pSp': -:'|:i:.,:.:v-;v ^:m^'i^ff : -:rfV:"-.-,:- -:v v- -.fe^j'.'-:\'"' : ''; '-:-"-'-;- ''-.' v-' : ':

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4acessw0ie5 e043 JACOBSON 010

VEGA GOLD EXPLORATIONS INC. PROTON WAGNETOIBETER SURVEY

GODIN LAKE PROPERTY GOUDREAU-LOCHALSH AREA

DISTRICT OF ALGOfflA, ONTARIO

RECEIVED"*f 2 81982

MINING LANDS SECTION

F.T.Archibald, B.Se.Geologist March 15, 1982.

42ceesweie5 ee43 JACOBSON 010C

Table of Contents

Summary

Location and Access

Topography

General Geology

Economic Geology

Specifics of Survey

Results

Conclusions

page

1

2

2

3

3

4

5

6

Appendix

Map- Proton Magnetometer Survey Scale: I inch to 400 feet

VEGA GOLD EXPLORATIONS INC. IDAGNETDfflETER SURVEY GOOIN LAKE PROPERTY

GOUOREAU-IOCHALSH AREA DISTRICT OF ALGOIKIA, ONTARIO

Summaryt

This report covers the results of the Proton magnetometer survey

run over the property during the month of March, 1982. Approximately .

6.12 miles of line was traversed over claims SSIfl 5825II to 582517

inclusive. Stations were taken at 100 foot intervals on lines 400 feet apart.

The purpose of the survey was to delineate any mineralized zones

and to attempt to delineate the geological structure underlying the

claim group.

Two areas of high to moderate magnetic signature were encountered

during the survey. One corresponds to a magnetite rich diorite intrusive

or coarse grained basic flow with associated magnetite-pyrrhotite rich

shears. The other corresponds to banded iron formation or magnetite-

pyrrhotite rich shears.

Pyrite-magnetite-pyrrhotite rich shears in the area have been

found to contain significant amounts of gold. Many of these shear zones

lie at or in close proximity to the contacts between diorite intrusives

and metavolcanic units, and between coarse grained- magnetite rich

basic flows and the fine grained metavolcanic flows.

Location and Accesst

The property is located approximately 20 miles to the northeast

of the town of Wawa, in the District of Algoma* Northern Ontario. It

is approximately A miles to the southwest of Lochalsh and 14 miles to the

northeast of Goudreau* Lochalsh is on the Canadian Pacific Railway line

and Goudfceau is on the Algoma Central Railway line* A gravel road connects

Goudreau to Lochalsh and comes within one mile of the claim boundary*

This road is intersected by a gravelled forestry access road from the

town of Dubruilville, which is connected with the Trans Canada Highway.

Further access can be made by float plane to Godin Lake.

The claims surveyed consist of seven unpatented mining claims

numbered:

5SIKI 582511 ssn)

SSmre M c men5Sm 5B25I3 CCM CQ7CT7SSffl 5825IA SSni 582517

Topographyt

The property surveyed is generally flat lying in relief. Approximately

50^ of the claim group is covered by low-lying alder-spruce covered over

burden. A few outcrops are found in the northwest and northeast sections

of the property. These sections are covered by mature poplar and birch

vegetation cover.

A few jack pine ridges of sand are found in the northwest section

of the property. These glacial morraine/dune ridges trend in a north-

south direction.

The central portion of the claim group is overlain by open swamp

ar eas .

General Geologyt

The oldest rocks are of Precambrian age* Archean metavolcanics

and metasedimentary rock units have been intruded by granodiorite, quartz

porphyry, felsite porphyry, and diorite units t Younger diabase dykes of

two ages cut all the other formations generally in a northwest-southeast

direction.

The general geological strike of the rock units is in an east-west

direction and dipping steeply to the south.

The major dykes and siliceous fracture systems are found to strike

at angles parallel to and discordant to the regional geological strike in

generally three directions J northwest-southeast, northeast-southwest, and

east-west.

Economic Geology i

The area is noted for its past production in gold and silver,

although minor amounts of copper, zinc, and iron are also found.

The gold in the area is found to occur in fissure-type quartz-

carbonate veins, and pyrite-rich shear zones. Rany of these shear

zones lie at or in close proximity to the contacts between the basic

metavolcanic and diorite-granodiorite intrusive units. They also occur

within acid rich metavolcanic and granodiorite units.

The shear zones striko in generally an east-west direction and

several of these lie on strike with the Pick/Cline Wind deposit, the

Edwards Consolidated Wine deposit, and the Magino/Algoma Summit Wine

deposit. Reports indicate that the past producers in the area collectively

produced over 78,000 ounces of gold and,13,000 ounces Of silver in the

past.

Specifics of Surveyi

The survey was completed with the USB of the Exploranium-

Geometrics 'Unimag 1 Proton magnetometer. It has a digital readout with a

sensitivity of plus or minus 10 gammas.

Station readings were taken at intervals of 100 feet on lines

spaced at 400 feet apart. Where abnormally high or low readings were

encountered, stations were taken at 50 foot intervals. Some 6.16

miles were traversed during the survey* in which some 335 readings

were taken.

The accuracy of the readings was increased by averaging two or three

readings, especially in areas of high magnetic fluctuation, or until

fluctuations decreased to a constant level. The range selector was changed

during high magnetic fluctuations.

The 'world gamma range* setting on the instrument was brought down

to a scale relative to the airborne magnetics of the area when plotting

the final resultant readings. Results, after plotting corrections for

diurnal drift, are plotted at 500 gamma intervals. Base plans are plotted

at a scale of I" to 400 feet.

Actual field work was completed during the month of March, 1982.

Results!

Several areas of moderate to high magnetic signature have been

encountered during the survey* These signatures are elongated in an

east-west to northwest-southeast direction; paralleling the regional

geological strike.

Some of the magnetic responses are found to be as high as

5700 gammas above the normal background* Two areas of strong magnetic

signature have been encountered*

Trend A is an area of moderately high magnetic signature found in

the north and mid-eastern section of the claims. The highest responses

lie on lines 12 West, 40 West and 60 West,

Trend B is an area of moderate magnetic signature in the southern

portion of the claim group. The highest responses lie between lines

32 West and 48 West.

.'A f-.---'

Conclusionst

Two areas of high to moderate magnetic signature have been

traversed during the survey.

Anomalous trend A outlines a diorite intrusive unit or coarse

grained basic metavolcanic flow unit with a high disseminated magnetite

content. In the extreme northwest of the claim group, narrow bands

of either iron formation or pyrrhotite bearing shears have been traced

by the magnetics.

Anomalous trend 8 traces a narrow banded unit and coincides with

a pyrite-pyrrhotite bearing shear. The basic flow unit in this area

probably has a higher than normal magnetite content, which is

normal of the rock in close proximity to the shears throughout the

general area.

These zones should be further delineated and detailed by running

lines at 200 foot spacings, and also by geological mapping of the

claim group.

Toronto, Ontario.March 15, I9B2. F.T.Archibald, B.Se.Geologist.

VEGA GOLD EXPLORATIONS INC. CRONE RADEM V.L.F. ELECTROMAGNETIC SURVEY

GODIN LAKE PROPERTY GOUOREAU-LOCHALSH AREA

DISTRICT OF ALGOB1A, ONTARIO

* 42ce8sweies ee*3 JACOBSON O2O Summary!

This report covers the results of the V.L.F. electromagnetic survey

which was run over the property during the month of March* 1982*

The purpose of the survey was to further delineate any known min

eralized zones or conductive shear zones which cut through the area.

Rock outcrops are scarce and overburden covers 90?6 of the claim

group. Swamp overburden covers between one-third and one-half of the

claims surveyed.

Some 7.25 miles of line was traversed during the survey. Readings

were taken at 100 foot intervals on lines spaced at 400 feet apart.

Three east-west anomalous trends were encountered during the survey*

Some of these have parallel bands up to 100 and 200 feet away from the

main trend/zone. These anomalous trends correspond with steeply dipping

pyrite-pyrrhotite-magnetite rich shear zones which parallel the regional

strike.

Some of these zones, generally averaging 5.0 feet or less in width,

have associated copper, zinc and gold values.

MINING LANDS SECTION WINING LANDS SECTION

0043 JACOBSON 020C

Table of Contents

Page

Summary I

Location and Access 2

Topography 2

General Geology 3

Economic Geology 3

Discussion or Equipment 4

Specifics of Survey 6

Results 7

Conclusions B

Appendix

Map- Dip Angle measurements Scale- I " to 400 feet

Map- Field Strength measurements Scale- I " to 400 feet

Location and Access i

The property is located approximately 20 miles to the northeast

of the town of Wawa, in the District of Algoma, Northern Ontario* It

is approximately 4 miles to the southwest of Lochalsh and 14 miles to the

northeast of Goudreau. Goudreau is on the Algoma Central Railway line and

Lochalsh is on the Canadian Pacific Railway line* A gravel road connects

Goudreau to Lochalsh and comes within one mile of the claim boundary*

This road is intersected by a gravelled forestry access road from the

town of Dubruilville, which is connected with the Trans Canada Highway*

Further access can be made by float plane to Godin Lake*

The claims surveyed consist of seven unpatented mining claims

numbered!

SSffl 58251ISSfll 582512SSin 582513SSM 582514

SSW 582515SSm 582516SSItl 582517

Topography t

The property is generally flat lying. Approximately 50^ of the

claim group is covered by low-lying alder-spruce covered overburden.

A few outcroppings are found in the northwest and northeast sections

of the property. These sections are covered by mature poplar and birch

vegetaion cover.

A few jack pine sand ridges are found in the northwest section

of the property. These glrcial morraine ridges trend in a north-south

direction.

The central portion of the claim group is overlain by open

swamp areas*

:M* General Geoloqyt

; The oldest rocks are of Precambrian age* Archean metavolcanics and

metasedimentary rock'units have been intruded by granodiorite, quartz

porphyry, felsite porphyry, and diorite units. Yuungei diabase dykes of

two ages cut the other formations generally in a northwest-southeast

direction*

The general geological strike of the rock units is in an east-west

direction and dipping steeply to the south.

The major dykes and siliceous fracture systems are found to strike

at angles parallel to and discordant to the regional geological strike in

generally three directionst northwest-southeast, northeast-southwest, and

east-west.

Economic Geology:

The area is noted for its past production in gold and silver,

although minor amounts of copper, zinc and iron are also found.

The gold in the area is found to occur in fissure-type quartz-

carbonate veins, and pyrite-rich shear zones. Iflany of these shear zones

lie at or in close contact between the basic metavolcanic and the diorite-

granodiorite intrusive units. They also occur within acid rich

metavolcanic and granodiorite units.

The shear zones strike in generally an east-west direction and

several of these lie on strike with the Pick/Cline Mine deposit, the

Edwards Consolidated Wine deposit, and the Wagino/Algoma Summit Wine

deposit. Reports indicate that the past producers in the area collectively

produced over 78,000 ounces of gold and 13,000 ounces of silver in the

past.

Discussion of Equipmentl

The Crone Radem V.L.F. electromagnetic unit utilizes

higher than normal frequencies and is capable of detecting small

sulphide bodies and disseminated sulphide deposits. It accurately isolates

banded conductors and operates through areas of high noise or interference

levels.

This method is capable of deep penetration but due to the low

frequency used, its penetration is limited in areas of clay and conductive

overburden. The components of dip angle in degrees of magnetic field

component, field strength of the magnetic component of the V.L.F. field,

and out of phase component of the magnetic field are measured at each

station.

There are several channels or stations available, each with a

different frequency. A channel is selected so that it is parallel to the

general strike of the area. If this cannot be determined or if the

station is off the air, then orthogonal stations are used to define the

areas with possible conductors.

The dip angle measurement measures the angle of inclination from

horizontal of the direction of the resultant V.L.F, or the amplitude

of the major axis of the polarization ellipse. It is detected by a minimum

on the field strength meter and is read from an inclinometer with a range

of plus or minus 90. A conductor is designated by a true crossover

pattern of the readings. The measurement is taken from an audio null

when the instrument is held in a vertical position, after turning

perpendicular to the direction in alignment with the V.L.F. field.

The V.L.F. field is found by an audio null or minimum field strength

measurement when the instrument is held in a horizontal position. The

accuracy of the dip angle measurement is plus or minus one-half a degree.

mThe field strength measurement defines the shape and the attitude

of the conductor by the strength of the field in the horizontal plane

or the amplitude of the m?, j or axis of the polarization ellipse. It is the

maximum reading obtained from the field strength meter when the instrument

is rotated in the horizontal plane* and is measured as a percent of normal

field strength established at a base station. The field strength of the

V.L.F. stations drifts with time, and must be adjusted with the base

station every few hours. The field strength measurement'has an accuracy of

plus or minus two percent.

The out of phase component of the magnetic field, as a percent

of the normal primary field, is sensitive to the lower order of conductivity

than the dip angle measurement and is used to locate conductors of a low

order of magnitude. It is a measurement of the secondary field produced

by a ground conductor which is in a different phase than the primary

field. This is the minimum reading of the field strength meter obtained

when measuring the dip angle. The measurement has an accuracy of plus

or minus two percent.

Specifics of Surveyi

The survey was completed with the use of the Crone Radem V.L.F.

electromagnetic instrument*

Station readings were taken every 100 feet on lines spaced at

400 feet apart* Base station readings were run on a base line at 400

foot intervals and were tied into frequently throughout the. survey*

Some 7.25 miles or 383 stations were done in total while traversing*

The station of Annapolis Maryland was used throuhout the survey

as both Seattle Washington and Cutler Mains were out of operation for

either part of or throughout the total period that the survey was run.

Annapolis Maryland, with a frequency of 21.4 Khz** although it was

orthogonal to the geological strike of the area, showed up significant

results.

Base plans are plotted at a scale of I inch to 400 feet , the same

scale used when the rest of the Vega Gold Exploration Inc. property

was surveyed. Actual field work was completed during the month of

fflarch, 1982.

Results!

The survey delineates several east-west anomalous trends of weak

conductive strength. Thesa anomalies parallel the regional geological strike.

Interpretations have been aided by geological* topographical*

and magnetic data.

Anomaly A is a weak anomalous trend which traces a pyrite-

pyrrhotite-magnetite bearing shear zpne that dips steeply at 5 to 15

degrees. It has been traced between lines O West and 20 West* and shows

up again between lines 36 West and 4A West as a very weak conductive

zone. This zone shows up strongest on line 12 West where it parallels

an outcropping of banded iron formation.

Anomaly B is a weak anomalous trend found between line 16 West

and line 52 West where it has been traced for at least 3600 feet before

it continues off the property on either and. This anomaly follows a

steeply dipping pyrite-pyrrhotite rich shear zone.

Anomaly C is a discontinuous and weakly conductive zone found

paralleling and some 100 to 200 feet to the south of anomaly 6. It has

been delineated on lines 36 West and 44 West. This anomaly corresponds to

a pyrite rich shear zone.

Anomaly E is a moderately strong to strong anomaly which outlines

an area of 'swamp 1 overburden between lines Q West and 6 West.

Anomaly F is a very weak anomalous trend which outlines an area

of weakly conductive 'swamp* overburden.

Conclusions t

Three significant zones have been outlined on the Vega Explorations

Inc. claims by the V.L.F. electromagnetic survey,

Anomaly A corresponds with a pyrite-pyrrhotite bearing shear zone

with associated banded iron formation. This zone has been found to have

minor amounts of copper and zinc mineralization.

Anomaly B corresponds with a pyrite-pyrrhotite rich shear zone.

Anomaly C is a weak shear zone paralleling anomaly B.

Anomaly O corresponds with a pyrite bearing shear zone.

The strongest diamond drill hole targets outlined by the survey

are as follows t

Anomaly A between lines 8 West and 16 West

Anomaly B and C between lines 32 West and 44 West

Anomaly O between lines 44 West and 52 West

These zones occur in basic metavolcanics close to the contacts

with diorite intrusive units and magnetite riel' - coarse grained

volcanic flow units. Significant gold values have been found in many

of the siliceous/acid rich east-west trending shear zones which cut

through the area surrounding the surveyed claim group.

Toronto, Ontario.march 15, 1982. F.T.Archibald, B.Se. Geologist,

42ceesweies 0043 JACOBSON 900

Ministry o(NaturalResources

Ontario.

Report ol Work(Geophysical, Geological, Geochemical and Expenditures)

oTho M ining ,

ELECTROMAGNETICS.

Imiruclioni: - Pltttt t ype or p'lnt. l' number of mining claims iriueritd

exceeds *psc* on I*MI form, attach i lin. Not*: - Only d*ys credit! calculated in the

"Expendilurei" (action may he entered rt ^. in l h* "Expend. Dayi Cr." eoiumni,

. L^ffX 6T__^ Oo r' ot "** * hltownship o r A(M

JACOBSONr(tV"

" VEGA GOLD EXPLORATIONS -INC.ffurvijy Pnmpnny [Survey On'ci (Uniicultir) to odlf.s)

Protpactor'i l.fconc* No.

T 943Total' Mill's of lino C^.t

7.25Name end Adilross of Author (of Ooo-fnchnlr*l raport) , , . ,,.-.. i ,, ^702-100 Adolaido St. West Toronto, Ontario M5H-1S3

Spnclaf Provisions CrcilitsJJoqiinitod Mining Claim^Trayorsod (l ist in nuinciinall iotructloni

For first survey:

Enter 'lO doys. (Th'u Includes line cutting)

Tor each additional lurvr y; using (ho Slime grid:

Tutor 20 days (for each)- O thor

Hootogical

i Haystiuctlont

Complete reverse side find fintnr loliil(s) here i

Cl.ilrn

40

. . ....

D.iys per Cl/ilm

l)orne Credits

Vote: S()Pcinl provisions crrdits do r.ot .ipply to Airborne Survoyi.

PflcJ'orriotrlc

Or.ys perC.'.nim

)ondituros (oxcluclos |;o\vci sliipping))C of Vi/ork Per f or mod

orrncci on Clsini(t)

:ul.itlon of Expenditure Oayi

Total nxpcndlturos

CrL'rtilt Tola!

Days Credit*

f6 1 4- IS 1,1 1

Mining Clii'm,"r*rix

SSM^

i'.'\, '1

j'vv's'f,*;'

t 'WK'fi' fyfe;J^Jt^^

. / '

^^V^V^L"

f1" " ' - ' ;

Nur'nhqr

582511 582512 , .

582513

502514

582515

582516

582517

rxpftiui.Oyiy* O.

N

'.' 'i'/1 V-

?^1' "'- .y '',js(

^-j . ' .' .

";- W

' ftl:I,' -" i

^ ,, RECEIVED l

Vae/u ' ' ' l . : - 'Z. --. -

2IS : -;ON-2198e l1 "^^ MINING LANDS SECTION

WAY27-VX

n^iy

4

'l '

on tit

Instruction!Total D.iyt Creilitt may ho .ippoiilor. .-d rtt the clnlrn holilor'j choice. Cuter nijinbor of d,:ys cn.')il* | or clnlin ii-.lf.i. tod In columns ut right.

ul^t nuif'l'Cf of milling t. lit its cove ̂ H !)y thij

f ./ork.

.- ..~- _ _ ...-.-.. . -..-~. ..- -.l Oat e of no|X)rt TnoconloJ Holder or Ajcnt (Cigiuiture) J

Ma r . 1 5 , 1 08 2 j p t T t A RCH in ALD ^^ J

SK:

Certification Vniifyiny Rnpoii of Woikl hereby ceil if y Hut l h.ivc .1 personal onr) intiimtc knowledge of the facts sot Until in the Report ol Work .unloved licicto, hjving ivifoiiiii' p.l l! 'or witiv.'S'ji'i! '..'in.'! ilurii',,j .ind/oi iflcr ils complttion .md the nnncxnd repoit is true.

Marne anil Pos!,'l Aild.-- c*

To con i'.o,

i fortifying

702-100 Adelaide St. \tesh al..it:vo. M5II-1S3

Cvitifli o by (Si j

Ontario

Minlstryof Geotechnical2alural Report Resources -OKU '

Approval

Tile

Mining Lends Comments

To: Geophysics

Commenti

"(pproved Wiih to tee again with correction*

DTo: Geology - Expenditures /C- mmenti

[~] Approved [~] With to lee (gain with correctloniOete Signature

To: Geochemistry

Commenti

f) Approved LJ With t o lee e galn with correct'oniSignature

'f.':'#. \ J To: Mining Lands Section, Room 6462, Whitney Block. (Tel: 5-1380)

1693(81/10)'

:l1982 06 07 2.4825

Mining RecorderMinistry of Natural Resources75 Elgin StreetP.O. Box 669Sault Ste. Marl t, OntarioP6A 5H2

Dear Madam:

We have received reports and naps for a Geophysical (Electromagnetic and Magnetometer) Survey submitted under Special Provisions (credit for Performance A Coverage) on Mining Claims SSM 582511 et al, In the Town ship of jacobson.

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

Yours very truly,

E.F. AndersonDirectorLand Management Branch

Whitney Block, Room 6450Queen's ParkToronto, OntarioM7A 1W3Phone: 416/965-1316

J. Skura/amc

cc Vega Gold Explorations Inc. Toronto, Ontario

cc Mr.F.T. Archibald Toronto, Ontario

Legend

Annapolis Maryland 314 Khz

V CroX* W

Vfe

Mag contour 250 Gamma Interval

Fivld Strength contour 20

12O - 140

140 - 160

160 - 180

180 ~ 200

f 200

bas*

52 w

Magnetometer

VEGA GOLD EXPLORATIONS INC.Jacobson Township ; Ontario

i

t l INCH s 400 MET

42C08SKC105 0043 JACOBSON

Legend

Annopolis Maryland 214 Khi

-ve.ve

Mag contour 250 Gamma Interval

Field Strength contour 20

120 - 140 o

baselin* B

l t

0043 JACOBSON210

i

60 56

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\\

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52 w

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VLF - EM Dip Angles

VEGA GOLD EXPLORATIONSJacobson Township ; Ontario

INC

scale : l INCH 5 400 FiET

O rf CriSt A/ -0tW.

Legend

Annapolis Maryland 214 K hz

-ve

Mag contour 350 Gamma interval

Fi*ld S trength contour 20

12O - 14O

140 - 160

160 - 180

180 - 2OO

f 200

bo f *

52 w

VLF-IW Field Strength Measurement

VEGA GOLD EXPLORATIONS INCJacobson Township ; Ontario

scale : l INCH - 400 FEET

220