r.j. the properties mcgowan, of...portions of gutcher lake and irene lake respectively. the selkirk...

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ABOTOSSAWAY010

REPORT ON AGEOPHYSICAL SURVEY

OVER THE PROPERTIES OFR.j. MCGOWAN,

ABOTOSSAWAY TOWNSHIP,SAULT STE. MARIE MINING DIVISION,

ONTARIO

MAY 2 3 1984

P.O. Box 2028 Wawa, Ontario May 18, 1984

R.G. Reid, B.A.Sc.S.M. Sears, B.A., B.Se.

GEOLOGISTS

v : P.O. Box 4, #370 - 625 i iowe Street, Vancouver, B.C. V6C 2T6 Telephone: (604) 683-0417

-i-

SUMMARY

Ground magnetometer and VLF-EM s-j^veys have been

conducted upon twenty unpatented mining claims located in

Abotossaway Township and owned by R.J. McGowan of Vancouver,

British Columbia.

The resulting data has delineated a total of

24 distinct targets which are felt to be worthy of addi

tional follow-up work. A two-phase exploration program

involving linecutting, prospecting, and rock sampling, geo

logical mapping, limited geochemical (soil) sampling, detailed

geophysical surveys, trenching and diamond drilling is recom

mended. Costs for these programs are estimated to be

S136 000 for Phase I and S332 000 for Phase II should the

latter be justified.

Respectfully submitted,

Russell G. Reid, B.A.Se. Geologist

Wawa, Ontario May 18, 1984

Seymour M. Sears, B.A., B.Se. Geologist

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TABLE OF CONTENTS

SummaryTable Of Contents lacesNEean 0044 ABOTOSSAWAY

IntroductionProperties Location and AccessRegional GeologyRegional MineralizationPrevious Work On The PropertiesSurvey Procedure and Instrument InformationDiscussion of Results

Jackson Lake Selkirk Lake Gutcher Lake

Conclusions and RecommendationsCost Estimates

Jackson Lake Selkirk Lake Gutcher Lake

BibliographyStatements of Qualifications

List of Figures

Figure 1: Property Location MapFigure 2: Location MapFigure 3: Claim Map^igure 4: General Geology

List of Maps

Map No.637-AB-A1 Jackson Lake Magnetometer Survey637-AB-A2 Jackson Lake VLF-EM Survey637-AB-B1 Selkirk Lake Magnetometer Survey637-AB-B2 Selkirk Lake VLF-EM Survey637-AB-C1 Gutcher Lake Magnetometer Survey637-AB-C2 Gutcher Lake VLF-EM Survey, Fraser Plot637-AB-C3 Gutcher Lake VLF-EM Dip Angle Survey

010C

Page

i ii

I 3 7

II 15 1820202426293131323334 36-37

24

610

Pocket Pocket Pocket Pocket Pocket Pocket Pocket


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INTRODUCTION

A Combined ground magnetometer and VLF-EM survey

has been completed upon 20 unpatented mining claims' in

Abotossaway Township, Sault Ste. Marie Mining Division,

Ontario, on behalf of R.J. McGowan. The work was carried

out between January 21 and February 13, 1984, by

D. Belanger and G. Young of Manwa Exploration Services Ltd.

of Vancouver, British Columbia.

The surveys were conducted for the purpose of

detecting geophysical targets which may be associated with

economic deposit:, of gold and/or base metals, as well as

provide some tsc/c data upon which to base future explora

tion programs on. the claims.

The area has seen a considerable amount of

exploration work in the past, and hosts several prospects

from which past production of gold has taken place. A

comprehensive regional overview of the geology and minerali

zation discovered to date by previous workers is included

along with a discussion (and accompanying maps) of the

survey results.


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PROPERTY LOCATION

R. J. MCGOWAN ABOTOSSAWAY CLAIMS

REGIONAL LOCATION MAP

FIGURE 1

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PROPERTIES LOCATION AND ACCESS

The properties of R.J. McGowan being discussed in

this report all lie in Abotossaway Township (formerly

Township 28 Range XXVI) in the Michipicoten Area of Nor

thern Ontario, approximately thirty-two (32) kilometres

northeast of the town of Wawa, Ontario (Figures 1 and 2).

A total of twenty (20) claims are held in this township.

The most westerly claims, the Gutcher Lake Group,

consists of two (2) non-contiguous, unpatented mining claims,

SSM 640285 and SSM 640286 (Figure 3). The claims include

portions of Gutcher Lake and Irene Lake respectively.

The Selkirk Lake Group is composed of three (3)

contiguous, unpatented mining claims east of Selkirk Lake.

They are numbered SSM 640282 to 640284 inclusive.

The Jackson Lake Group contains fifteen (15) con

tiguous, unpatented mining claims in the vicinity of Jackson

Lake in the northeast section of Abotossaway Township (Fi

gure 3). The mining claims, are numbered SSM 640267 to

640281 inclusive.

Access to the claim groups held in Abotossaway

Township is best obtained by float-equipped, fixed-wing

aircraft, available from Hawk Junction or Wawa, Ontario.

Work could be expediated on portions of the claim groups

by utilizing helicopters, which are available on a regular


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\DUBREUIVILLE

Vx

ABOTOSSAWAY TOWNSHIP

K) KM

R. J. M c GOWAN

LOCATION MAP

Moy 18, 1984j FIG. 2

.

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basis from White River (40 km northwest) and from Wawa

during the summer months.

The general area of the claim groups may be

accessed using existing logging roads and a four-wheel

drive vehicle. A road leading west fron Goudreau siding,

passes north of the Jackson Lake Group to the old Ego

Mines Ltd. camp north of Mall Lake. This camp may also

be accessible by a road leading south from 'Mile 15' of

the gravel road from Highway 17 {Trans-Canada Highway) to

the town of Dubreuilville (Figure 2),

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JACKSONLAKEGROUP

GUTCHELAKEGROUP

SELKIRK j LAKE

4J GROUP

R. j. MCGOWAN

CLAIMABOTOSSAWAY TWP SAULT STE MARIE M. D. SHEET M - 166

*

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REGIONAL GEOLOGY

The Abotossaway Township claims are situated within

the Archean "greenstone" belt of the Michipicoten Area,

Northern Ontario.

Rocks within this belt are the result of the

cyclical deposition of metavolcanic and metasedimentary

sequences. The progression of volcanic activity has been

described by Goodwin (1966) as:

"1) widespread and prolonged effusion of predominantly basalt lava flows, through

2) extrusion of rhyolite-dacite-andesite pyroclastics, followed by

3) extensive hot-spring and fumarolic activities with attendant wallrock alteration leading to subaqueous deposition of banded iron formation, and concluding with

4) renewed mafic effusion."

The Wawa, Ontario area is thought to be underlain

by rock sequences from a minimum of three (3) cycles of

volcanism, from a number of different volcanic centres

{Sage, 1981).

The margins of the greenstone belt are defined by

underlying younger massive to gneissic granitic rocks. Nu

merous granitic and gabbroic dykes, sills, and stocks

intrude the rocks of volcanogenic origin, and may be the

subsurface equivalents of the extrusive volcanic rocks

(Goodwin, 1966).


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Rocks of the Wawa belt have been complexly folded

about fold axes trending both east-west and northwest-

southeast. Major faulting of the belt has occurred along

north-northwest trending fault planes, with left-lateral

offsets of up to five (5) kilometres being noted (Goodwin,

1966).

The Township of Abotossaway is located near the

northern margin of the Wawa greenstone belt. It is underlain

by a thick sequence of mafic metavolcanic rocks, flanked on

the south and northwest by significantly thick piles of

felsic metavolcanic and metasedimentary rocks (Figure 4) and

dipping near vertical. The occurrences of iron formation in

narrow east-west trending bands in the western half of the

township at the mafic-felsic metavolcanic contact indicates

the volcanogenic sequence is younger towards the north. Iron

formation also occurs within the mafic metavolcanic rocks,

and may be accompanied by minor felsic metavolcanic units.

Numerous felsic intrusive stocks, sills, and dykes

occur within the township, the largest of which is the

Butcher Lake Stock. This intrusive body is a light grey,

porphyritic to coarse-grained granodiorite measuring approxi

mately two (2) kilometres in diameter. Margins of the stock

are gradationally felsitic, with 'serrated' contacts and

little evidence of contact metamorphism in the adjacent

wall rock (Goodwin, 1966). The central phases of the stock


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grade into feldspar or quartz porphyritic rocks (Collins

and Quirke, 1926).

The lack of contact metamorphic effects and the

proximal location of felsic intrusive rocks to nearby

felsic pyroclastic metavolcanics indicate the felsic intru

sive rocks may represent ancient volcanic necks and feeder

dykes for extrusive volcanic activity (Goodwin, 1966).

The metavolcanic-metasedimentary rocks of Abotossaway

Township are tightly folded about the 'North Range Syncline 1

(Goodwin, 1966) in the north, and the Alden Lake Anticline

to the south (Sage, 1983). Both fold axes appear to trend

west-northwest across the township. The area is also cut

by two (2) major north-northwest trending fault zones with

very apparent left-lateral movement.


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LEGEND

Ag. Au, Py

FELSIC INTRUSIVE ROCKS

IRON FORMATION

CLASTIC METASEDIMENT

FELSIC METAVOLCANIC

MAFIC METAVOLCANIC

Geologicol contact (assumed)

Fault (assumed)

Miner mineral occurrence

Major mineral occurrence

Major occurrence, underground workings

Past producing mine

Silver. Gold . Pyrite

( AFTER THE ALGOMA CENTrtAL S. HUDSON BAY RAILROAD COMPANYl GECX.OGICAL COMPILATION MAPS.

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REGIONAL MINERALIZATION

The Michipicoten Area of Northern Ontario is

estimated to have produced more than thirty million tonnes

of iron ore, and almost two hundred thousand ounces of

gold since the start of mining operations in 18S9 (Good

win, 1966). Production of iron ore in the past has corae

from six deposits, and gold from eleven deposits, including

one past producer of gold in Abotossaway Township. Almost

one hundred mineral occurrences have been recorded in the

Michipicoten Area, including over fifty gold, more than

thirty-five iron, four base metal, one asbestos, and one

niobium (Goodwin, 1966). Current producers in the area are

limited to che Helen-MacLeod iron mine north of Wawa, and

a small open cut gold mine south of Wawa owned by

Bridgett Lake Resources.

The iron deposits of the area occur as long,

narrow zones of banded iron foniiation at the stratigraphic

top of felsic pyroclastic units, prior to the reverting of

the volcanic cyrle to thick, massive mafic volcanic flo*s.

The typical iron formation is composed of (in descending

stratigraphic order) graphitic chert, banded chert, massive

pyrite, and siderite units. Certain units may be more

abundant, while others are locally absent in the various

iron ranges of the area. Abundant alteration of underlying

'alsic volcanics, including carbonatization, ,,iica depletion

and iron enrichment has been noted and is most pervasive


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proximal to the iron formation.

The Township of Abotossaway r.ay be considered to

contain a minimum of three separate bands of iron forma

tion. The ranges in the southwest corner of the township

are relatively thin, consisting of banded chert-magnetite

with minor siderite and little pyrite. e northwest iron

ranges may be part of the Evans Creek iron formation,

which is composed of chert and magnetite, with interbedded

clastic sediments (Sage, 1983).

The eastern iron ranges form the previously tested

(1920's) Rand No. 2 deposit. The iron formation (strati-

graphical ly from bottom to top) consists of siderite, py-

k rite, and thinly, beaded chert. The sulphide facies of the

formation is most developed, and varies in thickness to

greuter than thirty (30) metres locally. The Rand No. 2

was explored as a possible source of pyrite for the pro

duction of sulphuric acid, and reserves were Jast estimated

at 13 600 000 tons grading 24.0 to 25.1 percent sulphur

by Superior Acid and Iron Limited (1925?) (Sage, 1983).

The known gold occurrences in the Michipicoten Area

are proximal to, or within several of the felsic intrusive

stocks. Tt has been observed, both in the free state and

bound with sulphides (pyrite and chalcopyrite), and generally

occurs within quartz-carbonate veins. .These veins occur within

fractures and along shear zones as she; c stringers or as

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larger lenses of relatively limited strike length (Goodwin,

1966). The vein assemblage has generally been found to be

quartz -f calcite ankerite tourmaline hornblende arsenopyrite

pyrrhotite pyrite chalcopyrite sphalerite galena (Frohberg,

1935).

A general correlation of gold mineralization to

surrounding geological setting has bean found to exist in

the Michipicoten Area. The majority of notable gold and base

metal occurrences are directly associated with felsic intrusive,

porphyritic bodies which have been emplaced in or marginal

to large felsic pyroclastic units (Goodwin, 1966).

Abotossaway Township is the host of numerous gold

occurrences, including the past producing gold m iri north

of Murphy Lake (Figure 4). All known occurrences are associated

with felsic intrusive stocks, most notably the Gutcher Lake

Stock. This large body of granodiorite with quartz-feldspar

porphyry phases may be linked to five (5) gold occurrences,

both within the intrusive and near the margins of the stock.

The Murphy Lake Mine has been attributed to the smaller

porphyry stocks north of Murphy Lake, The gold occurs in

quartz-carbonate veins and stringers filling fractures and

shear zones. Other felsic intrusive stocks within the township

show minor mineralization, although exploration of the areas

has been extensive but sporadic.

The Kozak Lake gold occurrence in the - southeast


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corner of the township, first discovered in 1927, has since

been intensively explored. A total of five (5) mineralized

zones of narrow quartz veins and fracture filling have been

defined. The mineralization includes galena, sphalerite, pyrite

and chalcopyrite as well as gold. The zones occur in a

highly carbonatized and schistose felsic roetavolcanic {Sage,

1983).

Other gold occurrences in Abotossaway Township are

located with the mafic metavolcanic units in random quartz-

filled fractures and shear zones.

l


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-iD-

PREVIOUS WORK ON THE PROPERTIES

The following data has been obtained from files

of the Assessment File Research Office of the Ontario

Geological Survey, Toronto, Ontario.

The two claims in the western portion of

Abotossaway Township, the Gutcher Lake Group (Figure 3),

were originally staked in 1955 for Ego Mines Ltd., when

the area was first opened for staking by the Algoma

Central Railway. Some reconnaissance geophysical surveys per

formed by Ego Mines in the early 1960's may have included

the Gutcher Lake group, although no record of the results

have been found.

The most westerly claim (SSM 640286) was investigated

by Ego Mines Ltd. in 1966. Their work culminated in a

303-foot diamond drill hole locate- near the eastern boundary.

The hole passed through intermedia ..d and felsic metavolcanics,

as well as two zones of iron formation (elevrn and twenty

feet respectively). Assaying indicated that the upper iron

formation was nearly 'barren 1 of gold and copper, while the

lower zone was anomalous in gold (0.015 ounces/ton over 5.0

feet) and copper (0.14 percent over same).

Both Gutcher Lake claims were included in an option

agreement between United Canso Oil and Gas, and' Ego Mines

Ltd. in 1976. United Canso personnel performed a horizontal

loop EM survey over the western claim, a magnetometer survey


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-16-

over the eastern claim, and geological mapping of both

during 1977 and 1978. The western claim was found to

have a strong electromagnetic conductor striking north-south

near the eastern boundary, in the same area as the pre

viously discussed diamond drill hole. The eastern claim was

found to be underlain by the Gutcher Lake Stock, and was^

magnetically dormant, save a miner magnetic 'high 1 near the

northeast corner of the claim. A number of sulphidic quartz

veins and felsic dykes have been observed on this claim.

The Selkirk Lake Group (SSM 640282 to 640284) appears

to have been explored minimally in the past. No data sub

mitted for provincial assessment credit is recorded, although

this claim block was previously administered by the Algoma

Central Railway (ACR). The area was, however, included in

a large-scale (three townships) project under a joint venture

agreement between the ACR and Getty Mines Ltd. The Getty

Mines program included an airborne geophysical survey, con

tracted to Aerodat Ltd. in 1973. The survey shows a series

of relatively strong, isolated magnetic 'highs' on the claim

group, which may be of interest, but were not investigated.

Although there is abundant evidence of prospecting

(old trenches and pits), there is, very little available

information on the Jackson Lake Group (SSM 640267 to 640281).

However, two diamond drill holes were completed on present

claim SSM 640273 by Albert A. Coppellan in 1969, Little


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data of assistance in assessing the possibilities of this

claim group, however, was provided.

A major gold occurrence has been recorded adjacent

to the Jackson Lake Group in ACR files east of Jackson

Lake. No information regarding this occurrence has been

located in Government files. *

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-IB-

SURVEY PROCEDURE AND INSTRUMENT INFORMATION

t A compass grid was established on each of the

claims (or claim blocks) to accommodate the two surveys.

Lines were established in a north-south direction every 100

metres with stations, measured by hip chains every 25 metres

and marked by flagging. A base line was cut and chained on

the Jackson Lake and Selkirk Lake properties, and chained

in by compass lines on the two Gutcher 'Lake claims- for

survey control. All lines were established prior to execution

of the surveys due to extreme snow conditions.

The VLF-EM survey was conducted along this grid

using a Sabre VLF-EM receiver. The Annapolis, Maryland (N.A.A.)

transmitting station (21.4 kHz) was utilized. Measurements re

corded at each station included the horizontal component of ,

the Field Strength of the transmitted signal and the Dip

Angle of the null. The observed Dip Angle data was later

filtered using a mathematical technique devised by Fraser

(1969) which is designed to eliminate "noise" and render

the anomalous crossover data contourable, and thus easier to

interpret. The resulting Fraser Filtered data was then plotted

at a scale of 1:2500 and the positive (*) values contoured

(Maps 637-AB-A2, 637-AB-B2, 637-AB-C2). The dip angle raw

data is shovm in profile form for the Jackson Lake (637-AB-A2)

and Selkirk Lake (637-AB-B2) properties. A separate plot of

the raw dip angle data is shown for the Gutcher Lake Group

(637-AB-C3).


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The magnetometer survey was conducted using a

Geometrics Model G-816 Portable Proton magnetometer. This

instrument measures the total intensity of the earth's

magnetic field in gammas. A main Base station was es

tablished on each of the separate properties with subsi

diary floating Base stations at other appropriate locations.

These stations were utilized during the survey in deter

mining the diurnal variations of the magnetic field. Mag

netic intensities were observed, and the diurnally corrected

data was reduced to a 59000 gamma base and plotted at

a scale of 1:2500 and contoured (Maps 637-AB-A1, 637-AB-B1,

and 637-AB-C1).


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DISCUSSION OF RESULTS

JACKSON LAKE

The magnetometer survey on the Jackson Lake group

has outlined a series of east-west trending weakly magnetic,

relatively narrow magnetic zones (Map 637-AB-A1). These fea

tures are cut by at least two north-northwest trending

magnetic highs, which appear to be diabase dykes. These

extend from:

i) 300 North on Line 12 East through600 South on Line 16 East.

ii) 275 North on Line 3 West through975 South on Line 1 East.

Three other north-northwest trending features (more

discernible from the VLF-EM survey results) are recognizable.

These include:

i) a broad {100-200 metres) zone of lowmagnetic relief trending from 200 Northon Line 15 East to 600 South onLine 19 East.

ii) a broad magnetic low zone passing through the east half of Jackson Lake trending approximately from the Baseline (0) on Line 9 East to 400 South on Line 11 East.

iii) a somewhat less recognizable low trendingthrough the long narrow lake (Buck Lake) on Line 1 East, seemingly parallel to the earlier mentioned diabase dyke. This zone passes from 300 North on Line 2 West through 300 South on Line 3 East.

These latter three features may represent removal

or alteration of magnetic minerals along shear zones, and


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will be further discussed with the VLF-EM results.

Two other significant features are apparent.

Firstly a persistent, narrow magnetic high (from 1 200 -

4 000 gammas above background) that extends from 500 South

on Line 7 East in a northwest direction through 275 South

on Line 3 East and then appearing to swing back towards

the east through 200 South on Line 3 East to 275 South

on Line 5 East. This zone appears to reflect a folded

magnetic horizon, and may provide some clues in any future

understanding of the structural aspects of the property.

Secondly, the magnetic high values occurring on

the bottom end of Lines 2 East, 3 East and 4 East (and

possibly 6 East), may represent the upper edge of an iron

formation (that which hosts the Rand Deposit) depicted on

maps by previous workers (e.g. Bruce, 1940).

The VLF-EM survey, in a broad sense, produces a

very similar picture as that of the magnetic data (Map

637-AB-A1). A series of east-west trending, relatively broad,

weakly conductive horizons, are delineated by the Fraser

Filtered data. These are strongly enhanced in three north-

northwest trending linear zones, coincident with those referred

to in the earlier presentation of the magnetometer survey

results. The axis of fifteen (15) of the stronger conductors

are shown superimposed upon the- magnetometer survey map

(Map 637-AB-A2), where they have been lettered from "A^1 to


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"J," for reference purposes. The character and possible

source of these are summarily listed below:

rnnrlnrtnrc "A " "A " "A " anH "A "conductors A1 . A2 . A3 ana AA - yery strong; relative iy

broad; east-west oriented; from 100-300 metres long; confined to a north-northwest linear zone; have an association with a weak magnetic low. Possible cause - sulphide concentration within selective horizons, localized within shear zone.

Conductors "B", "C" - moderate to strong, relatively narrow; east-west oriented; 100 metres long; occurring within a postulated north-northwest trending linear zone; associated with a weak magnetic low feature; possible cause - shear zone localization of sulphides {as above).

Conductor "D" - weak to moderate; relatively nurrow; east-west oriented; in excess of 300 metres long; strongest point associated with a magnetic high anomaly; possible cause - weak strata-related conductor enhanced at its junction with a crosscutting diabase dyke.

Conductor "E" - weak to moderate; narrow; east-west oriented; greater than 300 metres long; no magnetic association; possible cause - cultural features associated with roadway.

Conductor "F" - weak to moderate; relatively broad; 200 metres long; no magnetic association with its strongest point; possible cause - unknown.

Conductors "G", "H", and "I" - moderate to strong; relatively broad; east-west oriented; greater than 100 metres long; occurring within a postulated north-northwest trending linear zone; associated with a weak maonetic low feature;

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-23-

possible cause - localization of sulphides, in selective stratigraphic horizons, within a shear zone.

Conductor "I^1 - moderate to weal^ not fully defined due toproximity to edge of property; northwest oriented; less than 100 metres long but open to south (off of pro perty); no magnetic association; possible cause - may be weak sulphide concentration in stratiform unit, may be connected along strike to Conductor "I", but cannot be sure due to interference caused by a powerline separat ing the two.

Conductors "J" and "V . moderate to strong; narrow w

to relatively broad {"J^1 ); west-northwest oriented; both are single-line features, but the associated' lower magni tude conductors along strike suggest that the two fea tures join together on a competitor's claim which is situated in-between.


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SELKIRK LAKE

The magnetometer survey on the three Selkirk Lake

claims shows a number of narrow, irregular, weak (300 gammas

above background) linear trends of limited strike length

(Map 637-AB-B1). Three small magnetic "high" values appear

to indicate a narrow diabase dyke, passing from 250 South

on Line 4 East in a north-northeasterly direction through

275 North on Line 6 East. Two other clusters of "high"

values (1 000-2 000 gammas above background) on s ing l e-lines

also appear to reflect diabase dykes although their exact

orientation is undeterminable from this information.

The Fraser Filtered VLF-EM data (Map 637-AB-B2) shows

similar .veak linear trends, but these trends have a fair

degree of continuity. The stronger portions of the anomalous

zones, although themselves very weak conductors, are designated

as "A"-,. "B", "B,|" and "C" on the magnetometer survey map

(637-AB-B1), and discussed, briefly, below:

Conductor "A" - weak; consists of three short (100-metre) conductors crudely aligned along one curvilinear west- southwest trend; relatively broad; no definite magnetic association; possible cause - weak sulphides within stratigraphically bound - unit.

Conductors "B", and "B," . weak; relat , yely narrow; are very

likely joined together just south of the property, if so, then have a curvilinear shape covering in excess of 800 metres; no recognizable magnetic association;


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possible cause - weak sulphides in a stratigraphically confined unit.

Conductor "C" - weak; very broad (probably influenced by a second conductive zone, this being the westward exten sion of Conductor "B"); greater than 100 metres long; occurs on north flank of a strong magnetic (high) anomaly; possible cause - enhanced sulphide associated with the junction of a weak sulphide-bearing strati graphically bound sequence and a diabase dyke.


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-Zb-

GUTCHER LAKE

The West claim of the Butcher Lake group has

a relatively complex magnetic character {Map 637-AB-C1).

The western two-thirds (2/3) of the claim displays a

variety of values ranging from 200-300 gammas below to

up to 1 000 gammas above the background observed in near

by volcanic terrain. This pattern is likely accounted for

by the existence of local iron formation within the vol

canic sequence as detected by previous workers (Ego Mines,

1968).

The eastern third (1/3) of the claim has a

generally uniform magnetic pattern with values generally

700-800 gammas above that expected in volcanic terrain, more

in lino with a granitic rock signature. Two highly magnetic

zones (4 000 and 6 000 gammas above background) near the

edge of the two recognized terrains (100 South and 125

North on Line 4 East) probably represents the earlier

mentioned iron formation, possibly enhanced by its proximity

to the granitic intrusive contact.

3 moderate to weak conductors are apparent from

the Fraser Filtered VLF-EM data (Map 637-AB-C2). Although

they appear as distinct anomalies they are likely related,

forming part of a horseshoe-shaped conductive zone, arched

around the west end of the Gutcher Lake granitic (trondhje

mite) stock. The three conductors are lettered "A", "B" and


This report may not be reproduced in whole, in part, or in summary without the written permission of Manwa Exploration Services Lid

GUTCHER LAKE

The West claim of the Butcher Lake group has

a relatively complex magnetic character (Map 637-AB-C1).

The western two-thirds (2/3) of the claim displays a

variety of values ranging from 200-300 gammas below to

up to 1 000 gammas above the background observed in near

by volcanic terrain. This pattern is likely accounted for

by the existence of local --iron formation within the vol

canic sequence as detected by previous workers (Ego Mines,

1968).

The eastern third (1/3) of the claim has a

generally uniform magnetic pattern with values generally

700-800 gammas above that expected in volcanic terrain, more

in line with a granitic rock signature. Two highly magnetic

zones (4 000 and 6 000 gammas above background) near the

edge of the two recognized terrains (100 South and 125

North on Line 4 East) probably represents the earlier

mentioned iron formation, possibly enhanced by its proximity

to the granitic intrusive contact.

Three moderate to weak conductors are apparent from

the Fraser Filtered VLF-EM data (Map 637-AB-C2). Although

they appear as distinct anomalies they are likely related,

forming part of a horseshoe-shaped conductive zone, arched

around the west end of the Butcher Lake granitic (trondhje

mite) stock. The three conductors are lettered "A", "B" and


This report may not be"reproduced in whole,, in part, or in summary without the written permission ot Manwa Exploration Services Ltd

-27-

"C" and their axis ar shown on the magnetometer survey

map (Map 637-AB-C1), and discussed below:

Conductor "A" - weak to moderate; relatively narrow; north east trending; greater than 300 metres long; no observed magnetic association; possible cause - iron formation warped around north edge of granitic pluton.

Conductor "B" - weak to moderate; narrow within a broad weakly conductive zone; greater than 200 metres long; no recognizable magnetic association; possible cause - iron formation near granitic contact.

Conductor "C" - moderate; undefined width; undefined length, but potentially 200 metres; no magnetic association; possible cause - sulphides in shear zone or raft of volcanics within granitic pluton.

These three anomalous features deserve cautious

interpretation due to the complex attitude of the volcanic

rocks near the granitic intrusive in this area. Previous

workers (United Canco Oil and Gas, 1972 and Ego Mines

Ltd., 1966) interpret the iron formation in this area to

swing around into a north-south direction. It this is true,

a VLF-EM survey conducted along a north-south grid and

utilizing a transmitter station at right angles to the

strike is of only limited effectiveness.

The East claim in the Gutcher Lake group appears

at first glanc* to have a rather featureless magnetic

expression, typical of that expected in some felsic intru

sive rocks. Values are from 400-900 gammas above the

___________________________ MANWA EXPLORATION SERVICES LTD..

sf: .; ;This report may not be reproducedm whole, in part, or in summary without the written permission of Manwa Exploration Services Ltd.

background observed in adjacent volcanic rocks. However,

closer examination shows a central area of lower magnetic

relief (490 to 920 gammas) sandwiched between zones of a

higher background (1 100 to 1 390 gammas). This pattern may

represent two different phases of the intrusive stock, or

one of the crosscutting "fracture filled" structures referred

to by previous workers (Studemeister, 1983). In either case,

this phenomenon may be a useful guide for future explora

tion within this pluton.

Three very weakly conductive horizons were detected

by the VLF-EM survey (Map 637-AB-C2), all trending approxi

mately east-west. Since this orientation appears to be

favourable for the emplacement of gold-bearing quartz-carbonate

veins in adjacent properties (e.g. Murphy Lake Prospect,

2 km east), they may deserve additional follow-up work.

They are lettered "D", "E", and "F", and can be described

collectively as follows:

Conductors "D", "E", and "F" - weak; relatively narrow; from 100 to 400 metres long; east-west trend; no definite magnetic association at this scale; possible cause - east/west, shear related, weak sulphide concentration.


This report may not be reproduced in whole, in part, or in summary without the written permission of Manwa Exploration Services Ltd.' '

-29-

CONCLUSIONS AND RECOMMENDATIONS

The magnetometer and VLF-EM surveys on the

Abottossaway Township claims of R.J. McGowan has produced

numerous conductive zones that may represent favourable gold

or base metal-bearing horizons. Since drill testing of each

of these targets would be costly at this time, it is

recommended that a comprehensive field program consisting of

linecutting, prospecting, geological mapping, orientation

geochemical (soil) sampling, moveable transmitter geophysical

surveys, renching and diamond drilling be conducted upon the

claims in a two-phase program. The main thrust of the pro

gram should consist of detailed prospecting of any known

occurrences on the properties and near areas of anomalous

conductivity.

Particular attention should be given to the follow

ing:

Jackson Lake

The three north-northwest trending structures con

taining Conductors "A^,. "A2 ", "A3 ", "A4 ", "B", "C", "G",

"H", and "I" should be thoroughly evaluated to attempt to

determine their apparent significance in the emplacement of

gold mineralization. A horizontal Loop (HLEM) survey using

both north-south orientation and selected east-west orientation

to define the character of the anomalies would be very

useful.


This report may not be reproduced in whole, in part, or in summary without the written permission o( Manwa Exploration Services Ltd.

-30-

Conductors "O", "J^1 , "D", and "F" should bc

examined carefully for stratiform type of mineralization.

Selkirk Lake

All three conductors should be explored looking

for both stratiform sulphide zones, and crosscutting quartz-

carbonate vein filled structures.

Gutcher Lake

The iron formation on the West claim should be

located accurately by mapping and detailed horizontal loop

(HLEM) surveys. Any sulphide-bearing horizons should be

sampled and analyzed for gold. The East claim should be

carefully prospected, especially in the centre strip which

shows somewhat lower magnetic expression.

The cost?, relating to a two-phase exploration

program on these claims are estimated as follows.


"'This report may not be reproduced in whole, in part, or in summary without the written permissbn of Manwa Exploration Services Ltd.

-31-

COST ESTIMATES

Jackson Lake

PHASE I

Linecutting30 km e S2507km .

Geological Mapping, Prospecting and Sampling

Analytical Costs500 soil @|157sample S? 500* 200 rock @S257sample 5 000 '

Geophysical Survey (HLEM) 20 km Q 1200/km

TrenchingAccommodation and TransportationField SuppliesSupervision, Drafting and

Report Writing

PHASE II

Diamond Drilling 1 000 metres

Analytical Costs 600 samples

SubtotalContingency @ 15Jt

Total

Sl20Anetre

S257sample

S 7 500

16 500

19 cnn ^ buu

4 00010 00013 5004 000

12 OOPS 80 000

12 OOP

Supervision, Drafting and Report Writing

S 120 000

15 000

15 OOPSubtotal $150 000

Contingency @ 10X 15 OOP Total

S 92 000

S165 000


^ TWs repot t may not be^eprc)duced in whole Jn part, or in summary without the written permission c4 Manwa Exploration Savic*.

-32-

Selkirk Lake

PHASE I

Linecutting5 km @ SSOO/km S 1 500

Geological Mapping, Prospecting and Sampling 3 000

Analytical Costs150 soil @Sl57sample |2 250x , Knn 50 rock @S257sample 1 250 ; d auo

Trenching 5 000 Accommodation and Transportation 2 000Supervision, Drafting and

Report Writing 2 OOPSubtotal |17 000

Contingency @ 12* 2 040Total S19 040

PHASE II

Diamond Drilling300 metres @ S1507metre |45 000

Analytical Costs100 samples @ S257sample 2 500

Supervision, Drafting and Report Writing 7 500

Subtotal S55 000Contingency @ 15* 8 250

Total 163 250


This reporl may noS be'reproduced in whole, in part, or in summary without the written permission of Manwii Exploration Services Ltd.

-33-

Gutcher Lake

PHASE I

Linecutting5 km @ SSOO/km S 1 500

Geological Mapping, Prospecting and Sampling 4 500

Analytical Costs100 soil @|157sample S1 500* . nnn 100 rock 0S257sample 2 500 ' 4 uuo

Geophysical Surveys (HLEM)5 km of detail @ SSOO/km 1 500

Trenching 5 000 Accommodation and Transportation 3 500Helicopter Access

4 hours @ SSOO/hour 2 000Subtotal 5 22 000

Contingency @ 155t 3 300Total ' S 25 300

PHASE II

Diamond Drilling500 metres @ SISO/metre S 75 000

Analytical Costs200 samples @ |257sample 5 000

Supervision, D r afting and Report Writing 10 OOP

Subtotal S 90 000Contingency @ 15* 13 SCO

Total $103 500

Respectfully submi'Russell G. ReidV B. A. Se. Geologist

Oa^A-^^.

Wawa, Ontario Seymour M. Sears, B. A., B. Se. May 18, 1984 Geologist


.YhJSieport may not be" reproduced in whole, in part, or in summary without Ire written permission of Manwa Exploration Service* Ltd

BIBLIOGRAPHY

AFRO. Ontario Ministry of Natural Resources, Ontario Geolo gical Survey, Assessment Files Research Office, Toronto, Ontario.

Bruce, E.L. 1940. Geology of the Goudreau-Lochalsh area; Ont. Dept. Mines, vol. 49, pt. 3, pp. 1-47.

Burns, C.A. 1968. Ego Mines Ltd. Report on the Property of Ego Mines Ltd., Algoma District, Ontario for C.A. Burns Consulting Ltd.

Burwash, E.M. 1935. The Michipicoten-Missinaibi area; Ont. Dept. Mines, vol. 44, pt. 8, pp. 1-26.

Coleman, A.P., ano Willmott, A.B. 1902. The Michipicoten iron ranges; Univ. Toronto Studies, Geol. Ser., No. 2, 83 p.

Collins, W.H., and Quirke, T.T. 1926. Michipicoten iron ranges; Geol. Surv. Can., Mem. 147, 175 p.

Frohberg, M.H. 1935. The gold deposits of the Michipicoten area; Ont. Dept. Mines, vol. 44, pt. 8, pp. 39-83.

Gledhill, T.L. 1925. Goudreau-Lochalsh gold area, District of Algoma; Ont. Dept. Mines, vol. 36, pt. 2, pp. 50-86.

Goodwin, A.M. 1961. Some aspects of Archean structure andmineralization; Econ. Geol., vol. 56, No. 5, pp. 897-915.

1962. Structure, stratigraphy and origin of ironformations, Michipicoten area; Bull. Geol. Soc. Amer.,. vol. 73, pp. 561-586.

_____ 1964. Geochemical studies at the Helen iron range; Econ. Geol., vol. 59, No. 4, pp. 684-718.

1966. The Relationship of Mineralization toStratigraphy in the Michipicoten Area, Ontario; in TheRelationship of Mineralization to Precambrian Stratigraphyin certain Mining Areas of Ontario a,id Quebec, GeologicalAssociation of Ca-:ado, Special Paper No. 3.

Moore, E.S. 1931. Gaudreau and Michipicoten gold areas, District of Algoma; Out. Dept. Mines, vol. 40, pt. 4, pp. 1-54.

Morrison, L.G. 1978. Ego Mines Ltd. Geological Report on South- west Claims of Abotossaway Township, Province of Ontario for United Canso Oil and Gas Ltd.


Tula report may not be reproduced in whole, in part, or in summary without the written permission of Manwa Exploration Service* Ltd

-35-

Sage, R.P. 1979. Wawa Area, District of Algoma; p. 48-53 in Summary of Field Work, 1979, by the Ontario Geolo gical Survey, edited by V.G. Milne, O.L. White, R.B. Barlow, and C.R. Kustra, Ontario Geological Survey, Miscellaneous Paper 90, 245 K.

^ 1980. Wawa Area, District of Algoma; p. 47-50 jm Summary of Field Work, 1980, by the Ontario Geolo gical Survey, edited by V.G. Milne, O.L. White, R.B. Barlow, J.A. Robertson, and A.C. Colvine, Ontario Geological Survey, Miscelleneous Paper 96, 201 p.

^ 1981. Josephine Area, District of Algoma; p. 37-40 TnSummary of Field Work, 1981, by the Ontario Geolo gical Survey, edited by John Wood, O.L. White, R.B. Barlow, and A.C. Colvine, Ontario Geological Survey, Miscellaneous Paper 100, 255 p.

^ 1982. Josephine Area, District of Algoma; p. 28-33 InSummary of Field Work, 1982, by the Ontario Geolo gical Survey, edited by John Wood, Owen L. White, R.B. Barlow, and A.C. Colvine, Ontario Geological Survey, Miscellaneous Paper 106, 235 p.

White, A.M. 1978. Ego Mines Ltd. Geological Report on SSM 407890, Abotossaway Township, Ontario.


This report may not be reproduced in whole, in part, or in summary without the written permissbn of Manwa Exploration Services Ltd.

-,5b-

STATEMENT OF QUALIFICATIONS

I, RUSSELL G. REID, of Windsor, Ontario, do certify

that:

1. I am a consulting geologist for Manwa Exploration Services Ltd., P.O. Box 2028, Wawa, Ontario.

2. I am a graduate of the University of Windsor with a Bachelor of Applied Science, Geological Engineering in 1982.

3. I have worked as a geologist and geological assistant on a full-time basis since 1982; prior to that as a geolo gical assistant for one field season.

4. I have not received directly or indirectly, nor do I expect to receive any interest, direct or indirect in the Abotossaway Township claims.

5. This report has been prepared based upon field work carried out during January and February, 1984; and research and drafting completed partly under my supervision during -late March to early May, 1984.

6. I hereby authorize R.J. McGowan to use this report in any manner he deems necessary.

Respectfully Submitted,

P.O. Box 2028Wawa, Ontario Russell G. Reid, B.A.Se.May 18, 1984 Geologist


;4 ', 'This report may not be reproduced in whole, in part, or in summary without the written permission of Manwa Exploration Services Ltd.' ' '

• H&v-

-37-

STATEMENT OF QUALIFICATIONS

I, SEYMOUR M. SEARS, of the town of Wawa, Ontario,

do certify that:

1. I am a consulting geologist currently under contract with Manwa Exploration Services Ltd., P.O. Box 2028, Wawa, Ontario.

2. I am a B.Se. graduate in Geology and a B.A. graduate in Psychology from Mount Allison University, Sackville, New Brunswick.

3. I have been practicing my profession continuously since 1972.

4. I have not received directly or indirectly, nor do I expect to receive any interest, direct or indirect in the Abotossaway Township claims.

5. This report is based upon field work carried out partly under my supervision during January and February, 1984.

6. I hereby authorize R.J. McGowan to use this report in any manner he deems necessary.

Respectfully Submitted,

P.O. Box 2058Wawa, Ontario Seymour M. Sears, B.A., B.Se.May 18, 1984 Geologist


This r.port may not be reproduced in whole, in part, or in summary without the written permission of Manwa Exploration Services Ltd,

0044 ABOTOSSAWAY 900

Ministry of Natural Resources File.

OntarioGEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL

TECHNICAL DATA STATEMENT

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s)Township or Area /)*# TV J S/? CJ#

Claim HnMer(s) K -

Survey Company./ Author of Report. Address of Author

/9 If x. TR V .

/ ~##S.

A? g"

Covering Dates of Survey.

Total Miles of Line Cut —

S(linecutting to office)

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical —Electromagnetic.

DAYS per dxim

—Radiometric-Other^,^.Geological.Geochemical.

AIRBORNE CREDITS (Special provision crcditi do not apply to airborne lurveyi)

Magnetometer. .Electromagnetic . Radiometric

DATE:

(enter dayi per claim)

SIGNATURE:of Report or Agent

Res. Geol..

/l .ji

. Qualifications L- - b l j '

Previous Surveys File No. Type Date daimlfll&CEIVED

MINING CLAIMS TRAVERSED List numerically

(number)

Z.2.

.Z.Z.2.

TOTAL CLAIMS.

637 (6/79)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations ——— Station interval '2- J

Profile scale .———————

l 3 J Q Number of Readings Line spacing

1 3 J

-e. {.S- G.JF.

Contour interval /rf 4*3

/rf i46*)l?-7 0*n

GRAVITY ELECTROMAGNETIC MAGNETIC

Accuracy —Diurnal corr Base Station Base Station

Instrument Coil configu Coil separati AccuracyMethod: Frequency

Parameters i

Instrument .Scale consta Corrections

Base station

Elevation ac

*sra)c rnnstant — I ^ G t*. ~*- A-

,.,-timi mrthnH /rf O \J J *J G J& rt S *? /^T^T S 0 *J

rh^k-m interval (hour-:) /rf ti X 1 rt* ~l 6/AJ&' //0k.*

lotion ami valne V A f/ 4 # L tr - ^ T *? J fiS .

5 rt 4 # c/ \JJ-F - /C'/rj ^tTCtfr^x-*ration W 7 /7

AJ/4 r y*[Sf Fixed transmitter CD Shoot back D In line CD Parallel line

Z/.*/ xftf* - /JAJA/4P0L, r /rf /W y/.** A ({specify V.L.F. station) , '

^M.urrri/^X'/^dA/r/r'i. /v^ 57*^6 r#; d/fi tf*J6L2f oF As^i..L .

nt .- . .

ma HP

V?]\\P a nH loratinn,'

y

rnrarv

!J

InstrumentMethod l l Time DomainParameters — On time .

- Off time— Delay time— Integration time.

Power.Electrode array — Electrode spacing . Type of electrode

fi Frequency Domain _ Frequency -——^ — Range ________

GEOPHYSICAL TECHNICAL DATA

GROUSjiiSURVEYS — If more than one survey, specify data for each type of survey

Number of Stations ——

Station interval———Jfc. Profile scale —————— Contour i

L2-L3.**

AJ

Number of Readings 13/1 Line spacing /l?/? ,*t

1 3J* ,

dInstrument felst)*? C. f b ' PtffTOtf rt 6 s) If T

4~ X Accuracy — Scale constant ———t t * f**. t~~*.

Diurnal correction o \J i/J GBase Station check-in interval (hours). Base Station location and value -——.

O

O

O cd13w w

InstrumentCoil configuration Coil separation — Accuracy ————— Method:

Parameters

f \J I

^ /7

AJ/4

CSf Fixed transmitter D Shoot back r

D In line D Parallel line

(iptcify V.L.F,, D/ P

d

InstrumcntScale constant.Corrections made.

Base station value and location

Elevation accuracy.

Instrument

2;o^-*

323o:X,

Q jj JQQ2;

M^J^rjn*-HinM tt

Method D Time Domain Parameters — On time ———

- Off time ——

time.

Electrode array— Electrode spacing . Type of electrode

l l Frequency Domain—. Frequency ————— Range ________

f Mini&lryofNaturalRftources

Ontftfio

Report of Work (Geophysical, Geological, Geochemical nnd Expenditure1.)

3-fi

S

Tho Mining Act

MImtruellon*: - Pit*** type or print. ' ' *" 't

~ I f number of mining claims truvrrsetl T. iceeds space on ihii form, attach a list,

Note: - Only d.iyl credill calculated In th* "Expenditurti" section may b* entered In th* "Expend. Onyl Cr," columns,

~ Do not uu ihad*d *f ms below.Type of S urvayTsT Townihip or Area

[Pr os pe'c tor's i Licenee'Wb.

k

Survey Company

Name and Addrets of Author (of Oco-Technlol report)

s. sgA,^ ^oy

p*i i A to) Total Miles of tina Cut

Credits Requested per Each Claim in Columns at rightSpecial Provisions

, For first turvey:

Enter 40 dayi. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Grological

Geochemical

Electromagnetic

Magnetometer

ftadionrtetric

Days per Claim

-2SL.ScO

O; vi per r *im

Days per Claim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)Type of Work Performed

P(rform*d on Claim(t)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Day' Credit!

Instruction!Total Days Credits may b* apportioned at the claim holder's choice, Enter number of days credits per claim selected In columns at right.

Mining ClaimPrefix Number

^40

140

110

t~

7.82

i~ li-265

Expend. Days Cr. Prefix

Mining ClaimNumber

SAULT. STE. MAR E

R rrrrrv

A.M.

7i9i9iiPiiJii.2iiiSi:

UND5 5EC

Expend. Days Cr.

-P,M,

Total number of mining ctnims covered by this report of work.

Certification Verifying Report of Work; ; l hereby certify that l have a personal end intimate knowledge of the facts set forth in the Report of Work annexed hererbviiWing performeaj/ic work ",: or witnessed same during and/or after Its completion and the annexed report is true. _____

Name and Postal Address of Person Certifying

1368-

Date Cartified

MANWA EXPLORATION SERVICES LTD-RECEIVEDland Management Brancfi

d

8f

APR 101984l -;. r,. YUNDT j

J. !?. MOriTCN

'.V. U GOOD

-' R. 0643

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RECEIVEDAPR l 0 1984

MINING LANDS SECTION

P.O. Box 4, #370 - 625 Howe Street, Vancouver, B.C. V6C 2T6 Telephone: (604) 683-0417

April 24, 1984 Your FIle:52 Our FIle:2.6607

Mrs. M.V. St.Mining RecorderMinistry of Natural Resources875 Queen Street EastBox 669Sault Ste. Marie, OntarioP6A 5H2

Dear Madam:

We have received naps for a Geophysical (Electromagnetic) and Magnetometer) survey submitted under Special Provisions (credit for Performance and Coverage) on Mining Claims SSM 640267 et al In the Area of Abotossaway.

This material will be examined and assessed and a statement of assessment work credits will be Issued.

Yours sincerely.

S.E. YundtDirectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3 Phone:(416)965-6918

A. Barr:me

cc: R. J. McGowan1174 Edgewood Road North Vancouver, B.C. V7R 1Y9

cc: Mr. M. de Quadros Box 2028 Wawa, Ontario POS 1K9

April 24. 1984 Your File: 52-84 Our File: 2.6607

Mr* R. J. McGowan 1174 Edgewood Road North Vancouver* B.C. V7R 1Y9

Dear Sir:

RE: Geophysical (Electromagnetic and Hagnetometer) Survey submitted on Mining Claims S5M 640267 to 86 Inclusive In the Area of Abotossaway

We have received one set of plans for the above-mentioned survey. In order to complete your submission please provide the following:

a) a second set of maps, dated and signed by the author of the report

b) a signed cojy of the report, 1n duplicate

For further Information, please contact Mr. F.H. Matthews at (416)965-6918.

Yours sincerely,

S.E. YundtDirectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario H7A 1W3 Phone:(416)965-6918

D. K1nv1g:mc

cc: Manwa Exploration Services Ltd Box 2028 Wawa, Ontario POS 1KO Attention: Mr. M. deQuadros

cc: Mining RecorderSault Ste. Marie, Ontario

MANWA EXPLORATION SERVICES LTD.

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P.O. Box 4, #370 - 625 Howe Street, Vancouver, B.C V6C 2T6 Telephone: (604) 683-0417

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CLAIM MAPScale l : 20,000 ABOTOSSAWAY TWP. Sheet - M. I66

CONTOUR INTERVALS AT O, 250, 500 IOOO, I500 6, 2000 GAMMAS.

NOTE: Datum subtracted 59,000 gammas.

ANOMALOUS ZONE

CONDUCTOR AXIS

H B &TO KAMA V- 00 If42C02NE02I1 0044 ABOTOSSAWAY 220

R. J. M c G O W A N

TYPE OF WORK

MAGNETOMETER SURVEYPROJECT

SELKIRK LAKE GROUP ABOTOSSAWAY TWP.


AREA

SAULT STE MARIE M.D.

SCALE

: 2,500DRAWN BY

S OSOLNiK

DATE

Feb. 29, 1984WAR OR SHEIfc'T No

637- AB- B

SCALE l : 2,500 ((cm * 25 metres )

METRES 50 25 O 50 IOO 150 ?00 METRES

0.5

MURPHY LAKE

4+00 N

3 + OO N

2+OON

l-t-OON

BASE LINE

SELKIRK LAKE

DEGREE OF DIP ANGLE (IcmMO 0 )

4+-OOS

Road

64O283 640283

CLAIM MAPScale l : 20,000 ABOTOSSAWAY TWP. Sheet - M. I66

LEGEND

INSTRUMENT : SABRE VLF-EM

TRANSMITTER STATION : ANNAPOLIS

FREQUENCY : 2I.4 Khz

CONTOUR INTERVAL : IO units

OPERATOR : G. YOUNG

)- DIP ANGLE

FRASER PLOT CONTOUR

R. J. M c G O W A N

VLF SURVEY DIP ANGLE S FRASER PLOT

SELKIRK LAKE GROUP ABOTOSSAWAY TWR


AREA


SCALE

-2.500DRAWN BY

S. OSOLNIK

DATE

Feb. 29, 1984MAP OR SHEET No

637-AB-B2

SCALE l : 2,5OO ( l cm s 25 metres )

METRES 50 25 O 50 100 150 2OO METRES

42C02NE02I1 0844 ABOTOSSAWAY

v^isi^r-wfwsvsawws'ita

WEST CLAIM

IRENE LAKE

000^4000

04SE L/A/Eo-y-oo

2-f COS

3-/-OOS

3 + 50 S

EAST CLAIM

2 + 5O N

V-——1000

2 + OON

— I + OON

O

O

UJ 00

UJro

UJ ST

.J

UJin

CLAIM MAPABOTOSSAWAY TWP

SHEET- M.166

Scale IX2" S l mile

Contour intervals at 500, 750, 1000, and 1250 gammas.

Instrument : Geometrics G-816 ProtonMagnetometer.

NOTE : Datum subtracted 59,000 gammasContour intervals at O, 1000, 2000, 3000, 4000, 5000 and 6000 gammas.

Instrument : Geometrics G-816 ProtonMagnetometer.

NOTE : Datum subtracted 59,000 gammas,

ANOMALOUS ZONE

CONDUCTOR AXIS

fat A y - oow

CLIENT

GUTCHER LAKE

R. J. M c G O W A NTYPE OF WORK

MAGNETOMETER SURVEY o {f(f,L^*' ^

PROJECT

GUTCHER LAKE GROUP


AREA

ABOTOSSAWAY TWP. SAULT STE MARIE M. D.

SCALE

: 2.000

DRAWN BY

S. OSOLNIK

DATE

April 4 t 1984

MAP No

637 X AB-CI

METRES 100

SCALE l : 2 ,OOO

50 O

f l cm - 20 metres )lOO 200 METRES

42C02NE021I 0C44 ABOTOSSAWAY 240

WEST CLAIM

OLU

-J

LU CM

-J

LU

ro -J

CLAIM MAPABOTOSSAWAY TWPj

. SHEET-M.I66 -4

Scale IX2" S l mile

N

LU LUin

CONTOUR INTERVALS AT 0,10,20.6 30 UNITS

l-h 75 N

l + OONIRENE

LAKE

BASE LINE 0+00

l +OO S

2+OOS

3 + OOS

3 + 5O S

O-J

EAST CLAIM

2 + 5O N

- 2 +OON

l + OON

BASE LINE

LEGEND

INSTRUMENT : SABRE VLF-EM

TRANSMITTER STATION : ANNAPOLIS

FREQUENCY : 21.4 KHz

OPERATOR : 6. YOUNG

GUTCHER LAKE

CONTOUR INTERVALS AT 0,5,10 t* 1 5 UNITS

- 0 01'-

CLIENT

R. J. M C GOWANTYPE O F WORK

VLF-EM SURVEY - FRASER PLOT;PROJECT

GUTCHER LAKE GROUP


AREA


SCALE

: 2.000

DRAWN BY

S. OSOLNIK

DATE

April 4, 1984MAP No

637 X AB-02

METRES 1OO

SCALE l ' 2,000

50 O

cm - 20 metreslOO 200 METRES

42C32NEfii2ll 8044 ABOTOSSAWAY 250

IRENE LAKE

LUo-j

LU CM -J

LUro

LU

t-J

CLAIM MAPABOTOSSAWAY TWP

SHEET- M. 166

Scale (/2" s l mile

BASE LINE O+OO

i -f OO S

2+OOS

3 + OO S

3+5O S

LU

EAST CLAIM

GUTCHER LAKE

7

CLIENT

R. J. M c G O W A NTYPE OF WORK

VLF-EM DIP ANGLE SURVEYPROJECT

GUTCHER LAKE GROUP


AREA


SCALE

: 2.OOODRAWN BY

S. OSOLNtK

DATE

April 4 t 1984MAP No

637 X AB-C3

METRES 100

SCALE l - 2 ,OOO

50 O

C l cm = 20 metres )100 200 METRES

42C02NE0211

CLAIM MAPScale l 20,OOO ABOTOSSAWAY TWP

767.5 2OOO X 1150 J)

LU

CM

CONTOUR INTERVALS AT 0,500,1000,1500,2000, 8 3000 GAMMAS

NOTE : Datum subtracted 59,000 gammas.

ANOMALOUS ZONE

CONDUCTOR AXIS

l

;L IE NT

R. J. MCGOWAN

TYPE OF WORK

MAGNETOMETER SURVEYPROJECT

JACKSON LAKE GROUP ABOTOSSAWAY TWP.


AREA


SCALE

: 2,500DRAWN BY

S. OSOLNIK

DATE

Feb. 29, 1984MAP OR SHEET No.

637- AB- Al

SCALE i : 2,500 ( ! cm a 25 metres )

METRES 5O 25 O 50 !00 150 200 METRES

DOHERTY LAKE

CLAIM MAPScale l 20,000 ABOTOSSAWAY TWP

LU

CM

LEGENDDEGREE OF DIP ANGLE (lcm-20 0 )

r^F"

o o o

4- 4- 4-

^ o 2O CM ST

l l

INSTRUMENT: SABRE VLF-EM

TRANSMITTER STATION '- ANNAPOLIS

FREQUENCY : 21.4 KHz

CONTOUR INTERVAL : 20 units

OPERATOR : G. YOUNG*

N

/' D IP ANGLE

FRASER PLOT CONTOURO

tu00-I

LU

.J

CI l E NT

R. J. MCGOWAN

TYPE OF WORK

VLF SURVEY - DIP ANGLE S FRASER PLOTPROJECT

JACKSON LAKE GROUP ABOTOSSAWAY TWP


AREA

SAULT STE MARIE M.D

SCALE

: 2,500DRAWN BY

S OSOLNIK

DATE

Feb. 29, 1984MAP OR SHEET No.

637- AB - A2

SCALE l - 2,500 ( l cm s 25 metres )

METRES 50 25 O 5O I OO 150 200 METRES

r.j. the properties mcgowan, of...portions of gutcher lake and irene lake respectively. the selkirk...

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