LARRY NOEL GERVAIS - Ontario

GERARD LAMBERTGEOSCIENCES l v Z- ^ Consultation et genie-conseil en geophysique.'.

LARRY NOEL GERVAIS

Frecheville - Holloway Property

flztbeson Area

Frecheville fe Holloway Townships, N.E. Ontario

Larder Lake Mining Division

N.T.S. 32D/12

Report on Induced Polarization Surveys

32D12SE2029 2.24682 HOLLOWAY 010

Val Senneville, Quebec

December 10, 2001

V i

Gerard Lambert, P.Eng.

Consulting Geophysicist

144, me George, C.P. 2355, Rouyn-Noranda (Quebec) Canada J9X 5A9Tel. : (819) 762-3182 Fax : (819) 762-5364 Email: [email protected]

Larry Noel Gervais________________Frecheville - Holloway property, IP. surveys

TABLE OF CONTENTS

Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

Property description, location, access . . . . . . . . 2

Description of the I.P. surveys . . . . . . .. . . . . . . . 5

Results and interpretation . . . . . . . . . . . . . . . . . . . 6

Conclusion and recommendations . . . . . . . . . . . . 9

Appended:

Scale

Resistivity 1 1.P. pseudo-sections . . . . . . . . . 1:5,000

Apparent resistivity contour maps withI.P. anomalies superimposed . . . . . . . . . . . . . 1:5,000

Polarization (Phase I.P.) contour maps withI.P. anomalies superimposed . . . . . . . . . . . . . 1:5,000

Larry Noel Gervais________________Frecheville - Holloway property, I.P. surveys

Introduction

During the month of December 2001, ground geophysical investigations consisting namely in Induced Polarization (I.P.) surveys, were carried out over the Frecheville-Holloway property in the Matheson area, for Prospector Larry Noel Gervais of Timmins.

The purpose of these surveys was to provide appropriate geoscientific information about the underlying lithologies and to map with a better accuracy the distribution of disseminated and stringer sulfides in the bedrock, these sulfides being potentially of economic interest if they are found to carry significant concentrations of base and/or precious metals. Considering the incomplete or inadequate I.P. coverage from past geophysical work, the present I.P. surveys were also meant to complement the geophysical coverage and understanding on the property.

This report describes the work done and discusses the results obtained and the interpretation of the data. Recommendations for any future work are presented in the conclusion.

The I.P. survey was carried out between Dec. 1 st and Dec. 12., 2001, by crews of Remy Belanger Geophysics of Rouyn-Noranda, Quebec.

Property description, location and access

The Frecheville-Holloway property is situated in the northeastern portion of Holloway and southeastern portion of Frecheville townships, in northeastern Ontario (Larder Lake Mining Division). The center of the survey area is located at about 48 km to the north of Larder Lake and 60 km east of Matheson. The survey area is easily accessible by vehicle, as highway 101 passes just 100 meters south of the grid. Please refer to Figures 1. and 2. on the next two pages, showing location maps of the property, at scales of 1:1,000,000 and 1:100,000 (N.T.S. 32D), respectively.

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-^LARRY NOEL GERVAIS

FRECHEVILLE ft HOLLOWAY TWPS.

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LARRY NOEL GERVAIS

FRECHEVILLE ft HOLLOWAY TWPS


The Frecheville-Holloway property consists of a block of four contiguous unpatented mining claims, situated in Holloway and Frecheville townships. The I.P./resistivity compilation maps appended to this report illustrate the shape of the claim blocks which was covered by the present surveys and also show the property boundary, the claim lines and the claim numbers (1225218, 1225410, 1225408 and 1222454).

Description of the I.P. surveys

The Induced Polarization surveys were carried out over a grid which consisted of cut picket lines oriented north-south (000 0 ), spaced every 200m and chained/picketed every 25m. The grid lines were turned off from base line 0+OOrnN (Azimuth 0900 ) which coincides with the Frecheville-Holloway township line. Survey lines go from L-2200mW to L-OOOmE. The (0,0) point is located at the four corners of Frecheville-Holloway-Stoughton-Marriott townships. Tie lines 400N and 800S were also established to control the survey lines. A total of 20 kms of cut lines constitute the grid, including the base line and tie-lines,

The Phase I.P. surveys were carried out using a dipole-dipole electrode configuration. The dipole dimension was 50 meters and successive separations at multiples of 11=1 to n-6 times the dipole dimensions were used, in order to investigate at depth. A total of approximately 13.4 line-km of I.P. data was thus gathered by operator Remy Belanger over the course of the survey.

The I.P. equipment used for the survey consisted of l 0 ) a Phoenix EPT-1 transmitter operating at 1.0 Hz, powered by a 2 kilowatt, model MG-2 motor generator. The phase angle (measured in milliradians) between the transmitted current and the received voltage was measured by 2 0 ) a Phoenix Turbo V-5 Phase I.P. receiver, measuring the phase shift (induced polarization effect) and also the apparent resistivity of the earth at each "n". The phase angle is a direct measure of the polarizability or chargeability of the underlying earth.


The results of the I.P. surveys are presented in the appendix, namely in the form of pseudo-sections of the apparent resistivities and the measured phase angles, at the scale 1:5,000 as well as on plan maps at l :5,000 showing respectively the contours of the apparent resistivity at n=2 and the contours of the Phase (polarization) at n=2. These plan maps also display the interpreted I.P. anomaly trends using symbols which are explained in the accompanying legend.

Results and interpretation

The Induced Polarization method is probably the best geophysical prospecting tool when investigating for base or precious metals in geological environments such as the Harker-Holloway mining camp. The I.P. technique is capable of mapping most types of metallic sulfides, even when they do not conduct, which is often the case with structure-hosted gold mineralization associated with disseminated and stringer sulfides in fractures. Furthermore, the I.P. technique can also discriminate between "poor" E.M. conductors associated with electrolytic conductivity such as porous shear zones and overburden depressions (causing no recognizable I.P. effect), and "poor" E.M. conductors caused by low-conductivity metallic mineralization, such as stringer sulfides or sphalerite-enriched sulfides (recognizable I.P. effect).

The apparent resistivity measurements often provide very useful structural information and greatly help in mapping major lithological contacts and faults (the latter usually expressed as more or less linear resistivity lows). The performance of the I.P. method can occasionally be hampered by conductive overburden cover such as lacustrine clays, and sources of man-made cultural noise (power lines, metallic fences, etc.) when present.


In this particular case, a 50-meter dipole dimension was chosen because of its penetration capability and its ability for outlining potentially large, deep and wide pyrite-mineralized zones having a significant depth extent. With the n=6 expanders, this 50-meter dipole-dipole IP. survey should be able to successfully detect metallic sulphide mineralization in the bedrock to depths in excess of 100 meters.

The thickness of the overburden layer is quite variable within the survey area, but its largest range is not expected to exceed 25 to 30 meters, generally speaking.

* Resistivity

The resistivity pattern, as shown on the n^2 apparent resistivity colour contour map, and also on the resistivity pseudo-sections, provides a very faithful image of the relief of the bedrock surface and of the intrinsic resistivities of the underlying overburden and bedrock lithologies. Most of the high resistivity ^ 2,000 ohm-meters) areas, abundant in the north portion of the grid, are most probably associated with bedrock ridges and subcrops (areas of thin overburden).

Quite often also, the definition of high resistivity zones provides help in outlining harder, more felsic rocks or hydrothermally-altered (silica and/or carbonates) horizons, a good tracer tool for metal-enriched environments.

These high resistivity zones and patches make up about one third of the survey area and are distributed according to the colour resistivity contour map (shades of red and purple) and should be visited in the field as there is a fair chance that more or new bedrock exposures will be found, hopefully helping in further understanding the geology and the structure of the property.

Larry Noel Gervais________________Frecheville - Holloway property. I.P. surveys

Elsewhere within the survey area, several low-resistivity (less than 200 ohm-meters) domains define areas where the water-soaked overburden layer probably thickens significantly, possibly up to 30-40 meters, or becomes particularly clay-rich in the areas of lowest resistivity. These areas of low resistivity are usually associated with bedrock troughs, sometimes of structural origins. Very commonly in archean terranes, low-resistivity lineaments are typically associated with major bedrock structures such as shear zones and open fracture planes.

There does not appear to exist any isolated resistivity lows that could be attributable to conductive metallic mineralization such as massive sulphides or graphite.

* Polarization (I. P. effect)

Referring to the I.P. pseudo-sections and the ^2 Phase (I.P.) contour map and its accompanying legend, it will be observed that the interpreted I.P. anomalies were classified according to their "strength" (i.e. the probable "massiveness" of the causative metallic material) and their degree of definition (a well-defined I.P. anomaly is one which displays a clear, unambiguous triangular shape on a pseudo-section), as well as according to the behavior of the apparent resistivity.

Conductive, semi-massive and massive metallic mineralization (graphite and/or massive sulfides) will typically cause a marked decrease in the measured apparent resistivity, in addition to a strong I.P. anomaly. So will a mineralized shear corridor carrying disseminated or stringer sulfides. As the concentration of these metallic materials decreases, the drop in the resistivity becomes more negligible, but the I.P. effect still remains. The symbols used in the interpretation of the data are explained on the compilation maps and on the pseudo-sections.

Larry Noel Gervais________________Frecheville - Holloway property, IP. surveys

The Induced Polarization measurements show the presence of two units in the bedrock exhibiting moderately anomalous I.P. behavior, distributed as linear trends oriented roughly east- west, in areas of low to moderate resistivity.

The first trend is located between lines 2200W and 1800W at or near the base line DOON and appears to remain open to the west. It is incompletely closed-offto the north. It is associated with a strong resistivity ridge and could simply be the result of high background polarization. Its proximity to the surface however allows one to anticipate that its cause may outcrop at surface and therefore warrants a ground verification.

The second anomaly trend is more interesting. It is located between 1200W and 200W at about 550S-600S. It originates from a deep source (probably around 60-75 meters), occasionally becomes wide (on lines 1200W and 400W) and is best defined on line 400W between 525 S and 450S. There is a slight suggestion that the apparent resistivity decreases above this I.P. anomaly, therefore it may be due to weakly or moderately conductive metallic material (stringer sulphides, flaky graphite). The appreciable width of the response on lines 1200W and 400W makes this response appealing. This second I.P. anomaly trend deserves further testing by diamond drilling, in the view of delineating metallic sulphide mineralization in the bedrock. Drill holes should be positioned so as to intersect the mineralization at 90 to 125 meters vertically below surface.

Conclusion and recommendations

The Induced Polarization surveys which were recently completed over the Frecheville- Holloway property for Prospector Larry Noel Gervais have successfully defined one zone characterized by a well-defined, moderately strong IP. effect, located in low resistivity environments.

With only limited knowledge of the property area, it is difficult from a geophysical point of view alone, to rate the I. P. anomalies discussed above in terms of their economic potential, especially if one is exploring the property for gold. But it is highly probable that the "strongest"

Larry Noel Gervais________________Frecheville - Holloway property, I.P. surveysI.P. anomalies on lines 1200W and 400W will probably be caused by disseminated or stringer metallic mineralization such as pyrite in the bedrock, at depths of about 60-75 meters below ground surface.

Recommending further work on this property, it is advisable to visit all the high resistivity areas in search for potentially new bedrock exposures. This will hopefully allow to obtain some lithological samples and to possibly allow an explanation for the I.P. trend along the base line on lines 2200W and 2000W.

The other anomaly trend at 500S-600S, particularly on lines 1200W and 400W deserves further investigation by means of diamond drilling, aiming at intersecting the mineralized units at about 100-125 meters below ground surface. The choice of priorities will however require some input from other sources of geoscientific information, such as airborne and ground magnetic survey maps, compilations of past work and of nearby showings and mineralized drill intersections, as well as an analysis of the magnetic relief and resistivity trends in conjunction with a regional geological and a structural compilation.

Val Senneville, Quebec

December 10, 2001 Consulting Geophysicist

10

ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No:Recording Date:

Approval Date:

Client(s):

136071

177382

188436

298698

Survey Type(s):

Work Report Summarv

W0280.01919 Status: APPROVED2002-DEC-13 Work Done from: 2001-DEC-012002-DEC-19 to: 2001 -DEC-1 2

GERVAIS, LARRY NOEL

OBRADOVICH, THOMAS JOHN

ROBITAILLE, ROBERT ROCKY

ISERHOFF, CHARLES SAMUEL

IP LC

Work Report Details:Perform Applied Assign

Claim* Perform Approve Applied Approve Assign Approve Reserve

L 1204299

L 1222454

L 1225408

External Credits:

Reserve:

32,338 32,338 SO SO 32,338 2,338 SOSO SO 51,000 31,000 SO 0 SOSO SO 51,338 S1,338 SO 0 SO

S2.338 52,338 32,338 32,338 32,338 S2.338 SO

SO

SO Reserve of Work Report*: W0280.01 91 9

50 Total Remaining

Status of claim is based on information currently on record.

Reserve Approve Due Date

SO 2003-DEC-08

SO 2004-DEC-19

SO 2004-DEC-19

SO

32D12SE2029 2.24682 HOLLOWAY 900

2002-Dec-20 08:44 Armstrong_d Page 1 of 1

Min !~try ofNorthern Developmentand Mines

Date:2002-DEC-19

Ministere duDeveSoppement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

LARRY NOEL GERVAIS P.O. BOX 43 TIMMINS, ONTARIO P4N 7C5 CANADA

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

Dear Sir or Madam

Submission Number: 2.24682 Transaction Number(s): W0280.01919

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 STEVEN BENETEAU by email at [email protected] or by phone at (705) 670-5855.

Yours Sincerely,

Ron GashinskiSenior Manager, Mining Lands Section

Cc: Resident Geologist

Larry Noel Gervais (Claim Holder)

Assessment File Library

Larry Noel Gervais (Assessment Office)

Thomas John Obradovich (Claim Holder)

Robert Rocky Robitaille (Claim Holder)

Charles Samuel Iserhoff (Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:17806

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LARRY NOEL GERVAISTimmins, Orrt.


Induced Polarization surveys

Contours of the Phase (i.P. effect)SO meters dfpoles

Data processing and interpretation by

G. Lambert, P.Eng.

LAMBERT GEOSCIENCES LTD.

December 2001

Frecheville Se Hollow.ay Twps., N.E. Ontario

Scale 1:5,000

N.T.S. 32 D/12

l.P. survey by: Rtmy Baiangtr

LEGENDDIPOLE-DIPOLE ARRAY

t ne a

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VPLOT POINT

11-1,2.3.4.5,6

instruments: Phoenix IPT-J Tx, Turbo V-S Rx Frequency; 1.0 Hi Operator: Ra my Belanger D

231.

318.

Apparent Resistivity 377- (Ohm-metres)

4-10.'

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Polarisation Increase wlthoi of the apparent resistivity.Disseminated to stringer to sulphides, discontinuous gi rich sulphides. Also olterecMETALLIC MINERALS, MASSIVE MAONt

Poorly defined polarisation with no apparent resistivity Small quantities of sulphld veins, sometimes noisy rea problem*. MAGNETOE. CLAY OR

32D12SE2029 2.24682 HOLLOWAY

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LARRY NOEL GERVAISTimmins, Ont.


Induced Polarization surveys

Contours of the apparent resistivity 50 meters dlpotes

a processing and interpretation by

Lambert, P. Erg.

1BERT GEOSCIENCES LTD.

cember 2001

Frecheville Se Holloway Twps., N.E. Ontario

Scale 1:5,000

N.T.S. 32 D/12

t.P. survey by: Remy Belanger

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(milSiradians)

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any ilflnlflcantOtssemlnated to stringer to semi- massive sulphfdg*. discontinuous graphite, sphalerite rich sulphides. Also altered, pyrlttzed itruetuMETALUC yiNCRALS, MASSIVE MAGHCTTTE, MICACEOUS MIND

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32D12SE2029 2.24682 HOLLOWAY 220

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INTERPRETATION

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Logarithmic Contours

INTERPRETATION

Polarization increase, accompanied by a significant decrease of the apparent resistivity.

Polarization increase without a marked decrease of 1he resistivity.

Poorly defined or noisy polarization anomaly, no resistivity signature.

D

Scale 1:500050 100 15C

metres)

LARRY NOEL GERVAISINDUCED POLARIZATION SURVEY

FRECHEVILLE-HOLLOWAY PROPERTYFrecheville A Holloway Twps., (NTS 32D/12), Ontario

Date: 01/12/09 Interpretation by: G. LAhMBERT, P. En g.aamy Soiangor Geophysics

32D12SE2029 2.24682 HOLLOWAY 230

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11=5

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7+00 S 6+003 5+00 S 4+00 S 3+00 S 2+00 S 1+00 S 0+00 I+OON 2+00 N 3+00 N-30 -.70 -,B5 -.30 -1.2 -.23 -JO 1 2.2 1.1 -.10 -.30 -t.5 -li -.JO fitter

7+00 S 6+00 S 5+005 4+00 S 3+00 S 2+00 S 1+00 S 0+00 1+00 2+00 N I+OON-I.* -JO -.90 -T.I -13 -9.4 -6.9 -6J -S.7 -6.4 -4.7 -4.1

-4.3 -i.Z -1.7 -* -t. lfilter

1=1

n~2

n=3

RES

L1000

LIO

INTERPRETATION

Resistivity (Oh m-met res)

INTERPRETATION

Phase (mRadfans)

Metal Factor (ipAes'lOO)

Line 200 W

Dipole-Dtpole Arrayna

Filter *

* ** * *

* * * *= 50 M

V - X 11=1,2,3,4,5.6plot pbjnt

Instrument: Phoenix IPT-1 Tx, Turbo V-5 Rx Frequency: 1.0 Hz Operator: Remy Belanger

LogarithmicConburs

INTERPRETATION


Polarization increase without a marked decrease of the resistivity.

Poody defined or noisy polarization anomaly, no resistivity signature.

Scale 1:50005C ^ LJI-II 50 100 150 200 250

(mstrss)

URRY NOEL GERVAISINDUCED POLARIZATION SURVEY

FRECHEVILLE-HOLLOWAY PROPERTYFrecheville ft Holloway Twps., (NTS 32D/12), Ontario

Date: 01/12/09 frrpr3h*to by: G. LA^D^T, r.Eng.

Remy Belanger Geophysics

32D12SK2029 2-24682 HOLLOWAY 240

IP MF 40 100.

J

20J 50.

-i——l—————i——l——l——l——i——l——l—————l——i——l——r T——i——i——i——i——r ~i————i——i——i——i——i——i——r

OJ -I——l——Li

MF IP r 100 40

-50

7+00 S 6+00 S 5+00 S i+QOS J+OOS 2+00 S 1+00 S 0+00 I+OON 2+00 N 3+00 Nfiltar

11=1

0=4

0=5 0=6

255 2H 190 173 164 10) t IS 222 Ut 644 W1 195 149 190 US 111 113 107 117 141 120 147 578

Si529

265

3(1 DI

Q-Q7+003 6+00 S 5+00 S 4+00 S J+OOS 2+00 S 1+00 S 0+00 t+OON 2+00 N 3+00 N

filtar

11=1

(1=2

11=3

11=4

11=5

JO -.40 -SO -t.1 -.70 -.60 .74 -.30 -.30 -JO -.70 -U -.60 -.90 -1.1 -I.I -l -.90 -1.1 -1.2 -t.1 .90

7+00 S 5+00 S 5+005 4+OCS 3+00 S 2+00 S 1+00 S 0+00 t+OON 2+00 N 3+00 Nfilter 2.8 -I.* -4.1 -6.3 -*.3 -5.1 5.S -1.4 -U -.SO -1.5 -6.2 -H -i -9.5 -}.9 -8.8 -H -9.4 -7,8 -19 -7.5 1.6

filtar

(1=4 (1=5 0=6

filtar

n-1

(1=3

n=4

0=5

.1=6

filter

0=6

RES

L 1 000

L10

INTERPRETATION

Resistivity(Ohm-melres)

INTERPRETATION

Phase (mRadlans)

Metal Factor (ipAes*lQQ)

Line 400 W

Dipole-Dipole Arrayanoa

Filter*

* ** * *

# * * *plot pbjnt

a^50 M

0=1,2.3,4,5,6

Instrument; Phoenix IPT-1 Tx, Turbo V-5 Rx Frequency: 1.0 Hz Operator: Remy Belanger

Logarithmic Corrtours

INTERPRETATION




Scale 1:500050 100 10 25Q

(metres)


FRECHEVILLE-HOLLOWAY PROPERTYFrwhwille 4 Holloway Twps,, (NTS 320/12), Ontario

Date: 01/12/09 Interpretation by: G. LAMBERT, P.Eng.

32D12SE2029 2.24682 HOLLOWAY 250

IP 40

MF

20j 50.

0.

fitter

filter

11=1

n^2 (1=3 11=4 11=5

11 = 2

(1=5 11=6

7+00 S 5-WQS 5+00 S ucos 3+00 S 2+00 S 1+00 S 0+00 1+00 N 2+00 N 5+00 N266 198 2-5 1(5 IBS 215 JM 272 1019 552 4*1 JBJI J)1 JI9 491 lil 229 ZZi 297 537 502 12K

7+00 S 5+00 S 5+00 S 4+00 S 3+00 S 2+00 S -4S- 1+00 S 0+00 1+00 N 2+00 N S+OON-1,1 -U -,IO -.40 -,O -.15 -1.1 -.20 U l -.60 3.1 .50\ -.50 .60 -1.2 -.90 1.2 5.S

7+003 5+00 S S+QOS 4H50S 3+00 S 2+00 S 1+00 S 0+00 1+OON 2+00 N 3+00 N-4.1 -5.S -.50 -2.2 -1.1 -M -3.3 -.70 U 1.9 -1.5 .80 1.5 -1.1 1.2 -7,9 -3.9 -i.S -1.8 -1.S I.* .60

1.! '.l

fitter

fittar

n=2 0=3

MF IR RES100 40 .JOOK

i !f j

.50 LzO L1000

INTERPRETATION

Resistivity(Ohm-mefres)

INTERPRETATION

Phase (mRadfans)

Metal Factor (ip/ras'IOO)

Line 600 W

Dipole-Dipole Arrayj noa

Filter

plof pbJnt

0 = 50 M

0=1,2,3,4,5,6

Instrumenl: Phoenix IPT-1 Tx, Turbo V-5 Rx Frequency: 1.0 Hz Operator: Remy Belanger

Logarithmic Contours 5 75 in 5' AD( 1U"

INTERPRETATION

Polarization increase, accormpanied by a significant decrease of the apparent resistivity.



Scale 1:5000500 SO 100 t SO 200 250

(metras)


FRECHEVILLE-HOLLOWAY PROPERTYFnchwHto 4 Holloway Twps,, (NTS 320/12), Ontario

Date: 01/12/09 interpretation by: G. LAMBERT, P.Eng.

Remy Betangor Geophysics

32D12SE2029 2.24682 HOLLOWAY 260

IP MF 40 1 00.

J

50.

oJ oj

l———l———l———T

, . 'S . ,

MF IP .100 40

l

u50

Lo

[20

Lo

7+00 S 5+00 S 5+00 S 4+00 S 3+00 S 2+00 S 1+00 S 0+00 1+00 N 2+00 N 3+00 Nfilter 151 1M 154 1SS 147 IW 31] W 2446 2063 662 171 272 57 IW 374 217 903 I1K UK 2SK

7+00 S 5+00 S 5+00 S 4+00 S 3+00 S 2+00 S 1+00 S 0+00 1+00 N 2+00 N i+OON.14 I.* -.10 iS ( '-.SO -M -M -l -I.I

filter -.50 -.60 -.2} .10 .80

[1=1 --40,

(1=2

11=5 11=6

7+00 S 6+003 5+00 S 4+005 3+00 S 2+00 S 1+00 S 0+00 1-H30N 2+00 N J+OONfilter

i.*

flHw

fittar

(1=3

11=6

-3.3 -3.9 -1.3 2.6 S.4 S.B .M 2J -.20 1.6 2.9 -.40 -5.1 -J,* -3.7 -19 -5.9 -2.1 -5.1 .W .90 .90 .40 ffar

n=2

11=3

11=6

RES-100K

.1000

L10

INTERPRETATION

Resistivity(Ohm-metres)

INTERPRETATION

Phase (mRadians)

Metal Factor (ip/res'100)

Line 800 W

Dipole-Dipole Array

Filter*

* ** * *

* * * *\ x 0=50 W

W 0=1,2,3.4,5,6 plot pbjnt

Instrument: Phoenix IPT-1 Tx, Turbo V-5 Rx Frequency: 1.0 Hz Operator: Remy Belanger

Logarithmic . i 5 2 3 s 7s in Contours l, 1A A i, S,/i, 10,...

INTERPRETATION

Polan'zation increase, accompanied by a significant decrease of the apparent resistivity.


Poort/ defined or noisy polarization anomaly, no resistivity signature.

Scale 1:50005C O 50 100 150 200 250

(metres)


FRECHEVILLE-HOLLOWAY PROPERTY frecheville 4 Holloway Twps,, (NTS 32D/12), Ontario

Dote: 01/12/09 Interpretation by: G. LAMBERT, P.Eng.

Belanger Geophysics

2-24682 270

2/1 ''-Q — -

32D12SE2029 2.24682 HOLLOWAY

29

032D12SE2029 2.24682

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Documents

LARRY NOEL GERVAIS - Ontario