GEOPHYSICS REPORT FOR GOLDWRIGHT EXPLORATIONS INC. … · The magnetometer survey was carried out using an Envi Magnetometer made by Scintrex Ltd. The lines were spaced 100 meters

Dan Patrie May 4,2005

GEOPHYSICS REPORT

FOR

GOLDWRIGHT EXPLORATIONS INC.

ON

THE

RENABIE

PROPERTY

SAULT STE MARIE

MINING DIVISION

ONTARIO

TABLE OF CONTENTS

INTRODUCTION

SUMMARY MID RECOMMENDATIONS

PROPERTY

CLAIM DESCRIPTION

PROPERTY LOCATION At'i\ID ACCESS

TOPOGRAPHY AND VEGETATION

INSTRlJME~lATION AND WORK DONE

MAGNETOMETER SURVEY

INDUCED POLARIZATION SURVEY

INTERPRETATION

CONCLUSIONS

PERSONNEL

CERTIFICATE OF QUALIFICATIOI\

LETTER OF CONSENT

GRID SKETCH

MAPS

Page

1

1

3

3

3

4

4

4

5

6

6

Page 1

INTRODUCTION

The Renabie property total field magnetometer and induced polarization survey covered

in part claims situated in Brackin Township, Northeastern Ontario, Sault Ste Marie Mining

Division.

The total field magnetometer and induced polarization were done to establish areas of

magnetic elevation which could be due from disseminated sulphide mineralization.

The following report summarizes· the results of the previous work, the work carried out during

the current program and the results obtained from that work.

SUMMARY AND RECOMMENDATIONS

Between April 14, 2005 to May 4,2005 a total field magnetometer survey and an induced

polarization survey was completed on portions of the Renabie Property.

A total of 13 kilometers of a total field magnetometer survey and 12.5 kilometers of

induced polarization was surveyed with encouraging results with elevated magnetic zones and

areas of elevated chargeabilities was discovered which is a typical signature for many gold and

base metal properties.

It is recommended that the following program be carried out to complete the evaluation.

1. Establish grid lines at 100 meter intervals over the total claim group.

2. Induced polarization and a total field magnetometer survey to establish areas of

magnetic and disseminated sulphide content.

Page 2

3. A surmner program ofIvIMI soil sampling. "

4. A summer prospecting program.

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

CQuld be considered to further evaluate the economic potential of the property for mineralizatiQll'

Respectfully submitted,

Daniel F. Patrie

Geology and Geophysics Technologist

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APRIL 2005

DAN PATRIE

EXPLORATION LTD,

SCALE 1 INCH=200M

Page 3

PROPERTY

The property consists of 4 unpatented mining claims in Brackin Township, Sault Ste Marie

.Mining Division, Ontario.

MINING CLAIM

3004827

3004828

3004837

3004839

TOTAL

TABLE 1

RENABIE PROPERTY

SAULT STE MARIE MINING DIVISION

CLAIM DESCRIPTION

DUE DATE

MAY 04/053

MAY 04105

MAY 04/05

MAY 04/05

PROPERTY LOCA nON AND ACCESS

UNITS

16

16

15

15

62 UNITS

The Renabie Property mining claims are located adjacent to the old Renabie Gold Mine

and access to the claims is from highway 101 between Wawa and Chapleau by turning north onto

the Missenabie road and then east onto the old Renabie mine road and then on freshly cut ATV

trail the property where the sUlVeys were done ..

Page 4

TOPOGRAPHY AND VEGETATION

The Renabie Property is covered with a mixture poplar, birch and cedar trees with low

lying swampy areas.

INSTRUMENTATION AND WORK DONE

MAGNETOMETER SURVEY

The magnetometer survey was carried out using an Envi Magnetometer made by Scintrex

Ltd. The lines were spaced 100 meters apart in most part and readings were taken at 25 meter

intervals along the lines. The Envi Mag has the capability to measure the total field and using an

Envi Magnetometer as a station 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 0.1 nt may be obtained with these instruments under ideal conditions.

While in gradient mode which was not done at the time the unit has the accurate means of

measuring both the total field and the gradient of the total field and measuring both sensors

simultaneously to calculate the true gradient. In gradient mode the instrument sharply defines the

magnetic responses determined by the total field. It individually delineates closely spaced

anomalies rather than collectively identifying them under one broad magnetic response.

Also when doing a gradient survey the instrument enables you to conduct a gradient

survey during a magnetic storm because of the technique of simultaneously measuring the two

Page 5

sensors cancels out the effects of diurnal magnetic variations. 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 13 kilometers of magnetic readings were tak~ on all lines with 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 is then downloaded to a computer for plotting.

INDUCED POLARIZATION SURVEY

The induced polarization survey was a pole dipole survey was a 4 level with an 'a' spacing

of 50 meters. A high powered 12 kilowatt transmitter with an 18 hp motor generator was used to

transmit power made by Walcer Geophysics and an IPR-12 receiver made by Scintrex Ltd., for

collecting data. The survey was done using electrodes at every station connecting electrodes to

the receiver with 4 lengths of wire. The receiver picks up the current being transmitted and

calculates the chargeability and resistivity of the rock and is stored at each location and then at the

end of the day the data is downloaded to a computer for plotting.

There was a total of 12.5 kilometers of induced polarization surveyed.

Page 6

INTERPRETATION

The magnetic survey did pick up any strong magnetic anomaly running in a north south

diirection across the grid with elevated magnetic values of200 to 600 nT above background.

The induced polarization did pick up slightly elevated chargeability anomalies of

approximately double the background values. See maps for better interpretation.

CONCLUSIONS

Both surveys picked up anomalies above background values and with only a portion of

the claims were covered the property should be looked at in more detail is recommended.

Due to a lack of geological information from the property, it is suggested that on-going

work should consist of a program of more ground geophysics, prospecting and possibly drilling

any anomalies found to evaluating the results obtained.

Daniel F. Patrie

Geological and Geophysics Technologist

May 4, 2005

C. Brent Patrie

Val Therese, Ontario

Jodie Steinke

Spanish, Ontario

Joel Solomon

Massey, Ontario

Dan Patrie

Massey, Ontario

Dean Muncaster

Spanish, Ontario

Steve Damboise

Spanish, Ontario

Victor Beaudry

Massey, Ontario

PERSONNEL

CERTIFICATE OF QUALIFICATION

I, Daniel F. Patrie do hereby certify:

I. That I am a geology and geophysics technologist and reside at Hwy 17 west, Massey, Ontario,

P. O. Box 45, POP IPO,

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 practiced my profession continuously since that time and prior to that since 1972, I

have been an active prospector,

4. That I supervised the geophysics survey on the Renabie Property. Sault Ste Marie, Ontario

Mining Division.

Daniel F. Patrie


May 04, 2005

LETTER OF CONSENT

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

Exploration Inc., using in whole or in part my Geophysics report on the Renabie Property situated

in the District of Algoma, Sault Ste Marie Mi?ffig 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 May, 2005, in the District of Sudbury.

Daniel F. Patrie


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L. C. 13 KMS

MAG 13KMS

1. P. 12.5 KMS

APRIL 2005

'" DAN PATRIE

" EXPLORATION LTD.

SCALE 1 INCH=200M

Mx CAL RES CAL RES Ohm~m Ohm"m

5.5

300001.-----,-----------,------------,-----------,-----------,-----------,------------,-----------,-----------,-----------,------------,-----------,-----------,------------,-----------,-----------,-----------' 130000

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25000~ // '" t-25000

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0+00 E 1+00 E 2+00 E 3+00 E 4+00 E 5+00 E 6+00 E 7+00 E I I I I I I I I

Riter 5.56 4.93 5.63 5.73 6.03 5.95 5.52 5.36 5.28 5.' 5.34 5.49 5.46 7.03 4.64 5.1 Riter

MlC 590-820 n=1 5.4 __

4.2 4.B 5.9 5 .• 5.2 5.2 5.2 5.7 n=1

n=2 ~ 5.B •. 3 5.7 5.7 5.5 5 .• 5.6 4.7 n=2

n=3 6.5 6.2 5.9 5.5 5.6 5.B 5.5 5.2 5.2 5.6 6.B 6.4 n=3

n=4 6.3 6.7 7.2 5.5 5., 6.1 5.8 5.6 5.7 5.6 7.3 5.1 5.6 5.2 2.6 n=4

0+00 E 1+00 E 2+00 E 3+00 E 4+00 E 5+00 E 6+00 E 7+00 E I I I I I I I I

Riter 14100 9970 13000 12300 12700 14900 15400 18300 20900 27200 22600 17300 17100 24300 15900 10600 Filter

CALCULATED RESISTJVrTY n=1 3700/ / - - nJ/~ ,,,. ,- "., 19J

23099 30077 19428 18505

I 11236 19322 n=1

,~~~ ..... "~,/ n=2 25013 22800 14536 10881 8896 n: 2

~-n=3 24569 /0229 '\910~ 1472/ 24294 24011 17671 n=3

\04B / 5194 ( n=4 16262 11 429 10906 15497 20927 45935 9786 16169 n=4

Geosoft Software for the Earth Sciences

Mx mVN

- 7.5

Mx 590-820

CALCULATED RESISTIVITY

Pseudo Section Plot 0+00 N

Po l e~Dipo l e Array a no a

Filter ~ rWl , ,

* * , / , /

* * , /

'to" a 50 m * * plot po int

* *

Logarithmic 1 1 5 2 3 5 7 5 10 Contours , .,",. , , .. .

INTERPRETATION • Strong increase in polarization

occomponied by marked decrease in resistiv ity.

o Wel l defined increase in po larization without marked res istivity decrease.

o Poorly defined polarization increase with no resistivity signature.

" Low resistivity feature.

2 29793 • Sca le 1 :2500 25 o 25 50 75 100 125 150

metres

GOWWRIGHT INDUCED POLARIZATION SURVEY

RENABIE BRAKIN TWP. 0=50

Date: 02/05/2005 In terpretat ion: B. PATRIE

DAN PATRIE EXPLORATION LTD.

Mx mVN

5.8

4.7

MxSQ0..820

CALCULATED flESISlIVITY

CALRE8 CALRES Mx Ohm·m Ohm~m mVN

13000-1,-- ----,---- - -,------ ,-------,--------,---------,---------,-------,----- ---.------,----------,---------,------, 1 '3000 5.8

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7+008 6+008 5+008 4+00 S 3+00 S 2+00 S I I I I I I

Filler 5.32 5.63 5.42 5.46 5.69 5.35 4.98 5.29 5.31 5.54 5.55 4.76 5.62 Filter

n=l 4.7 4/

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n=2 5 .• 5.7 5.5 5.6 5.4 5.4 5.5 0=2

~3 5.9 6.2 5 .• 6 6.4 n=3

n=4 5.7 6.5 6.2 5.5 5 .• 6.5 6.8 n=4

7+00 S 6+00 S 5+00 S 4+008 3+00 S 2+00 S I I I I I I

Riter 7940 6100 6090 6560 5610 4670 6340 6090 6540 11 200 10300 8050 12100 RIter

n=1 4911-- 5243 5754 6223 6669 3997 vi 6432

\ 7618 n=1 CAlCULATED RESlSTM TY

n=2 8855 9453 ~7194 3317

~., ~C 12037 n=2

n=3 ~ J 6610 ./J 3968 ~ 16799 20222 n=3

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Geosof t Software for the Ea rth Sciences

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p lot point

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INTERPRETATION • Strong increase in po larization

accompa nied by marked decrease in resistivity.

D Well defined increase in polarization witho ut ma rked resistivity decrea se.

o Poorly defined polarization increase with no res ist ivi ty signature.

... Law resistivity f eature.

2~ 29193 25

IIiiiI a

Sca le 1 :2500 25 50 75 100

metres

GOLDWRIGHT

•

125 150

INDUCED POLARIZATION SURVEY RENABIE BRAKIN TWP.

0=50 Date: 02/05/2005

Interpretation: B . PATRIE


Mx mVN

M.ot59(1.820

CALCULATeD RESISTIVIT'I'

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CALCUlATED RE$lSTMTY

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INTERPRETATION • Strong increase in polarization

accompanied by marked decrease in res isti vity.

IJ Wel l defined inc rease in polarization without marked resistivi t y decrease.

o Poo rly defined polariza t ion increase with no res ist ivity signat ure.

25 1IiiiiI

Low resistivity feature.

2. 297\9~ Scale 1 :2500

a 25 50 75 100 125 150

metres

GOLDWRIGHT INDUCED POLARIZATION SURVEY RENABIE BRAKIN TWP.

0=50 Date: 02/05/2005

Interpretation: B. PATRIE


Mx mVN

7.2

6.8

6.6

6.4

6.2

6

5.8

5.6

5.4

5.2

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CALCULATED RES1STMTY

CALRES CALRES Mx Ohm"m Ohm*m

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16000l I I

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10+00 S 8+00 S 6+00 S 4+00 S 2+00 S

s.1? 6.67 I

6.81 ,

6.~a I , , I

5.94 I ,

s.b , I

6.06 Filter 7.08 6.44 6.01 6.37 6.5 6.08 5.65 5.5 5.32 5.59 5.61 5.5 5.92 6.23 Filter

n=1 7.6 6.2 6.2 6.2 5.8 6.1 6.4 6.2 6.2 5.5 4.8 4.9 4.9 5A 5.' "001

11=2 6.8 71 5.8 6.5 6.1 6A 6.6 6.9 6A 5.6 5.5 6.6 5.1 5.1 5.3 5.3 6.4 n=2

n=3 7.3 6.9 @ 5.2 6.7 6.8 7.2 6.3 5.5 5.5 5.2 6.5 @ 5.9 SA 5.5 6.5 6A 6.1 n=3

0,", 6.9 ~ ~ ~ 6.' 7.2 6.5 5.6 5.6 6.5 6A 6.7 6.2 5.9 5.9 6.5 6.3 6.2 5.6 5.8 0,",

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n=1 170021

~ 8120 9313~ 15729 15054-

S 5550

C:--? \~ n=1

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n=3 15888 n=3

L 9/ -'330r: ( ~1 \ 0=4 13334 10517 14756 ---:3b294 18417 11445 12454 21762 11848 19311 0,",

mVN 7.2

7

Mx 590-820

CALCULATED RESISTMTY



Po le- Dipo le Array a na a

Filter ~ \ CJ * *

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plot point

* *

Lo g a ri t h mic Co ntours 1, 1" 5, 2, 3, 5, 7" 5, 10,"""

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25 IIiiiIII

INTERPRETATION Strong increase in po larization accampanied by marked decreose in res ist ivity"

Well defined increase in pola ri zation without marked res ist ivity decrease "

Poo rly def ined po larization increase wit h no res istivity sig natu re"

Low resist ivity feature"i$,!l

~ 2979@ 2 0 ~-.. Scale 1 :2500

o 25 50 75 100 125 150

metres

GOWWRIGHT INDUCED POLARIZATION SURVEY RENABIE BRAKIN TWP.

0=50 Date: 02/05/2005

Interp r etation : B" PATRIE


Mx mVN

1.'::r

6.5

5.5

4.5

CALRES Ohm'm

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180001 I

16000 , I i

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1~ I I

10000~ I I

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CALRES llhm'm

---- - T-------r-----__.-----_,_-----,------~,_----~-----__.-----_,_----___, ,20000

--- .......... - -----

I

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13962

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5,6

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118<12

11810

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5.6 5.7

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11334

15263

5.4 5,3

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6.3 5.6 5.6

6.0 5.9 5.5

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, 12UOU

12180

___ ,4~9 ___ -

10001

I 10100

'W111

5.1 '" 5.5

5.' 5.3

5.6 5,4 5.1

5.9 5.1

2+00 N , 11100

10203

129::7

15474 1C808 12906

~~---2-'~ 1343S

5.5

5.1 5.1

5.2

5.2

, 1 ~oo:J

10479

11487 11799

5.3

6 .1

4+00 N 10200

10614 -155""'----'1'5939

n=2

FI:cr

n=4

GeosorL Soflwure ror Lh e EurLh SCiences

7

.5

5.5

4.5

Mx mVN

CN.l;_'IAJ.1! .-{~~11\' 1 1Y

* *


Filter

* * * *

*

Po le-Dipole Array a na

, , , , ,

a

'.f a plat point

50 m

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

• o

o

..

25

INTERPRETATION Strong increase in polarization accompanied by marked decrease in resistiv ity.

Well defined increase in polarization without marked resistivity decrease.

Poorly derined polarization increase with no res istivity signature.

Low resistiviLy f eature .

2919 u

Scale 1 :2500 o 25 50 75 100 125 150

metres

GOLDWRIGHT INDUCED POLARIZATIOIN SURVEY RENABIE BRAKIN TWP.

0=50 Date: 02/05/2005

Interpretation: B. PATR IE


Mx mVN

9 .5

9

8.5

8

7.5

6.5 6

5.5

5

CALCULATl:O RCSr.;l T/vHY

CALRES Qhm' m

16000-1 r---.--------,------~-----~------r_-----.__-

I

14000~ I

I 1 2000~

I I

10000J1 i

8000 : I I

6000 -4 I I

~.---- ---------- ------------------- --------------4000J '---__ ~ _ ___ _ J-____ _ ,

CAL RES Ohm'm

-~------'-------' I 16000

I

~ 14000 I I H 2000 !

L1QODO I I

~800U I I !-- 6000 I I 14000

10+00 S 8+00 S 6+00 S 4+00 S 2+00 S 0+00 N 2+00 N -~~6~.~6~~---.6~.2~'-------"6.~;4.---------.b~.~.·----------'5~~-------'5~.;"'--------5~,;~6-----55.~ks_----'5r,_~~,-----.6."i5,_----fA~.~"-----7~_;~5,_--------7'~_n,---------"r..8ffi,----------T'.~;~,_--------(C~.M._--------.G~.~~---------,7.tW.---------'"~.6~3---------55_~~5,_----'5d_~~-----.5.~~5,_----'5~_5'3-------~5.~~9._----.6~.~"-------.6~.~""--------~6 .68 Filter Filter

n=2

n=3

H iler

fl=1

n=3

/ '/'.5 W 7 .1~8.1 G

-/~

,-' ,., '.3 6.' 6.' 6.'

'.7 5.5 ,., 5.1 5.5 0.5 6.4 6.'

!i .3 5.9 5.9 55 6.6 ti.ti

8.5 6.3 6.1 5.5 5.6 6.4 5.8 5.6 5.6

'.3 J/ G 6'

7.5

6.2

7.5

7-'

, ..

46

'.5

,.2 5.'

' .7

5.9 5.::;

6.' 6,3

fi2 n=1

' .9 5.3

5.3 5.5 5.2 7 .-1

5.::1 5.8 5.2 5.3 8.6

10+00 S 8+00 S 6+00 S 4+00 S 2+00 S 0+00 N 2+00 N --~:,~"f' oo~~------~1~~'~--------~,71~~. ---------u, o~;oo~------~,,7.1~~OO~--------,~,~An~n---------'11~~~OO'_-------'1~'O~'OOO_--------.9~~lo_--------'9~2~7',_--------"9M~'On_--------"M~'~OO,_------~MMT.~D,_--------66't:'~o_--------'5~;~,0,_--------6_61~eCo_--------55,f,. ~mo---------'s~w~o,_--------•• t,~mo---------'6500~o'_--------'~~\oO---------.9~m~O,_--------7HO~20,_--------'Rt.6~~------~.4~d~20~--------~67~~OO---------,,~~o Alwr

6371 11759 6552 17filll ~7547~~

13~ ~ 1470; 14954

11185 5!l50 1502{}

13151 13378 8765 9232

1~10B 13333 9245

8623 11490 4219

6943 9261 14435 3995

6022 4322

9438 6370 4086

3010

3369

3518

3629

5040

71'165

;; Ii" 10505 ~

5272

6859

Geosoft Software io r the Earth Sciences

Mx IIIVN

!=Ui

9

8.5

8

7.5

6.5

6

5.5

- 5

CALCULATED nEs mn \i1TY

* *


Fi lter

* * * *

* *

Pole-Dipo le Array o

, ,

no

, /

'd plot point

o

o 50 m

Logarithmic Co ntours 1 .5,2, 3, 5, 7 . 5 , 10, ...

• []

o

25 !MI

INTERPRETATION St rong increase in polarization accompanied by marked decrease in res istivity.

Well defined increase in polarizat ion without ma rked resistivity decrease.

Poorly definerl polarization increase with no resist iv ity signature.

Sr:C1 le 1 :2500 o 25 50 75 100 125 150

metres

GOLDWRIGHT INDUCED POLARIZATION SURVEY RENABIE BRAKIN TWP.

0=50 Date 02/05/2005

Interpretation : B . PATRIE


Mx mVrv

9

8.5

8

7.5

7

"1 '"

5.5-

SJ

CALCLlATEC RE!l13TMlY

CALRES Uhm<m

20000-1 ,----,--- ------,-

I ///'-.---..". 18000l // '~,

I // -.... .............. 1600°1 // ''-~_

I / -... -.... .... 14000i /'

I 120001

I

1UOOO-i I

BOOO i I

GOOOJ '-----'-----

10+00 S , a55

n=1 u.2

0.8

10+00 S , 13C>OO

I

'"

1.1

0.8

I 19300

7.1

6.8

6.6

I

15~U


65

6.27

67

6.6

I 12100

6.3

6.2

8+00 S I

6.06

6.3

8+00 S , 10800

5.7

' .8

5.7

4326

5550

5.1J

6.5

I 12100

5.57 6_92

5.5

5.9

S'''~7 IU

7.5- - 7.1

6+00 S , 14300 "t'!oo

6',5.1 !.I610

18Z14 12117

14512 13333

12120 11409

7 _09

6.5

' .2

~.3

, 10000

_10043

7552

"'''

-----------,--------,-------,--------,--------,-------,-----------------,-------,--------,--- -

4+00 S , 79JI

9.5

' .4

4+00S I

!"Il/1f!

4W 5

804 0

076

9.2 9A

0.5

9~ b.'

5226 --

I l5:m

5236

1l.44

8:"

I fiIi:1O

6.,2

7.5, ___ ~

a.6

9.3

, ohm

72

'1302

2+00 S , 7.11

5.3

5.5

7.2

2+00S , 1438

3186

592G

,-

6 .24

5.7

5.9

62

, 6590

I S.9J

6 .3

6.1

I (6140

5.1

-T-

I

5.67

5.8

6A

, 633U

6.1

0+00 N I

5.72

5.7

6.'

0+00 N , '/1:£0

::.Ii

5A

5.':'

b.!1

filMl

5.3

5.8

I 7070

5.8

CALRES Mx Ohm"m

- ---------.-- - ---.- ----' Izmoo I ~18000 I f-1 600f1 I I 1-1400U i

1-1lUoo I

~10000 I

IIlVN r 9

8.5

7.5

5.5

6

----------- ~- ~8000 5.5

I

558

"

5';

I 76',0

5.6

6618

11558

2+00 N 5~6

".4

6 .1

2+00 N 74~0

7025

7 840

5.2

8H2fI

--~-----~-----'-------~ ' BOOO

I 5.43

6.1

01811

MA 1

s-'

6797

f\153

. 5.78

I

"90

628

6.1

6.6

8716

BV4 B198

4+00 N , 5.22

4.5

c:: _'''_97_ 9W8 9515 9428

Filter

'1"'3

n=-1

Filter

n=1

n=2

n=3

n=4

* *


Filter * •

* * * *

Pole-Di pole Array a

, ,

n o

/ /

a

'of a plat paint

50 m

Logorithm ic Contours 1.5, 2, 3, 5, 7.5, 10, ...

• []

o

25 IIiiI

INTERPRETATION Strong Hlcrease In polarizatIOn (lccompanred by marked decrease in resistivity_

W~II defined Increase In polarization withDut marked reslsllvi ty decrease .

Poorly defined polarization increase with no resls t! vlly signature.

Low resistivity feature .

2 029193

Scale 1 :2500 o 25 50 75 100 125 150

metres


0=50 Date: 02/05/2005



Mx mVN

.'>bS X.,s20

7.5

n.!'>

6

5.5

CAL RES CALRES Ohmom Ol1m<m

240001 ,-----.----------,-----------,----------~----------_,----------T - ,-.. -----~,-----_,,------.,_------,,_-----~-----~-----_,,------T'------,,_-----,'------r'-----_,,------T'------r'-----_,,------.,------,· ------.----------,-----------,----------" I ~OOO

22000~ 20000~

,

18GOO~ I

16000~

14000J1

1 2(jOO~ I

10WD, I

aOGOl 6000J "-____ ~ ____________________ _L __________ _L __________ _L __________ ~ __________ L__·

~2?'oOO I ,-20000 ,

t-180oo I : 16000

( 14000 I , 12000 I 1- 10000 I t--SOOO I

- ,-----~~-----~-----~-----~---------' LSO'JO

10+00 S 8+00 S 6+00 S 4+00 S 2+00 S 0+00 N 2+00 N 4+00 N -~~~,~~---_o'~----_.~,~----_o~,._----=.c'~=----_.~,,---------_.~·~--------~'~------~~f' ,c--------~·~---------.~'._--------a~' ~----<d',_-----_.".t',-,,_--------oj'"'--------_ct'._--------~'~--------_c~'._--------_.t'~----<j'"'----_.i',_--------_.t' c---------oj·;---------_.t',--------=-2.,~=-------~~,,---------~'~----_.~';_----=~,

F~L",

11=1

n=2

n-=3

FI:er

n=1

,-=,

0=3

- 7.12 (/8 65.1 6.6H 6.56 6.13 5.75 6.31 6.31 6.49 6.18 6.46 6.75 " ;;.89 !iSi 6.27 5J36 5.18 iI.8a 5.02 5.27 5.24 5.11 5.04 ::1.1 ' ".cr1 4.92 4.C!5 Filter

5.9 6.9

7.2

G61'J _______ -'962,.

11094

'.3 G.G

6.8

72 58

6.15

lSJoo 21600

5.a

6.7

8+00 S I

17800

5.4

",.7

5.2 6.4 6.5

6.' 6.7

7.2

doo 14;>00 17!iOO

5.7

5.2

6.5

5.8

6+00 S , l/1UU

5.6

5.8

.J .- E~- ~ ,- ~ ~r-~ .. , .~ .. <"" '4997 '\ 2730 J "; ,( /~ 2~", ~ \ 0340

5.5

6.7 7.2

7. 7

5.6 6.9

7880 lOSD

~---------~~~----..

4 4lifi

10323 8033 6772

"'"

4+003 9/00

5.9

13972 11 111

5.9

6 ."-

5.7

66

12182

5.7

2+00 S I

~7

5.2

8539

5.4

5.1

10060

5.3 5.5

5.5

10700

5.9

5'

0+00 N lokm

~/"" ~ ~ "". 74732

~. ,7",~ ...

4.8

5.8 5.3 4.0

5.7 5.3 5A

70200 11100

~ ffi~\

73523 717GO ~683J 8736

'0577

13056 15031 86f3

5.2

12572

6373

5.5

5.3

2+00N I

10900

57

5 .7

'3448

12449

11092

11114

4.9

4.7 4.3

) 5

9480

9989 ______ ·, 0185

8047

8~62

9!)49

8210

~ ~7414

4.3

5540

4+00 N , 6060 Filter

-,560 n=1\


Mx mVfIJ

7.5

6.5

-, 5.5

4.5

CALCl II Ul'niOFS~

* *


Filter

* * * *

* *

Po le-Dipo le Array

a

, ,

no

, /

/ /

't{

plot point

o

rWl )

a = 50 m

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

• o

D

25 IIjjII

INTERPRETATION Strong Increase In polarization acco mpanied by marked decrease in resist ivity.

Wel l defi nerl increase in polarization without marked resistivity decrease.

Poorly defined polarization Increase with no resistiVity signature

Low resistivity feature.

6)) 2:;, '« t0 0

Scale 1 :2500 o 25 50 75 125 150

metres


0=50 Date : 02/0!J/2005


DAN PATRIE EXPLORATION LID.

0 C) L!)

o C)

'"

o C) N

C)

o ~

o

C) o ~ ·

o o <;l

0 C) .... ·

0 0 I/") •

0 0 <L> •

CO 0 r-.. ·

-100 0

r 0

5709()

57095

57089

0 0

-100 a

100 200 300 400 500 600 700

r --J 0 0

57107

100 200 300 400 500 600 700

800 900

800 900

U1 0 C)

.... C) C)

"" o o

N o o

o o

o

• ~ o o

· W CO> o

· .... 0 0

· U1 0 0

, m 0 0

, ..... 0 0

, CD o o

cb o CO

50

57277 57261

57207 57198 57193 57184 57179 57173 57169 57161 57156 57154 57151 57147 57143 57137 57132 57128 57124 57120 57115 57110 57105 57101 57094 57087 57077 57059 57037 57013 56953

TMI (CONTOURED ~ 250nT) FULL COLOUR SCAL BAR

o Scale 1 :2500

50 100

, -- --

2 29793 . . ......... •

GOLDWRIGHT TOTAL FIELD MAGNETICS SURVEY

RENABIE ONTARIO BRAKIN TOWNSHIP

BASE STATION CORRECTED DATUM SUBTRACTED; a nT

REFERENCE FIELD; INTERPRETATION BY; B. PATRIE

150

DRA WN BY; DAN PATRIE EXPLORATION LTD.

Documents

GEOPHYSICS REPORT FOR GOLDWRIGHT EXPLORATIONS INC. … · The magnetometer survey was carried out using an Envi Magnetometer made by Scintrex Ltd. The lines were spaced 100 meters