h. ferderber geophysics ltd, j geology r.a. campbell, b.se. j

GEOPHYSICS LTD

42MHSE0101 OP91-730 BENOIT 010

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REPORT ON THEAIRBORNE MAGNETIC AND

VLF-ELECTROMAGNETIC SURVEYSON THE PROPERTY OF

PETER HANLEYBENOIT TOWNSHIP

LARDER LAKE MINING DIVISION, ONTARIO

RESPECTFULLY SUBMITTED BY:

H. FERDERBER GEOPHYSICS LTD,

Val d'Or (Quebec) June 14, 1991

R.A. Campbell, B.Se. Geology

42A08SE0101 OP91-73O BENOIT 01OCTABLE OF CONTENTS

INTRODUCTION . . . . . . . . . . . . . . . . . . .

PROPERTY DESCRIPTION, LOCATION AND ^CCESS . . . . .

GEOLOGY AND MINERALIZATION . . . . . . . . . . . .

INSTRUMENTATION AND SURVEY METHODS . . . . . . . .

VLF-EM Svstem . . . . . . . . ; . . . . . . . .

Tracking Camera and Video Centre . . . . . . .

Survev Parameters . . . . . . . . . . . . . .

DATA PRESENTATION . . . . . . . . . . . . . . . . .

SURVEY RESULTS AND INTERPRETATION . . . . . . . . .

VLF-Electromagnetic Survev . . . . . . . . . .

CONCLUSIONS AND RECOMMENDATIONS . . . . . . . . . .

REFERENCES . . . . . . . . . . . . . . . . . . . .

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H. FERDERBER GEOPHYSICS LTD

REPORT ON THE

AIRBORNE MAGNETIC AND

VLF-ELECTROMAGNETIC SURVEYS

ON THE PROPERTY OF

PETER HAWLEY

BENOIT TOWNSHIP

LARDER LAKE MINING DIVISION, ONTARIO

INTRODUCTION

On May 23, 1991, airborne magnetic and VLF-electroraagnetic surveys were flown over the property of Peter Hawley in Benoit; Township, Larder Lake Mining Division, Ontario. Magnetic and VLF- electroraagnetic data was collected by the airborne division of H. Ferderber Geophysics Ltd. The survey was flown from a base at Val d'Or, Quebec. A total of 19.38 miles of data was collected.

The magnetic survey provides data which helps outline the underlying geological structures and helps identify any potential economic concentrations which may contain variations in accessory magnetic minerals. The results of the VLF-electroraagnetic survey define conductive zones which may represent shear zones and.or metallic sulphide deposits containing gold and/or base metal mineralization.

PROPERTY DESCRIPTION, LOCATION AND ACCESS

The property of Peter Hawley is comprised of 4 claims, covering 160 acres in lots 10 and 11 of Concession III, Benoit Township, Larder Lake Mining Division, Ontario. The claims are registered with the Office of the Mining Recorder in Kirkland Lake and are listed below.


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L1151916 L1151917 L1151918 L1151919

The property is located 14 miles northwest of the town of

Kirkland Lake, 17 miles southeast of Matheson, and 14 miles north

of the village of Kenogami Lake. Provincial Highway 11, north from

Kenogami Lake, bisects the property. Bush roads cross the western

claims. A gas pipeline lies trends north along the eastern

boundary and a power line crosses he property, trending northwest

and north.

Most of the claims are forest covered. Colvin Lake lies 500

feet east of the property. The eastern claims exhibit low

topographical relief and a small hill trends north across the

western claims. Outcrop exposure is fair over the western two

claims.

Supplies, services and qualified manpower are available in the

Kirkland Lake-Matheson area.

GEOLOGY AND MINERALIZATION

The claim block is located in the western part of the Abitibi

Volcanic Belt of the Superior Province of the Canadian Shield. The

Abitibi Volcanic Belt extends for nearly 350 miles in a west-east

direction from Timmins to Chibougamau. It is host to a variety of

precious and base metal deposits including the Timmins, Kirkland

Lake, Noranda, Val d'Or, Matagami and Chibougaroau mining camps.

The Abitibi Volcanic Belt is composed of a complex assemblage

of interbedded volcanic and sedimentary rocks intruded by a variety

of intrusives, from ultrabasic to granitic in composition. The

rocks are Archean in age and have been metamorphosed to the

greenschist facies. Numerous late Precambrian diabase dykes cut

formations of the belt. The rocks generally strike east-west, have


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a vertical dip and are highly folded and faulted. Geological interpretation of the Abitibi Volcanic Belt is complicated by both the wide scattering of outcrop and the complex structural relationships.

The Ontario Division of Mines, Map 2205 - the Timmins-Kirkland Lake Geological Compilation Series (at a scale of l inch equal to four miles). Map 2215 - Benoit and Maisonville Townships (at a scale of l inch equals to 1.2 miles) and the Ontario Ministry of Natural Resources Preliminary Map P873 at Benoit Twp., outline the geology underlying the area containing the claims. The Ontario Geological Survey, Mineral Deposits Circular 18, Gold Deposits of Ontario - part 2, 1979, describes the old gold deposits, prospects and occurrences in the vicinity of the property.

The data presented on these maps suggests that the claims are underlain by mafic and ultramafic rocks lying near the southern edge of an intrusive body. These rocks are comprised of serpentinite, peridotite, gabbro and diorite. They include sone zones of basalt and small intrusions of syenite. The contact with the intermediate to mafic metavolcanic rocks strikes west- northwest, 900 to 250 feet south of the property. Approximately 0.5 miles east of the claim group, the mafic and ultramafic intrusive rocks are in contact with felsic metavolcanics, north of the intermediate to mafic metavolcanics.

Several pits have been excavated in the central and northwestern parts of the c-laim group, uncovering northwest trending quartz veining, sulphides and nickel mineralization. In 1951 Ole Hagen drilled three holes in this area, intersecting asbestos veinlets in serpentine. A copper showing (Map 2205) has been found on the property near the north-central boundary.

The property is located l mile northwest of the past Au-Ag producer, the Davidor Mine. The gold and gold-silver tellurides are situated in northwest striking quartz-carbonate veins and lenses in a carbonate NSO'fy trending shear zone in mafic


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metavolcanic rocks. A total of 277 ounces of gold and 50 ounces of silver were produced in 1918 and between 1936 to 1938. The recovered grade was 0.21 oz/ton gold. The Hawley property lies along strike of the shear zone.

The Bergstand gold occurrence is located 0.6 miles north of the property in a felsic porphyry dyke and quartz veins within intermediate to mafic metavolcanic rocks. Low gold values were reported in a 1921 program of pitting and trenching.

In Benoit Township, within 4.5 miles of the property, numerous gold occurrences have been discovered in metavolcanic rocks; Bunting, Cotterill, Skjonsby, Scotvold-Nelson, Erickson, Noranda, Thompson-McLeod, Keefe and Carlson occurrences.

INSTRUMENTATION AND SURVEY METHODS

The survey was completed using a 1972 Cessna 172, fixed wing aircraft, call letters CF-EWK, owned and operated by H. Ferderber Geophysics Ltd. The pilot and navigator/operator were M. Turcotte and D. Monastesse respectively, of Val d'Or and Vassan.

Geophysical sensors were mounted in modified wing tips. The geophysical, navigation and data acquisition systems are in the following pages.

Magnetometer

The magnetometer used was a GEM Systems GSM-11, high sensitivity airborne proton (Overhauser) magnetometer. The instrument continuously measures the Earth's magnetic field a 0.01 gamma sensitivity for l reading per second to 10 readings per second at 0.1 gamma absolute accuracy. For this survey four readings per second were collected. The analog output is on 3 channels, from l to 10,000 gammas full scale.


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VLF-EM System

A Herz Totem 2A VLF-EM System was used to measure the changes

in the total field and in the vertical quadrature field on two

frequencies simultaneously with an accuracy of J.%. The primary

transmitting station of Cutler, Maine (NAA) frequency 24.0 kHz was

employed.

Radar Altimeter

The ground clearance was measured with a King 10/10 A radar

altimeter. The survey was flown at a mean clearance of 300 feet

with the altimeter producing an accuracy of 5% (15 feet) .at this

altitude.

Tracking Camera and Video Centre

A RCA TC-200 colour video camera and Galaxy 200 video centre

was used to record the flight path on standard VHS type video

tapes. Manual fiducials were indicated on the picture frames for

reference with digital printout. Flight path recovery was aided

using a Panasonic Colour Video Monitor-31300 and Video Cassette

Recorder AG-2500.

Data Acquisition System

A Picodas Group Inc. PDAS 1100 data acquisition system

featuring seven analog inputs with two frequency inputs and

external interfacing was used. A Termiflex corp. ST/32 Keyboard

control unit and Sharp Corp. LCD display unit are connected to the

data acquisition system. At present this system stores the

altimeter VLF-1 in-phase, VLF-1 quadrature, VLF-2 in-phase, VLF-2

quadrature, magnetic field (coarse), magnetic field (fine), and the

fourth difference (noise), and fiducials on 3.5 inch floppy disk

drive. The data is then printed out in digital and profile form.


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Survey Parameters

The survey was conducted on lines oriented at 030 and 210 degrees, flown at an average aircraft altitude of 300 feet and a speed of approximately 90 miles per hour. Geophysical responses were collected at data points spaced at 33 foot intervals along the lines. The lines were spaced at 440 feet intervals. Navigation was visual using topographical maps, at a scale of one inch to 1320 feet, manual fiducials, and the flight path recovery system as references.

DATA PRESENTATION

Flight lines, fiducial points and geophysical responses were reproduced from the topographical maps at a scale of one inch to 1320 feet (1:15,840). The outline of the claim block and claim nap are shown on each map sheet.

The aeromagnetic data was corrected for diurnal variations by using a base line as a reference. The data was then contoured at 20 and 100 gamma intervals and presented on Map MG-1.

The VLF-EM was transferred from the Totem 2AG memory to profiled form. Base values were determined for the VLF-EM total field profiled data. These values were used to correct for

variations in transmitter strength and the corrected total field values were plotted on Map EM-1. The positive total field values were contoured at intervals of 2%. The conductor axes were determined and labelled A, B, C, etc. No priority was attached to the labelling system.

A geological interpretation of the magnetic data plus conductor axes are shown on Map GI-1.


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SDRVEY RESULTS AND INTERPRETATION

The data collected by the magnetic survey form west to west- northwest trending isogams, generally decreasing northward and southward from the centre of the property. The highs are probably caused by a ultramafic intrusive body (serpentinite and peridotite) surrounded by mafic intrusive rocks (gabbro and diorite), see Map GI-1. The ultramafic and mafic intrusive rocks appear to underlie approximately 7 5* of the property, bifurcating to the southeast. The pits, sulphides and nickel mineralization are located in these magnetic highs.

The magnetic values surrounding the highs suggest that the northwestern and southeastern corners of the property are underlain by intermediate to mafic raetavolcanic rocks. The southern contact of the intrusive body trends west, 0.25 miles south of the property. The copper occurrence is thought to lie near the northern contact in the central part of the property.

Linear magnetic lows strike west-northwest and west-southwest across the northern part of the surveyed area. These lows are probably caused by units of felsic metavolcanic rocks, intercalated with the intermediate to mafic metavolcanic rocks.

VLF-Electromagnetic Survey

Two conductive zones, A and B are situated on the property and zone C lies just south of the claim block. Zones A and B are located near the power line and may be caused by culture or may represent underlying bedrock features. Zone A trends northwest along the northern edge of the high defining the position of the mafic intrusive body. This zone could be caused by a small shear zone lying along a mafic intrusive and an intermediate to mafic metavolcanic contact and possibly containing the copper mineralization.


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Zone B is comprised of two short conductors trending west

across the north-central part of the claim group. This zone is

situated near pits, quartz veining and sulphide mineralization and

may represent a mineralized shear in mafic intrusive rocks.

Conductive zone C is located just south of the property. The

conductors appear to be caused by small shears in mafic intrusive

rocks and metavolcanics, striking east-northeastward towards the

southeastern boundary.

CONCLUSIONS AND RECOMMENDATIONS

The maps produced by the data collected by the airborne

magnetic and VLF-electromagnetic surveys provide additional

information which better defines the geology and structures

underlying the Hawley property in Benoit Township. It appears that

75% of the property is underlain by ultramafic and mafic intrusive

rocks. Nickel mineralization has been discovered near the northern

edge of the high outlining the location of ultramafic rocks and

sulphides and quart veining lie in the surrounding mafic

intrusives. The 0.75 mile wide intrusive body narrows and

bifurcates to the east. Bands of intermediate to mafic

metavolcanic rocks underlie the northeastern and southeastern

corners of the claim block. The southern intrusive contact trends

westward, 0.25 miles south of the property, in contact with

metavolcanics to the south. The intermediate to mafic metavolcanic

rocks, to the north, are intercalated with bands of felsic

roetavolcanic rocks.

Two potential shear zones are delineated on the property by

the positions of conductive zones A and B. Zone A lies along a

metavolcanic-mafic intrusive contact and may contain copper

mineralization and Zone B is located over pits, quartz veining and

sulphide mineralization.

GEOPHYSICS LTD

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The potential exists on the property for nickel mineralization

in the mafic and ultramafic intrusion and for gold and/or copper

deposition in the metavolcanic rocks thought to underlie the

northeastern and southeastern corners of the claim block. Further

work on the property is warranted. The claims should be prospected

mapped and mineralization sampled. Underlying geology and

structures should be better defined and extended in overburden

covered areas by conducting ground magnetic and electromagnetic

surveys over the claims. Areas of interest with thin overburden

cover could be stripped and mineralization sampled.

Respectfully submitted by,

H. FERDERBER GEOPHYSICS LTD.

R.A. Caropbe11, B.Se. Geologist

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REFERENCES

Ontario Department of Mines and Northern Affairs, 1971Geological Report 92, Geology of the Bourkes Area and Map 2215 - Benoit and Maisonville Townships, by H. L. Lovell.

Ontario Division of Mines, 1972Map 2205, Timmins-Kirkland Lake Geological CompilationSeries .

Ontario Ministry of Natural Resources, 1979Gold Deposits of Ontario, Part 2, by J. B. Gordon, H. L. Lovell, J. de Grijs and R. F. Davie.

Ontario Ministry of Northern Development and Mines, 1985.

Summary of Field Work and Other Activities, OntarioGeological Survey, Misc. Paper 126, Synoptic Mapping of the Kirkland Lake - Larder Lake Areas, District ofTemiskaming, L. S. Jensen, P. 112.

.

jJJJJJJ1Jl1111JllililililiII

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The potential exists on the property for nickel mineralization

in the mafic and ultramafic intrusion and for gold and/or copper

deposition in the metavolcanic rocks thought to underlie the

northeastern and southeastern corners of the claim block. Further

work on the property is warranted. The claims should be prospected

mapped and mineralization sampled. Underlying geology and

structures should be better defined and extended in overburden

covered areas by conducting ground magnetic and electromagneticsurveys over the claims. Areas of interest with thin overburden

cover could be stripped and mineralization sampled.

Respectfully submitted by.


/f A — ̂R. A. Campbell, B. Se.Geologist

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The potential exists on the property for nickel mineralization in the mafic and ultramafic intrusion and for gold and/or copper deposition in the metavolcanic rocks thought to underlie the northeastern and southeastern corners of the claim block. Further work on the property is warranted. The claims should be prospected mapped and mineralization sampled. Underlying geology and structures should be better defined and extended in overburden covered areas by conducting ground magnetic and electromagnetic surveys over the claims. Areas of interest with thin overburden

c cover could be stripped and mineralization sampled.

JlRespectfully submitted by,


R.A. Campbell, B.Se. Geologist

42AMSE0101 OP91-730 BENOITl

020

COMBINED GEOPHYSICAL SURVEYS, PROSPECTING AND GEOLOGICAL REPORT

ON THEBENOIT TOWNSHIP,

LARDER LAKE MINING DIVISION,RESIDENT GEOLOGY, KIRKLAND LAKE, ONTARIO

Val d'Or (Quebec) December 17, 1991

Peter J. Hawley, B.Eng., B.Se. Geology

P.M. GEOLOGICAL CONSULTANTS LTD. MINING, PETROLEUM AND EXPLORATION855 A. HOSPITAL BLVD.. VAL DOR. QUEBEC. J9P 2N4

TEL: (819) 825-9073 FAX: (819) 8244460

42AOSSE0101 OP91-730 BENOIT 020C

TABLE OF CONTENTS

1. Property Description, Location and Access . . . . . . . . . . . . . . l

2. Geology . . . . . . . . . . . . . . . . . . . . . . . . - . - - - - - l2.1 Regional Geology . . . . . . . . . . . . . . . . . . . . . . - l2.2 Property Geology . . . . . . . . . . . . . . . . . . . . . . . 2

3. Economic Geology . . . . . . . . . . . . . . . . . . . . . . . . . . 33.1 Economic Geology near the Property . . . . . . . . . . . . . . 33.2 Economic Geology on the Property . . . . . . . . . . . . . . . 4

-J. Geophysica'i Survey Methods and Instrument Data . . . . . . . . . . . 4

5. Geophysical Survey Results and Interpretation . . . . . . . . . . . . 65.1 Magnetic Survey . . . . . . . . . . . . . . . . . . . . . . . . 65.2 Electromagnetic Survey . . . . . . . . . . . . . . . . . . . . 7

6. 1991 Prospecting on the Property . . . . . . . . . . . . . . . . . . 10

7. 1991 Geological Program . . . . . . . . . . . . . . . . . . . . . . . 11

3. Conclusions and Recommendations . . . . . . . . . . . . . . . . . . . 15

9. References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 16

Appendix

Appendix 1: Daily Log of Work ActivitieskAppendix 2: Assay Certificates and Sample DescriptionsFig. A: Detailed Geology of Area AFig. 8: Detailed Geology of Area BFig. C: Detailed Geology of Area CFig. D: Detailed Geology of Area D

Back Pocket

-iL-1 Horizontal LOOD Electromagnetic Survey (1777 Hz) HL-2 Hor'zonta 1 Loop Electromagnetic Survey (3555 Hz) Mag-1 Magnetometer Survey VLF-I V.L.F. Survey--i Prospecting Map G-l Geology

PROPERTY DESCRIPTION, LOCATION AND ACCESS

The property of Peter Hawley is comprised of 4 claims, covering 160

acres in lots 10 and 11 of Concession III, Benoit Township, Larder Lake

Mining Division, Ontario. The claims are registered with the Office of

the Mining Recorder in Kirkland Lake and are listed below.

L1151916 L1151917 L1151918 L1151919

The property is located 14 miles northwest of the town of Kirkland

Lake, 17 miles southeast of Matheson, and 14 miles north of the village of

Kenogami Lake. Provincial Highway 11, north from Kenogami Lake, bisects

the property. Bush roads cross the western claims. A gas pipeline lies

trends north along the eastern boundary and a power line crosses the

property, trending northwest and north.

Most of the claims are forest covered. Colvin Lake lies 500 feet

east of the property. The eastern claims exhibit low topographical relief

ana a small hill trends north across the western claims. Outcrop exposure

is fair over the western two claims.

Supplies, services and qualified manpower are availaole in the

Kirklanc Lake-Matheson area.

GEOLOGY

2.1 REGIONAL GEOLOGY

GEOLOGY AND MINERALIZATION

The claim block is located in the western part of the Abitibi

Volcanic Belt of the Superior Province of the Canadian Shield. The

Abit'.bi Volcanic Belt extends for nearly 350 miles in a west-east

direction from Timmips to Chibougamau. It is host to a variety of

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precious and base metal deposits including the Timmins. Kirkland Lake, Noranda, Val d'Or, Matagami and Ch'bougamau mining camps.

The Abitibi Volcanic Selt is composed of a complex assemblage of interbedded volcanic and sedimentary rocks intruded by a variety of irtrusives, from ultrabasic to granitic in composition. The rocks are Archean in age and have been metamorphosed to the greenschist facies. Numerous 'late Precambrian diabase cykes cut formations of the belt. The rocks gene-ally strike east-west, have a vertical dip and are highly folded and faulted. Geological interpretation of the Abitibi Volcanic Belt is complicated by both the wide scattering of outcrop and the complex structural relationships.

2.2 PROPERTY GEOLOGY

The Ontario Division of Mines, Map 2205 - the Timmins-Ki rkl and Lake Geological Compilation Series (at a scale of l inch equal to four miles), Map 2215 - Benoit and Maisonville Townships (at a scale of l inch equals to 1.2 miles) and the Ontario Ministry of Natural Resources Preliminary Map P873 at Benoit Twp., outline the geology underlying the area containing the claims. The Ontario Geological Survey, Mineral Deposits Circular 18, Gold Deposits of Ontario - part 2, 1979, describes the old gold deposits, prospects and occurrences in the vicinity of the property.

The data presented on these maps suggests that the claims are underlain by mafic and ultramafic rocks lying near the southern edge of an rntrusive body. These rocks are comprised of serpentinite, peridotite, gabbro and diorite. They include some zones of basalt and small intrusions of syenite. The contact with the intermediate to mafic metavolcanic rocks strikes west-northwest, 900 to 250 feet south of the property. Approximately 0.5 miles east of the claim group, the mafic and ultramafic intrusive rocks are in contact with

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felsic raetavolcanics, north of the intermediate to mafic

metavolcanics.

ECONOMIC GEOLOGY

The Ontario Geological Survey, Mineral Deposits Circular 18. Gold Deposits of Ontario - part 2, 1979, describes the old gold deposits,

prospects and occurrences in the vicinity of the property.

3.1 ECONOMIC GEOLOGY NEAR THE PROPERTY

The property is located l mile northwest of the past Au-Ag producer, the Davidor Mine. The gold and gold-silver tellurides are situated in northwest striking quartz-carbonate veins and lenses in a carbonate N30*W trending shear zone in mafic metavolcanic rocks. A total of 277 ounces of gold and 50 ounces of silver were produced in 1918 and between 1936 to 1938. The recovered grade was 0.21 oz/ton gold. The Hawley property lies along strike of the shear zone.

The Bergstand gold occurrence is "located 0.6 miles north of the property in a felsic porphyry dyke and quartz veins within intermediate to mafic netavolcanic rocks. Low gold values were reported in a 1921 program of pitting and trenching.

In Benoit Township, within 4.5 miles of the property, numerous gold occurrences have been discovered in metavolcanic rocks; Bunting, Cotterill, Skjonsby, Scotvoid-Nelson, Erickson, Noranda, Thompson-McLeod, Keefe and Car1 son occurrences.

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3.2 ECONOMIC GEOLOGY OF THE PROPERTY

Several pits have been excavated in the central and

northwestern parts of the claim group, uncovering northwest trending

quartz veining, sulphides and nickel mineralization. In 1951 Ole Kagen drilled three holes in this area, intersecting asbestos

veinlets in serpentine. A copper showing (Map 2205) has been found

on the property near the north-central boundary.

4. GEOPHYSICAL SURVEY METHODS AND INSTRUMENT DATA

The grid was established by cutting a baseline east and west from

post l of claim 1151919 in the centre of the property. North-south crosslines were cut at 400 foot intervals along the baseline. All lines

were chained and picketted at 100 foot intervals.

The magnetic survey was completed using a Gem Systems GSM-8 proton

precession aiagnetomter, recurring the total field intensity of the earth's

total field in gammas. It has a sensitivity ancJ repeatability of one

gammas or better. Magnetic readings were taken at 100 foot intervals

along the cross l : nes. A base station for determining the magnetic diurnal variations was established on line OW at 2+50N. The total field

readings, corrected for the diurnal variations were plotted on map ^ag-1.

All values are 58,000 ganmas olus plotted values. These values were

contoured at 100 and 1000 gammas intervals.

The very low frequency-electromagnetic survey was performed

employing a Geonics EM-16 unit with an accuracy of l*. The VLF method of

electromagnetic geophysical surveying uses powerful radio transmitters

set-up in different parts of the *orld for military communications.

Relative to frequencies generally used in geophysical exploration, this

frequency is considered high. These powerful waves induce electrical currents in conductive bodies thousand of miles away. The induced

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currents then produce secondary magnetic fields which are detected at

surface through deviations of the normal VLF field. This secondary field

from the conductor is added to the primary field vector, so that the

resultant field is tit!ted up on one side of the conductor and down on the

other side. The VLF receiver measures the field tilt with the in-phase

and quadrature components of the vertical magnetic field as a percentage

of the horizontal primary field (i.e. the tangent of the tilt angle and

elioticity). The transmitting station of Cutler, Maine (NAA), frequency

24.0 kHz was used.

Interpretation of the results is quite simple. The conductor is

located at the inflection point marked by the crossover from positive tilt

to negative tilt. The main advantage of the VLF method is that is

responds well to poor conductors and has proved a reliable tool in mapping

faults-shear zones, conductive mineralizations and rock contacts. The

major disadvantage is that because of the high frequency of the trans

mitted wave a multitude of anomalies from unwanted sources such as swamp

eoges. creeks and be taken in interpreting the results in certain areas

displaying t~ese topographical features.

In-ohas2 and quacraiure values were recorded at stations 100 feet

apart. I '-.s F .-aser (1968) .nethod of filtering was applied to the raw in-

jraie ra;a. " 'vs red'jct'an method :ransforc.s the zero crossovers to peaks

f:-.- :orto--"pg rur^oses arse helps reduce the geological noise component

:;.;ec '-'z tne * ~~ :~.-,ve~-, h igh transmitter frequency. The Frater

"'i'::-;?: :ata was ;"ct.tec r.-id the oosti.re values contoured at ICo

- -.5 - . a''i : * a.; V.--1. ::--:uct:r axe-:- ~ sre determined and "abellej A, 3.

T :'.:... . - : ;- : r." : v -v^; attacfec to t-3 Tac-el'i-^ system.

7'".: "-izorta! ": oop-e 1 ectronaqnet" c rea,'-:-: were take- at 1IC ~"oc:

: --r;-vi"; .T" :rg trs :"c;r"i-es. An Apex -arametrics ^ax* : .-i II ...r i t ae-s

.-S:d ^f't- a tran-sm-: ts-r-'E : 5-" ver i-eoaratio^ of 3CC reet at ~requenc : es z ~ 1~"7 arc :55b Hz.

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The MaxMin II is designed for measuring the ind^cec SECc'ida; y

electromagnetic field from a conductive body, that is a structure i \^\cr.

conducts electricity better than barren rocks. This particular instrument

has the advantage of flexibility over most other EM units in that it can

operate with different frequencies as well as having a variety of

di stances between transmitter and receiver. Five frequencies can be used

(222. 444, 888, 1777 and 3555 Hz) and with different coil separations.

By analyzing the characteristics of the curves and comparing the '.n-

phase-quadrature ratios, one can estimate width, dio, depth of burial and

conductivity thickness of a particular conductor. A good conductor such

as a massive sulphide or graphitic horizons will produce a cjrve going

from positive tnrough zero to negative and back again to positive. Both

the in-phase and quadrature will show greater deviation in the out-of-

phase component while a body exhibiting better conductivity will have a

greater deviation in the in-phase component.

The data collected by the horizontal loop-electromagnetic survey is

plotted on 2 mps, HL-1 (1777 Hz) and HL-2 (3555 Hz), and orofiled at a

scale of i inch equals 201. Conductor axes were determined, classified

ano "aoellec A, B, C, etc... The labels are applied for identification

purposes only.

5. GEOPHYSICAL SURVEY RESULTS ANO INTERPRETATION

5.1 Magnetic Survey

Map MAG-1 defines a complex pattern of isogams trending east-

southeast to north-northeast across the property. This contour

pattern is further complicated by the great amount of culture on the

property, highway and telephone line along line O and a high voltage

power line crossv-o the eastern claims. Eventhouah data was

collected on line O along the highway, the data wasn't used in

contouring, with the contour lines oeing postulated from data on

-7-

lines 4E and 4W.

The magnetic relief over the property is high, with "local

relief in the northwest corner of the claim group of up to 18,000

gammas. The strong highs (generally over 5,000 gammas) lying in the

northeastern claims must be caused by underlying rocks containing a

high magnetite content probably ultramafic intrusive rocks. At

least 3 sills of serpentinized perdotite appear to underlie the

western part of claim 1151918. These strong highs are surrounded by

areas of relatively high magnetic values suggesting that the

seprentinized peridotite is surrounded by a mafic intrusive body.

These rocks are probably gabbros forming a rough"!y circular body

underlying claim 1151918, the northwestern part of claim 1151919 and

the northwestern corner of claim 1151917. Nickel mineralization and

asbestos has been discovered in the high underlying the northwest

corner of the property.

Lows trending east-southeast across the property are caused by

underlying rocks of low magnetic susceptibilities, probably

intermediate metavolcanic rocks in 4 units. The magnetic values in

the remaining areas are indicative underlying of intermediate to

ma'Mc rocks. These rocks surround the mafic intrusive body and the

4 units of intermediate metavolcanic rocks. The copper occurrence

appears to be in mafic metavolcanic rocks near the eastern end of

the gabbro and near a contact with a unit of intermediate

metavolcanics.

5.2 Electromagnetic Survey

A total of 6 conductive zones (A to F) were delineated on the

nor-.zontal loop-electromagnetic maps and 5 (A to E) on the VLF-

e 1 aeromagnetic maps. The HLEM conductor axes on the two different

frequencies are coincident except for offsets on conductor A, line

4E and conductor E on line O being outlined on the lower frequency

HLE

M

SU

RV

EY

Zone A 6 c. D

Line

12W

8W 4 W

4E 12E

Li, ME

L8E,

L12E

L8W

4W

Topo

grap

hy

or Cu

ltur

e

Alon

g a

ridg

e

Al ong

a ri

dge

In swampy ground

A '1 o

: . 9

t h e

-f o w

j .

1 i n

e .

Magnetics

In

a low

In

a low

Along

the

sout

hern

ed

ge

of

a high.

In

a low

In

a high,

Across the

east

ern

edge

of

a

high.

East of

high.

Stre

ngth

Very

weak

Weak

Very

we

ak

Weak to

mo

dera

te

Weak

to

ve

ryweak

W .

:; H

\- l

-i

moderate

Weak

Weak

Caus

e

Change in

to

pogr

pahi

ea

1 re

1 i e

f .

Change in

to

pogr

aphi

cal

rel ie

f .

Cond

ucti

ve ov

erbu

rden

or

a

change in

re

l ie

f .

Poss

ible

shear

along

a ga

bbro

-maf

ic metavol-

c a n

i c co

ntac

t.

Poss

ible

shear

in mafic

me tavol canic rocks.

C u

1 t u r e .

Shea

r zo

ne across the

east

ern

edge of

the

gabbro body.

Shea

r zone in

mafic

meta

vol canics ea

st of

the

gabbro and

betw

een

2 units

of intermediate

metavolcanics.

E F

0 L4E

L12W

At th

e highway

Top

of

a hi

ll

A 1 o

r i g the

sout

hern

ed

geof

a

low.

In

a low

In

a strong

high .

Weak

Weak to

mode

rate

Weak

Cul ture or

a

mine

ralized

shear

along

the

sout

hern

co

ntac

t of

bedr

ock

inte

rmed

iate

and

mafic

meta

vol canics

rocks.

Poss

ibl

e sh

ear

inin

term

edia

te me

tavo

l-canics .

Over

a

pit

and

along

ash

ear

in se

rpen

t i n

i zed

per id

ot i te

.

VLF-EM SURVEY

Zone A 6 C D E

Topography

L 1 2

W al

ong

a ri

dge

L4W

east of

a

hill

LO

over a

powerl ine

Nort

heas

t of

a

powerl i

ne

Over

a powerl i

ne

Over

the

highway

on

line

0

Magn

etic

s

L12W is

along

the

nort

hern

S

sout

hern

edges

of

a hi

gh.

In a

weak high on

li

ne

12E.

In a

low

Betw

een

2 1 o

ws

Along

a linear narrow

high

.

Caus

e

Same as

HL

EM "A"

on L1

2W and

4E "C"

on

LO.

Poss

ible

sh

ear

on line 4W

.

Line

HLEM an

omla

y "B",

a shear

in mafic

meta

vol ca

ni cs

.

Cul tu

re

Cult

ure

Poss

ibly

caused by

cu

ltur

e on

li

ne

0 and

a sh

ear-

in

a

narrow mafic

meta

vol-

canic

unit

ea

st of

th

eg

abbr

o 6

betw

een

2 intermediate metavolcanic units.

-10-

only. Coincident VLF-Eh and HLEM conductor axes lie on line 12W - Conductor A, lines O and E - conductor E. VLF conductors B, O and A (Line 0) are located near HLEM conductors B and C. Descriptions and possible causes of the KLEM and VLF conductive zones are presented in the following table.

1991 PROSPECTING ON THE PROPERTY

The ourpose of the prospecting program was to locate outcrop exposures, mineralized showings past workings and topographic relief. By noting all the above the geological mapping, stripping and sampling program concentrated in areas with the best mineralized showings and secondary, with outcrop exposure.

Prospecting delineated a large outcrop ridge in the northwest corner of the property. Outcrop exposure is about SOS with steep ridges encountered. On line 12W/10N an excavated pit was found with a rock dump besides, no mineralization was seen but asbestos was present in most samples inspected.

At location 1+20W/3N an old pit was seen containing l-8% pyrite along shear planes. Also found was an old trench 50-60 feet on strike to the northwest. It is believed that this trench is located in overburden.

Along Highway 11 roadcut outcrop sf seen for a considerable length. Near the northern part 2 old workings were found on the east-west side of the highway. Both are located on strike with 1-2 foot shear containing fine pyrite.

Underneath the main powerline rock rubble of bull white quartz veining can be seen everywhere. Some of this rubble has been used to keep the powerline posts upright. Three small outcrop exposures were found in this vicinity with an increase in quartz veining rubble. It is believed

-11-

that the bull white quartz veining has originated from this area. On a knoll just south and east from the road cut outcrop is seen with moderate overgrowth. No other outcrop was located on the property.

7. 1991 GEOLOGY PROGRAM

During the fall of 1991 a geological program of stripping, washing, geological mapping and channel sampling was performed over selected areas of the Benoit Claim group. Results were discouraging in areas with mineralized showings and old working. The findings are discussed in detail below.

In the northwest corner of the claim group a large steep ridge is prominite. This ridge and high relief plateau has very good outcrop exposure and in the extreme N.W. corner an old pit is present. The entire ridge unit appears to consist of peridotite intrusive which has been altered in various degrees with the more altered forming serpentine and asbestos. All channel samples taken reported low values in Au, Cu, Ni over this entire area. A close examination of rock hand specimens show that the olivines and Ca-poor orthopyroxenes breakdown to serpentine. Products form finely disseminated secondary Fe-oxide grains. Decompo sition of these olivine grains begin on the periphery and along internal fractures producing anastomosing veinlets of cross-fiber serpentine or asbestos. Serpentine also contains secondary magnetite, to various

degrees, depending upon amount of alteration, within its matrix. This being the case the peridotite intrusive was probably injected with hydrous solutions, while it was being formed, resulting in certain areas becoming more altered that others. Magnetic high 8 low profiles may determine to what degree these areas have been altered and the geological trend and/or pattern if any of the alteration units.

Area l consists of an old pit sunk along a moderate strong shear striking 160" Az, dipping 72"E. An old trench was also found 50 feet to

-12-

the northwest on strike but appears to have been dug in overburden. This

area was power stripped and washed over an area measuring approximately

150 x 100 feet. The sheared dacite unit in and near the old pit contains

up to 10% fine disseminated 0.25-.50 inch laminae of pyrite within a

highly silicified matrix. The shear appears to have widths between 1.5- 2.5 feet and is viewed over a strike length of 60 feet. Assay results

display disappointing low Au, Cu, Ni values. In this area the dacite unit exhibits flow textures especially near the contact with a face change of

pillowed andesites. Bull white quartz veinlets are seen at the contact

wh:ch strike 170" Az and dip 700 to the east. The veinlets are barren as

seen by assays taken. The relick pillow rinds are poorly preserved but in areas viewed may indicate tops facing east.

In area 2 outcrop exposure along the Highway 11 allows one to view

the units as a cross section. At the northern end previous working of an old trench was found along and E-W trending shear. The dacitic unit is

moderately sheared, highly silicified and contains up to 105 fine disse

minated pyrite along the shear fabric. Fine micro-cubic pyrite with

concentration between 1-21 appears consistant throughout the unaltered

rock. The shear zone is very consistant and viewed over a strike length

of at least 150 feet with widths between 1-2 feet. The same shear zone is

present in Area C on the opposite side of the highway where an olc pit has been sunk.

Along the Area 2 exposure, which faces west, steeply dipping

jointing patterns are present which strike 220" Az and dip 75" south. Near

the bottom of the outcrop exposure a small flat shear bisects the unit

throughout with the trend of 22" Az strike and dipping 20" west. Also seen

near 3+00 north is the contact between the dacitic flow unit and andesitic

pillows which dips 750 E. Here the pillows can be seen as a globular mound

with the jointing pattern prevalent throughout. Again a norm of 1-21 fine micro-cubic pyrite is consistant throughout. Samples taken in this area reported low assay results.

-13-

In Area 3, which faces east, similar rock units are present. Near the north outcrop exposure a large pit has been sunk by previous workers along the previous described E-W trending shear zone. The shear is also highly silicified and along with containing ID-12% fine disseminated pyrite also exhibits globs of concentrated pyrite. Trace to 2\ magnetite is also contained within the sheared dacitic unit. The rocks in this area contain a norm back ground of X-2% fine microcubic pyrite within their matrix. The prevalent jointing pattern is common throughout with the same attitude as described above. Globular pillows and pillow rinds can be seen both or, top of the exposure and in section and again may indicate tops facing east but the pillow noses are not well decerned. At 2+50 north a small shear is seen which is not present on the west outcrop exposure. This shear exhibits the attitude of 110" strike with a dip of 450 north and has a 2-3 inch smokey grey quartz vienlets injected along the shear fabric. The vein contains 2-35 fine disseminated pyrite and samples taken reported low values.

Area 4 is an extension of Area 3 on top of a knoll 80 feet to the east. A stripped and washed area of approximately 160 x 80 feet was cleared. The outcrop exposure revealed the same jointing pattern with .25-1 inch bull white veinlets seen in area following the jointing trend. These veinlets do not have considerable strike length and samples taken reported low-nil values. Again the background norm of 1-21 fine micro cubic pyrite is present throughout.

Near the same area but 60 to 100 feet north are three small outcrop exposures under the main hydro line. These exposures contain a fair amount of bull white quartz veining rubble. Surface stripping by grub hoe revealed E-nl trending vein system(s) with the average width of the veining between 0.5-1.0 feet. One vein was followed along strike for a distance of 30 feet before pinching out. The bull white quartz veins are hosted in dacite with the vein injected along a fracture. The veining contains l-4t fine disseminated pyrite with Trace to \\ chalcopyrite. The best channel sample taken assayed 0.003 opt Au, Q.01% Cu/2.0 feet. The following is a description for channel sample.

Sample Number

0677

0678

0679

0680

0681

2456

2457

2458

2459

2460

2461

2462

2460

Rock Description

Sheared dacite with smears of S-10% pyrite, 1-21 pyrrhotite.

Silicified dacite with 30S quartz within matrix, sheared, rehealed, 51 pyrite, 31 pyrrhotite, 11 chalcopyrite

Sheared basalt, fine grained, slightly silicified, S-5% pyrite.

Bull white quartz vein, 3-6", sheared in parts, 1-33; pyrite, Ilk pyrrhotite.

Peridotite, serpentinized with micro asbestos fibres, 0.25", veinlet of pyrrhotite.

Bullwhite quartz vein with dacite, contact, 2-3S pyrite, trace-1% chalcopyrite.

Bullwhite quartz vein andecite contact, 6.0 ft NE on strike from #2456, 61 diss. pyrite, trace chalcopyrite.

Dacite with .25" laminae of diss. pyrite along weak shear plane.

Basalt, highly silicified, 1-41 diss. pyrite within chloritic matrix, l-2% chalcopyrite.

Bull white quartz vein, weakly sheared, rehealed 1-21 fine diss. pyrite suspended within matrix.

Bull white quartz vein massive, trace-1% fine pyrite.

Serpentinized peridotite, soft, talcose. 0.12-0.25" veinlets of pyrite/ pyrrhotite.

As above (re-assay)

Width (ft)

2.0

2.0

0.5

0.5

0.5

1.0

1.5

2.0

2.5

0.5

2.0

1.0

1.5

Au Opt

trace

Nil

trace

Nil

—

Nil

trace

trace

0.005

trace

0.003

trace

trace

Cu l

0.018

0.017

— —

—

0.002

0.023

0.016

0.032

0.210

0.017

0.010

0.009

0.056

Ni 1

0.006

0.002

— —

--

0.064

0.005

0.005

——

—

—

—

—

-15-

8. CONCLUSION AND RECOMMENDATION

The results of the 1991 prospecting, stripping, washing, geological mapping and channel sampling are disappointing. Previous airborne survey work indicated magnetic high and low trends in the north west corner of the property. These trends can now be explained by the presence of a serpentinized peridotite which contains various amounts of magnetite within its matrix. Along the micro layered or platty fabric thin laminae of pyrrhotite is present with the best channel sample assaying Q.064% Ni. Other sections of the property near the main Highway 11, (areas A, B, C, D) exhibit well developed shear zones, quartz veins and veinlets, which show that the mineralized trending units are shear related. All channel samples taken reported low Au, Cu, Ni values. What is of interest is the norm background of 1-21 fine micro cubic pyrite constantly throughout the dacite unit in this area. One possible explanation of poor assay results is that a free Fe ion from a Fe 3* to Fe 2* exchange has been incorporated into the dacite matrix. If this is the case then the lack of free Fe would inhibit the deposition of auriferous mineralization. Whole rock geochemistry should confirm this hypothesis.

The conductive zones are generally weak to very weak in strength. The sheared peridotite was picked-up on line 12W. On the property HLEH conductive zones (A(4E), B(12E), and (8W, 4W) define the positions of weak narrow shear zones in underlying mafic metavolcanics and gabbro in overburden covered areas.

Thus it is recommended that no further work be performed on the property due to the lack of economic mineralization anywhere.

Respectfully submitted by,

-16-

REFERENCES

H. Ferderber Geophysics Ltd., 1990Report on the Airborne Magnetic and VLf-electromagnetic survey on the Property of Peter Hawley, Benoit Twp., Larder Lake Mining Division, Ontario, R.A. Campbell.

Ontario Department of Nines and Northern Affairs, 1971Geological Report 92, kGeology of the Bourkes Area and Hap 2215 - Benoit and Maisonville Townships, by H.L. Lovell.

Ontario Division of Mines, 1972Map 2205, Timmins-Kirkland Lake Geological Compilation Series.

Ontario Ministry of Natural Resources, 1979Gold Deposits of Ontario, Part 2, by J.B. Gordon H.L. Lovell, J. De Grijs and R.F. Davie.

Ontario Ministry of Natural Development and Mines, 1985.Summary of Field Work and Other Acitivities, Ontario Geological Survey, Misc. paper 126, Synoptic Mapping of the Kirkland Lake - Larder Lake Areas, District of Temiskaming, L.S. Jensen, P.112.

APPENDIX l - DAILY LOG OF WORK ACTIVITIES

June June June Aug. Sept Sept Oct. Oct. Oct. Oct. Oct.

22. 199123. 199124. 199131, 1991

. l, 1991. 2, 19911. 19912. 19913. 19914. 19915. 1991

Oct. 5, 1991 Oct. 7, 1991 Oct. 8, 1991 Oct. 9, 1991 Oct. 10, 1991

Detailed Magnetic Survey Claims 1151918 S 1151919 Detailed Magnetic Survey CI a i us 1151916 ft 1151917 Detailed VLf-EM Survey Claims 1151918 ft 1151919 Detailed kVLF-EM Survey Claims 1151916 S 1151917 Detailed H. L. E. M. Survey Claims 1151918 ft 1151919 Detailed H. L. E. M. Survey Claims 1151916 ft 1151917 Prospecting Claims 1151919 S 1151918 Prospecting Claims 1151918 Prospecting Claims 1151916 t 1151917 Prospecting Claims 1151918 ft 1151917 General Geology, Mapping t,Sampling Claims 1151918 ft 1151919 Same as above Claims 1151916 ft 1151917 Detailed mapping and sampling Claims 1151918 t 1151919 Detailed mapping and sampling Claims 1151918 t 1151919 Detailed mapping and sampling Claims 1151916 ft 1151917 Detailed mapping and sampoing Claims 1151916 S 1151917

C.P. l P.O. 5GO 1481, AVENUE PERREAULT VAL D-OR (QUEBEC) J9P4P5 TEL: 18191824-4337 FAX: 1819)824-4746

LABORATOIRE D'ANALYSE BOURLAMAQUE LTEE

BOURLAMAQUE ASSAY LABORATORIES LTD.

P.H. Geological

Project Benoit

RockECHAimLLONS SAMPLES ......

CERHFICAT D'ANALYSES CERTIFICATE OF ANALYSIS

~"i^58711

16RGCUDE - . r. iRECEIVED FROM .......Peter..Hawley..

VAL D-OR KWtBECl

6 Au, 5 Cu, 5 Ni

91

Sample No. Au oz/ton

677678679680681

24562457

Trace Nil

Trace Nil

Nil Trace

Cu_*

0.0180.017

0.002

0.0230.016

Ni_\

0.0060.002

0.064

0.0050.005

C.P. l P.O. SBO 148. AVENUE PERREAULT VAL ITOR (QUEBEC! J9P4P5 TEL: (819) 824*4337 FAX: (819) 8244745

LABORATOIRE D'ANALYSE BOURLAMAQUE LTEE

BOURLAMAQUE ASSAY LABORATORIES LTD.

P.H. Geological

ECHANTIUJONS RockSAMPLES .....,.................

CERTIFICAT D'ANALYSES CERTIFICATE OF ANALYSIS

L*. 58810

VAL D-OR (QU6BEC. .. ..?.9................. 19 .....-?.1

recuoE Peter Hawlev ANALYSES fi AU 6 CuRECBVB) FROM ......."e.V:e.f...??".4.e.X................................. ASSAYS ......?...*-**f....r....V.H.

Sample No. Au oz/ton

245824592460246124622460

Trace 0.005 Trace 0.003 Trace Trace

Cu

0.0320.2100.0170.0100.0090.056

— I +OOW

OLD HIGHWAY II

LE

OE

NO

2b

Dac

ite,A

ndes

lte,in

clud

ing

Pillo

w

Lava

's

1 Q

uart

z V

tlnt,w

idth

in In

ches

Quo

rtz

Vein

C

halc

opyr

ite

PyH

te

Pyrr

hotit

e.P

illow

s w

ith to

ps I

ndic

ated

G

eolo

gica

l C

onta

ct

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ting

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PI

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ren

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/ Sh

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ith O

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SCA

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" *

20*

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Py A

AR

EA

2

CR

OSS

— S

EC

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N

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20 F

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—

15

FEET

—

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FEE

T

5 FE

ET

AN

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SIT

IC

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LO

WS

20*

W ^W

S

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S*~

f S

**

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l S O

HIG

HW

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88 •f CM

FIG

.. B

8 10

8 •i- ^r

60*

o o (O

AR

EA

3

CR

OSS

— S

ECTI

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2b Cpy

Py i o

LEG

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Doci

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cludin

gPi

llow

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's Ou

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V*ln

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Gtol

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rike

with

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E l"

* 2

0'

20 F

EET

—

15 F

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—

10 F

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—

5 FE

ET

—

AN

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SIT

IC

PIL

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S

o o 4-

O)

o o •t- IO

HIG

HW

AY

II

8 •i-o o * K)

FIG

. C

o o * CJ

z o o •4-

o o 5 CD

UJ o o 61-0

0 N

—

5+

00

N —

4+O

ON

—

AR

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4

2456

XI.O

',2-3

0XoP

y •T

r-l'/o

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-Nil A

u,.0

230X

*Cu,

.005

0XoN

I

AN

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ITIC

PI

LLO

WS

I700

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40

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L6Q

ENO

Doc

itt.A

ndtil

tt, in

cludin

gPi

llow

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'tQu

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t,wid

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olco

pyrlt

t Py

rltt

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.Pillo

ws w

ith to

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ttd

Gtol

ogico

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with

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- **^^^^

H

Ho

v

G]o

CD 10 01

DA i r. 01 issur

LARDER LAKE MINING RFCORnriVS OFFICE

".DWBHiP SUBJECTCook Twp.

'(T s3ESTRY

^s*vJ~- JrJTT i' w!

NOTICE OF FORESTRY ACTIVITYTOWNSHP 7 AHEA FALLS WITHW THE ___ i

WATABEAG MANAGFMENT UNIT Maisonville Twp.H D

MAY BE SUBJECT TO FORESTRY OPERATIONS. THE MNR UNIT FORESTER FOR THIS AREA CAN BE CONTACTED AT: P.O BOX "

TMC INfOMMATION THAT APPEARS ON THIf, MAP HAS RFKN OOMPILFD f I1OM VARIOUS SOUnCFS, AND ACCURACY IS NO l GUARANTFrn THO8FWISHING TO STAKl. MIN ING CLAIMS SHOULD CON SULT WITH TUP MINING nrcoROFR, MiNisrtw or*IORTHFRN OFVl-LOI* MFNI ANDMINFS. FORAI) DIMONAl INIOMMA1ION ON IMF 'HAHr, O!' THEi ANnr, SHOWN unuoN

THE TOWNSHIP OF

BENOITDISTRICT OF COCHRANE

LARDER LAKE MINING DIVISION

SCALE: 1-INCH-40 CHAINS

LEGENDPATENTED LAND '

CROWN l AND SALELEASESLOCATED LANDl ICENSC OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKlNGjr, HIGHWAYSRAILWAYSPOWER IINTSMARSH OR MIJSKFG

* or (p)

or CS(D

Loc LO

M R O S R O

"'/y l f N TFO S R O

NOTES

400' Surlar* nqM* ie*orvnli0n around all laU*nv c -^

Grovfl Rpsfrvp Shown Thus. |"

•mo' fronlngf on fUilli , l uKp withdrawn Iriiin r^pn'-.ition for proposed summer i' ,oi t

Si* * thdrtiwri fro^n Unltinq unclwr Section if Ihp Miiguiq At l i '

w Fil* Dnt^

PLAN NO.-M.326"/Oii J \Kli-

Or NATuPM REiOURCES' o AND MAi'KlN(; BKANi ri

POK IT O

l

k) C/I

m r ,

r*~

i"t

Q)

4M08SEU101 OPOl"-Ho BENOIT200

l

TRAIL .—

TYPE OF WORK

CLIENT

PROJECT

O >

HfN

Wl :

CLAIM MAP

i" /, mile

Vj"l

LEGENDTOTAL FIELD CONTOUR INTERVAL ? CONDUCTOR AXIS FIDUCIAL POINT LINE DIRECTIONSTATION USED: Ci ITLEK, MAINE, USA Ci40 U \i )

LESS THAN ZERO

AIRBORNE V.LF-EM SURVEY

PETER HAWLEY

H t l* t H. Ferderber Geophysics Ltd.

AREA

BENOIT TWP.ONT

SCALE'/4 mile

DRAWN BY

DATEJUNE 1991

MAP OH SHH1 NOEM-1

42AOBSE0101 6pei-73b BENOIT 210

K\V

7

TRAIL —.

'o,

TYPE OF WORK

CLIENT

PROJECT

BENOIT TWP

CLAIM MAP

bcnle l - 7. mile

N

LEGENDTOTAL FIELD CONTOUR INTERVAL 20

O FIDUCIAL POINT > LINE DIRECTION

BASE VALUE seooo GAMMASMAGNETIC LOW1000 GAMMAS 100 GAMMAS 2O GAMMAS

GAMMAs

AIRBORNE MAGNETIC SURVEY

PETER HAWLEY

H. Ferderber Geophysics Ltd.

AREA

BENOIT TWP,ONT

SCALEmile

DRAWN BY

DATEJUNE 1991

MAP OR SHU t NOMG-I

42A08SE01Q1 OP91-730 BENOIT 220

BENOIT TWP

f| AIM MAC

N)

LEGEND4

3

2

l

Cu

Ni

qs

ULTRAMAFIC INTRUSIVE ROCKS

MAFIC INTRUSIVE ROCKS

FELSIC METAVOLCANIC ROCKS

INTERMEDIATE TO MAFIC MFTAVOLCANIC HOCKS

COPPER

NICKEL

QUARTZ

SULPHIDES

SYMBOLSCONTACT (inferred from magnetic data)

CONDUCTOR AXIS (with label J

B1-730 BENOIT230

——^ f \ iT,5'

1 ? oI 4-c

Q PIT

4 OCCURENCE

TYPE OF WORK

GEOLOGICAL INTERPRETATIONCLIENT

PETER HAWLEYPROJECT

ft^\ Rflr*—^V^y'i) H Ferderber Geophysics Ltd.

AREA

BENOIT TWP.OIMT

SCALE n .1 - /4 mile

DRAWN BYMV1

DATEJUNE 1991

MAP OR SHEET NOGl-l

1 l 1 1 -l l 11 H

IO+OON '

~

5 + OON

P1/NSISI6

P2/II3I9I9 PI/1079048

SYMBOLS

HIGHWAY MOLD ROADBUSH ROADHYDRO LINEBURIED TELEPHONE LINECLAIM POST (LOCATION FOUND)CLAIM POST (APPROX. LOCATION)

EGEND

OUTCROPOUTCROP BOUNDARYTRENCHPITRIDGESWAMP

42A088F0101 OP91-730 BENOIT 240

PROSPECTING MAP

BENOIT TWP. ONTARIOScale f- 200'

Dm K B C

Work by: P. HAWLEY

Date N OV. '91

Map No p— |

K

10+OON

5 + OON

PV6JI24B P4/8SJB66 PJ/IOZ04 J P4/HSI9IU PS/ II S I9i8

BL O+OO

5+00 S

PI/ IHI9I8 P4/HSI9I7

kj ^i -j

l'4/ IIM'118

IM l I I M t it

IO+OOS

5-107. P y 1-27. Po

AREA l

PI/8C58M P2 /IOI BIO

P l/lfl J699

PI/495610

P l / 1 1 5 1 1 1 (, P2/IISI9I?

T

g

SYMBOLS

HIGHWAY IIOLD ROADBUSH ROADHYDRO LINEBURIED TELEPHONE LINECLAIM POST (LOCATION FOUND)CLAIM POST (APPROX. LOCATION)SWAMP

LEGEND3b 3c2b Mqv3"

AsbCpyPoPy

AREA

GABBROSERPENTINIZED PERIDOTITES,ASlIrE4AM9E.SlTE ' INCLUDING PILLOW LAVA'SQUARTZ VEINS,WIDTH IN INCHESASBESTOSCHALCOPYRITEPYRRHOTITEPYRITESTRIKE WITH DIPGEOLOGICAL CONTACTOUTCROP BOUNDARYTRENCHPITRIDGESHEARSEE DETAIL GEOLOGY MAP

42AOBSEQ101 OPB1-730 BENOIT 250

GEOLOGY MAPBENOIT TWP. ONTARIO

'w ole l" .'OH

Dm K B

Work by: R HAWLEY

NOV '91

Mop G~ l

P4/ MSI9IB

950Q

10+OON

5 + OON

P4/853B66 P3/IOZ94J P4/II3I4IQ P3/ IISI9IS

BL OiOO

5+OOS

10+OOS

SCM

-09O

II

liIP

BL-NOITl" OP

L

!WP

(C UN

L 10

CLAIM MAP

Ar;B D

SYMBOLS

HIGHWAY 11OLD ROADBUSH ROADHYDRO LINEBURIED TELEPHONE LINECLAIM POST l LOCATION FOUND) CLAIM POST (APPROXIMATE LOCATION)

LEGENDMEASUREMENT STATIONS ALONG PICKET L INES

READINGS OF EARTH'S TOTAL MAGNETIC FIELD

RECORDED READINGS ARE 5 8,000 PLUS PLOTTED VALUES

FORCE OF THE EARTH'S MAGNETIC FIELD (IN GAMMAS )MAGNETIC CONTOURS

BASE STATION

ELECTRICAL CONDUCTOR

INSTRUMENT USED : GEM SYSTEMS GSM-8

MAGNETOMETER SURVEY

BENOIT TWP, ONTARIOScale f- 200'

Dm K B

Work by. P HAWLEY

Date OCT / 1 991

Map No MAG-l

l U5I9I8

i o

270

CLAIM MAP' Scale i 1 50.000

[]

SYMBOLS

HIGHWAY IIOLD ROADBUSH ROADHYDRO LINEBURIED TELEPHONE LINE

CLAIM POST i LOCATION FOUND)CLAIM POST (APPROXIMATE LOCATION)

LEGENDMEASUREMENT STATIONS ALONG PICKET LINES ELECTROMAGNETIC READINGS - In Phase Component ELECTROMAGNETIC READINGS - Out of Phase Component W PROFILE - In Phase Component (Scale l" = 20 96) PROFILE - Out of Phase Component (Scale l" ~ 20 y*) COIL SEPARATION - 300 Feet INSTRUMENT- APEX PARA METRICS MAX MIN u ELECTRICAL CONDUCTOR POSc iRL F

- PENNATE

HLEM SURVEY 1777 Hz

B t NOIT 1WP ONTARIO

Work by P HAWLEY

NOV '91

M i,, rj.. H L -

"" f 'D.ttoi * U

ki

N

1 1 1 \ l M * l t,

1 f l l l M ') l l

T ^1l" s i , 'V-4 vT *" - v

-|Q ' *- \*

v .' 'l-K.; ^ *~-*.-**-i-JZ-Z-^Tf

LI l :r ,M l I WlN

CON

V,\.

CLAIM MAP',l Illf l SO,OUO

illdhWM II nth HI iA iHUSH U'l/u-

il II" i 'j|

h i'. H i- l l , l l MDNI l INF

' ! ^iM l '' t ( l Q( A l ION FOUND

le' -' i

LEGENDMEASUREMENT STATIONS ALONG PICKET LINES ELECTROMAGNETIC READINGS - In Phase Component ELECTROMAGNETIC READINGS - Out of Phase Component PROFILE - In Phase Component (Scale l" * 20 %) PROFILE - Out of Phase Component (Scale l" ^ 20 y*) COIL SEPARATION - 300 FeetINSTRUMENT- A PEX PARAMLIRICS MAX- MINI

ELECTRICAL CONDUCTOR - POSSIBLE"DEFINATE

HLEM SURVEY 3555 Hz

BENOIT TWP. ONTARIOl (H

h M

Work by P HAWLEY

:-,i, NOV 91

H L- 2

k. (t)•vi

PI/ IHI9I8 P4/IISI9I7

ki ^-vj

P*/ II9I9I8

10+OON

5 + OON

PI/II51916 |5 IO P 2/IISI9I7

P1/6JI24H P4/83JB66 PS/IOZ943 P4/II3I9I9PJ/II3I9I8

O+OO

5+OOS

PJ/IIJI8I9

IO+OOS

42A088E010lpfl1 290

Ut

'ic 1

NOI 1

\* '

\\

L 1!

CLAIf

|DTWIJ

\*^ "1

v'vbX^

L 10

iN

CON III

\\A M AP

' i III, 1 M 1 1 II M 1

SYMBOLS

H K .K WAY II

01 D HOAO

HUSH HOAO

HYDRO l INLHum L D TELF PHONE LINE

( l AIM CO', f l LOCATION RHl l.A|M POM ( APPROXIMAU UK.

LEGENDMEASUREMENT STATIONS ALONG PICKET LINES

FRASER REDUCTION METHOD USED

CONTOUR INTERVAL : - i o 7U

ELECTRICAL CONDUCTOR

INSTRUMENT USED : GEONICS EM - 16

STATION USED: CUTLER MAINE (240 KHZ)

FRASER FILTERVLF- E M

BENOIT TWP. ONTARIOSeul p l - ?.OO'

Drn K B

Work by Peter Hawley

Dote Oct, 1991

Map No VLF - l

h. ferderber geophysics ltd, j geology r.a. campbell, b.se. j

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