geotechnical report geological and geophysical …

42A12SE8905 2.14938 GODFREY 010

1493

GEOTECHNICAL REPORT

GEOLOGICAL AND GEOPHYSICAL SURVEYS

GODFREY TOWNSHIP PROPERTY

PORCUPINE MINING DIVISION

BY

ROBERTA BALD, M.Se., F.G.A.C.

February 10th, 1993

Lively, Ontario

rea 19

RECEIVED

MAR l 7 1993

MINING LANDS BRANCH

l

INTRODUCTION

The Godfrey Township property consists of eight contiguous,

unpatented claims situated about 13 km (8 miles) northwest of the

city of Timmins, Ontario (Figure 1). The property is located in

north-central Godfrey Township, in the Porcupine Mining Division,

District of Cochrane (Figure 2). The following claims were recorded

on February 28th, 1991: P1176409 to P1176412 inclusive, P1176544

and P1176545. The following two claims were recorded on March lith,

1991: P1176662 and P1176663. The author, Roberta Bald, of 189

Margaret Avenue, Lively, Ontario, is the holder of the mining

claims described in this report.

A metric grid was cut between June 8th and September 20th,

1991 on the property. The claims were then geologically mapped and

49 samples were taken. The samples were analysed for gold, copper

and zinc. Two geophysical surveys were performed: a magnetometer

survey and a Horizontal Loop EM survey.

ONTARIO

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42A12SE8985 2.14938 GODFREY 010C

TABLE OF CONTENTS

INTRODUCTION . . . . . . . . . . . . . , . . . . . . . . . . . l

LOCATION, ACCESS AND TOPOGRAPHY . . . . . . . . . . . . . . . . 3

REGIONAL GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . 4

PREVIOUS WORK . . . . . . . . . . . . . . . . . . . . . . . . . 6

LINECUTTING . . . . . . . . . . . . . . . . . . . . . . . . . . 9

GEOLOGICAL SURVEY . . . . . . . . . . . . . . . . . . . . . . . 9

MAGNETOMETER SURVEY . . . . . . . . . . . . . . . . . . . . . 12

HORIZONTAL LOOP EM SURVEY . . . . . . . . . . . . . . . . . . 14

CONCLUSIONS AND RECOMMENDATIONS . . . . . . . . . . . . . . . 14

REFERENCES . . . . . . . . . . . . . . . . . . . . . . . . . 16

CERTIFICATE . . . . . . . . . . . . . . . . . . . . . . . . . 18

APPENDIX . . . . . . . . . . . . . . . . . . . . . ' . . . . . 19

LIST OF FIGURES

FIGURE l LOCATION MAP OF TIMMINS SCALE l "e 150 MILES

FIGURE 2 LOCATION MAP OF GODFREY SCALE 1: 250 000

TOWNSHIP

FIGURE 3 CLAIM MAP SCALE 1: 20 000

BACK POCKET:

MAP l GEOLOGICAL MAP SCALE 1: 2 000

MAP 2 MAGNETOMETER SURVEY SCALE 1: 2 000

MAP 3 HORIZONTAL LOOP SURVEY SCALE li 2 000

1777 HZ FREQUENCY

MAP 4 HORIZONTAL LOOP SURVEY SCALE 1: 2 000

444 Hz FREQUENCY

3

LOCATION, ACCESS AND TOPOGRAPHY

The Godfrey Township claim group is located about 13 km

northwest of the city of Timmins, Ontario (Figure 1). The property

is located in north central Godfrey Township, in the Porcupine

Mining Division, District of Cochrane (Figure 2). The Kamiscotia

highway, Highway 576, cuts across the property (Figure 3).

Twentythree Mile Creek runs along the east boundary of the claim

group.

The claims are located in Lot 6, Concession IV and V of

Godfrey Township and are numbered as follows:

P1176409 SW 1/4, N 1/2, Cone V, Lot 6

P1176410 SE 1/4, N 1/2, Cone V, Lot 6

P1176411 NW 1/4, S 1/2, Cone V, Lot 6

P1176412 NE 1/4, S 1/2, Cone V, Lot 6

P1176662 SW 1/4, S 1/2, Cone V, Lot 6

P1176663 SE 1/4, S 1/2, Cone V, Lot 6

P1176544 NW 1/4, N 1/2, Cone IV, Lot 6

P1176545 NE 1/4, N 1/2, Cone IV, Lot 6

The property can be found on NTS map sheet 42 A/12. The center

of the claim group is located approximately at 48C 31' latitude and

81*29' longitude.

The claims are readily accessible by the Kamiscotia highway

which heads northwest from Highway 101 about 7.5 km west of the

center of Timmins. The baseline is a cut out lot line and the

eastern boundary of the claim group has been cut by other claim

holders north of the highway. During the course of this exploration

GODFREY TOWNSHIP

500m 1km

SCALE : 1:20,000

CLAIM MAP

sS/

FIGURE 3

DATE:JANUARY,93 BY-. RB.

4

program, a drill road was pushed northward along the eastern

boundary of the claim group to about the middle of Concession V,

where it veers off in a northeasterly direction. The two

northernmost claims were scheduled to be logged in the summer of

1992, but the author has not verified this in the field.

A high area of outcrop occurs just north of the highway,

covered by claims P1176411, P1176412 and P1176663. The southern

portion of the property is underlain by a cedar and spruce swamp,

along the old power line. Near the east boundary of the claim

group, the topography is low and swampy along Twentythree Mile

Creek. The rest of the claim group is covered by mature poplar and

birch.

REGIONAL GEOLOGY

The Timmins area is situated in the Abitibi Greenstone Belt of

the Superior Province of the Canadian Shield (Ginn et. al., 1964;

Pyke et. al., 1973). Many of the gold mining camps in Canada,

including Timmins, Kirkland Lake-Larder Lake, Rouyn-Noranda and Val

D'Or are situated in the Abitibi Greenstone Belt. Since gold was

first discovered in the Timmins area in 1909, over 60 million

ounces of gold have been recovered from over 37 mines, three of

which are still in operation. This ranks Timmins as the largest

gold mining camp in North America.

Timmins is also the location of Kidd Creek Mine, one of the

largest base metal mines in Canada, producing zinc, copper and

silver. Other smaller base metal mines have been in production in

5

the Timmins area including two in Godfrey Township. The Genex Mine

is located about 4 km southwest of the claim group and produced 240

tons of copper concentrate between 21.45% and 27.25%. The Canadian

Jamieson Mine, about 3.2 km northwest of the claim group, produced

816,173 tons averaging 2.44% copper and 4.22% zinc from April, 1966

to February, 1971 (Middleton, 1974; Northern Miner, 1966).

Most of the bedrock in the Timmins area is of Archean age. The

metavolcanic rocks consist of two groups, the Deloro Group and the

younger Tisdale Group. The older Deloro Group is for the most part

a calc-alkaline sequence, consisting of andesite and basalt flows

overlain by dacitic flows and dacitic to rhyolitic pyroclastic

rocks. Iron formation commonly occurs at or near the top of the

group. The Shaw Dome is the most extensive exposure of this group.

A major change in volcanism occurred between the Deloro and Tisdale

Groups. The base of the overlying Tisdale Group consists largely of

ultramafic metavolcanic rocks and basaltic komatiites. A sequence

of tholeiitic basalts overlies the basal ultramafic rocks and is

overlain by calc-alkaline dacitic volcaniclastic rocks.

Metasedimentary rocks which are in part, time equivalent to

the upper part of the Deloro Group and the entire Tisdale Group,

consist of a turbidite sequence and a thin overlying fluviatile

sequence and are called the Porcupine Group. Large ultramafic

intrusions were emplaced almost entirely within the Deloro Group.

Small bodies of quartz feldspar porphyry intrude the raetavolcanic

rocks and may in part be extrusive rhyolitic domes. Various small

to large granitoid intrusions were emplaced in the metavolcanic-

metasedimentary sequence. Three ages of diabase dikes cut the older

rocks in the area and generally trend north and east-northeast.

The Porcupine-Destor Fault Zone is a major structural break

which trends northeast across the Timmins area. The fault dips

vertically to steeply north. Two periods of folding have deformed

the rocks north of the Fault Zone, whereas south of the fault, the

main structural feature is the Shaw Dome, the axis of which trends

roughly east-west. The Archean rocks in the area have undergone

regional metamorphism to the lower to middle greenschist facies.

PREVIOUS WORK

Various provincial government geoscientists have done

geological and geophysical studies in Godfrey Township: Burrows,

1911; Finley, 1925; Hogg, 1954; Middleton, 1969, 1971 and 1974;

Middleton et. al., 1970; Pyke et. al., 1971; MacRae et. al., 1981.

Much mineral exploration has been done in Godfrey Township.

The area was first prospected for gold in the 1900's, mainly in

quartz veins in the quartz porphyry and microdiorite intrusions.

From the 1920's sporadically to the present, the area has also been

the target of base metal exploration with some success being

achieved in the late 1960's to early 1970's by the Genex and

Canadian Jamieson Mines Limited mines.

Many reports on exploration activities in the township have

been filed for assessment and are available at the Timmins

assessment office. Work on the present claim group was first done

in the mid-1950's by Harry Leblanc (T-507). Blasting of trenches

and pits revealed quartz veins and stringers "sparingly mineralized

with pyrite and chalcopyrite" in conglomerate (Hogg, 1954). A 503'

diamond drill hole cut rhyolite with sparse pyrite. A drill hole

casing was found on claim P1176663, just south of the outcrop area

on Line 5 South, which gave the highest zinc assays from an old

blasted out pit. The drill hole appears to have been drilled to

intersect the zone that was sampled in the present survey. A drill

hole shown on O.G.S. Preliminary Map P.2075, Timmins Data Series,

Godfrey Township, shows a drill hole in roughly the same location

as found in the field. The map notes the presence of galena,

pyrrhotite, pyrite and .Sphalerite in felsic metavolcanics (3a:

unsubdivided; 3b: ash, lapilli, tuff). It was probably drilled by

Hollinger Mines Ltd. (T-1460). It is unknown whether the core is

available for sampling and assaying at the drill core library in

Timmins.

An airborne Magnetometer and EM survey, covering a large area,

flew over the northern portion of the present claim group in 1963

(T-843) . No EM conductors were located on the present claim group.

Maps of the magnetometer survey were unavailable in the file.

Another, smaller airborne Mag and EM survey was done in 1964

by Mespi Mines Ltd. The magnetometer survey vaguely traced the

northerly trending diabase dike which crops out on the present

claim group. A wide north to north-northeast trending EM conductor

was outlined across the present property.

Cu-Kara Porcupine Mines Ltd. held a large block of ground in

the mid-1960's, including the present claim group (T-963).

8

Geological mapping was done as well as ground magnetometer,

Horizontal Loop EM and Induced Polarization surveys. Although the

Horizontal Loop EM survey was hampered by "deep conductive

overburden, noisy conductive shears and an extremely noisy

hydropower line along the road", two parallel, northerly-trending

conductors of moderate to poor conductivity were picked up. These

conductors were tested by diamond drill holes north of the present

claims and revealed fine-grained siliceous graphitic sediments,

probably causing the EM conductors. Six other drill holes were

drilled and telescoped core samples from this drilling is available

at the core library in Timmins. The magnetometer survey traced the

diabase dikes and a northerly-trending, magnetically low area

probably corresponding to sediments. The I.P. survey outlined a

strong, broad anomaly running north-south across the present

claims. It was tested by a drill hole just north of the present

claim group. The hole intersected sulphide bearing conglomeratic

sediments.

Recently, new work has been done on claims adjacent to the

property. In 1991 and 1992, Falconbridge Exploration cut lines, and

did magnetometer and EM (Horizontal Loop and VLF-EM) surveys over

an extensive claim block, essentially surrounding the present claim

group (T-3467). Generally, the magnetometer surveys traced the

diabase dikes. A few bedrock HLEM conductors were located to the

east of the present claim group and it was recommended that these

conductors be tested by drilling. Although not in the assessment

files, the author is aware that some drilling was done in this area

and gold values were obtained (Northern Miner, 1992, Appendix).

Another report was filed in 1991 for claims contiguous to the

southwest corner of the present claim group (T-3518) . The report by

Max Juby outlined the program of line cutting, magnetometer and

VLF-EM surveys that was done. Some EM conductors were located in

the program.

LINECUTTING

Under the supervision of the author, a metric grid was cut

between June 8th and September 20th, 1991 by Paul Provencher, South

Porcupine, Ontario and helpers. A north-south baseline was cut

along the old cut out lot line between Lot 6 and Lot 5. After the

baseline was put in but before the lines were cut, a baseline was

put in by Falconbridge Exploration, the holders of the claims to

the west and east of this property. Sixteen east-west lines were

cut 100 meters apart and picketed every 20 meters. A total of 14.32

km of line were cut on the property.

GEOLOGICAL SURVEY

The claims were mapped at a scale of 1:2,000 between June 28th

and November 21st, 1991. All the lines were walked looking for

outcrop and noting tree types, topography and overburden features.

Outcrop on the property is confined to three claims: the eastern

portion of P1176411, the western and south-central portions of

P1176412 and the northwestern corner of P1176663 (Map l, back

pocket) . The outcrops were mapped by pace and compass method. No

10

outcrop was found south of the highway and none was found on the

two northernmost claims.

The claim group is mainly underlain by a felsic fragmental

metavolcanic unit (Map l, back pocket), variously mapped by O.G.S.

geologists as a conglomerate (Hogg, 1954) or tuff-breccia-water

lain volcanic breccia-conglomerate and graphitic tuffs and

agglomerate (Middleton, 1974). A possibly bifurcating, north-

northeast-trending diabase dike, about 30 meters wide, cuts this

unit. Table l lists the rock types found on the property.

TABLE 1: Rock Types

1- Felsic Fragmental Metavolcanic Rocks: fragmental unit with 30

to 50% matrix and at least two types of fragments: a) white to

light grey rhyolite with quartz phenocrysts; and b) dark grey

to black argillite fragments, possibly graphitic

2- Diabase dikes: black, magnetic, medium- to coarse-grained,

massive; chilled against Unit 1.

The felsic fragmental metavolcanic unit is a foliated unit

with about 30 to 50% medium-grained, pinkish-buff coloured, rusty,

tuffaceous matrix containing some white weathering feldspar

crystals. Two kinds of fragments were noted: light grey to white

rhyolite fragments with small, clear quartz crystals; and dark grey

or black argilite fragments, locally possibly graphitic, generally

11

than the rhyolite fragments. The felsic fragments consist

of large (up to 20 cm diameter), white weathering, angular to

subangular rhyolite or quartz feldspar porphyry. These fragments

make up from 15% to 3(^ of the rock. The graphitic argillite

fragments are dark grey, soft, fine-grained, angular to subangular,

equant to very elongated parallel to the local foliation, which

trends 120*to 150*AZ. These fragments are locally finely laminated

and make up about 5% of the rock. Ubiquitous in the unit are

weathered out spherical to elliptical areas less than 0.25 cm long

which may possibly represent pumice fragments. It was noticed that

in general, the fragments seem to be larger near the trenches on

L5S, where some grab samples assayed up to 3400 ppm Zn, possibly

indicating this area may be a volcanic vent. Further detailed

mapping and possibly mechanical stripping is needed to confirm this

speculation.

A possible shear zone occurs at L3S, 6+4OmE.

The diabase dikes are dark brown on weathered surface, black

on fresh, magnetic, medium- to coarse-grained. They are chilled

against the fragmental unit.

49 samples were collected and analysed for gold, zinc and

copper (Map l, back pocket). The sample descriptions and locations,

and the assay certificates are found in the Appendix. Several of

the old trenches and pits were examined and sampled. Most are

associated with easterly-trending quartz veins or rusty, pyrite

bearing easterly-trending possible shear zones in the fragmental

unit. In some cases, the presence of pyrite-rich fragments was

12noted. Most trenches contain about 3% to 4% disseminated pyrite or pyrrhotite, but the southernmost pit contains up to J.0% sulphides, mainly as pyrite but trace amounts of dark brown sphalerite were also seen.

The metavolcanic rocks are locally cut by quartz veins and gashes. The quartz veins are generally translucent and locally vuggy. They are generally iron stained, but only rarely were any sulphides seen in the quartz. They trend from 020*to 090*AZ. Of the 49 samples collected for analysis, 16 of them were quartz veins and another 10 contained some quartz vein material.

MAGNETOMETER SURVEY

Under supervision of the author, a magnetometer survey was performed on September 23rd and 24th, 1991, by Wayne Pearson, Timmins, Ontario, using a Scintrex MP-2 proton precession magnetometer. This instrument measures total magnetic field and is sensitive to l gamma. Specification sheets are in the Appendix.

A base station was established at BLO, LIN. This base station was read before starting the readings of the day and was read again before going home. The baseline was tied in by taking a reading at the base station, then reading the 20 meter baseline pickets to BLO, L2N then reading the base station again and then reading BLO, L2N again, and so on for the entire baseline. Once this was done, the readings taken on the baseline could be checked for drift. It was found that the readings were always within 10 gammas of the tie-ins and thus no corrections were made to the data. Readings

13were taken at every picket along the baseline and all sixteenlines. Readings were taken halfway between the pickets when ananomaly was being approached. A total of 815 readings were taken onthe grid, over 14.24 km of line.

The results were plotted and the data contoured (Map 2, backpocket) . Six features, from A to F on the map, are described asfollows:

A: A north-northwesterly-trending high, located along the baseline near L3N and trending off the property, could possibly be a diabase dike.

B: A north-northwesterly-trending high, located on L4N and L3N, at

about 2+OOmE, trending northward off the property, could also be a diabase dike.

C: A wide north-south low, from L4N to L7S, between 5+OOmE and 6+OOmE, possibly indicating a magnetically low rock formation, such as felsic metavolcanic rocks. This low feature covers

most of the exposed felsic metavolcanic outcrops seen on the property. This could indicate that the rest of the property is underlain by more mafic, and thus more magnetic, rocks.

D: A long, narrow, northwesterly-trending high, starting from LIN, 2+SOmE to L10S, 7+OOmE and trending southward off the

property. It corresponds to diabase dike outcrops.

E: A short high within the large formational low, located at L1S, 54-20mE, corresponds to several trenches in felsic metavolcanic rocks. Two samples were taken in these trenches but assay values were low. In one of the samples, pyrrhotite was noted.

14

F: A northwesterly-trending high, from L8S, 2+OOmE to L10S, 3*20mE,

has a more westerly strike than the diabase dikes. It is

unknown what it represents.

HORIZONTAL LOOP EM SURVEY

Under supervision of the author, a horizontal loop EM survey

was conducted on September 25th and 26th, 1991, by Wayne Pearson

and helper. An Apex Parametrics MAXMIN II portable EM was used with

coplanar, horizontal coils. This instrument measures the in-phase

and quadrature components of the secondary field and expresses them

as percentage of the primary field. Readings were taken at 444 and

1777 Hz with a coil spacing of 150 meters (Map 3 and 4, back

pocket). A total of 521 readings were taken of both frequencies,

over 12.64 km of line. The instrument has a repeatability of

between +0.25% to +l%, depending on conditions, frequencies and

coil separation used. Specification sheets are in the Appendix.

Conductors located during the survey correspond to an old

abandoned power line in the southwest part of the grid and the

power and telephone lines along Highway 576. Elsewhere, the in-

phase component is generally flat. Several quadrature responses

probably are caused by near surface features such as creeks or

bedrock topography.

CONCLUSIONS AND RECOMMENDATIONS

The most important result obtained from this work is the

location of the zinc-bearing zone on L5S near 5+eomE. This zone had

15

been drilled previously but to the author's knowledge has never been assayed before. Sampling core from the 1964 drilling should be done if it is at the Drill Core Library in Timmins. Also the observation that the fragment size is larger near this area may be significant for exploration.

Although the Horizontal Loop EM survey failed to locate any conductors, a zinc-rich zone with little copper would not be detected since zinc is not a good conductor. The cultural features also interfered with the EM survey.

It is recommended that a search be made for the old drill core and samples taken if it is found. If the core is lost, a new drill hole should be drilled to test the zinc-bearing zone.

16

REFERENCES

Burrows, A.G., 1911: The Porcupine Gold Area; Ontario Bureau ofMines, Vol. 20, pt. 2, 39 p. Accompanied by Map 20e, scale linch to l mile.

Finley, F.L., 1925: Kamiscotia Gold Area, District of Cochrane;Ont. Dept. Mines, Vol. 34, pt. 6, p. 43-64.

Ginn, R.M., Savage, W.S., Thomson, R., Thomson, J.E. and Fenwick,K.G., 1964: Timmins-Kirkland Lake Sheet, Cochrane, Sudbury andTimiskaming Districts; Ont. Dept. Mines, Geol. Comp. Ser., Map2046, scale l inch to 4 miles. Compilation 1961, 1962.

Hogg, N., 1954: Geology of Godfrey Township, District of Cochrane;Ont. Dept. Mines, Vol. 63, pt. 7 (published 1955). Accompaniedby map 1954-4, scale l inch to 1,000 feet.

MacRae, B.A. and Deosaran, Maharaj, 1981: Godfrey Township,Cochrane District; Ont. Geol. Surv., Preliminary Map P.2075,Timmins Data Series. Scale l inch to 1/4 mile. Data compiled1980.

Middleton, R.S., 1969: Magnetic Survey of Godfrey and TurnbullTownships, in Summary of Field Work, 1969, ed. E.G. Pye, Ont.Dept. Mines, MP32, p. 50-53.

Middleton, R.S., 1971: Godfrey Township, District of Cochrane; Ont.Div. Mines and Northern Affairs, Prelim. Map P.639, Geophys.Ser., scale l inch to 1/4 mile.

Middleton, R.S., 1974: Godfrey Township, District of Cochrane; Ont.Div. Mines, Prelim. Map P.967, Geol. Ser., scale l inch to 1/4mile. Geology 1969

17 Middleton, R. S. and assistants, 1970: Turnbull and Godfrey

Townsh_,Lps, Cochrane District, Ont. Div. Mines, Map 2330,scale l inch to 1/2 mile.

Northern Miner, 1966, "Genex Shipping Copper Concentrate"; theNorthern Miner, September l, 1966, p. 13.

Pyke, D.R., Ayres, L.D. and Innes, D.G., 1973: Timmins-KirklandLake Sheet, Cochrane, Sudbury and Timiskaming Districts; Ont.Div. of Mines, Geol. Comp. Ser., Map 2205, scale l inch to 4miles.

Pyke, D.R. and Middleton, R.S., 1971: Distribution andCharacteristics of the sulphide ores of the Timmins Area; CIMTrans., Vol. 74, p.157-168.

Timmins Assessment Files: T-507, T-787, T-843, T-963, T-3467, T-

3518.

18

CERTIFICATE

I, Roberta Bald, of the town of Lively in the District of Sudbury, hereby certify:

1) That I reside at 189 Margaret Avenue, Lively, Ontario

2) That I received an Honours B.Se. in Geology from Laurentian University in 1975 and a M. Se. in Earth Sciences from the University of Manitoba in 1981.

3) That I have practised my profession as geologist since graduation.

4) That this report, finished on February loth, 1993, was written by me, based on geological field mapping, supervision of the linecutting and geophysical surveys, on my knowledge of the Timmins area, on previous geological reports and on assessment data obtained at the assessment office in Timmins.

5) That I am the holder of 10(^ interest in the claims described in this report.

6) That I am a Fellow of the Geological Association of Canada.

Dated at Lively, Ontario, this 10th day of February, 1993.

Roberta Bald, M.Se., F.G.A.C.

APPENDIX

The Northern Miner January 13,1992 3

ile IIMV l Falconbridge hits on Moneta ground^^ ̂ *^*^^ 1 l f l r~\ *ll * - ~ . f-t\J\ —^ -* I-. -^ ,. . -. , f * L _ . . . _ l,,.. 1-^1*.. * ~ f~* t L * J * * ' *

dan was charged e provincial min- rating the projecl ision.t plan is to have n limited opera- Hate April, bar- itacles as snow- i full production ,ust.the mine is still f i table at current IcDoulelt, who is ancis Oil Co. and a, Okla. Kaiser- ; 320Xo of Ma- ianding common

topes the compa- the black a year t that a big wild ing the palladi- lartcet still seems iian situation." aid Madeleine is isions with such imers as Canadi- i mining compa- own smelting fa-

leleine is also in i to benefit from ?eans to go with d catalytic con- nobiles.also announcedhas switched its

nat of a Quebecly to a federally any.the change in-

bec law does notwith non-Que-

iing companies.it 50'Hi interest

s Iles project.ridan Platinum

l he other half.looking ut the

with, or

II

Drilling a 600-metre-Iong geo physical anomaly on Moneta Porcupine Mines' (TSE) proper ty in Godfrey Twp., near Tim mins, Ont.. Falconbridge inter sected a narrow vein containing high-grade gold mineralization.

The 1.5-mcire interval as-j saycd 82.2 grams per tonne] over 1.5 metres including 306 grams over 0.4 metres. Concen trated within a 10-cm-wide quartz-carbonate vein, the gold is associated with cubic ar senopyrite.

The geophysical anomaly is represented by a 35-metre-| thick graphic argillite horizon and is thought to be the source of the carbonaceous alteration.

Moneta, which has staked 93 claims and optioned 13 claims ^ to cover the on-strikc potentialFort Knox raises additional S272.000

Most of the investors holding warrants in Fort Knox Gold Resources (TSE), including Inco (TSE), have exercised those warrants, raising S272,000 for further exploration on the Fawcett Twp. property near Shining Tree, Ont.

A total of 317,205 warrants, which each carried the right to purchase one flow-through Fort Knox share at Si on or be fore Dec. 31, 1991, were issued as part of a private placement last November. Fort Knox re cently traded at S 1.10.

Combined with the cash re maining in Fort Knox's kitty, the new financing will provide more lh;m 5350,000 for explo ration Richard Agar, Inco's di rector of acquisitions and prop erty management said the next phase would involve both drilling and ground geophysics

of the new play, believes mineralization may be structurally conlrolled by a number of faults which parallel the Porcu- pine- Destor fault.

Falconbridge is optioning 20 claims and is required to spend 5500,000 to earn a 5Wo interest in three lease groups in the Timmins area.

in incorporation (he company loDUUldc 111 (jl)C

the company's re from outside dcDoulell said,

meetings will n April or May re the company ffices.aid the various rolled by Sheri- or 90Xo of Ma ul that Sheridan ng any control

MacDougall MacDougall 8c MacTier Inc. are pleased to announce that

James J. Perrone, CFA

has joined ourInstitutional Research and Sales Department.

Mr. Perrone has extensive experience inmining equity research and

will service clients from our Toronto office(416) 977-0663

MacDougall MacDougall r k MacTier Inc. *4

SERVING CANADIAN INVESTORS SINCE 1858Offices in Montreal, Toronto, Quebec, London

MINERAL ECONOMICS SYMPOSIUM

Inco", with a 41 *)o interest in Fort Knox, rive ut l y look over iiMiMj^ciiK-nl ot the project idler Fort Knox intersected sig nificant widths of both nickel- copper and zinc-copper miner alization.

About half of the flow- through financing must be spent by February, the rest by the end of the year.

Melinga, Comaplex plan summer work

The first phase of explo ration on a 1,000-square-mile property in Griffin Lake-Culla- ton Lake area of the Northwest

at THE 1992 CORDILLERAN ROUNDUP .

January 27,1992 (Hotel Vancouver, Vancouver, Canada)

Valuation of Mineral Properties and CompaniesI'rofrsbiunal valuators will discuss the state-of-the-art techniques used in valuing mining properties and companies and the pit/alls they watch for. Attend this practical symposium and not only learn new techniques to apply on the job but gain an overview of the many ways in which valuations play t rote in decision making.

For further information, please contact David Brace at (604) 689-0046, Fax: (604) 68R-8370

AN ENGINEERED SOLUTION TO THE PROBLEM OF TWO MAN ANFO LOADING.

"

SAMPLE LOCATIONS AND DESCRIPTIONS

6T-1-91 : 3m E and 23m S of L1S, 4-*-4OmE; quartz-carbonate vein from side of north-south trench, rusty stained, local dark green-black chlorite (?) inclusions; contains some greyish carbonate as medium- to coarse- grained crystals; quartz vein is variable in width and appears to fill in joints.

BT-2-91 : 3m E and 21m S of L1S, 4-*-4OmE; quartz-carbonate vein from side of same trench as sample 1; similar to sample I but with grey host rock; rusty stained quartz and greyish carbonate; trace pyrite and i '/. pyrrhotite as local fine- to medium-grained crystals.

BT-3-91 : 3m E and 20m S of L1S, 4-i-4OmE; quartz vein from same trench as sample l, with grey fragmental host rock containing up to 27. fine- to medium-grained, disseminated pyrite and local pyrrhotite; rusty stained quartz .

GT-4-91 : 3m E and 17m S of L1S, 4*4OmE; felsic fragmental from same trench as sample l, containing clear, angular quartz crystals O.I cm diameter; also some cherty-buff- light grey fragments up to O. 5 cm; also some larger (up to 5 cm long) light grey felsic fragments with small black spots (sulphides?); both the matrix and the larger felsic fragments contain disseminated fine-grained sulphides; also small, angular, black argillite fragments up to l cm long; also some carbonate patches which weather brownish; overall about 3X sulphides as: magnetic pyrrhotite as fine-grained disseminations and as wispy patches; possible bornite? as small (l mm) locally cubic crystals, irridescent blue; and fine-grained pyrite crystals in some felsic clasts.

GT-5-91: lOm N and 6m W of US, 5^20mE; very foliated felsic fragmental, some foliation planes are covered with gold coloured, soft material, possibly sericite?; contains some graphitic argillite fragments; some vuggy quartz veining with small, clear quartz crystals; trace fine grained pyrite and possibly fine grained irridescent blue bornite; some brownish stained carbonate crystals along some fracture planes; rare black, glassy quartz crystals less than l mm diameter with concoidal fracture.

BT-6-91: iOm N and 6m W of LiS, 5*20mE; from piece of blasted out float; felsic fragmental, similar to sample 5, foliated with very rusty foliation planes; containing quartz crystals less than l mm diameter, some cherty looking quartz as pods, possible felsic fragments now flattened along foliation plane; sulphides occur as long streaks parallel to the foliation.

BT-7-91 : ilm S and 3m E of L3S, 6-*-4OmE; taken from cliff along possible shear zone?; felsic fragmental with black argillite fragments; containing clear quartz crystals less than l mm diameter; some carbonate crystals; trace pale coloured sulphides.

GT 8-91 : 7m E and 3m S of L5S, 5+4011^; from previously blasted area; dark grey felsic fragmental with black fine grained argillite fragments and cherty light grey fragments; containing quartz crystals less than l mm diameter; IX locally brassy coloured fine grained disseminated pyrite; some carbonate; locally sulphides are irridescent; also some pyrrhotite as wispy patches; this sample is from the area with larger than normal fragments.

BT-9-91: 9m E and 3m S of L5S, S+AOmE; from same previously blasted area as sample 8; similar to samples 7 and 8.

ST-1O-91: 6m W and 3m N of L5S,5*6OmE; rusty felsic fragmental from south side of trench.

GT-11-91: 4m W and 2m N of L5S, 5*6OmE; sulphide-bearing felsic clast, taken from vertical east wall of trench; with some green epidote along layers; some disseminated pyrite especially within dark inclusions.

BT-12-9is 4m W and 4m N of L5S, 5*60mE; taken from vertical wall of trench in rusty area; felsic fragmental with quartz veinlets less than 2 mm wide; trace to IX fine grained disseminated pyrite; felsic cherty looking white fragments and black fine grained argillite fragments; black, glassy quartz crystals less than l mm diameter.

GT-13-91S 3m W and llm N of L5S, 5*6OmE; rusty, foliated felsic fragmental on same outcrop as large clasts.

BT 14 91 s 9m E and 17m N of L5S, 5*6OmE; felsic fragmental containing carbonate veinlets; some dark sulphides, probably pyrrhotite (magnetic); also some granular medium- to coarse-grained quartz; also less than i '/, fine-grained disseminated pyrite.

BT-15-91: 41m N and 9m E of L5S, 5*6OmE; from 4 parallel quartz veinson side of outcrop, within a 2 m wide zone; local rusty stained, vuggy;the quartz veins narrow and pinch out on top of the outcrop.

GT-16-91! 1m W and 57m N of L5S, 5+6OIUE; from 3 irregularly trending and locally folded quartz veins up to 5 cm wide, locally brownish stained, no sulphides seen; similar to sample 15

BT-17-91: 1m E and 57m N of L5S, 5-*-60mE; taken along west edge of trench; from 2 small quartz veins running perpendicular to trench; rusty weathered felsic fragmental host rock containing pyrite.

BT-18-91: 7m W and 61m N of L5S, 5*6OmE; from folded 5 cm wide quartz vein trending into trench; sample also contains fine-grained host rock with IX pyrite; some magnetic pyrrhotite in quartz vein as blobs about 0.5 cm long.

BT-19-91: 50m B and 7m E of LO, 3*4OmE; some float in sample of pyrite- bearing felsic fragmental with small amount of quartz vein; quartz flooding noted near this sample.

BT-2O-91: 14m E and 46m S of LO, 3-i-4OmE; from rusty area of outcrop; dark grey felsic fragmental with black argillite fragments and white felsic fragments with 27. fine-grained disseminated sulphides in matrix, some irridescent and others magnetic; quartz crystals less than l mm diameter; locally, matrix contains 2 mm long, rectangular white possible plagioclase crystals.

GT-21-91: 19m E and 45m S of LO, 3+4OH1E; rusty area of outcrop; felsic fragmental containing IX fine-grained, disseminated pyrite and less than IX quartz eyes, less than l mm diameter.

ft:-22-91: llm E and 48m S of LO, 3*4OmE; rusty area of outcrop; felsic fragmental containing some pyrite and some streaks of pyrrhotite.

6T-23-91: 9m E and 56m S of LO, 3*4OmE; from rusty area of outcrop; felsic fragmental containing about l to 2X, large cubic pyrite crystals up to 3 mm diameter; quartz crystals; less than i '/, pyrrhotite as streaks; also some irridescent sulphide, possibly chalcopyrite? (soft, scratched by nail).

GT-24-91: 4m W of L1S, 3+SOmE; from rusty area of outcrop; felsic fragmental with minor pyrite; similar to sample 21

BT-25-91: 2Om S and 4m E of L1S, 4*20mE; float, quartz vein with some black-dark grey host rock inclusions; quartz is coarse-grained, locally brown- rusty stained; some pyrrhotite in host rock inclusions/wall rock and also contains some sericite.

GT-26-91: 16m S of L1S, 4*4OmE; from rusty area of outcrop; quartz flooding in felsic fragmental with brownish sericite? along foliation planes.

GT-27-91: 5m E and 14m S of L1S, 4*4OmE; quartz veins from quartz flooded area, locally rusty-brown stained; quartz veins are irregular and range from l to over 1O cm wide.

GT-28-91: 23m S and 23m E of L1S, 4*4OmE; from 2.5 cm wide quartz vein, trending O15 AZ, vertical dip; rusty stained, no sulphides seen.

GT-29-91: 3m E and lOm S of L3S, 6*4OmE; rusty stained felsic fragmental.

GT-3O-91: 19m S of L3B, 6-*-4OmE; rusty stained, foliated felsic fragmental, similar to sample 26.

GT-31-91: 6m E and 6m S of L5S, 5-*-4OmE; from same blasted area as sample 8 and 9; felsic fragmental containing thin veinlets of white, fine-grained, crystalline carbonate; less than i "/. fine grained, disseminated pyrite; also about 2.7. fine-grained disseminated sulphides with a darker, brassier, locally irridescent colour, possibly chalcopyrite?; some pyrrhotite along fragment edge; quartz crystals.

GT-32-91: lOm E and 6m S of L5S, 5*4OmE; quartz vein showing slickensides and rusty staining, locally looks greenish; some dark host rock inclusions as ribbons; from a discontinous, irregularly shaped gash of quartz about 3 cm at it widest point.

GT-33-91: 1m E and llm S of L5S, 5+6OIHE; from side of old blasted out trench; felsic fragmental with about IX sulphides as pyrite and magnetic pyrrhotite; contains some large buff greenish cherty looking fragments 5cm long, cut by quartz veinlets; also containing mottled fragments consisting of round to flower shaped areas about 2 mm diamater, possibly plagiocalse crystals?; with dark grey black aphanitic interstitial material.

BT 34 91: Im E and llm S of L55, 5*6OmE; from 5 cm wide portion of vein which pinches out; containing gold coloured sericite and

than IX pyrite; contains clear, very soft, radiating crystals in the form of wheat sheaves with milky white quartz between the radiating acicular crystals; also some dark green, soft chlorite rich host rock inclusions/blebs; sample is crumbly, sugary textured.

BT-35-91: 17m E and 12m S of L5S, 5*6OmE; float from l m diameter boulder from blasted area; felsic fragmental containing abundant quartz crystals about l mm long and some white plagioclase laths about 2 mm long; fine-grained sulphides occur in black argillite fragments; pyrrhotite seen in matrix; contains black argillite and cherty felsic fragments.

BT-36-91: 5m W and 4m N of L5S, 5*6OmE; from side of blasted out trench; felsic fragmental containing large, white, subangular to subrounded felsic fragments up to 2O cm diameter but most fragments are less than 7 cm; fine-grained dark grey matrix is locally rusty weathered; local rusty spots can be seen but no sulphides were seen.

BT-37-91: 6m E and 2m S of L1S, 3+OOmE; felsic fragmental containing trace fine-grained, disseminated pyrite in matrix.

BT-3B-91: 7m E and 36m S of L1S, 4*2OmE; rusty weathered, foliated felsic fragmental containing quartz crystals less than l mm diameter; trace fine grained, disseminated pyrite; some carbonate as veinlets and as fine to medium-grained crystals; wispy patches of magnetic pyrrhotite; some sericite.

BT-39-91: 16m E and 38m S of L1S, 4*2OmE; quartz vein with possibly two generations of quartz, one is milky white on weathered surface and grey on fresh surface and is cut by milky white to translucent quartz; local rusty stain; locally vuggy.

BT 4O-91: 17m E and 37m S of L1S, 4*20mE; quartz vein locally vuggy, no sulphides seen; local rusty staining.

BT-41-91: 18m E and 41m S of LIB, 4-*-2OmE; quartz vein, rusty stained, locally vuggy.

ST-42-91: 19m E and 41m S of L1S, 4*2OmE; locally vuggy quartz vein with local rusty stain, no sulphides seen; up to 5 cm wide.

BT-43-91: 21m E and 41m S of L1S, 4*20mE; quartz vein containing brownish "ribbons"; milky white quartz, medium- to coarse grained; up to 5 cm wide.

ST-44-91: 22m E and 41m S of L1S, 4*20mE; folded quartz vein, rusty along fractures, some dark greenish host rock inclusions; host rock near quartz vein margin is slightly schistose.

ST-45-91: 25m E and 54m S of L1S, 4^4OmE; quartz vein, locally vuggy, brown stained, local pods of fine-grained, light green, very soft sericite?; irregularly shaped.

46 91: 6m E and 47m S of L1S, 4-*-40mE; from narrow, fine-grained ary quartz vein, rusty stained; less than l cm wide.

BT-47-91: 13m E and 34m S of L1S, 4*40mE; quartz vein brown-rusty stained; local brownish greenish host rock "ribbons".

BT-4B-91: 25m E and 53m S of LIB, 4^4OmE; from narrow quartz vein, vuggy, brown stained.

GT-49-91: 7m E and 3m S of L5S, 5*40mE; felsic fragmental with quartz crystals less than l mm diameter; contains 2.7. f ine-grained sulphides including pyrite, blueish irridescent chalcopyrite? and possibly brown sphalerite.

ACCURASSAY LABORATORIESA DIVISION OF BARRINGER LABORATORIES LIMITED, REXDALE, ONTARIO

BOX 426KIRKLAND LAKE, ONTARIO, CANADA P2N 3J1

TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Onu, c. Chem (U.K.i, M.C.I.C., M.R.S.C., A.R.C.S.T.

44680 Certificate of AnalysisRoberta BaldTamarack Geo. S ProspectingBox 486South Porcupine, OntarioPON-1HO

Page

SAMPLE NUMBERS Accurassay Customer

252735252736252737252738252739252740252741252742252743252744252744252745252746252747252748252749252750252751252752252753252753252754252755252756252757252758252759252760252761252762252762

Gold ppb

GT-1-91GT-2-91GT-3-91GT-4-91GT-5-91GT-6-91GT-7-91GT-8-91GT-9-91

GT-10-91GT-10-91GT-11-91GT-12-91GT-13-91GT-14-91GT-15-91GT-16-91GT-17-91GT-18-91GT-19-91GT-19-91GT-20-91GT-21-91GT-22-91GT-23-91GT-24-91GT-25-91GT-26-91GT-27-91GT-28-91GT-28-91

5<5<5<5<5<5<5<5<5<5<5<5<5<5<5<5<5<5<55

<5<5<5 ^5<5<55

<5<52119

December 13 91

Work Order # : 911417 Project :

Check

Check

Check

LF-30 Per: sp X/fcuA

ORIGINAL



TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC.. Ph. D., c. Chem iom.), c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

44681 Certificate of flnalysisRoberta BaldTamarack Geo. 6 ProspectingBox 486South Porcupine, OntarioPON-1HO

Page;


252763252764252765252766252767252768252769252770252771252771252772252773252774252775252776252777252778252779252780252780252781252782252783252783

GT-29-91 GT-30-91 GT-31-91 GT-32-91 GT-33-91 GT-34-91 GT-35-91 GT-36-91 GT-37-91 GT-37-91 GT-38-91 GT-39-91 GT-40-91 GT-41-91 GT-42-91 GT-43-91 GT-44-91 GT-45-91 GT-46-91 GT-46-91 GT-47-91 GT-48-91 GT-49-91 GT-49-91

Gold ppb

<5 <5 <5 <56

<5 (5 <5 <5 <57

<5<5<5<5<5<5<5<5<5<5575

December 13 91

Work Order # : 911417 Project :

Check

Check

Check

LF-30 Per: s? LiU^

ORIGINAL



TEL.: (705)567-3361

President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Cm.), c. Chem (U.K.), M.C.I.c.. M.R.s.c., A.R.C.S.T.

44694 Certificate of Analysis

ProspectingRoberta BaldTamarack Geo.Box 486South Porcupine, OntarioPON-1HO

Page

SAMPLE NUMBERS Accurassay

252735252736252737252738252739252740252741252742252743252744252745252746252747252748252749252750252751252752252753252754252755252756252757252758252759252760252761252762252763252764252765

LF-30

December 16 91

Work Order # Project

911417

1

ustomer

GT-1-91GT-2-91GT-3-91GT-4-91GT-5-91GT-6-91GT-7-91GT-8-91GT-9-91

GT-10-91GT-11-91GT-12-91GT-13-91GT-14-91GT-15-91GT-16-91GT-17-91GT-18-91GT-19-91GT-20-91GT-21-91GT-22-91GT-23-91GT-24-91GT-25-91GT-26-91GT-27-91GT-28-91GT-29-91GT-30-91GT-31-91

Copperppm

24343958243853745350353143397

103225535448554657354376

555052

Zincppm

3415029013016097100

140016014059

13012084O<l526682

12015011012013048

110O658599110

Per: SY /JjUu^

ORIGINAL

ACCURASSAY LABORATORIESA DIVISION OF BARRINGER LABORATORIES LIMITED. REXDALE, ONTARIO


TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M .SC.. Ph. D., c . Chem iom.), c. Chem IU.K.J, M.C.I.c., M.R.S.C.. A.R.C.S.T.

44695 Certificate of Analysis

ProspectingRoberta BaldTamarack Geo.Box 486South Porcupine, OntarioPON-1HO

Page :


252766252767252768252769252770252771252772252773252774252775252776252777252778252779252780252781252782252783

GT-32-91 GT-33-91 GT-34-91 GT-35-91 GT-36-91 GT-37-91 GT-38-91 GT-39-91 GT-40-91 GT-41-91 GT-42-91 GT-43-91 GT-44-91 GT-45-91 GT-46-91 GT-47-91 GT-48-91 GT-49-91

Copper ppm

5316

6637565986

14876

12798

84

December 16 91

Work Order Project

Zinc ppm

653

1101300

75110

579

23

O

3400

: 911417

ican

LF-30 Per:

ORIGINAL

SCIIMTREXearth science division

Proton Precession Magnetometer for Portable or Base Station Use

features

MP-2

1 gamma sensitivity and accuracy over range of 20,000 to 100,000 gammas.Operates in very high gradients, to 5000 gammas per metre.Ultra small size and weight.Up to 25,000 readings from only 8 D cells.Battery pack isolated from electronics for corrosion protection.Battery pack easily extended for winter use.Light-emitting diode digital display, with complete test feature.Unique no-glare polarized reflector permits easy reading in bright sunlight.Indicator light warning of excessivegradient, ambient noise or electronicfailure.Digital readout of battery voltage.Rugged all metal housing for rough field use at all temperatures.Automatic recycling or external trigger features permit ready conversion to base station use.Short reading time.Broad operating temperature range.

SCIIMTPIEX

The MP-2 is a portable one gamma proton precession magnetometer for field survey or base station use. The optimized design of sen sor and circuitry using the latest CMOS com ponents has resulted in a very light weight, low power consumption, rugged and reliable magnetometer.

Light emitting diodes coupled with an in genious optically polarized reflector combine solid state reliability with easy reading even In bright sunlight.

A standard automatic recycling feature allows ready use of the MP-2, with suitable (optional) interfacing, as a base station recorder In analogue or ditigal form. Alternatively, a remote trigger can be used.

The noise-cancelling dual-coil sensor and elec tronics have been so designed as to effectively eliminate reading problems due to virtually all magnetic gradients which may be encountered In field survey conditions.

Dfl QnlMTPEX ''. MAGNETOMETER-.'MODEL M*-* . '. -

a world of discovery

TECHNICAL DESCRIPTION OF MP-2 MAGNETOMETER SCINTREX

RESOLUTION

TOTAL FIELD ACCURACY

RANGE

INTERNAL MEASURING PROGRAMME

EXTERNAL TRIGGER

DISPLAY

RECORDER OUTPUT (Optional)

GRADIENT TOLERANCE

POWER SOURCE

SENSOR

HARNESS

OPERATING TEMPERATURE TANGE

SIZE

WEIGHTS

1 Gamma.

± 1 Gamma over full operating range.

20,000 to 100.000 gammas In 25 overlapping steps.

Single reading — 3.7 seconds. Recyc. feature permits automatic repetitive) readlnqt. 3.7 seconds intervals.

External trigger input permits use of sampling Intervals longer than 3.7 seconds.

5 digit LED (Light Emitting Diode) readout dis playing total magnetic field in gammas or nor malized battery voltage.

Multiplied precession frequency and gate time outputs for interfacing with Incremental tape recorders (eg. Increlogger) for digital recor ding. As an additional option a digital to analogue convertor Is available for use with analogue recorders.

Up to 5000 gammas/metre.

8 alkaline "D" cells provlce up to 25,000 readings at 25 0 C under reasonable signal/noise conditions (less at lower temperatures). Premium carbon-zinc cells provide about 40V0 of this number.

Omnidirectional, shielded, noise-cancelling dual coil, optimized for high gradient tolerance.

Complete for operation with staff or back pack sensor.

-350C to +600C.

Console, with batteries: 80 x 160 x 250mm. Sensor: 80 x 150mm. Staff: 30 x 1550mm. (extended)

30 x 600 mm. (collapsed)

Console, with batteries: 1.8kg. Sensor: 1.3kg. Staff: 0.6kg.

SCINTREX LIMITED222 Snidercroft Road.Concord. Ontario, Canada L4K 185

0. IflCX C6-

IVIAXMIIM II- ElVI

m Five frequenciea: BBB, 4*34, SBB, 1777 and 3555 Hz.m Maximum coupled C horizontal-loop J operation with reference cable. ,': ':;;A t , -m Minimum coupled operation With reference cable. U Vertical-loop operation without reference cable.m Coil separatlona: SS, BO, 1OO, ISO , SQO and SSOm

twith cable J or 100,200,300,^00, BOO and BOO ft.m Reliable data from depthe of up to 1BOm C BOO ft J.K Built-in voice communication circuitry with cable,m T ilt meters to control coil orientation.

**7^'^#*^^

SPECIFICATIONS :

Frequencies i 222.444. BBS. 1777 and 3555Hz. Repeatability iModes of Operation! MAX: Transmitter coil plane and re

ceiver coil plane horizontal (Max-coupled; Horizontel-loop mode). Used with refer, cotte.

M l NI Tranemitter coil plane ltal end receiver coil plane ver tical (Min-coupled mode). Used with reference cable.

V.L. i Transmitter coll plane vert!-- eel end receiver coil plane hori zontal (Vertical-loop mode). Used without reference cable, In parallel lines.

85.50.100,150,800 GSSOm (MM P or 1OO. 200. 300, 4OO,8OOand BOO ft. (MMDF). ; Coil sepsrstlons hi VL.moda not ra- striated to fixed vslues. -. .

Parameters Readi - In -Phase end Quadrature compo nents of the secondary field In MAX end MIN modes. . :

- Tilt-engla of the total field In V.L. mods. ' ' -- ' ;

Coll Separatlonat

Readouts)

Scale Ranges i

- Automstlo. direct readout on 3Omm (3.5") edgewise meters - in MAX snd MIN modes. No null ing or compensation necesssry.

- Tilt angle end null In SO nrm edge wise meters In V.L.mode. - . .

In-Phsse: *Spy..t1CO* by pusn-

Readability:

Ouedrstune: tSQ * . tlCXDr. by push button switch.

Tilt: *75V. slops . . ' NulKVLJ: Sensitivity adjustable by separation switch.

In-Phsse and Quadrature i OSS V. to O.5V. ; Tilt J 1V.. . ..

O.25V. toil'/, normally, depending on conditions, frequencies and coil aeparation used.

TrHnsmltter Outputs - 222Hz :22QAtms- 444Hz :SOQAtma- ESS Hz : 12OAtms- 1777 Hz : 6QAtma-3555 Hz: 3OAtma

Receiver Batteries i 3V trans, radio type batteries (4). Life: approx. 35hrs. continuous du ty ( alkaline , O.5 Ah), less in cold weather.

Transmitter Bacteria a i

Referenda Cabla l

Voloa Link i

Indicator Lights i

12V S Ah Gel- type rechargoebto battery- (Charger supplied)

Light weight S- conductor teflon cable for minimum friction. Unshield ed. All reference cables optional at extrs cose. Please specify

Built-in intercom system for voice communication between re ceiver and transmitter operators In MAX end MIN modea, via re ference cable .

J

'J

•J

JBuilt-in signal end reference warn ing lights to Indicate erroneous readings .

TamparaturaRange) -4O*Cto*eO'C (-4O'Fto*14O'F). Receiver Weight i B kg (13 Ibs.)

'Transmitter Welghtt 13kg (23 Ibs.)

: Shipping Welghtl Typically SOkg (135Ibs.). depend- : ' ' Ing on quantities of referencecable and batteries included.Shipped In two field/shipping cases.

.^ 8p*olflo*elona aubjace to cnanga without notification

Jt

P A FI A NT B TRIGS LIMITEDSOD STEELCASE RD. E.. MARKHAM. OMT, CANADA. L3R 1G2Phone: (418) 495-161S Cables: APEXPARA TORONTO Telex :OB-SSe773 NOROVIK TCDR

42A12SE8905 2.14938 GODFREY

ntario 300

Geoscience Approvals Section Mining Lands Branch Willet Green Miller Centre 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (705) 670-5853 Fax: (705) 670-5863

Our File: 2.14938 Transaction #: W9360.00018

May 14, 1993

Mining RecorderMinistry of Northern Developmentand Mines60 Wilson Avenue1st FloorTimmins, OntarioP4N 2S7

Dear Sir:

RE: Approval of Assessment Work on mining claims P 1176409 et al. in Godfrey Township.

Ministry ofNorthern Developmentand Mines

Ministers du Developpement du Nord et des Mines

The assessment credits for geology and geophysics, sections 12 and 14 of the Mining Act Regulations, as listed on the original Report of Work, have been approved as of May 13, 1993.

Please indicate this approval on the claim record sheets.

If you have any questions please contact Dale Messenger at (705) 670-5858.

Yours sincerely,

Blair Kite(Acting) Senior Manager, Mining Lands BranchMi/es and Minerals Division

EM/j l Enclosures:

: I/Assessment Files Office Toronto, Ontario

cc Resident Geologist Timmins, Ontario

Mln^try ofNorthern Development

_ anrt MinesOntario 9

Report of Work Conducted After Recording Claim

Mining Act

A1//V if\c^Tranaaetlon Number

. GOOPeraoneJ Information collected on thli form li obtained under the authority of the Mining Act. Thil Information will be uaed for correspondence. Queatlona about

into ooHectlon ahotrtd be directed to the Provincial Manager, Mining Landi, MInlatry of Northern Development and MInea, Fourth Floor, 1M Cedar Street,

Sudbury, Ontario, P3E 6A5. telephone (705) 670-7284.

of firing* afsesmnenrwlSK oMorOltInstructions: - Please type or print and submit In duplicate.- Refer to the Mining Act and Regulations for requirements

Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

the Mining

^

G- 399 X 1193

Work Performed (Check One Work Group Only)WorkGroup

^Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorizedlilnrtfwonx

Assay*Assignment from Reeerve

— Type2,/jJ 6 C-WTTVr\)*?y ^ ̂OA- O 6-/ C/^ (^ ^t/^l/fc^/ ( /AOC-t^^/ O/AJtf- /|-S5A*^*t)

&&OPHV3ICAL &U R \J6VS (Mto&lJG-T&M&T&l^ *4- HL&M*).

RECFlvepMAR 1 7 1993

MINING LANDS BRANCH

Tot*' A*****"**"* Work Claimed on the Attached Statement of Costa S 7 A. &0& * **^

Note: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

Pereon* and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name

/Poe&erft &HL&

(attach a achedule H necessary)

Address

/#? MftRGflZ&r fl'i/e LJI/E& o/Jrr—— nCOORDED ——

ftB 19 1993

Pecpint

Certification of Beneficial Interest * See Note No. 1 on reverse side

l certify that at the time the work was performed, the claims covered In this work report were recorded In the current holder's name or held under a beneficial Interest by the current recorded holder.

Oats Recorded Holder or Agent (Signature)

tt*

Certification of Work Reportl certify that l have a persona! knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after

Its completion and annexed report is true.Name anoAddress of Person Certifying

Telepone No. Date Certified ByJSignature)

fa

For Office Use OnlyTotal Value Cr. Recorded Date Recorded

iyg. t"f/'9?Mining RecWer f

'earned Approval Dare

Dale N otice (or Amendments Sent

Dale Approved ..s '

i 11

ff Sil

CO; i-:

*s-

J*si S

ri

lig '\0 0

3Sb 8

*^i W

^8

8

i li:

K Cred

its y

ou a

re c

laim

ing

in th

is re

port

may

be

cut b

ack.

In or

der t

o m

inim

ize th

e ad

vers

e ef

fect

s of

suc

h de

letio

ns, p

lease

indi

cate

from

wh

ich c

laim

s yo

u wi

sh to

prio

rize

the

dele

tion

of cr

edits

. Pl

ease

mar

k (s

] on

e of

the

follo

wing

:

1. D

Cre

dits

are

to b

e cu

t bac

k st

artin

g wi

th th

e cla

im li

sted

last,

wor

king

back

ward

s.2.

(M

Cre

dits

are

to b

e cu

t bac

k eq

ually

ove

r all

claim

s co

ntai

ned

in th

is re

port

of w

ork.

3. D

Cre

dits

are

to be

cut

bac

k as

prio

rized

on

the

atta

ched

app

endix

.

In th

e ev

ent t

hat y

ou h

ave

not s

pecif

ied

your

cho

ice o

f prio

rity,

opt

ion o

ne w

ill be

impl

emen

ted.

Not

e 1:

Exam

ples

of b

enef

icial

inte

rest

are

unr

ecor

ded

trans

fers

, opt

ion

agre

emen

ts, m

emor

andu

m o

f agr

eem

ents

, etc

., w

ith re

spec

to

the

min

ing

claim

s.

Not

e 2:

If

wor

k ha

s be

en p

erfo

rmed

on

pate

nted

or

leas

ed l

and,

ple

ase

com

plet

e th

e fo

llow

ing:

l cer

tify

that

the

reco

rded

hol

der

had

a be

nefic

ial i

nter

est

in th

e pa

tent

ed

or le

ased

land

at t

he ti

me

the

work

was

per

form

ed.

Sign

atur

eDa

te

Ontario

MMMrytfDevelopment

and Mlneedu

int du Nordet dee mines

Statement of Costs for Assessment Creditfetat dee coott tux fine du crtdlt devaluation

Mining Act/Lot tur let mines

Traneactlon NoVN* de transaction

Personal Information collected on thta form li obtained under the authority of the Mining Act. Thlt Information wtll be used to maintain a record and ongoing ttatu* of the mining elalm(a). Ouettloni about this ooflectlon ahouM be directed to the Provlnolal Manager, Mining* Unda, MInlttry of Northern Development and Mlnee, 4th Floor. 159 Cedar Street, Sudbury, Ontario

SAB, telephone (708) 670-7264.

Lea renaelgnement* pereonnela oontenua dana la prisente formula aoni recueltna en vertu de la Lo) tur let mine* et tervkont 4 tenlr a Jour un registre dee oonceaelona mlnleret. Adretter toute question tur la coftece de cat renaelgnementa au chef provincial dea terrain* mlnlera, mlnistere du Devetoppement du Nord at dee Mlnee, 1M, rue Cedar, 4* etage. Sudbury (Ontario) P8i 6A6, telephone (706) 670-7264.

1. Direct Coete/CoQte directsTotals

Total globalAmount Montant

Ubour Meln-d'oeuvreField Supervision SupervWon tur le terrain

Contraotor'a and Coneurtant'e Fee* Drafted*

ettferexpert

MINING LAND i BRANTotal Direct Cottt

Totel dee coott dlreett

Note: The recorded holder will be required to verify •xpandHures claimed In tWa ttatement of ooata wNhln 30 day* of a request for verification. H verification l* not made, the Minister may reject for assessment work eJ or part of the assessment work submitted.

2. Indirect Coete/CoOto Indlrecte* * Note: When claiming Rehabimatlon work bxflreot cottt are not

allowable M ateewment work. Pour le rembouraement dee travaux de rehawmatkxi. le* coOt* InoVtott ne aont pa* admltelblet en taut que travaux

Typt

Trantportttlon Tranaport

Pood andLodgingNowrrNureetMbergemenlMobMiatlon andDarftobiHvatleiiMobm*atlonet

DescriptionType'

Amount Montant

Totals Total global

Sub Total of Indirect Cottt Totel pertW dee eopte Indlreete

AfttOUflt AltOWWW {HOl ytt9Vtt VlMI Mvl Of OVMI OOCVe^

Montant admlttMe (n'txoManl pa* M H d** ooMt eVtott;Total Value of Aaaeaament Creen

etal of Wract and MowaM* reot 00*1*)

Valeur total* e\i treeH

Not* : Le Wulalre enreglttnt sera term de verifier tot depense* dsmandeesdana le present etat des coOts dans las SO Jours sutvant une demande l eel effet. S) la verification n'est pa* *tt*ctuee, le rrdnletre peut rejeter tout ou une partle de* travaux d'evaruatlon presentee.

Fifing Oltcounta

1. Work filed within two years of completion It claimed at 10CW of the above Total Value of Assessment Credit.

Remltet pour depot

1. Let travaux deposes dans tot deux ant turvant tour achevement sort rembourses 1100 ̂ de la valeur totale tusmentlonnee du ere* devaluation.

2. Work filed three, four or five years after completion It claimed at SOH of the above Total Value of Assessment Credit. See celculattont below:

Total Value of Assessment Credit x 0.50 -

Total AtteMment Claimed

2. Lea travaux deposes trola, quatre ou cinq ana apt e* leur achevement aont rembourses a 60 H de la valeur totale du credit devaluation susmenttonne. Voir let calcult d-desaout.

Valeur totaltdu cr*dn devaluation Evaluation total* d*mand*t

x 0,50 -

Certification Verifying Statement of Coste\

l hereby certify:that the amounts shown are as accurate as possible and these costa were Incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that at(Recordad Holder, Agtnt. Position In Compmyhr,

.\i"i "to make this certification HI** M ,. l; - ! Mr ' f ' . ' '- -t——————-——-—- L _i r j.tt 109?

C? 1 ? (O* *

Atteetatlon de I'etat dee coOte

J'atteste par la presente :que les montants Indiques sont le plus exact possible et que ces ddpenses ont ete engagees pour effectuer les travaux d'evaluation sur let terrains Indiques dans la formule de rapport de travail ci-joint.

l am authorized Et qu'a titre de je suis autoris6(tltulllr* •nogulr*. reptistnltnl, post* cccup* dan* la compagnie)

a faire cetle attestation.Dal*

'Jots Duns cetle fo-mule. lO'SQu'il design* dps persc-nnes. le ma^rulm est u i; !'S* au sons

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Astronomic

LEGEND

DiabaseFelsic fragmentalmetavolcanic rocks

PYRITE

CHALCOPYRITE

SPHALERITE

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---" OUTCROP

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CLAIM POST ( LOCATED

CLAIM POST , ESTIMATED

CLAIM LINE

SURVEY PIN/ POST

NUMBER

O 20 40 60 80 100m

4 q Q^X ij} ttjf

GEOLOGICAL

MAP

Map 1SCALE: 1:2000

BY: R. BALD

LOCATION'.GODFREY TWR

DATE JANUARYJ99242A12SE8905 2 .1493B GODFREY 210

LAN-

L3N-

L2N-

UN

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CLAIM POST, ESTIMATED

CLAIM LINE

SURVEY PIN/POSTiCLAIM NUMBER

BASE STATION

INSTRUMENT: SCINTREX MP-2 PROTON PRECESSION MAGNETOMETER

Add 58,000 gammas to all readings

Contour interval - 5 00 gammas

O 20 40 60 80 100m

MAGNETOMETER

SURVEY

Map 2SCALE: 1:2000

BY; R. BALD

LOCATION: GODFREY TWR

DATE: JANUARY, 1992

42A12568985 2.14938 GODFREY 2S0

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42AI2SE8905 2.14938 GODFREY 330

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CLAIM NUMBER

INSTRUMENT: APEX PARAMETRICS MAXMIN li PORTABLE EM

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COIL SPACING s 150m

PROFILE SCALEs tem * 10V.

* READINGS

-READINGS

N-PHASE READINGS

QUADRATURE READINGS

O 20 40 60 80 100m

HORIZONTALLOOP

SURVEY

Map-3SCALE: 1:2000

BY: R. BALD

LOCATION: GODFREY TWP.

DATE; JANUARY. 1992

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Map ASCALE: 1 :2000

BY;R-BALD

LOCATION: GODFREY TWP.

DATE '.JANUARY ,199242A12SE8905 2.14938 GODFREY 240

geotechnical report geological and geophysical …

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