GEOPHYSICS REPORT ON THE WASHAGAMI LAKE PGE …...Claude Dubreuil Spanish, Ontario Brent Patrie...

GEOPHYSICS REPORT

ON THE

WASHAGAMI LAKE PGE PROPERTY

DAVIS TOWNSHIP

SUDBURY

MINING DIVISION

FOR

GOLDWRIGHT EXPLORATION BVC.

BY RECEIVEDJUN 1 1 2001

GEOSCIENCE ASSESSMENT _____OFFICE_____

Dan Patrie

Dan Patrie June 01, 2001

41I09NW2031 2.21553 DAVIS 010

TABLE OF CONTENTS

INTRODUCTION

SUMMARY AND RECOMMENDATIONS

LOCATION AND ACCESS

GEOLOGY

TOPOGRAPHY AND VEGETATION

CLAIM DESCRIPTION

INSTRUMENTATION AND WORK DONE

MAGNETOMETER AND INDUCED POLARIZATION SURVEY

INTERPRETATION

CONCLUSIONS

RECOMMENDED EXPLORATION PROGRAM

PERSONNEL

CERTIFICATE OF QUALIFICATION

LETTER OF CONSENT

MAGNETIC AND PSEUDOSECTION MAPS

BASE MAP

PAGE

1

2

3

3

3

3

4

4

5

5

6

41I09NW2031 2.21553 DAVIS 010C

Page l

INTRODUCTION

Goldwright Exploration Inc., acquired a group of 2 unpatented mining claims 32 units

located in Davis Township in the Sudbury Mining Division.

The property is underlain by rocks of the Huronian Supergroup and the Nipissing diabase

which are favorable host for economic Copper-Nickel-Platinum Group Element (Cu, Ni-PGE)

deposits.

In summary the Murray Lake Property shows to have considerable merit and warrants

further exploration work in order to evaluate its potential to host economic platinum group

element deposits.

As per request of the property owners a geophysics program consisting of magnetometer,

and induced polarization survey which began May 28th to May 31 st, 2001 and was carried out by

Dan Patrie Exploration Ltd.

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

program and the results obtained.

Respectively submitted,

Daniel F. Patrie

Geology and Geophysics Technologist

June, 2001

SUMMARY AND RECOMMENDATIONS

The Washagami Lake property is located in Northeastern Ontario , District of Sudbury, in

the Sudbury Mining Division.

The property is underlain by rocks of the Huronian Supergroup and the Nipissing diabase

which are favorable hosts for economic Copper-Nickel-Platinum Group Element (Cu, Ni-PGE)

deposits.

In summary the Washagami Lake property has shown to have considerable merit and

warrants further exploration work in order to evaluate its potential to host economic PGE

deposits.

Further exploration of the Washagami Lake property is warranted in proving its

considerable merit in hosting economic PGE, Ni, Cu and Au mineralization.

A program of 9.6 kilometers of magnetic and 9 kilometers of induced polarization survey

was done to explore the Washagami Lake property in Davis Township for its PGE potential.

The survey indicated a high chargeability anomaly with corresponding magnetic

anomaly running in an east west direction across the property which could host massive sulphides

or Platinum Group Elements (Cu, Ni-PGE).

Due to the lack of geological information the following programs are recommended to

complete the evaluation.

1. Completion of the grid lines over entire property.

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

3. Magnetometer and VLF surveys over remainder of property.

4. Induced Polarization over all of property.

5. Diamond drilling I. P. anomalies to establish sulphide content and geology.

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

should be considered to further evaluate the economic potential of the property for PGE

mineralization.

The following report summarizes the results obtained from the work carried out during the

current program and the interpretation is speculative.

PageS

LOCATION AND ACCESS

The Washagami Lake property is located north of town of Hagar, Ontario approximately

55 kilometers east of Sudbury, Ontario in Davis Township. Access to the property is by turning

north off highway 17 form the town of Hagar, Ontario and traveling some 20 kilometers up the

Washagami Lake logging road to the center of the property in Davis Township.

GEOLOGY

The Washagami Lake Property of Goldwright Exploration Inc. consists of a north

trending Nipissing gabbro sheet that may in fact be part of the same Nipissing gabbro body in

neighbouring Janes Township where Pacific North West Capital reported assay values ranging

from 7 g/t combined PGE's up to 49.7 g/t combined PGE's (Nov. 6/98 press release).

This intrusive contains numerous Cu/Ni showings with potential for PGE mineralization.

TOPOGRAPHY AND VEGETATION

The Washagami Lake property vegetation is currently a mix of alders, pines, willows and

younger coniferous trees in a gently undulating landscape and some areas there is swamps.

CLAIM DESCRIPTION

Consisting of 4 unpatented mining claims (41 units), the Washagami Lake property,

located in Davis Township in the District of Sudbury, Sudbury Mining Division.

TABLE l

WASHAGAMI LAKE PROPERTY, DISTRICT OF SUDBURY

CLAIM DESCRIPTION

MINING CLAIM NUMBER OF UNITS

1229735 06

1229736 16

1229741 04

1229742 15

TOTAL 41 units.

DAVIS TWP. Property Area

m M ills and 1 smelters

Mining operations

FIGURE 1: General location map, Davis Township property, northeastern Ontario

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FIGURE 3 General geological features and sample locations east claim block area on the south shore of Murray Lake (UTM coordinates. Zone 17)

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FIGURE 4: General geological features and sample locations, west claim block, west of Washagami Lake (UTM coordinates, Zone 17)

INSTRUMENTATION AND WORK DONE

MAGNETOMETER AND INDUCED POLARIZATION SURVEY The magnetometer survey was carried out using an EDA Omni-Plus Mag/VLF unit with

the total field being measured and an Omni-IV base station magnetometer for correcting magnetic drift. These are total field magnetometers which measure the magnetic field through the use of proton processional effects caused by the interaction of a magnetic field with a spin aligned,

proton rich fluid. An instrument accuracy precision and resolution of 0. l nt may be obtained with these instruments under ideal conditions. The VLF allows you to read the vertical in-phase, vertical quadrature, total field strength, dip angle and the ability to obtain as many as 3 VLF stations , but at the time no VLF was read. Microprocessors contained in these instruments allow for the collection of the readings along with the time and its position in digital form suitable for downloading to a computer for data processing. A total of 9.05 kilometers of magnetic readings were taken and readings were taken along the lines at 25 meter station intervals. The field measurements were corrected for diurnal variations of the earth's magnetic field by direct subtraction of the base station readings from the reading taken at the same moment in the field units. The corrected data was then downloaded to a computer and plotted on the total field magnetic map.

A total of 9.05 kilometers of induced polarization survey was done with an "a" spacing of 50 meters and 6 levels l to 6 read. The survey was a time domain pole dipole survey and was read with a Walcer MG-14 motor generator and a Huntec 12 kilowatt Model transmitter and a Scintrex EPR-12 receiver. The motor generator and transmitter were stationary on the end of the line being read and current transmitted through a wire with an electrode driven down through the

ground for a good contact and then transmitting current to that electrode from the transmitter by the transmitter man which is contact by radio to the receiver man. Ahead of the live current electrode is a crew of men driving electrodes in winter and using porous pots in summer at every station to be read and connected to the pots or electrode by length of wire from the receiver where the receiver operator picks up the readings with the receiver. The data is then downloaded from the receiver at the end of the day to a computer where the resistivity and chargeability is calculated and plotted using Geosoft software for the earth sciences in pseudosection maps.

PageS

INTERPRETATION

The magnetic of the property is quite homogenous overall, with a relatively quiet background relief on the order of 100-200 nT being interrupted with high amplitude anomalies on

the order of 300-6000 nT above background running in an east west direction across the grid leaving it open to the east and to the west. The two magnetic anomalies were centered at 2+00

south and 5+50 south.The induced polarization survey picked up two chargeability zones running in an east west

direction centered at 2+00 south on lines 1+25 west, 2+45 west and 3+50 west and also centered at 3+00 south on lines 4+45 west, 5+00 west, 5+50 west, 6+00 west and 7+35 west which

corresponds with the high magnetic anomaly in the same area. Also, there was a high chargeability zone on the ends of lines 7+35 west and 9+50 west starting at approximately 400 north on both lines and leaving the zone open to the north where the lines ended. The chargeability values run approximately 3 times the valued background and also corresponds with the magnetic anomaly and a resistivity low which suggests disseminated sulphides or a high concentration of sulphide

with a magnetic signature which should be investigated in more detail for its potential to host PGE mineralization with possibly high values.

The induced polarization survey proved successful in finding areas of high chargeability

with corresponding high magnetometer readings which merit more exploration work such as drilling these targets.

CONCLUSIONS

With the presence of a favorable geological environment for the localization of PGE mineralization of economic importance to further evaluate the property's potential the writer recommends an on going work program over the remaining claims and areas not already covered

on the property, consisting of line cutting at 100 meter intervals, magnetometer, VLF and induced polarization surveys to locate areas of disseminated sulphide.

RECOMMENDED EXPLORATION PROGRAM

The following program is recommended to evaluate the property for its potential to host a PGE deposit.

1. Complete the line cutting by extending all lines to the north and south andextending the grid to the east and west at 100 metre spacing as required to provide a control for geological, geochemical and geophysical work.

2. Geochemical sampling over target areas.3. Magnetometer survey over areas not covered.4. Detailed Induced Polarization survey at 50 m "A" spacing and 6 levels read..5. Geological mapping and sampling.6. Stripping, trenching over anomalous areas.As a result of encouraging data obtained from the recently completed geophysics survey

additional exploration on the property is recommended.

Daniel F. PatrieGeology and Geophysical Technologist

June, 2001

PERSONNEL

Dan Patrie Massey, Ontario

Bryan Patrie

Massey, Ontario

Claude Dubreuil Spanish, Ontario

Brent Patrie Elliot Lake, Ontario

Bronson Ede Walford, Ontario

Dwayne Steinke Massey, Ontario

Jody Steinke Massey, Ontario

Brent Jerome Massey, Ontario

Corey StDenis Massey, Ontario

CERTIFICATE OF QUALIFICATION

I, Daniel Patrie do hereby certify:

1. That I am a Geology and Geophysics Technologist and I reside at Hwy. 17 West, P.O.

Box 45, Massey, Ont, Canada, POP 1PO,

2. I graduated from Cambrian College Of Applied Arts and Technology, Sudbury, Ontario,

in 1987 with a diploma in Geological Technology with a one year certificate in Geophysics,

3. And I have practiced my profession continuously since graduation, as well as being an

active prospector since 1972.

4. That my report on the Washagami Lake PGE Property, Sudbury Mining Division,Ontario, is based on my personal knowledge of the geology of the area, and on a review of

published and unpublished information on the property and surrounding area.

Daniel F. Patrie

Geology and Geophysics Technologist (Dipl. T)June, 2001

LETTER OF CONSENT

I, Daniel F. Patrie, of the Town of Massey, Ontario, do hereby consent to Goldwright

Resources Inc., using in whole or in part my Geophysics report on the Washagami Lake PGE

Property situated the District of Sudbury, Sudbury Mining Division in a prospectus of statement

of material facts or for filing with government regulatory bodies as deemed necessary.

Dated at Massey, Ontario, this 4th day of June, 2001, in the District of Sudbury.

Daniel F. Patrie

Geology and Geophysics Technologist

ONTMIO MINISTRY OF NORTHERN DEVELOPMENT AND MINESTransaction No:

Recording Date:

Approval Date:

Client(s):303574

Survey Type(s):

W0170.30260

2001-JUN-11

2001-AUG-22

Work Report Summary

Status: APPROVED

Work Done from: 2001-APR-15

to: 2001-MAY-31

GOLDWRIGHT EXPLORATIONS INC

IP LC MAG

Work Report Details:

Claim*

S 1229735

S 1229741

S 1229742

Perform

SO

so816,918

316,918

Perform Approve

SO

SO

S16.918

316,918

Applied

S2.400

S1 ,600

S6.400

510,400

Applied Approve

S2.400

S1.600

S6.400

S 10, 400

Assign

soso

S4.000

S4,000

Assign Approve

0

0

4,000

S4.000

Reserve

soso

S6.518

S6.518

Reserve Approve

soso

S6.518

S6.518

Due Date

2001 -DEC-09

2001 -DEC-09

2001 -DEC-09

Status of claim is based on information currently on record.

41I09NW2031 2.21553 DAVIS 900

2001-Aug-30 10:13 Armstrongjd Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2001-AUG-23

Ministere du Developpement du Nord et des Mines

BRIAN JAMES WRIGHT GOLDWRIGHT EXPLORATIONS INC GENERAL DELIVERY HAGAR, ONTARIO POM 1X0 CANADA

OntarioGEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E6B5

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2 .21553 Transaction Number(s): W0170.30260

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact JIM MCAULEY by email at [email protected] or by phone at (705) 670-5855.

Yours Sincerely,

Ron GashinskiSupervisor, Geoscience Assessment Office

Gc: Resident Geologist

Goldwright Explorations Inc (Claim Holder)

Assessment File Library

Goldwright Explorations Inc (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16284

MINING LAND TENURE

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O Well defined increase irj poiorizotion without marked resistivity decrease .

O Poorly defined poiorizotion increase wfth no resistivity signature.

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Scale 1:5000O 50 100 150 200 250 300

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M000- 9nj V. - j" f - t" 2*0022000' g J ,.''' '""^--.y ^\. 7 L g -22000

9+00 S StOOS 4+OOS 3*00 S 2+OOS 1+00 S""•f 24800 32400 23200 23400 22900 20200 23900 2S300 27500 31000 2*500 29040 FMw

n*2 22347 21062^jMflOnfl^OlB*WL^ 11413 ^^DI34^^19640rf^2flT5ll-"i93Bfr^ta— TflflS /wSsfiSSSxTW n*2

n-3 77220^^1438^—28826^^047.^13999 j J8997 . 27834 27994 2BOS4 289*4 j l K4640 n-3

BM 34a07/ 2Z2?i Ssi^^lfel^^isi* [393B1 \ 23fi3~ 22806 237*7 J 40B17 n-4

n-S 23349 25231 l 4ffl6^^te4V^2757TvM533 \ 1*S5 "^0897 f 30499 n-5

IF* 25401 31744* ' *85A^2SJB2 Z7978 27099 * 19317 1 27180 n-fl

stoos s+oas 4+oos 3+oos 2+00 s i+oosFlttf 8.93 8.71 937 8.96 10.2 123 12.1 11.2 10.6 10,5 11.5 116 Rttv

C'1*1!)**^''** n-1 6.5 . 5.36 6.82 ,7.41. io.3 ii.ei U.I . 10.3*.^ 9.13 8.17 y 11.2 i 8.66 (fi Chargeability

n-2 7.92 6.ft-**^.82Xylfl.7 10.5 \ ftSlV IflL 12.1- 108^*-984 9.08 \ 11.3 n-2

S S s~*. l \ ^, ^v*^ """-^n-3 7.46 TST \8.1 /^8j 9.46 9.55. 11\ 12.8^*^11.5 10.5V 9.02 n-3

n^ 903 jrfa* 12— "^ 11.6 ^9-65 10.2 Si4 13.6 ^2 10.3 nM *T -*~^r 1 /^ -s^ \

n-6 13.2 * 11 10.2 11.9 —— 1^1— 122 * 15.1 14.2 n-6

DIHlllWllllIIIllli41I09NW2031 2.21553 DAVIS 260

Pseudo Section Plot 3+50 WPole-Dipole Array

a no a

' — ©n r®— iFiitpr 1 11

•k 4r X 'T ^ ^ yV J*

^^ ' a ^ 50 m * . * - 'x S

* * w plot point

Logarithmic , , t 0 -r c -7 c 1 A /x ^ , 1, 1 . b , 2, 3, D, 7.5, 10,.-. Contours


accompanied by marked decreasein resistivity .

D Well defined increase jn polarization

C Poorly defined polarization increase with no resistivity signature.

W Low resistivity feature.

t

'"f ' - -' \ -"•-

Scale 1:500050 0 50 100 15Q 2QQ 250 3PP

metre



Date: 01/06/2001 Interpretation: D. PATRIE

DAN PATRIE EXPLORATION LTD.

ResCafcOhm In

40000

39000-

30000-

25000-

20000

15000

MXMX 590-820

13

1Z5

12

11.5

11

10.5

109.9

9

8.9

B

ResCateOhm-m

r40000

35000

•30000

-29000

-20000

15000

7100 S 6+OOS s+oos 4+OOS 3*005 2*00 S MBSFMV33BOO 34700 31900

Calculated ReMiivQti toooe 46778

n-2 30403V441 ISjX

19800 18800 20800 25900 12890 13365 9424.1 14SBS

S&2 \ 7

29300 3240031530

29(00 33300 38600 FlUf ^ ^39904 * 43150 .52621 nfi^lctilated Reactivity/y J.... t'.snr 50B20 i

**23f .SW04

n*2

0-3

n*4

n-5

n-6

7*003 6*00 S 5*003 4*00 S 3+00 S 2+OOS 1+00 S11.2 10.5 10 RHW

.10-7 9.99 s.67 n*i ChargeaWrty8.83 9.06 8 36 8.73 9.29 1 2.5 1Z.5 12.2 10 9,81 9.97

10*^ 10.6^ 9.24 / i^n10.4 aa?^ -id /!

1.2 fn I 10.5 ^79

. ^. .

' ' 17.7 ^ 14.4 TV*

41I09NW2031 2.21553 DAVIS 270

Pseudo Section Plot 4+45 WPole-Dtpole Array

Filter

a = 50 m

w plot point

Logarithmic Contours

a

n

INTERPRETATIONStrong increase in polarization accompanied by marked decrease in resistivity .

Well defined increase In polarization without marked resistivity decrease.

Poorly defined polarization increase with no resistivity signature .


50Scale 1:5000

50 100__ISO 200^ES metre

250 300

GOLDWRfOHTINDUCED POLARIZATION SURVEY


Date: 01/06/2001 Interpretation: D- P.ATRlt


ResCato MXOtinfm Mi 590-820

35000-

30000

25000-

20000-

15000-

10000

13

12

11

10

9i

8-

Mx ResCaicMi 590-820 Ohm'rn

-35000

r 12

11

-9

'-B

-30000

-29000

-2DOOO

15000

10000

**OOS StOOS 4+00 S 3400 S 2-MWS 1*00 S^ ^ FWW31300 33000 28100 2550=3

CateuUed ResirtvHjt, 37^,, y^ ,JDW 1-a

4m*^3i4tar

2700 19600 14000 18100 20200 24000 24100 19600 20800 Fitw tt t 8319.2.^9666.2^ 3664.2^,63947 117724 16483 1330k——14147.^14214

•ffi37B* l! 2Z728257or^!

18^6 \ 3W2/ /470M

vSr26 9 u3e4 \an \ MOWu\r \,L

7311 n-2

n-3

n-4

n-6

10924

6*00 S 54OC S 4*00 S 3*00 S 2*00 S 1KJOS

n-6

41I09NW2Q31 2.21553 DAVIS 280

Pseudo Section Plot5+OOWPole-Dipole Array

na

Filter

a ^ 50 m

plot point

Logarithmic 1 159357510S^. i 'i l-ij, i., O, J, '.^ 1 lw.Contours

INTERPRETATIONB Strong increase in polarization

accompanied by marked decrease in resistivity.

a

a

Well defined increase in polarization without marked resistivity decrease .

Poorly defined polarization increase with no resistivity signature.


50

Scale 1:500050 100__150 200

H!5S metre

250 300

GOLDWRfGHTINDUCED POLARIZATION SURVEY


Date: 01/06/200' Interpretation: D , PA^RiE


ResCafcOlwn*ni

39000

30000

25000-

20000-

15000-

10000

MXM* 590-820

11.9

n

10.5

10

9.5

9

U l

8

Calculated

MX ResCatcMl 590-420 Otim-m

.-40000j

11

10.S

10

95

•9

i-8.9iL 8

-45000

-30000

25000

-20000

-19000

-10000

7*00 S **oos 5+00 S 4*003 3*005 2400S rwo sPllM-12200 34900 32300 21700 20500 26300 16200 1 7400 1 7200 19900 24800 29200 21600 23300 FltBT ^

19000.6 17B21^WM.S 8379.1 8011 14132 122947 ^.25920_.25648x^9285.2 npalCUlated RCSIStjVlty

TO1 \ 25S!^m92——1004T 1 37ST 19378 1947^

^3003 122T5\\3j7wSo749T~~150W'^ 1 7093 2DB75 13 ft4 \ 41

,-.— 1S734 1 3799 J 2232B \3S201

SVvzldb 19238 ZOlfes^ 27106\\41 ^^ ^V*" 'ifeoO T2832*--H86B

49B14

[f2

n-3

11=5

n-6

7+00 S 6400S 4400S 3+00 S 2+00 S 1+00 S

6.51FMr 10.1 8.84 9.35 9.06 8.58 10.1 113 10.7 10.4 10 8.22 9.02 9.09 9.39 FttW

6.89 ^545__5.73 8.92 v 11 ^11.9 v s.06^ 7 .08 ^5.33^ 7.26 7.21 . 8.5711=1 Chargeability

ri 1\

9.2\

S"!12.7 i3.S X 7.S9___^8.15,^ 6.81 691

n

T

87 9 .89 9.3 9.29 1 0.6 \12.5 lS.4 N. 8.61 age.^..'^ 7 .98

9.41 9.11 ^10.3 122 lis^ 9.W SfiW

9.97 10.6 10"3 8.53 9"84 \ t3.5 V 3.2S ,'12.9 J T O"5^"^10*3 8.53 Sfc4 \ 13.5 lif J (T2.9 J

11.1 \8 8.82 \ 10.9\ 14.3-^^^11.8 11.5

rt-3

[1=4

n-6

41I09NW2031 2.21553 DAVIS 290

Pseudo Section Plot 5+5OWPole-Dipoie Array

na

Filter

a = 50 m

plot point

Logarithmic Contours 5 2

INTERPRETATION

1Q

D

Strong increase in polarization accompanied by m arked decrease in resistivity .

Well defined increase in polarization without marked resistivity decrease.



50Scale 1:5000

50 100__150 200 250 300 "•"•" ' l

metre

COLDWRfOHTINDUCED POLARIZATION SURVEY


Date: O' /'06/2001 Interpretation: D. PATRIE

DAN PATRtE EXPLORATION LTD.tt boft'A-are 'or the Earth Sciences

ResCate MXOhm*m Hx 990-820

32000-1 12

30000-

28000-

24000

22000-

20000-

18000-

16000-

14000i

11

10 H

MXMX 590-0 20

-12

-10.5

10

8.5

•8

ReeCateOhm'm

-32000

-30000

26000

-24000

-22000

-20000

-16000

-14000

ttoos 5*00 s 4-nxa 3+00 s 2*003 1*00 sFlOr 30000 22000 18600 17200 20900 15700 16800 19800 18200 23500 22400 17100 Fit*

Calculated ReSMtMfitt 24039—-2S19S y13783i 5126.4 10228—^7688.7 42S8.9- S292 12K 21931^ 13370-_.18137 fffi*

~* ' '^ AVoL 374*1

d ReswtivTty^^^ S \

7T*^ 14338^ 18225 \ 2S

773 7 174J2 WfiS \S8l X ^^^^ ^^. *^^~ \ \ '

***7 f 52*^^071 13098-17119 JD131

.^ ̂ 21348^4133^1*96 V 128o9 19S48

149^^ 4SSOV^ 16458 1S30S

n-2

6*00 S 5+00 S 4+00 S 3+00 S 2+00 SFltW 888 9.18 8.4 8.65 10 t 11.4 9.48 9.84 9.09 9.36 9-24 9.34 FBe-

ChargeabiBty 11=1 7.16 7.05 643 7.os s.57 ( ^2.s y xJ-91~ J.os 7.01 e.es 6.32 ,8.92

0=2 773 7.63 7.69*"^ 9.37 \ 6.81 \ 9^5 \ 13.7\XB.S7y 907 ^124^^ 6.84 7.66 H*'.

n-3 10.4^ 8.45 ST22 9.95 8.43~~~'8.57 *H

nM 11 "X^a.99 ^tfb 9 *6 9.64 9

n"5

11=6

11,8 10.9 f 9-74

12^ '8.66 fO.3 10.7

41I09NW2031 2.21553 DAVIS 300

Pseudo Section Plot 6+00 WPole-Dipole Array

Filter

a = 50 m

w plot point

Logarithmic , i 5 o 3 5 7 5 10JT. l l . \ ^J , Z—— - .__l . ^-"l ' - ——'l ^*-Contours

INTERPRETATION•i Strong increase in polarization


O

D

Well defined increase in polarization without marked resistivity decrease .



50Scale 1:5000

50 100__150 2f*——

mat re

300



Date: 01/06/2001 Interpretation; D. PATRIE

DAK PATRIE EXPLORATION LTD.

ResCafc MXMX 530-820

soon49000

40000

35000

3000025000-

20000-

15000-

10000-

9

8.9

8-

7.5-

7

6.6-

i6J

MX ResCakMn 590420 Ohmln

9 r50000

-85

8

7.5

-7

6.5

6

-45000

-40000

-35000

-30000

r25000

-20000

15000

10000

7*006 ••cos 6*008 4*00 S 3+00 S 2*00 S 1*00 S 0*00 N 1+00 N 2*00 N 3*00 N 4*00 N 5*00 N

CalculatedFHW22200 23200 29800 18900 20700 17800 13200 19100 1UOO 20400 27100 33100 27700 38800 38000 38300 40100 41100 44800 30700 40800 36900 38700 40200 40200 FW*f

25188 29732 28873 t v 7866 161S3 8338.8 v 3832.6 6978.2 9132.1 18747 280B3 132033w 39906- 31464 32347*^22977 36139 3TS6j j 20044 22931——21964.X *ta-*' s** j l \ l /SZ?\ l rf*. '^-'"^ ——"r t l

80608 6134.9 /13630^--lSs67 f 23872 \ 27907 7 f4M71\ 127643 3482T 40043—-41482.*--43619 J 2n-2 27280 28038

n-3

J2 28875 i ^866

29B83/ 20806

1^.284811*11 2B81ffv187rSi1

3*617/17365 2D486 23878 Vnezl ** V V. \

tez 128B3

'23194^ 1

20932V 18699

22703* 15670— 16373

mdTS*38659 /49066 n-2

11*3

to^&ito y.46435 ^6808-^53623

469S1 /S4863

n-6

7+00 S 5+00 S 4*003 2*003 1+00 S 0*00 N 1*00 N 2+00 N 3+00 N 4+00 N 5+00 N

IV*2

n*3

n-4

n-9

n-6

FWer648 6.69 6.85 6.82 8.13 7.96 7.29 774 7.67 7.58 7.95 7.18 7.14 8.82 8.01 8.1 S 7.51 7.89 8.68 79 801 7.92 7.82 8.29 FiterChargeability ni1 532 5.33 452 5.73 e.8i ^4.ae 563——~s.94 6.15 6.31 ^.5.74 s.2 7.11 ^^.s.ei *7.62 6.3^ 4.43 ^^.3.82 4.77 5.1 s 5.39 ^ 6.39 e.38 n^i Chargeability

S S99r""*6.06 7.42 7,18 737 7.31 6.3 6.53 7 6.S2 .9.79 *6.73

\.f*^sdx 6.81 713 ^66*'1X.7.73__, 7.55 7.12 6.12 7.46 8.04 5.98 sil

9.25 X.7.86__^7.87__^S-Oar^^Ti 6.88 805*' 7.9S^ 9.43 9.83——-10.4

6.54 6.78\ 9.* 11.18.6 8-28-^7.75,8.63 9.13 9.17 \ S.11

8.86

1

8.45 6.66 6.46 6.75 6.76 n-2

rae —797—--ana-- ai———811 n-3

8.76 6.98 9.1 9.5 9.49 n-4

11.7 -^T54- 10.5 10.8 10.8 0=6

41I09NW2031 2.21553 DAVIS 310

Pseudo Section Plot 7f 35 WPole-Dipole Array

a na a

Filter I±La = 50 m

w plot point

Logarithmic Contours 1 , 1.5, 2, 3, 5, 7.5, 10, .

INTERPRETATION

a

Strong increase in polarization accompanied by marked decrease in resistivity .

Well defined increase jn polarization without marked resistivity decrease .



50Scale 1:5000

50 100 150 200 250 200emetre



Date: 01/06/2001 nterpretation: D. PATRIE


Re*Cate MXOhro'm Mi 580-820

40000-, 9

35000

30000-

25000-

20000-

15000

10000-

7.5

6.3

"~i—————r~ -i—————r~ n—————T-

MX ResCalcMX 590-820 Ohm'm

9 r-40000

35000

30000

-25000

•20000

13000

10000

s

7.5

6.6

4*00 S 34QOS 2400 S 1*00 e 0*00 N 1*00 M 3+OON 4*00 N

atom

n-6

Flter 1 3700 12300 12800 15600 17000 20600 23200 27900 29100 25400 2910D 3*700 30700 29400 27000 30300 29700 3t800 34400 Ffftar "fei 9909.3.^*805.9 10382 .9764.8 11676 11472 13210 204*1^.23178 v 15319——14606 18811 v 8516.2 ^ 17221-^.12014 10590 1328* ^ 21890 20941

n-2 10186 12386 ^^OK t&BIS 11978 y/TsSOS 19620*-^2S4'(!rX^704*^25S36^**.19173^__.2^8 18259^32702^*731841X^168^ J^lS9X**-2?407^27B35 n-2

n*S 20336*^12245 13314 18374.2^,^1*16 &SBO 2W50 /tt

\O4348x--1W80 13216 12978 \171341 27263 131812 l^tsVv 433MlO^3DlB8S l tHtt/.,.—— .\ V V V V \ *VV\\1 V——S J l \\

Tt-S 28721\\.1911.3'J-,14679—~14306 11934\ 20MO \28344 33601 ^*-343SO\ 4848? \ \20889.^,2S759/ 36648 \ SfllftC^SBSfleX' 52?72X"*33591 n-6

3M\ ' -J6405~ 329S7 \24J63 2152^ 311219

4+ODS 3+OOS 2+00 S 1+00 s 0+00 N 1*00 N 2*00 N 3+OON 4*00 N

B.32 9.46 8,57- —— 867 9.61 11.4

11=2 7.05 7.38 6.73

0=3 748, __ .7.09 712 7.59'*—^.* 9.01

7.72 7.47 7.97 \.926

0=5

n-6

6.98 y"*8 86^*^,7.29__^.91-.__?7a_ ^8.1^^ 7.31 7.01 n-2

/B.4S 9 96 8 .67 9,3 8 .83 8.76 S.29 0=3

7,7 J 9.39 l 10.8**N.8.52 10.1 --— s*~[1=5

9,16 829 8.48 ^ 10.6 11.5 * 9.41 V 10.3 0=6

^41 J 8 .35 10.1 11.3 ^9.44 iffl /14.9

\ \ V *829 8.48 \10.6 1 1.5 * 9.41 \ 10.3

41I09NW2031 2.21553 DAVIS 320

Filler 74S 7.23 7 .98 8 .48 796 7.46 7.32 6.83 7 .52 7 28 7 .88 8-26 793 8.5 S 75 8 .48 862 8.19 7.7S FitWChargeability n,, *.B6 5.04 501 4.3 5.19 539 6.72 esi s.s?- 6.42

Pseudo Section Plot9+SOWPole-Dipole Array

Filter

a ^ 50 m

w plot point

Logarithmic Contours 1 , 1.5, 2, 3, 5, 7.5, 10,

INTERPRETATION

a

Strong increase in polarization accompanied by m arked decrease in resistivity .

\iVell defined increase in polarization without marked resistivity decrease .


Low resistivity feature .

Scale 1:500050 100 150 200 250 JOG

metre


L4/CE PROJECT

Date: 01/06/2001 interpretqticn: D. PAIR!E


GEOPHYSICS REPORT ON THE WASHAGAMI LAKE PGE …...Claude Dubreuil Spanish, Ontario Brent Patrie...

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Transcript of GEOPHYSICS REPORT ON THE WASHAGAMI LAKE PGE …...Claude Dubreuil Spanish, Ontario Brent Patrie...