32D04NW0377 OP92-282 ARNOLD 010

VICTORIA LAKE PROPERTYMORRISETTE, ARNOLD, LEBEL TOWNSHIPS, ONTARIOLARDER LAKE MINING DIVISIONO.P.A.P. FILE NUMBER OP92-282

FINAL REPORT

Graham Long, B.Sc., Geologist

PiO i

TABLE OF CONTENTS

Page Summary i

1 .0 Introduction............................................................................................ 1

2.0 Property Location and Access........................................................ 1

3.0 Land Position......................................................................................... 3

40 Previous Work...................................................................................... 3

5.0 Geology.................................................................................................... 55.1 Regional Geology,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 55.2 Property Geology,,,,,,.,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 9 Q

5.2. 1 Stripped Zone * 1 ,,,,,,,,,,,,,,,,,.,,,,,,,,,,,,, 1 45.2.2 Stripped Zone *2,,,,,,,,,,,.,,,,,,,,,,,,,,,,,,, 16

6.0 Geophysics,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 186.1 Instrumentation and Survey Procedure.,,,,,,,,,,,,, 18

6. 1 . l Magnetometer.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 1 86.1.2 VLF EM- 16,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 19

6.2 Results,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 196.2. 1 Magnetometer,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. 1 96.2.1 VLF EM- 16,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 19

7.0 Conclusions and Recommendations,,,,,,,,,,,,,,,,,,,,,,. 20

References.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, 22

Figure 1 Claim Location MapFigure 2 Geology of the Abitibi Greenstone BeltFigure 3 Geology of the Timmins Kirkland Lake AreaFigure 4 Sample Location Map- Morrisette and Arnold TownshipsFigure 5 Sample Location Map- Island in Victoria LakeFigure 6 Stripped Zone* l - Detai led Geology MapFigure 7 Stripped Zone*2- Detailed Geology Map

Appendix 1 Statement of QualificationsAppendix 2 Legend- Geological SymbolsAppendix 3 Sample DescriptionsAppendix 4 Assay Sheets

Table 1 Table of Lithologies

SUMMARY

During the 1992 field season the Victoria Lake Property situated

approximately 10 Km northeast of the town of Kirkland Lake, and 1 Km

northeast of the town of King Kirkland, Ontario, was subjected to an

exploration program financed by O.P.A.P. grant No. OPG92-146 and the

author.

The program consisted of establishing a grid system along a strike

length of 2.8 Km, over a portion of the Murdoch Creek Fault Zone which has

remained relatively untested to date. A geophysics program consisting of

gradient mag and V1F was carried out over the grid as well as geological

mapping and prospecting. The remaining areas outside of the grid and

within the property boundaries were selectively examined for their

economic potential.

This report covers in detail the results of the exploration program.

1.0 INTRODUCTION

An exploration program carried out on the Victoria Lake Property,

held in good standing by Mr. Glenn J. Mullan, of Dubuisson, Quebec, was

carried out during the 1992 field season. The program conisted of

establishing a grid system covering approximately 2.8 Km of strike length

over a relatively untested portion of the Murdoch Creek Fault Zone, which

is a splay off of the Kirkland Lake main break.

Lines were spaced at 100m intervals and stations established every

25m.

Geophysics consisted of a gradient mag survey as well as a one

station VLF survey. Geological mapping and prospecting was carried out

over the grid as well as detail mapping and sampling of two stripped zones

produced by a previous company.

Ground outside of the grid system was selectively chosen for

prospecting and sampling.

2.Q PROPERTY LOCATION AND ACCESS

The 43 claim property is located approximately l Km northeast of the

town of King Kirkland and some 10 Km northeast of Kirkland Lake, Ontario

(see Figure 1). The ground is within the Kirkland Lake resident geologists

area and encompasses the intersection of Morrisette, Arnold and Lebel

townships. All of these townships are in the Larder Lake Mining Division,

District of Timiskaming and covered by N.T.S. map sheet 32D/4 The

intersection of the townships is located at latitude 48* 11'23" and

longitude 79*53'l O".

MORRISETTE TWP

982340,1 982341 ] 982342 '! 111152411 \\ 1930 , 1111929 , 1111926 ( 1111925

,__j__j__\,^Jr---A--r-'—^-^-982339, 1 982338 ' 1111525 Jl H1932-] 1111931J 1111928 j 1111W7 ]'rfl1924

MURDOCH CREEK FAULTJONE (APPX. LOCATION)

B MISEMA LAKE- MIST LAKE FAULT ZONE ED HARGREAVES (APPX. LOCATION)

Lia KENAKOTT-KIRKLAND

KIRGOOD

' l 982335

982327 i 982330 982333 l 982336

LEBEL TWP

982326 i 982331982332 , 982337

ARNOLD TWP

N

VICTORIA LAKE

,'JBIDGOOD MINE ROAD TO KING KIRKLAND j)

l ,^--*''* f,' a

_______\\ BIDGOOD *2 MINE________

VICTORIA LAKE PROPERTY

CLAIM LOCATION MAP

_____meters- -

O 500 1000

Figure

The property Is easily accessed by by taking the Bidgood Mine

road,from highway 66, northeast to the south end of McTavish lake where a

boat can be launched thereby accessing the central portion of the claim

group. This is also the best access to the peninsula and island located in

Lebel township. A gravel road leading north from the town of King

Kirkland, cuts the northwestern corner of the property and gives access to

old skidder roads and footpaths on the property.

An old road leading in a southwesterly direction from Esker Lakes

Provincial Parks road, and located just north of the North Arm of Victoria

Lake, leads to the Ronal Red Lake shaft area located at the most northern

portion of the property.

30 LAND POSITION!

The 43 unpatented mining claim property is held in good standing and

1005? owned by Mr. Glenn J. Mullan of Dubuisson, Quebec.

40 PREVIOUS WORK

As far back as 1936, the property was considered to hold high

potential for an economic deposit as is suggested by the add by Kenakott

Kirkland Gold Mines Ltd. appearing in the September 3,1936 issue of the

Northern Miner. The add states that the property is similar to those on the

West Kirkland Lake camp and contains similar host lithologies to those on

the Bidgood property lying emmediately to the south. A vague reference to

free gold is made in the add stating that the occurence is located at the

intersection of two shear zones located in the eastern portion of the then

existing property.

In 1947, Ronal Red Lake Gold Mines Ltd. carried out prospecting,

mapping and drilling in the area of the Ronal Red Lake shaft, on the George

Tough claim group, which is encomposed by the present day Victoria Lake

Property.

Numerous shears were discovered in the outcrop and as a result some

stripping in two locations as well as eight (8) x-ray drill holes were put

down. None of the core samples contained any significant amounts of gold,

but grab samples containing as much as 2.05 oz/t (S71.75 gold at 135/oz)

were reported.

More recently in 1989 the the property was subjected to a combined

airborne magnetic and VLF-electromagnetic survey carried out by

H. Ferderber Geophysics Ltd for Trinity Explorations Ltd. The survey

outlined 5 potential fault zones and three probable shear zones.

In 1990 under option to Pamorex Minerals Inc., the company stripped

and sampled two areas over the Murdoch Creek Fault zone. Of particular

interest was an assay of 0.18 oz Au/ton over a 3 foot length.

5.0 GEOLOGY

5.1 REGIONAL GEOLOGY

The townships of Morrisette, Lebel and Arnold are located in the Abitibi

Subprovence which itself is located in the southeast margin of the

Superior Structural Province. The Abitibi Subprovince, more commonly

refered to as the Abitibi Greenstone Belt, encompasses the town of

Timmins , Ontario in the west, Val d'Or, Quebec in the east, and the towns

of Matagami and Chibougamau, Quebec in the North (see Figure 2).

The Abitibi Greenstone Belt is a folded geosynclinal belt consisting of

volcano-sedimentary lithologies(see Table 1). All of the rocks , with the

exception of proterozoic intrusives, are Archean in age and have been

metamorphosed to the subgreenschist facies. Numerous igneous intrusives

including stocks, dikes and sills crosscut all of the rocks of the belt. The

major structural features of the greenstone belt consist of the

Destor-Porcupine fault in the north and the Cadillac-Larder Lake fault in

the south (see figure 3). These two deep seated fault zones are responsible

for numerous gold deposits.

The volcanic rocks were formed during cycles of volcanism that

consisted of komatiitic volcanism followed by tholeiitic, calc-alkaline,

and ultimately alkalic volcanism. The rocks of each group are refered to as

a supergroup. A supergroup is divided into groups according to major

changes in the chemistry of the rocks (Jensen, 1981).

ABITIBI , l. /s- GREENSTONE Ji

Abitibi Greenstone Belt

Granitic rocks

Mafic intrusions

Ultramafic rocks

Early Precambrian sediments

Km

40 60 Mi

Middle Precambrian sediments

Volcanics

Munro Group(Goodwin and Ridler. 1970)

en

Figure 2. Geology of the Abitibi greenstone belt (after Goodwin end Ridler 1970)

LAKE ABITIBI t t'l 1^1 i l i

'BATHOLITH'••-t-^^^'-vV'Vii-^v/c;- s;-V-"-^^ ,\,:r^jl'.V'f

!^^\ \ xk-

It t t t t t t t \.K t tttttttl

^J\t t t t t t t \t t t t t t t tttttttltttttttl tttttttl

.,,,. ttttttt 1

v v v v v v LAKE V vvvvvvvvv

"- "

tit t t t t t |t t 1*i-'- 'N-./ 'J T l. t t t t t 11 t t |"'r''''.-VVt \ t t t t t V t t - ,: l l - , \

t tV ttttttt t'irs /V."^\

KENOGAMISSI ltt t t fiU;. -;V'^n ATI i^^i ITL i T l t t It TT, - '~. i x

~^ i ' .C* t -* l - ^ v~, ' '-., ^'''TTTTTTTTTT T I TT T I IT,^.,, ;: ^'^:'rr ;,;-,- MATACHEWAN VtttVttt t t ttVttt t t tt t t tt ttVt'f: "'-';'' ''T" '^^'Wt^tSVS-ROUND LAKEtVtVlVtVtVtV

t tt\^tt TttBATHOLITHttttttt t ttttttttttttttttttttt

LEGEND

UPPER SUPERGROUP

Alkalic Volcanics(Timiskaming Group)

Calcalkahc Volcanics

( Blake River Group) Tholeiitic Volcanics

(Kinoievis Group) Komatiilic Volcanics

(Stoughton Roquemaure Group and Larder Lake Group)

LOWER SUPERGROUP

Sedimentary Rocks ( Porcupine Group)

Calc-alkalic 4 Tholeiitic Volcanics

(a Skead S Catherine Group) (b.Hunter Mine Group)

Komatiitic Volcanics

(WabewawaGroup)

O 12 Mi

20 Km

Figure 3. Geology of the Timmins-Kirkland Lake area (after Jensen 1978)

8

Table 1: Table of Lithologies

CENOZOIC

Pleistocene and RecentGlacial tills, esker deposits, proglacial lacustrine sands and silts, aeolian sands, peat

Unconformity PRECAMBRIAN

ARCHEAN

LATE MAFIC INTRUSIVE ROCKS Diabase

Intrusive Contact

LATE FELSIC INTRUSIVE ROCKSOranite, syenite, and related porphyritic dikes and sills

Intrusive Contact

EARLY MAFIC AND ULTRAMAFIC INTRUSIVE ROCKSDiorite, gabbro, anorthosite gabbro, peridotite, and lamprophyre

Intrusive Contact

FELSIC TO INTERMEDIATE METAVOLCANICS Dacite, andesite, and rhyodacite

METASEDIMENTSLimy sandstone, quartzite, and quartzitic conglomerate; meta-arkose and arkosic conglomerate; pebble conglomerate and breccia; slate and chloritic conglomerate

Disconformity

EARLY FELSIC INTRUSIVE ROCKS Quartz-feldspar porphyry

Intrusive Contact

MAFIC TO INTERMEDIATE METAVOLCANICS Basalt and Andesite; interflow sedimentary rocks

(after Rupert and Lovell; 1970)

In the Kirkland Lake- Noranda area the supergroups are divided into upper

and lower sections. The lower supergroup consists of the Pacaud tuffs

which occupy the lowest and oldest stratigraphic horizon, followed by the

Wabewawa group, the Catherine group and the Skead group. These groups

represent komatiitic, tholeiitic, calc-alkalic and alkalic lavas.

In the Upper Supergroup, the basal komatiitic succession is refered to as

the Stoughton-Roquemaure Group on the north limb of the syncinorium and

as the Larder lake Group on the south limb of the synclinorium. The

overlying tholeiitic, calc-alkalic, and alkalic successions are refered to as

the Kinojevis, Blake River, and Timiskaming Groups respectively (see

Figure 3).

5.2 PROPERTY GEOLOGY

The Victoria Lake property lies entirely within the Kinojevis Supergroup

comprised of tholeiitic metavolcanics. The property is predominately

underlain by intermediate volcanics comprised of andesite flows with the

possibility of some andesitic tuffs. A mafic volcanic, pillowed basalt flow

, and an intermediate to felsic pyroclastic breccia, cut by quartz feldspar

porphyries occur in the northeast corner of the property in Morrisette

township (see Map l in bavk pocket). These units, with the exception of the

felsic intrusives, are sheared and carbonitized by the Murdock

Creek-Kennedy Lake Fault zone which is a secondary splay off of the

Cadillac-Larder Lake Main Break. A gabbro plug intrudes the intermediate

volcanic host rock in Arnold township, as well as in a portion of

Morrisette township, and is sheared and carbonatized by the Misema

Lake-Mist Lake fault zone which is another off shoot of the

Cadillac-Larder Lake Main Break. In Lebel township, the island in Victoria

Lake is sheared and carbonatized but is not believed to contain high

economic potential.

A cut grid of approximately 22 Km was established over the Murdock

Creek-Kennedy Lake Fault Zone. The baseline was positioned in order to

parrallel the fault, the wing lines were spaced at 100 meter intervals

with stations every 25 meters (see Map l in the back pocket).

With the exception of a small andesite breccia outcrop located at

L11 +00 W, 3+75 N , the western portion of the grid contains no outcrop,

thus leaving the geological interpretation to the geophysics surveys. Since

the area is magnetically flat, it is assumed to be underlain by

intermediate metavolcanic flows with the possibility of interbedded tuffs.

The eastern portion of the grid contains abundant outcrop (see Map 4 in

the back pocket). The predominant rock type is a pillowed basalt. This unit

does not appear to be of any economic importance although a few boulders

were observed to contain fine to medium grained euhedral pyrite in some

instances in quantities of H?5. It is known that massive sulphide deposits

will have halos of sulphides extending away from the deposits,particularly

in pillow selvages, therefore it may be possible to trace these minor

sulphide occurences along strike of a known structure, to an economic

occurence.

Flanking the basalt to the south, is an intermediate to felsic pyroclastic

breccia or agglomerate. The pyroclasts range in size from lapilli to bomb

sized fragments and have been sericitized and carbonatized in the

ntsema Lake - Mist Lake Fault

samples 507-510, Inclusive

LEGEND

V9 Tuff (intermediate)

3G Gabbro

q-cc v Quartz-carbonate vein

/x Shear

. 507 Sample location and number

SAMPLE LOCATION MAP - MORRISETTE AND ARNOLD TOWNSHIPSafter O.B.M. 20 17 5800 53300 SCALE: 1: 20 000 Figure A.

12Nt

502 LEBEL TOWNSHIP

VICTORIA LAKE

505

NOTE: all of the rocks on the island have been carbonatized.

LEGEND

V6 Andesite

V9 Tuff

Ml Schist (sericitized)

. 507 Sample location and number

Shear

SAMPLE LOCATION MAP - ISLAND IN VICTORIA LAKE after Map No. 53a, Township of Lebel SCALE: 1: 400 Figure 5.

13

deformation zones. The agglomerate unit has a strike of approximately

057 D Az, and an approximate width of between 75 to 100 meters. The

quartz feldspar porphyry units cut the mafic volcanic rocks but were not

observed to cut the agglomerate. South of the agglomerate unit there are

no outcrops, therefore deriving an interpretation from the magnetic map

(see Map 1 in the back pocket) the response appears to be that of an

intermediate volcanic, most likely an andesitic flow unit.

The quatrz feldspar porphyry units found on the east grid, contain

phenocrysts of alkali feldspar ranging in size from 1-2 mm to Hem, the

latter crystals taking on hexagonal shapes, in a groundmass of medium

grained quartz and alkali feldspar. A few quartz veins containing minor

amounts of pyrite were discovered in a quartz feldspar porphyry on line

8+00 E at station 1+50 S. No economic results were obtained from

assaying the vein material, but it is evidence that the system contains

hydrothermal fluids and that the intrusive could have forced the fluid into

the existing fault zones carrying with it and concentrating already

existing mineralization.

A timbered shaft occurs on line 3+00 E at approximately 0+95 N. The

shaft is partially filled in and is described by E. K. Fockler (1947) as being

an old test pit put down on calcite veining on or close to a

porphyry-andesite contact. This is the earliest reference made to the

shaft. It was most likely put down by earlier prospectors to which Fockler

describes their work as being desultory.

14

5.2.1 Stripped Zone *1

This stripped area is centrally located 16 meters west of Line 4+00 E,

station 1+50 S (see Figure 6.) The 5-10 meter wide trench has a trend of

approximately 285*Az and was stripped and washed as part of an

exploration program carried out by Pamorex Minerals Inc. in August of

1990.

The stripped area exposes a shear zone which is believed to be a portion

of the Murdock Creek-Kennedy Lake Fault Zone. The shear has an overall

trend of approximately 55*Az (range: 48'-67'Az), dips steeply to the

north, and has an exposed width for approximately 38 meters. The host

rock is an intermediate-felsic tuff breccia or agglomerate. Undeformed

portions of the rock unit show felsic pyroclasts ranging in size from

lapilli to bomb size, with the long axis of the pyroclasts paralleling that

of the predominate shear, hosted by an intermediate aphanitic matrix.

The main shear zone is highly sericitized and carbonitized thus giving it

a buff brown color. Graphite can be found in the central portion of the

shear as well as in secondary shears trending at oblique angles to the main

zone. The principle mineralization occurs as fine grained euhedral pyrite

disseminated in amounts ranging from trace to ^9?. An exception to the

overall disseminated pyrite can be found on the west side of the trench

where a gossaned area occurs. The agglomerate appears to have been

effected by an influx of iron rich fluid. Numerous lapilli and bombs have

been replaced by pyrite. Although samples from this area did not yield any

economic gold assays, they were anomalous compared to other samples

from the stripped area. This pyrite enriched zone could be an important key

VI O, undeformed

small lapilli, 2cm long, replaced by pyrite.*v"fc

*\v, WATER FILLEDf1 ''"^^^*^^" G * 522•*J-. i j* -** ^

523 i?

pyroclasts from 2 mm-10 cm in length, long axis trending at 072* Az.

\,-*;#.*V

^r'X-*//S^- .^SSfc-i X// Vi***-.-,, -'.i? 'v'V.-./^ --^^ ^-^ -Jta^•520 r-^-if ^^ A V'j: s

undeformed block, slightly rotated within shear.

"*o

/^B19* .4^•".•..V-tii. ,vrf. ^-' m

pyritized bombs10-20 cm long, 5-10 cm wide.

LEGEND

V10 Agglomerate

Ml Schist (sericitized)

,vv:.i; Overburden

^~ Shear

^ Fault

^o Strike and dip

* 507 Sample location and number

Gp

6

Fu

qv

., -. \je-\j /s//, -' -..V" i ' ...•:tu^,. *~. vi*- ^^ s y .i tvjj.- -^fc

^^fe^/ WATER NLLED " ^^^^^^^^^5,^

^' .^^;m... ^4^.s.af^''^Vflsw^^*-*^' "S5p*^-^*^f ̂ ^

.rt* i'^'i'TV'.^'J. -...

^^\

'^,.

Note: all of the above rock unit has been carbonatized to some extent, therefore it is not mentioned on the map.

15

Graphite

Gossan

Fuchsite

Quartz vein

STRIPPED ZONE * l DETAILED GEOLOGY MAP SCALE: 1:200Figure 6.

16

in future work in the area.

5.2.2 Stripped Zone *2

This stripped area is centrally located on line 2+00 E at station 1+50 S

(see Figure 7). The 6-22 meter wide trench has a trend of 322"Az, and was

stripped and washed as part of an exploration program carried out by

Pamorex Minerals Inc. in August of 1990.

This stripped area exposes the Ronal Red Lake showing which is a

sericitized shear zone trending approximately 305*Az (+X- 10'). The shear

is weakly mineralized with disseminated pyrite rarely exceeding 195. In

the southern portion of the stripped area, Pamorex obtained a gold assay of

6240 ppb (0.18 oz Au/ton) over 3 feet (see Figure 7). They also report the

same shear averaging 2400 ppb (0.07 oz Au/ton) across 3 to 4 feet for

approximately 35 feet along strike before being cut off by another shear

zone.

The host rock is an intermediate-mafic pillowed basalt. The basalt is

locally brecciated and locally contains well preserved pillows as well as

hyaloclastic texture. In the northern portion of the stripped area the

contact between the basalt and the overlying agglomerate is exposed for a

distance of just over 4 meters. The contact strikes along 042"Az and dips

50" to the north. The agglomerate is strongly serecitized, moderately

carbonatized and iron stained. The unit is highly sheared at 360"Az and

contains up to ^disseminated pyrite locally.

,.—**fc*\./~\ V10 17

LEGEND

WATER FILLED

Agglomerate

Basalt

Overburden

Pillow structure

Brecciated

Hyaloclastite

Sample location and number

Shear

Fault

Pomorex channel sample 0.18ozAuXtonover3feet

STRIPPED ZONE *2 DETAILED GEOLOGY MAP SCALE 1:200 Figure 7.

18

6.Q GEOPHYSICS

6.1 Instrumentation and Survey Procedure

6.1.1 Magnetometer

The Proton Precession Magnetometer, GSM-8, was used to carry out the

magnetometer survey on the Victoria Lake Property. The proton

magnetometer uses the precession of spinning protons or nuclei of the

hydrogen atom in a sample of hydrocarbon fluid to measure the total

magnetic field intensity.

The total magnetic intensity, as measured by the proton magnetometer is

the magnitude of the earth's field vector independent of its direction. The

measurement can be expressed as a length (ie. 50,000 gammas) of the

earth's field vector. A local disturbance, say 10 gammas, would add (or

subtract) to the undisturbed field of 50,000 gammas in the usual manner

of vector addition. Since the proton magnetometer measures the magnitude

of the resultant vector (whose direction is almost parallel to the

undisturbed total field vector), that which is measured is very nearly the

component of the disturbance vector in the direction of the undisturbed

total field. Thus the change in total field intensity is called the anomaly

(Spence, 1989).

The data was collected at 25 meter intervals using a GSM-8 Proton

Magnetometer. Base readings were taken approximately every hour and

then used at the end of the day to correct for the fluctuations in the

earth's magnetic field. The data was plotted on a map scale of 1: 5000 and

contoured at a 100 Nt interval.

6.1.2 VLF EM-16

The VLF transmitting stations operating for communications with

submarines have a vertical antenna. The antenna current is thus vertical,

creating a concentric horizontal magnetic field around them. When these

magnetic fields meet conductive bodies in the ground, there will be

secondary fields radiating from these bodies. The VIF Em-16 measures the

vertical components of these secondary fields (Spence, 1989).

The Cutler, Maine transmitter station was chosen because of its

favourable orientation to the geology and structure of the property.

Readings were taken at 25 meter intervals along the cut lines of the grid,

using a Geonics EM-16 with both the in phase and quadrature being

recorded. Profiled data as well as Fraser filtered data were plotted on a

scale of 1: 5000, copies of which accompany this report.

6.2 Results

6.2.1 Magnetometer

The total field survey was useful in outlining the basalt unit in the

eastern portion of the grid system. Of special interest would be the 360

meter long magnetic low trending along 075* Az between lines 1+00 and

4+00 east. The western portion of the grid is relatively flat and might be

interpreted to be underlain by intermediate metavolcanics.

6.2.2 VLF EM-16

The Vlf survey was successful in delineating a number of anomalies, the

strongest and most interesting of which trends along 065' Az. This trend

coincides approximately with the trend of the Murdoch Creek Fault Zone

20

and more than likely represents the fault itself.

7.0 Conclusions and Recommendations

The exploration program carried out on the Victoria Lake Property,

consisting of 43 unpatented mining claims and. located at the junction of

Morrisette, Arnold and Lebel townships in Ontario, has proven that the

ground holds tremendous gold potential. The program has confirmed that

the essential elements for an economic deposit exist. In Morrisette

township the stripped zones expose auriferous, highly sheared and

carbonitized fault zones related to the Murdoch Creek Fault Zone. The

stripped areas contain quartz stringers and veins, disseminated pyrite

mineralization as well as chromium mica alteration. The volcanic host

rock also contains quartz feldspar porphyry intrusives containing

mineralized quartz veins.

The spatial association of felsic intrusive bodies with gold

mineralization is well known. Studies have shown that the emplacement of

an intrusive body will cause dehydration of the host rock at the contact

while remobilizing mineralization away from the contact area. These then

enriched fluids can accumulate in fractures and fault systems and in many

instances form economic deposits.

Prospecting in Lebel and Arnold townships turned up other shear systems

on the property. In Arnold township a quartz carbonate vein was discovered

within the Misema Lake- Mist Lake Fault Zone. Further work is required in

the area where the sample was taken in order to properly assess the zone.

21

The island dividing Victoria Lake and McTavish Lake is essentially all

sheared and carbonatized but appears to hold low potential for an

economic deposit.

In order to evaluate the full potential for a gold deposit on the property,

the western portion of the grid system should be continued to the north

boundary.

A Max-Min survey should be carried out over the entire grid system in

order to delineate any mineralized fracture systems that the VLF and

magnetometer surveys could not detect. Targets of interest should then be

drill tested.

22

REFERENCES

Cattalini, S., Chartrand, F. 1990. Massive Sulphide Deposits in Northwestern Quebec. In The Northwestern Quebec Polymetallic Belt. Edited by M. Rive, P. Verpaelst, Y. Gagnon, J.M. Lulin, G. Riverin and A. Simard. The Canadian Institute of Mining and Metallurgy, Special Volume 43.

Campbell, R.A., Report on the Combined Airborne Magnetic and VLF-Electromagnetic Survey on the Murdoch Creek Fault Property of Trinity Explorations. Lebel, Morrisette, and Arnold Townships, Larder Lake Mining Division, Ontario. H. Ferderber Geophysics, 14p., 1989.

Colvine, A.C., et al. 1988: Archean Lode Gold Deposits in Ontario; Ontario Geological Survey, Miscellaneous Paper 139, p. 136

Easton, R.M., and Johns, G.W. 1986: Volcanology and MineralExploration: The Application of Physical Volcanology and Facies Studies; P.2-40 in Volcanology and Mineral Deposits, edited by John Wood and Henry Wallace, Ontario Geological Survey, Miscellaneous Paper 129, 183 p.

Grabowski, G., Lovell, K, Guindon, D., and Bath, A.C. 1988. Kirkland Lake Resident Geologist's District-1987; in Report of Activities 1987, Resident Geologists, Ontario Geological Survey, Miscellaneous Paper 138, p251-284

Hogg, W.A., Geological Report No. 29,1964 15p., Arnold and Katrine Townships,0ntario Department of mines. Accompanied by Map No. 2061, Scale, 1 inch to 1/2 mile.

Jenson, L.5., 1981: Gold Mineralization in the Kirkland Lake- Larder Lake Area; p. 59-65 in Genesis of Archean, Volcanic-Hosted Gold Deposits, Symposium Held at the University of Waterloo, March 7, 1980, Ontario Geological Survey, MP 97, 175p.

Meyer, G., Grabowski, G., Lovell, H., Guindon, D., and Bath, A.C.1990. Kirkland Lake Resident Geologist's District-1989; in Report of Activities 1989, Resident Geologists, Ontario Geological Survey, Miscellaneous Paper 147, p255-272

23

Meyer,G., Grabowski, G., Lovell, H., Guindon, D., and Bath, A.C1989. Kirkland Lake Resident Geologist's District-1988; in Report of Activities 1988, Resident Geologists, Ontario Geological Survey, Miscellaneous Paper 142, p267-300

Pearson, V., Leve geologique de la propriete Lebel, Canton Lebel et de Morrisette, Kirkland Lake, Ontario, 93p. October 1988. Exploration Brex Inc.

Rupert, R.J., and Lovell, H.L, Geological Report 84, 27p.,1970, Geology of Bernhardt and Morrisette Townships, Ontario Department of Mines. Accompanied by Map 2193, Scale, 1 inch to 1/2 mile.

Spence, I., 1989: Geophysical report, Conglomerate Lake Property, High Frontier Resources.

Turcotte, R., and Lambert, R., Val d,0r Geophysique, Leve Geophysique propriete de Exploration Brex Inc., Project Lebel et Morrisette, Province de Quebec, Mai 1988, 8p., Vlf report with accompanying map.

Turcotte, R., and Lambert, R., Val d'Or Geophysique, Leve Geophysique propriete de Exploration Brex Inc., Project Lebel et Morrisette, Province de Quebec, Mai 1988, Sp., Mag report with accompanying map.

Watson, G.P., and Kerrich, R., 1983: Macassa Mine, Kirkland Lake; Production History, Geology, Gold Ore Types and Hydrothermal Regimes, p.56-74 in The Geology of Gold in Ontario, edited by A.C. Colvine, Ontario Geological Survey, Miscellaneous Paper 110, 278p.

Map No. 53a, Township of Lebel, Scale: 1 inch to 1,000 feet.

APPENDIX 1

STATEMENT OF QUALIFICATIONS

l, Graham G. Long, residing in the city of Rouyn-Noranda, in the province of Quebec, hereby certify that:

1. l am an exploration geologist and have been practicing my profession since 1988.

2. l graduated from Concordia University, Montreal, Quebec, with a Bachelor of Science degree in Geology in 1988.

3. l am a member in good standing of the Northwestern Quebec Prospectors Association.

JANUARY, 1993

Graham G. Long, B.Sc., Geologist

APPENDIX 2

SYMBOLES UTHOLOGlQUES

RQCHES VOLCAfffQUfS ARCHEENNES

V ftocftet votcentques mdetermmees

VI Aocnes voicanrqvet falsigues ou intermediates

V2 fthyoM.

V3 Trachyte

V4 Daota

V5 H off f t volceniquet mtarmediaires Ou /netiques

V6 Andante

V7 Sasaita

V8 ftochei pyioctastiQues indetermnees

V9 fu/

VlO Agglomerai

VI 3 floc 1*1*t volcamoue* uHremalique*

ftOCHfS SEDIMENTAtRES A/tCHfEfV/VfS

S Roche* sedimmntaires indeiermineei

St Conglomeiat

S 2 4*-* 01*

53 (?I'*utv*c*r

54 Argi/itt. share, ardinse. pttylrade

S 5 Quart t He

fQRMATlQNS Df fCft ARCHEENNES

FI fotmaiion da far indetermmee

F 2 Formation da tar sullurae

F3 formation da tar OMydea

F4 formation da far carbonatae

ftOCHES SEDiMEWAlXES fftOTEftOfOlOUES

P Roc t** * teaim+ntiiret tndeiarmmeet

n Arkose

P3 Cf*ui**c**

P4 Queritite tt gf f t

PS Argiliie. shale ardoite at pnyt/ade

P6 Fcrmetion de fer

P7 Oo/omt* et muir e t rochet a carbonetas

P8 Tillitt

ftOCHfS SEOlMfNTAIRES PALfOZOtQUfS

ftOCHfS MfTAMQttPHlQUfS

M ftocffs /nfitmorpfiiqucs t

Ml Schisie

MS Migmatite

Hit

MB

M9

MIO

Ml 1

M12

1

IS

1O

IF

IE

IG

1C

1A

1M

IN

IT

ID

IP

18

IX

12

IR

2

2T

2M

2O

2L

3

3G

3N

3R

3L

30

Gne/ss

Amphioolite

Gnnula,

Mrlonitf

Quirlitte

Miibre

aocHes inrmsivES

Rochet trtttusives fitsMtues indelerminees

Srenae

Syenite Quannque

Syenite t teldspeth tlcelin

Syenite qutrtltqve e teldspith tlcelin

Gnnite

Ctenite e teldspeth elcelm

Montonitt QuMftntjue

Momontte

Momodiofire QUirtiiQue

Tonalite

Granodiorite

Pegmatite

Aloilile

Aplite

Crenophyfe

Rhyolite et leifite intrusive

Roches intrusive* inlermediiirer tndeterminees

Diorite guirltitfue

Moniodiortte

Diorite

Limpropnyre intermediate

Rocttfs intrusive* maliQues indtteimmets

Cibbro

Ivorite

Anortnosne

lamprophyre rrtettque ou nidelermine

Diabase

4 ftoches mirusives vttratnafiques

4P Peridotite

4H Hornblendite

Serpentinite

Dunite

4S

40

4Y

e ultramatique

l Gouverrtemtni du Quebecl Mini*l*f* da l En*(gie ei das Raaiourcesl 5*cl*ur d*t m*fi**

LEGENDE DE LA COMPILATION GEOSCIENTIFIQUE

(2e ddilion, 1984)

SYMBOLES D ANOMALIES GEOCHIMIQUES ETSYM80LES O'ANOMAIIES MINERALOGIQUES

DES ALLUVIONS

SK SEDIMENTS Df RUISSEAU

f- StOIMCNTS DC fONO DE LAC

SO SOLS

IS fAL/X Of SURfACl

ve

K

ML

fA

SVMBC LES DE.S ANOMALIES GEOPHYSIQUES

f f basset valours

r* LCVE DE POLARISATION PttOVOaUEf a** de hevM

f f LEVESDEPOTeHTIELSPONTANC

LECTROMAGNfTlQUeS Afft/ffl/S (tt TURAIf* ase let SYM* ** cowanttonnels id) mufti frequence* texcluanl f /tvfl/ri

potntilM indique la mode puisttoue ih)

•f ' f 'f ' 0 - La t- ^ f (bf radiophase. f pha

A j9 A ,'. AFMAG /ef SYSiemeS muti requence^ts j f H) large ur d'anomelie rapponee: le ^fi f^ direction du leve (gf sysfemes en

' auires syslemes semi-aeroportes

HOCHES

MINI RAUK LOUHOSIBA TTCEI

FORAGE ALLUVIONNAIRE

Les tonal di lortlt tineurs geocfurmguet font delimiters pir ant ligne di contour nnlermant I'idtrtiiticanort du genre di leve it fitemmpue pit li tymbole dta etimerta fmterfl.

CCHANTILL ONNAGllSOLf

fCHAH TIL L ONHAGf DC BLOC IRK A TIQUf

f f f f ti-S f i Jt t ^ ^ rf

x/-

LfVf eLECTmMAGNfriauEACHIEN SrSTEMCINPUT III3 ctniux llvec pfOduit conductivity - 4p*nset*r. mltatl Ibl3 cirtiun Id 4 ciniu* tdl 5 ciaiuf tel 6 cima* If! Ino- mlli* mtgnetiqu* coincident! lg! inomat* rmgntoqui fux- lipost*

LEVtS ELECTROMAGNf TIQVES AU SOL tllsWemf* A cidres honioniau* llvec produn conductivite-toaiS' icuf. mhosllblsystfmes t cidns vtniciuxlcisrstemex

tn mode pulsatotre

LFVES MAGNETlQUfS f AXES DE HAUTES VALEURSI: Illllnlnttbllusol

L6VE CRAVIMfTfttQUf: talhaut grawnttnqve Ibtbas&m-

...ASONDAGE ALL UVIOHNAIRC lint molonMut In mtttn t onjchil. On i&nanpj&a que las lonoagcs aluvxynjott soni repottes sufti coucfts 3

LEVE RAOIOMETRIQUE OU DE SPfCTDMfTWf DCS HAY- OfllS GAMMA: til uranium Ibl thonum id nppon untnmm/ thorium (di lolillilpotisvum

SVMBOLES DES INTERSECTIONS ET ZONES MINERALISEES

^,HAUS f E

T de i* substance if^vu et tonQueur ae la i&a ll*'

SYMBOLES DE SONOAGES

SONDAGE VERTICALlapremie'e couche bthologique renconltee v est droite ei * numero d'xJennticjtion du somtige #u Jessus on

e si un fournal de sondage e*nie tons Jes dossiers

SOMOA Gf POUH AL IMfN T A TIQN EN EA Ut a premie ft coucne lifhofogtQve renconnee y esr mdiguee adrone et lg numero a'ldentiltcttton du sondage AU itessus dusymboie f un fournal de sondage e*tsit oans tes dossiersconsultts

SONDA Gf INCL fNt A VEC PRQJEC J ION HOWZQN TAL f (eiprofondevrconnuetbipratondtufincQnnua Sondage inclmt nvec pro/efi'On ttontoniiie df la tt rtcmpfe La frototKleitr vtmcj** du mrvr rerra^i y est en metres a gauche et le nurr&o d'^entificatfon JkjdessuS Ou A dt&te Ce num&o O dont'tcatori e*actorwn a cat* donnf dons us dLsse consumes et ne figt/re sur /j cane Oe cixnomfon t}ue fes iQwniuM df sondage sont a

SUFFIXES POUR LES MINERAUX DES ROCHES SYMBOLES ST1UCTURAUX

b

c

d

e

f

gh

i

biotite

chlorite

disthene

epidote

feldspath jindeterrr

grenat

hornblende

talc

1

h

m

n

une) o

P

Q

'

carbonate

sericite paragonite

muscovite

nepheline

fekJspath-potassique

plagioclase

quaitichloriloide

s

1

u

V

W

a

yt

staurotide

tremolite adinole

amphibole (mdeteiminet

"ve me de

tourmaline

sillimanite

pyroxene

teolile

SUFFIXED POUR COMPOSITION. ORIQtNE ET ALTERATION

0

0y

s1*

Ift

COMPOSITION

felsique

mafique

ultramalique

OfllGINE

se di mentai re

vofcanique

intrusive

w

aU

rr

e

j 0*

ALTERAriON

amphibolide

Sihcifi4e

alb ii, see

pyniisee

* p idol is**

porphyrin***

ctilonnsee

A"

x

r

t.

*

ertcitisee

carbonatite

serpentinite**

alteration potass iq ne

alteration indelermmee

skarn

corneenne

SUFFIXES POUR LES SUBSTANCES D'lNTERET ECONOMIQUE

MINERAUX ET ROCHES

Am

Ay

Ap

Asp

Ba

Be

Bs

Bo

Cp

Cn

Ch

Cr

Ci

Cor

Cv

amianie

anthophyllite

apatite

arsenopyrite

barytine

beryl

bismuth

bornite

chalcopyrite

chalcosine

chert, jaspe

chromite

cordierite

corindon

covelline

Fp

FI

Gn

Gp

H err

[1m

Mt

Me

Ma

Mi

MdMo

feldspath

fluorine

galene

graphite

i hematite

ilmenite

magnetite

malachite

marcasite

mica

min^raux decoratits

molybdenite

Pn

PC

Pm

Py

Pi

Po

Ra

Sh

Sd

Si

Sp

Sm

Su

Ta

pentlandite

pier re de construction

pierre ornementale

pyrite

pyrophyllite

pyrrhotine

mmerauB radtoaciits

scheelite

siderose

ftilK*

sphalerite

spodumene

sullures (indetermines)

lanial'te

* a t/i* /'

. * e * .

T f f 9* f

a a t .1

+/ / /t t t tt

-f///U * * mf

"T~/ / /*

'aa*

-f//a * t tt-t-/ f*^

* * c rf

//o/

f

t t/ 71

1C •i

f

1* t

,/ /"tr i.

a * '

f ff f

*2sfc.

AFFLfUREMfNTS (a) 'sole, fb} aire d'aftlewements

CONTOURS GEOLOGIQUES /al connu (bt piobablx ou presume. ictd'apresievetgfophystques(AIR SOL)

STRATIFICATION. SOMMET DETERMINE (alho/uontale. fbl inclmee. (c) verticale. (di pendage nondetermine, (si renversee

STRATIFICATION. SOMMfT NON DETERMINE {a)hontoniafe. {b) incline*, fcf vertical*, td) pendage nondeter mint

SCHISTOSITE OU CLIVAGE OU FOLIA TIQN {Plan SI t(al honionttl. fbl incline . (c) vertical. Id) pendage nondetermine

SCHISTOSITE OU CLIVAGE OU fOLIA JION (Plan S2Ila! horitontal. (b) melin*, {ci vertical tdl pfitdage nondetermine

vet tic ale

DIACLASES (a) horttontales. (bf incline**, (c) verticates. (d) sysiemes multiples

LINEATION la) horizon! alt (b) mclmee. {ci verticale. (di plongee non determmee

CONTACT DE COULffS

SYMBOLES GEOMORPHOLOQIQUES

STRIfS GLACtAIRCS la) sens du mouvement connu.fbl mconnu

MORAINE FFtONTALf

fSKERS (al sens d*tcoutemenr connu. ibf mconnu

UMITfS DE TRANSGRESSION MARINE OU OfSUBMERGENCE LACUSTRE (a)connue. (b)presumee

SYMBOLES DES GJTES MINERAUX

STOCKWORK

/fxXXXXm a

XXa a

X*

f/'fyx

mt y /v

r lw*" ' * "

* aa a-

* aH e-

B B

/t aX M

A

ISOGRADE DE MfTAMOftPHlSME Le tomfnef d** point f s mdiQutt le sent cr&ssant du grade de meiamofprttsme Le nom du{dest mtntraKev't

edit de t isograde ou iHilsl esttsontf presttntfsi

LINEAMENT fobtenu par pftoto interpretation/

PLIS

ANTIFQRMfS (a) plan a*iat dtftrmtn* (t) pietum*

ANTlFORMfS OEVfRSfS talplen t*ialdeierm.i*. (bf prtfsumt!

SYNfORMES fa) plan etiml Mlermm*. W pfeittvntt

SYNFOHMES DfVtflSfS f ml plan a..*/ otffcvm-W. fbipresumt

PUS D'ENTRAINEMENT fat de*tre. (bf tenfttrt (ulrlistt avfc otj sans plonyea tt pendayet

AXC DE PLISSEMENT AVfC PtONGEf

FAILLES. ZONES Df CISAiLLfMCNT (a) CWM* (b/ presumee. (cj d aor f s leves geopf^YSiQues. id! incline*, (e) avrc tens de deolacement. (H avec aftais-tment (Itrcercte plem indique le cortt at'a-lltH. igt faifitt df

de charnage presumee

SYMBOLES DES INSTALLATIONS MINltflCC

PUI7S Df MINE lAVfC CHfVALfMENT. fat v*n*atfbl incline

PUITS o EXPLORATION ISANS CHEVALEMENII /a;vertical. Ibl incline

PUITS ABANDONNfS

TRANCHE f

GRAVIERES OU SABLItRES (a) en f.pto'tn** ft fabandonnet

MINE A cifi OUVERTOl olivine

i

SUFFIXES POUR STRUCTURES PETROGRAPHIQUES ET TEXTURES CARACTERlSTIOUES

tfMi turbidite*

iittuii L\ brechi'orme

A breche tecionique

A breche intrusive

A breche pyroclastique

m breche explosive

A breche de coulee

A hyacioclastique

UlQ

(D

0

acH

*

porphyre 'p'*

porphynque

variolinque.

amygdalaire

a spinifex

rubanee [

cisailiee C

it ae W.- df 0ft

iiQ~.. 4 5O".. rf*

spherutttique

S^^UiQi\dcnO /r/v

X

F1LON lin vttns fOfrm tt dimtnvon l

H-ON tm pouvmnt tom tuimtti tn inim ttmtraon t Fmehmim dtltctntt

AMAS M/NtRAL/Sftfn ynin tom* tt dimtnsnnl

AMAS MINCRALISf Ir* pom** itrm pim***ttn-tion i rtctitat at it ant l

moice ou POINT MINEKALISE

INTERSECTION M1HERALISEE DANS UN SONDAGE

GAlCHieS OEXPLORA1ION A fLANC Of COIIAU tADITI ftt tn uttoe. fbf totndonntt

GAlCRtfS DC PRODUCTION A FLANCOf COTCAUItt en ustge. Ibl tbtnoonnft

CHANTIfHS SOUTCKRAIN3 pralondnx en meuel

BATIMENTS

HALDC DE MINIRAI

f ARC A DECHETS

APPENDIX 3

Sample *

501

502

503

504

505

506

507

508

509

510

511

512

513

514

515

516

517

518

519

520

521

522

523

524

525

526

527

528

529

530

531

532

Rock Type

V6? Y9?

Y6? Y9?

M1

Ml

Ml

M1

V9

Y9

V9

V9

Y9

MKY9)

M1(V9)

MKY9)

M1(V9)

MKY9)

V10

Ml

Ml

Ml

Ml

MI(YIO)

V10

MI(YIO)

MI(VIO)

Y10

qtz-cc vein

MI(YIO)

Ml

V7

qtzvein

qtz-cc vein

Alteration

wk ser, strcc

wk sil, str ser,

strcc

strser

strser,

mod ser, modcc

str ser, modcc

wkcc

strcc

wkser.wkcc

modcc

mod ser, strcc

str ser, strcc

str ser, modcc

str ser, modcc

str ser, strcc

strser

strser

atr ser , wk cc

str ser, strcc

str ser, strcc

str ser , mod cc

Fe stained

Fe stained

Fe stained,

str ser, modcc

Fe stained, str ser

Fe stained

str ser, modcc

str ser, Fe stained

strcc

Fe stained

Mineralization

trpy

trpy

Fe stained

tr cpy,Pbs,py

trpy

none

none

trpy

trpy

none

trpy

trpy

trpy

258 py

trpy

158 py

1-2*py

Gp, 1*py

trpy

trpy

trpy

gossan

gossan

trpy

trpy

gossan

trpyTr py, tr Gp

trpy

15? py

trpy

trpy

Twp

Lebel

Lebel

Lebel

Lebel

Lebel

Lebel

Lebel

Lebel

Lebel

Lebel

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

Morrisette

MorrisetteMorrisette

Morrisette

Arnold

Au As?3v( oob

4

3

0

1

1

2

1

^

^

^

1

3

2

4

O

4

5

10

3

4

9

19

180

6

19

78

93

10

6

O

3

4

APPENDIX 4

XRAL 16-NOV-92 RAPPORT R 130 Ref. Dossier 510-RY Page 1 De 1

Numero AU PPB

1052110522105231052410525

919

180619

1052610527105281052910530

1053110532

7893106

•O

1•d

LES LABORATOIRES XRAL 150, tie RUE ROUYN-NORANDA QUEBEC J9X 2H6 TEL (819)764-9108 FAX: (819)784-4673Membre du Groupe SGS (Societe Generate de Surveillance)

[XRAL 11-SEP-92 RAPPORT R 96 Ref. Dossier 312- Page 1 De 1

Numero AU PPB

1050110502105031050410505

1050610507 1050S1050910510

1051110512105131051410515

1051610517105181051910520

43

•O11

21

1324

el

45

103

LES LABORATOIRES XRAL 150, 13e RUE ROUYN-NORANDA QUEBEC J9X 2H8 TEL (819)764-9108 FAX: (819)764-4673Memtare du Groupe SGS (Societe Generate de Surveillance)

l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l lo o4-oCN

O O4- O)

o o4-00

o o

o o4- co

Oo4-LO

o o

o o4- ro

O o4-CN

O O4-

Oo4- o

o o4- cn

o o4-00

Oo4-

o o4CD

O O4LO

Oo

o o4 ro

O O4CN

O O4

o o4o

UJo o4

LU O O4CN

LoJ O O

ro

UJo o

LU O O4-LO

LU O O4- co

UJo o4-

LJ o o4-00

LJ O O4-

LU O O4- o

64-OON

54-OON

44-DON

3+OON

24-OON

14-OON

-Baseline

1+OOS

24-OOS

34-OOS

812

64-OON -

54-OON -

44-OON -

34-OON -

2+OON -

14-OON -

BaselineAZIMUTH 057*

14-OOS -

44-OOS

54-OOS

64-OOS

*94

.897 \ ..917

.899 \ .913

.888 N .901

3+OOS

VICTORIA LAKE

2+OOS -

5+OOS -

6+OOS -

o o(M

OO-hO CM

O O4-

o o4-00

o o

o o4- co

o o4-LO

o o

o o-t-

o o+(N

Oo4-

o o4- o

o o4-O)

o o4-00

o o4-

o o4-CD

O O4- in

o o

o o4-

o. o4-CM

oO4-

o o4- o

LU Oo4-

LU O O4-CM

LU O O4- ro

LU Oo

LU O O4-

LU o o4-CD

LU O O4-

LU o o4- cx)

LU O O4-CD

LU O O4- o

i i l i i i i i l i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i i

DECLINATION 11*30'W BASELINE AZIMUTH 057*

LEGEND

INSTRUMENT: GEM SYSTEMS GSM-8PROTON MAGNETOMETER

SURVEY BY: D. FERDEBER CONTOUR INTERVAL: 100 NANO TESLAS

MAGNETIC DEPRESSION

ADD 57,000 NT TO EACH STATION

100

SCALE 1:5000

200i

METRES

400

VICTORIA LAKE PROPERTY

MAGNETIC SURVEY

MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION

DATA BY: D.F.

DRAW BY:

APPROVED BY:

SCALE: 1:5000 METRIC

DATE: JANUARY. 1993

NTS: 32 D/4

MAP No.

i i i i i i i i i i i i i i i i i i i "i i i i i i i \ i i i i i i i i i i i i i i i i i i i i i i i i i r~in r~i i i i i i i i i i i i i i i i i i r i i i i i i i l i i i i i i i i i i i ' i i i i i i i i i i i i i i i i i i i i

o o4- oCM

O O4-cn

o o4- oo

o o4-

o o4-CD

O O4-LO

o o4-

O O4- ro

O O4-CN

O O4-

o o4- o

o o4-CT)

O O-hco

o o4-

B:o o4 co

o o4-LO

Oo

o o4- ro

o o4- CN

O O4-

o o4- o

LU O O4-

LU O O4-CM

LaJ O O4- ro

LaJ O O

LU Oo4-LO

UJo o4- co

LU Oo4-

LUo o4-00

LUo o4-O)

LUo o4-o

64-OON

54-OON

44-OON

34-OON

24-OON

14-OON

l-Baseline

14-OOS

24-OOS

34-005

BaselineAZIMUTH 057*

44-OOS

54-OOS

64-OOS

+1J3U+25 +8IJ f+16

VICTORIA LAKE

64-OON H

54-OON H

44-OON H

34-OON H

24-OON H

14-OON H

14-OOS H

24-OOS H

34-OOS H

.. 4+OOS H

54-OOS H

64-OOS H

o o4- oCN

O O4- cn

O O4- oo

o o4-

o o4-CD

O O4-

O O

o o4- ro

O O4-CN

O O4-

o o4- o

o o4-CD

O O4- co

o o4-

o ofCO

o o4-LO

Oo 4-

o o4-K)

O O O 0004-4-4-CN T- o

LU O O4-

LU O O4-CN

LU O O4- ro

LU Oo4-

LU O O4-

LU O O4-CD

LU O O4-

LU o o4- oo

LU O O4-

LU Oo4- o

.L-U4-I-. l l i l l i i l i l l i l l l i l l i l i i l i l i i i i i j i i i i i i l l l l l l l

DECLINATION 11'30'W BASELINE AZIMUTH 057*

LEGEND

INSTRUMENT: GEONICS EM-16 SURVEY BY: D. FERDEBER STATION: CUTLER, MAINE, 24.0 KHz OPERATOR FACING NORTH

PROFILE SCALE: 1cm = 50?S IN PHASE AND QUAD.

IN PHASE QUADRATURE

————--1 — — ••••i AXIS OF ANOMALY (WEAK. MODERATE, STRONG)

100

SCALE 1:5000

200

i

METRES

400

VICTORIA LAKE PROPERTY

VLF-EM SURVEYPROFILED DATA

CUTLER, MAINE, 24.0 KHz

MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION

DATA BY: D.F.DRAWN BY:APPROVED BY:

SCALE: 1:5000 METRICDATE: JANUARY, 1993NTS: 32 D/4

MAP NO.

2

l l l l i i l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l i l l l l I l l l l l l l l l l l l l J l l l ( l l l .1 l l l ( l l l l l l l l l l l l l l l l l l l l l lo o4- o(N

O O4- cn

o O+DO

Oo4-

o o4-CD

O O4- LO

o o

o o4- ro

O O4- CM

O O4-

o o4- o

o o4-

o o4- oo

o o4-

o o4CO

o o4-LO

Oo4-

o o4- ro

o o4- CN

o o4-

o o4- o

LU O O4-

LU Oo4-CNI

LU O O4-

UJ O O

UJo o4-

LU o o4-CD

LU O O4-

LU o o4-00

LU O O4- cn

LU o o4- o

6+OON

54-OON

44-OON

34-OON

24-OON

14-OON

-Baseline

1+OOS

24-OOS

34-OOS

Baseline7 ' AZIMUTH 057'•17

'4+UDS"

54-OOS

64-OOS

VICTORIA LAKE

64-OON -

54-OON -

44-OON -

34-OON -

24-OON -

14-OON -

14-OOS -

24-OOS -

3+OOS -

44-OOS -

5+OOS -

64-OOS -

oCM. CM

O O4- oCM

O O4- cn

o o4- oo

o o4-

o o4- co

o o4-

o o4-

o o4- ro

O O4- CN

Oo 4-

o o4- o

o o4-

o o4- co

o o4-

o o4

o o4-LO

o oo o4- 4-

O O4- CN

o o4-

o o4- o

LU O O4-

LU O O4-CM

LU O O4-K)

LU O O

LU O O4- m

LUo o4- co

LUo o4-

LUo o4- oo

LUo o4-

LUo o4- o

l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l l t l l l l l" l l l l l l l l l l l l l l l l l l l l l l i l l l l l l l l l l l l l l l l l l l l l l l l l l

DECLINATION 1T30*W BASELINE AZIMUTH 05T

LEGEND

INSTRUMENT: GEONICS EM-16 SURVEY BY: D. FERDEBER STATION: CUTLER, MAINE, 24.0 KHz OPERATOR FACING NORTH

CONTOUR INTERVAL = 10 UNITS

...AXIS OF ANOMALY (WEAK, MODERATE. STRONG)

100

SCALE 1:5000

200

i

METRES

400

VICTORIA LAKE PROPERTY

VLF-EM SURVEYFRASER FILTER DATA

CUTLER, MAINE, 24.0 KHz

MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION

DATA BY: D.F.

DRAV1/N BY:

APPFtOVED BY:

SCALE: 1:5000 METRIC

DATE: JANUARY, 1993

NTS: 32 D/4-

MAP NO.

3

T l—l l l l l l I l l IIII -j—j—ri—i—i—i—i—i—n—i—i—i—i—i i i i i i i i i i i r~i'' ' ' ' i i i i i i i i i i i i i i i T~I—i—i—i—i—i—r~i i i i i i rni i i i i i i i i i i i i i i i i i i i i i i i i r~i i i i i i i i i i i r

o4- oCM

6+OON

5+OON

4+OON

3+OON

2+OON

1+OON

-Baseline

: 1+OOS

2+OOS

3+OOS

4+OOS

5+OOS

6+OOS

oCO

o o4-CD

T

O o

O O

00

O O4-

Oo00

o o4- to

^z.

Oo 4-

o o4-LO

o o4-CD

o oNt-

AU.

o o4-K)

Ak

o o4-o o

0o

o o

0o:Lcti

o ooooo oooo4- 4- 4- 4-

ooo ooo4-4-4-

o o4-

o o4-o o4-

o o4-

LU O O4-

LU o o•4-

UJo o4-

UJo o4-

LU O O4-

LJ o o4-

LU o o4-

LU O O4-

Ld O O4-

LJ Oo 4-

0o

0olo

0o0o-f-oo

0o-fr-

0o 0o0o

0o0o 0o 0o

+5

LU O O

LU O O

CM

LU O O

LU LUO . OO O

UJ

CD

LU O O

aseline AZIMUTH 057-

64-OON -

"5+OON -

4+OON -

34-OON -

24-OON -

1+OON -

LU O O

LU O O

oo CD

LU O O

O

l li t i i i i i i r i t i i i i i i i i i i i l i l ' ' i i l ' ' ' l ' ' ' ' l ' ' ' i i i i i i i i i i l i l i l i i i l i i l i i i l i i i i i i i l i i i i i i i l i i i l i i i l i i i f i i i f l l M l l l l l l l l l l l f l l

lg10

li

1+OOS -

2+oos -

-34-OOS.-

4+OOS -

5+OOS -

6+OOS -

LEGEND

Y5 BasaltY6 AndesiteY l O Agglomerate (including lapilli tuff)Ml SchistQFP Quartz feldspar porphyryB Exploration shaft

SL Pillow structureqv Quartz vein

i ^ Fault l ShearA Pyroclastic breccia

HJH Claim post^ Swamp/;/, x Outcrop: large, small^ Stripped zone

.v. Old road~* x

O Diamond drill hole collar

100

SCALE 1:5000

200

i

METRES

400

VICTORIA LAKE PROPERTY

GEOLOGY MAP

MORRISETTE TOWNSHIPDISTRICT OF TIMISKAMING, ONT.LARDER LAKE MINING DIVISION

DATA BY: D.F.

DRAWN BY:APPROVED BY:

SCALE: 1:5000 METRICDATE: JANUARY. 1993NTS: 32 D/4

.III.