.g. supplies, mobilization and demobilization).

Hfcr.trte- — - flt,U L A r. t; f'/i

KB 04p,**ivn

Transportation Costs ? (8|9iS)iUj1lll

1

Food and Lodging Costs

9W

R P r c i \7 c P*

Cost Per Unit of work

@. ?06

Q isoP /S 00- ' Y

'.W™* 1 ' —————i u u-i: -'•'•JiNG biv. —————————

•1997 mj^8i4i5j6.

To tal Value of Assessment Work

f ' t- 2 4 1997

Calculations of Filing Discount i^lNING LANDS BRANCH

Total Cost

3, J ' GO^ /SoS-6A l'Y/, 606

-^ ————/5} f Ô

f

1. Work filed within two years of performance is claimed at 10007o of the above Total Value of Assessment Work.2. I f work is filed after two years and up to five years after performance, it can only be claimed at 5007o of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 = Total $ value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

l, D /Pitt- f f~- , do hereby certify, that the amounts shown are as accurate as may(please print full name)

reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on

the accompanying Declaration of Work form as

to make this certification.(recorded holdej/agent, or state company position with signing authority)

l am authorized

0212 (02/96)

Signature

(cX2!~

Date

Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment OfficeApril 4, 1997 933 Ramsey Lake Road

6th Floor Sudbury, Ontario

Scott A. Rivett P3E 6B5Mining Recorder ,-,,,,-v ~ -, n mmOntario Government Building Telephone: 705 670-5853227 Howey Street, Box 324 Fax: ( 705 ' 670-5863Red Lake, ONPOV 2MO

Dear Sir or Madam: Submission Number: 2.17095

Status Subject: Transaction Number(s): W9720.00008 Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

NOTE: This correspondence may affect the status of your mining lands. Please contact the Mining Recorder to determine the available options and the status of your claims.

If you have any questions regarding this correspondence, please contact Bruce Gates by e-mail at [email protected] or by telephone at (705) 670-5856.

Yours sincerely,

ORIGINAL SIGNED BYRon C. GashinskiSenior Manager, Mining Lands SectionMines and Minerals Division

Correspondence ID: 10704

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.17095

Date Correspondence Sent: April 04, 1997 Assessor: Bruce Gates

Transaction NumberW9720. 00008

First Claim Number

1 184554

Township(s) 1 A rea(s) StatusBELANGER, LITTLE BEAR LAKE, Approval

Approval

April 04,

Date

1997KNOTT

Section:14 Geophysical IP 14 Geophysical MAG 14 Geophysical VLF

Assessment work credit has been redistributed, as outlined on the attached Distribution of Assessment Work Credit sheet, to better reflect the location of the work.

Correspondence to: Recorded Holder(s) and/or Agent(s):Mining Recorder Daniel PatrieRed Lake, ON MASSEY, ONTARIO

Resident Geologist PERRY VERN ENGLISHRed Lake, ON RED LAKE, Ontario

Assessment Files Library JERROLD MILTON WILLIAMSONSudbury, ON EAR FALLS, Ontario

Page: l


Distribution of Assessment Work Credit

The following credit distribution reflects the value of assessment work performed on the mining land(s). Please contact the Mining Recorder to determine if this affects the status of your claims.

Date: April 04, 1997

Submission Number: 2 .17095

Transaction Number: W 9720.00008

Claim Number Value Of Work Performed

1184554 0.00

1143537 11,950.00

1184553 4,000.00

Total: 3 1 5,950.00

Page: l


i mm ut ri t.

\

00 CD (X)

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH VHE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HERfcON

09 i

Knott Twp. (M.-2472) G I809

H84554

—— r — ~ — - - H--_ ^ . — _ — — ,. — — , l

.— ------x- .. _ u -

H4431I

11442^9

I20967

12096791202220

2I53941210034

_________(

2153921215393

6M

Fredart Lake Area (M^24I5) c 1779

r-noCD

LO

CM l.

o.h?c oiO)

THE TOWNSHIP OF

BELANGERDISTRICT OF

KENORA(PATRICIA PORTION)

RED LAKE MINING DIVISION

SCALE:1-INC^4O CHAINS

LEGEND

PATENTED LAND CROWN LAND 8At E LEASESLOCATED LAND LICENSE OF OCCUPATION MINING RIGHTS ONLY SURFACE RIGHTS ONLY

l ROADSIMPROVED ROADS KING'S HIGHWAYS RAILWAYS POWER LINES MARSH OR MUSKEG MINES

-CANCEI PATENTED S.R.O,

* C.e

NOTES400' surface rights reservation along the shores of all lakes and rivers

G.3742ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

CD fO CD

O CD CN

\

CDm

o mcc

00 QJ00

TRIM LINE

1200W 1100WT

1000W 900WT

800W 700W -r 600W 500W 400W 300W 200WT

100WT

1200W 1 10OW 1OOOW 900W 800W 700W 600W 500W 400W 300W 200W 100W

•z*

100Scale 1:5000

O 100 200 300

(metres)

CHARGEABILITY ANOMALY

52N02SW0011 2.17095 KNOTT 210

Canadian Zeolite LimitedBelanger Grid

Claim ana Base MapDan Patrie Exploration Limited

1200W 1100W 1000W 900W 800W 700W 600W 500W 400W 300W 200W 100W

1200W 1100W 1000W 900W 800W 700W 600W 500W 400W 300W 200W 100W

RElCE V1dDf frb. k ItfR 2 4 1997 '-'i .

MININGiLANDSBRANCH

•'—ft

71)9 3'

100Scale 1:5000 '

100 200 300

(nrwtrM)

l52N028WM11 2.17085 KNOTT 220

U Canadian Zeolite LimitedBelanger Grid

VLF Dip Angle PlotTx. Station : Cutler, Maine, USA, 24.0 kHz.

Dan Patrie Exploration Limited

1200W 1100W 1000W

C/)8

900W 800W 700W 600W 500W 400W 300W 200W 100W

1200W 1100W 1000W 900W 800W 700W 600W 500W 400W 300W 200W 100W

RECEIVED* fob-l mR 2 41997 *"7. 1

MINING LANDS BRANCH

100Scale 1:5000

o 100 200 300

(mctrw)

S2N02SW0011 2.17095 KNOTT 230

Canadian Zeolite LimitedOrid

VLI l raser l ilier PlotTx. Station : Cutler, Maine, USA, 24.0 kHz.

5-Point Fraser RlterDan Patrie Exploration Limited

1200W 1100W 1000W 900W 800W 700W 600W 500W 400W 300W 200W 100W

1200W 1100W 1000W 900W 800W 700W 600W 500W 400W 300W 200W 100W

RECEIVED

241997 ,

MINING LANDS BRAMOH

100Scale 1:5000

o 100 200 300

62N028W0011 2.17095 KNOTT 240

Canadian Zeolite LimitedBelanger Grid

Total Field Magnetic PlotBase Station Corrected

Datum Subtracted : 59300 nlDan Paine Exploration Limited

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