geol - geoch rpt wabikoba l proj no 1119

l l l l l l

42ci3sweiee 2.10538 WABIKOBA LAKE 010

NORANDA EXPLORATION COMPANY,-LIMITED (no personal liability)

GEOLOGICAL - GEOCHEMICAL REPORT

WABIKOBA LAKE

Thunder Bay Mining Division NTS 42 C/13

RECEIVEDMOV 18 1987

MINING LANDS SECTION

PROJECT NO. 1119 HEMLO DISTRICT

KATE HEARN GEOLOGIST

1111111111111111111

li nil^^ 42CI3SWaiei8 2.10538 WABIKOBA LAKE

TABLE OF CONTENTSx

TITLE

1.0 INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . .

3 A TTYDTriDATTr^M li T G T f\ D V

4.0 REGIONAL AND ECONOMIC GEOLOGY . . . . . . . . . . . . . .

5.0 FIELD PROGRAMS . . . . . . . . . . . . . . . . . . . . . .

5.2.2 Structure . . . . . . . . . . . . . . .

FIGURES AND MAPS

Figure 1 Regional Geology, Location Sketch, Claim GroupMap 1 Property Geology 1:5000 ScaleMap 2 Soil Geochemistry 1:5000 Scale

APPENDICES

Appendix 1 Sample DescriptionsAppendix 2 Certificates of Analysis

nun0

PAGE NO.

1

1

1

3

444455666

7

2appendedappended

appendedappended

l l l l l l l l l l l l l l l l l l l

1.0 INTRODUCTIONi.

A reconnaissance geological mapping program and humus sampling

program was carried out on the Wabikoba property during the periods June 3

- 16 and September 1-5, 1987. Program objectives were to evaluate the

gold potential of the claims. The property lies on the north limb of the

Hemlo Syncline. The rocks of the area consist of Archean mafic to felsic

raetavolcanics and associated metasediments, intruded by the Musher Lake

Pluton. A number of copper-lead-zinc, and Au mineralized iron formation

showings are located north of the property.

2.0 CLAIM LOCATION, OWNERSHIP AND ACCESS

The Wabikoba claim group comprises 12 contiguous claims wholly

owned by Noranda Exploration. Claim numbers are as follows:

TB 939551 TB 939554 TB 939574 TB 939577TB 939552 TB 939555 TB 939575 TB 939578TB 939553 TB 939556 TB 939576 TB 939592

The property is located on the north shore of Solong Lake and is

accessed by two wheel drive vehicle along an all weather gravel road that

intersects Highway 614, six kilometers north of the junction of Highway 17.

The claims are reached by canoe from the south shore of Solong Lake.

3.0 EXPLORATION HISTORY

Noranda Exploration conducted a base metals exploration program

in the area during 1976. The Dotted Lake Airborne survey was performed

with follow-up ground geophysics. An EM survey outlined a major conductive

zone along the southeast trending swamp on the Wabikoba property. However,

vertical loop ground geophysics indicated the conductors were weak and of

poor quality and the claims were allowed to lapse.

i X' -'"r'//"'. ( '\ "o'w -* i -.-j r*

A/ V s. . , TO INTERMBIXA7E METAVOLCANIGS

."-^ - WABIKO,

^^i^^:i^^i^^M;;;^';?H^^ ,-'

tt* l h* k H MUM

K T.S ftfwwit* mm, m/H. m/i, m/i

'Ir- * — S -~ —- Y \ -^ l •"" \ •^•(X^^xlV '\'-~Nr'*/* i""! 1"- *"/ — '•'' V^l s \ \. * s li' nA ' n^~— ' *y v '*''~ S""'^/!/! "~ "~ N \ ^ ' ~ ^ -.•l/^x*"/ ̂"* \*" T" ^ x l 7 "*J l N — i x ** l ^ c-*Vw.

l ^P The property was subsequently staked in 1983 by Norman Resources.

A precious metals exploration program was conducted consisting of

l geological mapping, prospecting, and a 'B 1 horizon soil survey. Results of

m the soil survey revealed a localized copper anomaly south of the major

swamp. Gold values returned were less than threshold levels. There is no

l record of further work.

Noranda staked twelve claims over the former Norman Resources

l property in October, 1986 based on the favourable geology of the area.

l 4.0 REGIONAL AND ECONOMIC GEOLOGY

l The property lies on the north limb of the Hemlo Syncline, within

the Wawa-Shebandowan Belt of the Superior Province. The belt is comprised

l of Archean mafic to felsic metavolcanics and associated metasediments

. intruded in the north by the Dotted Lake Batholith, in the south by the

Musher Lake Pluton and in the central region by an approximately east

l trending amphibolitic metagabbro. A series of approximately north trending

lProterozoic diabase dikes crosscut the entire package.

The rocks of the area have been complexly folded faulted and

metamorphosed to the amphibolite facies.

Historically, the area attracted interest for its base metal

l potential, due to its proximity and lithologic similarity to the

Manitouwadge mining camp. A number of copper-lead-zinc and iron formation

l showings are located north of the property (Refer to OGS Map 2147).

| Recent activities in the Hemlo mining camp have provided the

impetus for extensive precious metals exploration activity in the area,

l Qued Resources has conducted a program of geologic mapping, trenching and

drilling immediately north of the Wabikoba Property. Results from the

l program have outlined stratabound gold mineralization within iron rich

m interflow sedimentary sequences. Drilling has returned values of up to

•025 oz/r Au over 3 meters.

l l l

5.0 FIELD PROGRAMS

5 . l Personnel

l Noranda Personnel were as follows:

K. Hearn - Geologist

P. Grossman - Junior Geologist

B B. MacLachlan - Prospector

T. Goranson - Junior Geologist

lm 5.2 Geological Mapping

A reconnaissance mapping program was completed on the property

j between the dates June 3 to 10, 1987. Pace and compass traverses were

spaced 240 meters apart controlled by a flagged line bearing 125 degrees.

l The control line, traverses and grid lines are plotted on the accompanying

map. Rock exposure is limited to the north eastern claims.

5.2.1 Property Geology

fl The north eastern portion of the claim group is occupied by a

horizon of mafic volcanics, flanked by a sequence of felsic pyroclastics,

l sediments, and subordinate mafic agglomerate. The mafic volcanics are dark

green grey, massive to semi-schistose and chlorite rich, with rare felsic

* fragments apparent in some exposures. To the south west the mafic volcanics

l are interbedded with minor, variable width horizons of mafic sediments,

me tagreywackes, and arkosic sandstones.

l Sequences of felsic agglomerates border the mafic volcanics to

^ the north and the south. Fragments are generally leucocratic, fine to

medium grained, in a gneissic intermediate matrix. Fragments in the

l eastern sections of the southern agglomerate horizon contain large milky

white quartz eyes up to .5 mm in size forming 10% of the rock by volume.

f Fragments decrease in size and quantity toward the north.

l l l

Massive felsic volcanics form the southern portion of the

pyroclastic-sediment sequence. The volcanics are light grey pink in colour

and gneissic to heterogeneous. The felsic volcanics pinch out in the east

and are bordered by a mafic fragmental, and a narrow band of metasediments.

m The mafic fragmental consists of mafic homogeneous fragments, 2-3

centimeters in size, in a felsic matrix. The rock is fragment supported,

l Metasediments are variable in character ranging in nature from

metagreywackes to chlorite-garnet schists. Sediments in the north east are

interbedded with narrow felsic tuffaceous bands.

M Intrusives on the property range from mafic to felsic in

composition. A coarse grained araphibolitized gabbro forms a southeasterly

l trending dike in the northern felsic agglomerate sequence. Two limited

occurrences of feldspar porphyry are located in the north eastern area of

l the claims. Felsic and mafic dikes were noted throughout the property but

M were too small (^5m in width) and discontinuous to form mappable units. A

portion of the Musher Lake Pluton occupies the remainder of the property,

l Exposure is very limited with granodiorite subcropping in the margins of

swampy areas.

l5.2.2 Structure

l

l

l

l

l

l

The metavolcanic and metasedimentary rocks are steeply south

dipping with a strike of approximately 125 degrees. Scarp faces border

both sides of the linear swamp suggesting a possible shear zone. Dike like

intrusives of mappable size tend to be concordant to stratigraphy.

5.2.3 Mineralization

Sulphide mineralization was noted in some felsic fragmentals as

finely disseminated pyrite in the matrix.

l5.3 Lithogeochemistry

l Twenty-three rocks samples were forwarded to TSL for analysis of

gold content. Six samples were also analyzed for major oxides. No

anomalous gold values were returned.

5*4 Ao Horizon Soil Survey

l Soil sampling was carried out over the north eastern corner of

the property. Targets were weak conductors located along a linear swamp,

p as indicated by the Dotted Lake Airborne survey, and anomalous values for

gold and copper in 'B' horizons soils, as determined by the Norman

Resources survey,

l Three hundred and three soils were collected between the

granodiorite - greenstone contact to the southwest and the north boundary

p of the claim group, along north bearing grid lines with a spacing of one

hundred meters at twenty-five meter intervals. Samples were submitted to

Chemex Labs of Mississauga, Ontario for analysis of gold content by fire

l assay with a neutron activation finish.

l 5.4.1. Results

. Most of the samples collected returned values of t./** 2 ppb Au.

~ The highest value was 20 ppb Au. Using a 4 ppb Au contour, a possible

l anomalous trend exists between 7+OOE to 10+OOE and 1+50S and 0+50N with

spot highs of 6, 8 and 20 ppb Au. This trend is sub-parallel to strike and

is underlain by a contact zone between felsic fragraentals and mafic tuffs

M and sediments. This trend should be investigated with hand stripping and

prospecting. Although weak, it is significant in that it overlies a

8 felsic-mafic contact.

l

l l l l l l l l l l l l

CONCLUSIONS AND RECOMMENDATIONS

The Wabikoba Lake property was found to be underlain by mafic

flows, tuffs, interflow sediments and felsic agglomerates. These rocks

strike to the northwest and dip steeply to the south. They underlay the

northeastern half of the claim block. The southeastern half is underlain

by granitic basement rock. Associated with a sediments pinch out against a

felsic-mafic contact is a weak Au anomaly in the humus. This anomaly has a

4 ppb lower contour and highs of 6, 8, and 20 ppb.

The fe lsic-mafic-sediment package is correlatable to a similar

package to the northwest which contains weakly anomalous Au in the rock

(600 ppb).

It is recommended that detailed mapping and prospecting be

conducted over the northeastern half of the property. A detailed

magnetometer survey is also recommended to aid in the definition of

individual units and the granite - greenstone contact. Hand trenching is

also recommended over the weak Au anomaly in humus.

ully submi t ted , Exploration Co., Ltd. onal liabilityI Nor?

(no

1 ^* ^DV

inda pe rs

1

1 f

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l l l l l

Kate^ Hearn Geologist Hemlo District


APPENDIX I

SAMPLE DESCRIPTIONS

l l l l l l l l l l l l l l l l l l

SAMPLE DESCRIPTIONS

Wabikoba - 1119

H31501 Intermediate Fragmental: Dark grey green, fine grained, stretched felsic fragments l cm x 3 cm, 15%, gneissic appearance, trace pyrite.

H31502 Felsic Volcanic: Pink, fine grained, gneissic with wisps of biotite.

H31503 Felsic Fragmental: Pink grey, medium grained, gneissic with 27, small quartz eyes, pyrite 3%

H31504 Intermediate Fragmental: Dark grey green, fine grained, cherty beds? Felsic fragments in chloritic matrix.

H31505 Feldspar Porphyry: Grey with pink euhedral feldspar porphyroblasts (.5 mm in size, 10 % of rock.

H31506 Mafic Volcanic: Dark grey green, fine grained, schistose, silicified, carbonatized banding.

H31507 Mafic Volcanic:

H31508 Quartz-Feldspar-Biotite Gneiss: Stretched felsic crystals in quartz biotite rich matrix. (lapilli tuff?).

H31509 Coarse Fragmental: Coarse grained felsic fragments, milky quartz eyes in chlorite rich matrix. Fragments sub- angular, up to 10 cm in length, distinct fragment margins.

H31510 Medium Feldspar Fragmental: Felsic Fragments, up to 5 cm in length in mafic amphibole-chlorite rich matrix.

H31511 Chlorite-Garnet Gneiss: Blebs and disseminated sulphides.

H31512 Felsic Volcanic: Light grey, very siliceous, slightlyporphyritic character. Diffuse grain boundaries on subhedral feldspar phenocrysts, Rusty pitting. Garnet?

H31513 Metasediment: Brown, muscovite, biotite, quartz, very soft, granular, slightly schistose.

H31514 Feldspar Porphyry: White euhedral feldspar phenocrysts, 10%, O cm in size, in serai-schistose matrix.

H31515 Felsic Volcanic (Fragmental?): Pink grey, highly siliceous,porphyritic layers 2 cm wide, 3/m , biotite rich layers, l cmwide, 10/ra, trace sulphides, bleached hairline fractures.

H31516 Mafic Volcanic: Chlorite rich schist, rare felsic fragments, coarsely crystalline carbonate veining.

H31517 Felsic Volcanic: Small felsic fragments in felsic matrix. Chlorite biotite rich layers with garnet.

H31518 Fine Felsic Fragmental: Small felsic fragments, 1-2 cm in size in


siliceous matrix. Coarse pyrite associated with wisps of biotite.

H31519 Felsic Volcanic: Light brown grey, gneissic texture with biotite enriched bands, slightly porphyritic--feldspar phenocrysts with diffuse margins, trace muscovite, trace sulphides in silicified narrow bands.

H31520 Mafic Volcanic: Minor sediment bands, trace sulphides.

H31521 Metasediment: Brown, semi-schistose, quartz, feldspar, biotite.

H31522 Metasediment: White grey, coarse granular texture, f eldspa^quar tz .

H31523 Felsic Fragmental: Fine felsic fragments in quartz-feldspar- biotite matrix.

3760-0 Felsic Volcanic

3765-A Felsic Volcanic: Py 2-37,.

3765-B Mafic Schist

APPENDIX II

CERTIFICATES OF ANALYSIS

Ministry ofNorthern Developmentand Mines

Geophyslcal-Geologlcal-Geochemical Technical Data Statement

"Ontario

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) RF.OLQGICAL/GEOCHEMICAL

Township or Area Wabikoba Lake Area___^_

Claim Holder(s) Noranda Exploration Company. Limited———

960 Alloy Drive. Thunder Bav. ON P7B 5G2

Survey Company Nnraprfa F.vpl oral- inn Dnmpany, 1. i m i t-p H——-

Author of Report Kate Hear.n______________________Address of Author Bag #8. Marathon, Ontario POT 2EO

Covering Dates of Survey June 3 - September 5, 1987(linecutting to office)

Total Miles of Line Cut ^——-—^_———_——^_^___—__

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.—Magnetometer_—Radiometric——-Other-^———-

DAYSper claim

Geological20/939554

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer. .Electromagnetic.

DATE:.

(enter days per clairn)

SIGNATURE

Res. Geol.. .Qualifications.

Previous Surveys File No. Type Date Claim Holder

N

•iiHNHC

MINING CLAIMS TRAVERSED List numerically

TB 939551(prefix) (number)

939552

939553

939554

939555

939556

939574

939575

.939576....................

..9395.77.................

.93.9.5.7.8....................

.961592.................

SECTION.

TOTAL CLAIMS. 12

l

837 (85/12)

GEOPHYSICAL TECHNICAL DATA

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

Number of Stations _________________________Number of Readings —Station interval .——.—^—--.———^———-—.—-——————.^—Line spacing —————Profile scale^——————^^———^————————-———.———-^,——-—.——-——.Contour interval.

Oi

H N

O D Q z;

W

Instrument.Accuracy — Scale constant.

wDiurnal correction method.Base Station check-in interval (hours). Base Station location and value -—-—

ELECTROMAGNETIC Coil configurationCoj] separation

Arrnrary

Method: CD Fixed transmitter CD Shoot back CD In lineFrpmipnry

* ' (specify V.L.F. station)

CD Parallel line

Parameters measured.

Instrument.Scale constantCorrections made.

Base station value and location.

Elevation accuracy.

Instrument .___.——————————————————————————————————————————— Method D Time Domain CD Frequency Domain

Parameters - On time ___________________________ Frequency -————

-Off time.—..-...————,—-——————^—-——. Range ———————

— Delay time

— Integration time.PHPower.

Electrode array — Electrode spacing .

Type of electrode

SELF POTENTIALInstrument^————^-—-—————————.———————--^————-—— Range.Survey Method ————^——————-—————^^————--—^-—-————...——..—.————

Corrections made.

RADIOMETRICInstrument.Values measured .

Energy windows (levels)—-—-————...—--—.^———————^.,—.—^—-—..———.——Height of instrument_____________________________Background Count.

Size of detector ,—^—.^..^^—.—^^^—^^.,———.—.^—...——.....^—..^.^—....^^—.

Overburden -^———————--..—-—.^^-——^-————^—-—--—..——.-———-.————.{type, depth — include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of survey.——--————-—————^——————— Instrument -—-—————.————^^—..-————————

Accuracy.—--——-————————^———————--——-Parameters measured.

Additional information (for understanding results).

Type of survey(s)

Instrument(s)(specify for each type of survey)

Accuracy————--—————^—-——(specify for each type of survey)

Aircraft used——--——-——-——---———-—————^-——.—————-

Sensor altitude-

Navigation and flight path recovery method.

Aircraft altitude________________________________Line Sparing Miles flown over total area——^—.-—.————-.—————.—..-.——.-—Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples t.Wn 939577, 939551. 939554, 939552. 939555

Total Number of Samples 3o3 ! 23 Type of Sample_____Humus : rock

(Nature of Material)Average Sample Weight 400-500g humus;l-2kg rock

Method of Collection grub hoe———————————

Soil Horizon Sampled—22———— Horizon Development moderate

Sample TVpth 2-8 cm______

Terrain. flat

Drainage Development—PoorEstimated Range of Overburden Thickness .0-10

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Mesh size of fraction used for analysU Ring pulverized 30 seconds and sub-sampled from pulverized

fraction.

ANALYTICAL METHODSValues expressed in: per cent S)

p. p. m. ODp.p. b. S

Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)

Ofhprs Au and whole rock————————————

Field Analysis .tests)Extraction Method. Analytical Method- Reagents Used__

Field Laboratory AnalysisNo. ————————— .tests)Extraction Method.

Analytical Method - Reagents Used,——

Commercial Laboratory (303 soil s: 23 rock tests) Name of Laboratory Technical Service Labs

Extraction Method—————————————————— Analytical MpQuxMO R fire assay. N.A. finish

Reagents Used ____________________

GeneraL General.

Ministry of Report of WorkNorthern Developmenttind Mines (Geophysical, Geological,

Ontario : GeochejmcaUan&Expefiditure

J t t 'td

ed

42C13SWei08 Z. 18538 WABIKOBA LAKE

j wabikoba Lake ^'Prospector's Licence No.

i A34387

T ype o. Su' fev'sl

Geological Mapping and BeneficiationCiairfTHolcier(s)

Noranda Exploration Company, LimitedAddress

Suite 1300 - 4 King Street West, Toronto, Ontario M5H 1B6Survey Company Trj atc o ( Survey (from Si to)

Noranda Exploration Company, Limited

900

]total Miles of line Cut

Name and Address of Author (of Geo-Technical report)

Kate Hearn, Bag #8, Marathon, Ontario POT 2EO

j Day j Mo. i Yr. j Day | Mo. j Yr, j

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)

Date

Sept,24, 1987Certification Verifying Report of Work

1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report k true.

Name and Postal Address of Person Certifying

r -1 -- . - . .••....ucnon, Ontario POT 2LO

Ronna F. Tergie, P.O. Box 2656, Thunder Bay, OntDate Certified

Sept. 24, 1987CerUWGi by

1362 (85/12)

Minislry ofNorthern Developmentand Mines

^ Ontario

Report of Work

(Geophysical, Geological, Geochemical and Expenditures)

x^

Mining Act

- If number of mining claims traversed exceeds space on this form, attach a list.

Note: — Only days credits calculated in the "Expenditures" section may be entered m the "Expend. Days Cr." columns.

— Do not use shaded areas below.1 VPe o* '3u^vey(s J

Geological Mapping and BeneficiationClaim Holcler(s)

Noranda Exploration Company, LimitedAddress

Suite 1300 - 4 King Street West, Toronto, OntarioSurvey Company

Noranda Exploration Company, LimitedName and Address of Author (of Geo-Technical report)

Kate Hearn, Bag #8 Marathon, Ontario POT 2EO

1 1 ownjhip or Area

j Wabikoba Lake &-&2O^Prospector's Licence No.

i A 34387

M5H 1B6fbatc of Survey (from Si to) JTotal Miles of line Cut

j Day j Mo. ! Yr. j Day j Mo. j Yr. j

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

'' Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Man Days

Complete reverse side and enter total(s) here

! Geophysical

- Electromagnetic

j - Magnetometer

- Radiometric

j - Other

: Geological

Geochemical

Airborne Credits :

Note: Special provisions Electromagneticcredits do not apply "to Airborne Surveys. , Magnetometer

. - ] Radiometric

Expenditures (excludes power stripping)'Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total Expenditures

S 3336. 90 H- 15

Total Days Credits^

= 222

Instructions Total Days Credits may be apportioned at the cl.jim holder's choice. Enter number of days credits per claim selected in columns at right.

Date

Sept. 24, 1987Recou^d Holder or Agint ^Signature)

-. f:r ~?^l^ct-J^^* /-^f

Certification Verifying Report of Work

Claim Prefix l Numbe

939551^15

939552

939553

939554

939555 y/

•j:gr 939574 rf.

Total number of mining claims covered by this

For Office Use OnlyTotal Days Cr.lPVe Recorded Recorded

l hereby certify that l have a personal and intimate knowledge of the facts set fefrth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.


l* P7B 5G2Date CertifiedSept.24,1987

1362 (85/12)

,. Ministry ot Northern Development and Mines

Ontario

*ftyf voyls) l

Report of Work

(Geophysical, geological. Geochemical and Expenditures)

of Sufvev's

Mining Act

— If numbei of mining claims traversed space on this form, attach a list.

days -credits calculated in the ures" section, may be entered

in the "Expend. Days Cr." columns-- Do not use shaded areas below.

Townshipor AreaGeochemical . -.Wabikoba

_JNojra^daÊ^lqraf-iorj^ ^ ^^.^^ -..—..____i

[Prospector's licence No.A 34387

Address

Suite 1300 - 4 King Street West, Toronto, Ontario M5H 1B6Survey Company JDate of Survey (from 81 to)

Noranda Exploration Company, LimitedName and Address of Author (of Geo Technical report)

Kate Hearn f Bag #8, Marathon, Ontario POT 2EO

.j .P.?.XJ..MO. J Yr^j pay j Mo. j Yr.

[Total Miles of line Cut

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions . Davs DerGeophysical u^^

For first survey: . E.ecuomagnetic ^

includes line cutting) . Magnc , ometer ,

i- L . .. . . - Radiometric 1 For each additional survey: ou u ei v iusing the same grid: j i

- Other Enter 20 days (for each)

Geological

Geochemical j

Man Days l Days pe , j Geophysical j C|vai ;,

Complete revrfke side - ff J* -Electromagnetic and enter tofaWs/Keat•^ j^t i—... -.

^ f/ i - Magnetometer

• GC* 7r^^ ——. l , 1 ^-/wdiometric

*tyfr V ^'0""'

^TÔft Geological *^j ft^ !

ASft^Geochemicai 9

Airborne Credits Tff i Days per Claim

Note: Special provisions Electromagnetic *

to Airborne Surveys. Magnetometer

j Rsotomeuic

Expenditures (excludes power stripping)

Performed on Oaimis)

Calculation of Expenfluu'e Days Credits Total

Total Expenditures Days Credits

S -r- 15 "

Instructions

Mining ClaimPrefix ; Number

1

TB 939551 '

939577

mB, 939555,^v.-..,....,-'-'-..- . -

. ' ""* . *"

,- -v . -i -r^-

'*V^': iJ 't-"*; "* "" -

-:-'-'-;

' ' v - - 1

' - V r ~ ' ' *J "i,--:V '-.- ' '

'"^!.

- ^

Expend.Days C'.

-- -- --

Mining ClaimPrefix j Number

j

OsissllHb""~"St" "BFmm— - --ijJTPt.......W-i'v*? -

'•yf\* J^V-.'i

" VMI'--ixiQS] - . '.- ; '- - -iySjyUJ

J "JftiVi^PKîW

- '.- * . l .

Si-Si'U'H'v'^Jj

*4mTotal number of mining

Expend.Days Cr.

3

Total Days Credits may be apportioneo at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

For Office Use UmyMining Mecoraer

DateOctober 1,1987

RecpftTJd Holder or Agent (Signature!

Certification Verifying Report of Work———————————————————:———x————.—————————————————————————————————————————————————————————————^*-f———————-————.., l. ————————————————————————————-———————

hereby certify that l have a personal and intimate knowledge of the facts set fo/fh in the Report of Work annexed hereto, having per r witnessed same during and/or after its completion and the annexed report is true.

formed the work


Ronna F. Tergie, P.O. Box 2656, Thunder Bay, Ontario P7B 5G2Date CertifiedOctober

y -(Signature)

\Assessment Work Breakdown

(

Man Days arc based on eight (8). hour, l ccii;:ical or Line-cutting days. Technical days include work performed by ---consultants, draftsmen, etc.. . -. - " "

Y

Type of SurveyGeochemical

Technical Days Credits

Line-cutting Days Total Credits

Days per Claim

Dayt per Claim

LEGEND

A H3I500

GRANODIORITEGABBROFELDSPAR PORPHYRYMETASEDIMENTSa) Interbedded Lapilli Tuff A Metasediments

FELSIC METAVOLCANICSAgglomerateQuartz Eye Agglomerate

MAFIC METAVOLCANICS Agglomerate

Contact, AssumedFoliation, DipOutcrop Distribution, Sample Location

Swamp

Grid Line/Flagged Control Line

— - Claim Line- - - - Traversea Claim Posts, Located 7 Unlocated

Winter Road

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WABIKOBAGEOCHEMICAL SURVEY

PPB au PROJECT: WABIKOBA PROJECT # : 1119

contour intern,! : BASELINE AZIMUTH : 90 Deg.

SCALE - 1: 5000 DATE : 11/12/87 SURVEY BY : LB. NTS : 42C/13

FILE: C1119WAB T"S f*i f™ . .. 'P" T" IMHPAMnA FYPTrtPATinK ^ ,rs^s?

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geol - geoch rpt wabikoba l proj no 1119

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