MAG & VLF SUR ZEEMEL L PROP

lEOtPHEH53B09SWZaei8 53B89SW0e38 ZEEMEL LAKE 010

REPORT

ON

MAGNETJ J AND VLF-EM SURVEYS

ON THE

ZEEMEL LAKE PROPERTY

DISTRICT OF KENORA, PATRICIA MINING DIVISION

NORTHWESTERN ONTARIO

FOR

SANTA MARIA RESOURCES LTD.

NTS 53 - D/9

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March, 1987

RECEIVED;,i'K j O

MltllNG LANDS StCTlON

Stephen B. Medd, B.Se,

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TABLE OF CONTENTS

53Be9swa088 ZEEMEL LAKEl . O SUMMARY

2.0 INTRODUCTION

3.0 PROPERTY DESCRIPTION, LOCATION AND ACCESS

Figure No. l - Property Location and Regional Geology

Figure No. 2 - Claim Sketch

4.0 TOPOGRAPHY AND VEGETATION

5.0 PREVIOUS WORK

6.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIATION

7.0 PROPERTY GEOLOGY

8.0 DESCRIPTION OF GEOPHYSICAL PROGRAM

9.0 RESULTS AND INTERPRETATION

9.1 Lithology9.2 Faulting and Shearing9.3 Folding9.4 Alteration

10.0 CONCLUSIONS

11.0 REFERENCES

010C

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APPENDICES

A CERTIFICATE OF QUALIFICATIONS

B TECHNICAL DATA STATEMENT

Back of report

lLIST OF DRAWINGS

lNO. SMZ-1 MAGNETOMETER SURVEY

VERTICAL FIELD READINGS:n map pocket

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NO. SMZ-2 MAGNETOMETER SURVEYVERTICAL FIELD CONTOURS

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NO. SMZ-3 VLF-EM SURVEY - Tx NLKINPUASE AND QUADRATURE PROFILES

NO. SMZ-4 VLF-EM SURVEYFILTERED INPHASE CONTOURS

M II

NO. SMZ-5 COMPILATION MAP

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1.0 SUMMARY

Ground magnetic and VLF-EM surveys were carried out during

October and November, 1986, and February, 1987, on the 'Zeemel

Lake property of Santa Maria Resources Ltd.

Magnetic data in conjunction with regional geclogical dat.-i

were used to outline two units of multiple zoned iron

formation interbedded with mafic metavolcanics that cross the

property in an east-west direction. Clastic metasediments

are interpreted to underlie the northern part of the prope.-rty

and to separate the two iron formation - mafic volcanic

units. Part of a biota te-hornblende tonalitic intrusion ^.s

interpreted to underlie the southern part of the property.

On the basis of magnetic discontinuities, six fauIts/shears

trending r.orth-northwest to north-northeast are interpreted

to cross the east-west striking stratigraphy. An earlier

generation of faults/shears cross the strati graphy

subconcordantly in an east-northeast direction and are

slightly offset in spots by the later faults/shear:*. These

structures are especially significant where they are

associated with areas of abated magnetic response within iron

formation, possibly reflecting the hydrothermal alteration of

magnetite to grunerite ^ sulfides and the possible deposition

of gold. Five areas of pronounced abated magnetic response

have been identified within the two iron formation-mafic

volcanic units. Based on the above information, five drill

target fences have been selected.

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2.0 INTRODUCTION

The following report describes the results of a ground

magnetic survey and a VLF'-EM survey conducted during October

and November, 1986, and February, 1987, over the Zeemel Lake

property of Santa Resources Ltd. The two surveys were

performed in order to delineate lithologioal units and

structural trends, and to locate conductive zones of sulfide-

bearing iron formation, other stratabound massive or

disseminated sulfide mineralization, and shearing, all of

which might host gold.

3.0 PROPERTY DESCRIPTION, LOCATION AND ACCESS

The Zeemel Lake property is located approximately 70 miles

north of the town of Pickle Lake in Northwestern Ontario,

three miles south of Opapimiskan Lake (Fig. No. 1). The

northwestern corner of the property is covered by Zeemel

Lake. A block of 45 contiguous, unpatented, mining claims,

form the property (Fig. No. 2). To the north, the Zeemel

Lake property is bounded by a large claim block held by a

consortium of companies that include Dome Exploration

(Canada) Ltd., Inco Ltd., Esso Minerals Canada and Lacana

Mining Corp. This block of claims contains the Musselwhite

gold deposit and the Snoppy Lake gold zone. To the east, the

Zeemel Lake property is bounded by a 53 claim property held

under a Joint Venture Agreement among Power Explorations

Inc., H.J. Hodge and W.G. Beach. Claim numbers and

recording dates are as follows:

—-r:--- -. -

r . ' - 3 -r. /o.-*

SANTA MARIA RESOURCES LTD

ZEEMEL LAKE PROPERTY V Patricia M.D., Ontario

UPROPERTY LOCATION AND REGIONAL GEOLOGY

GEOCANtX LTD TQBQHTO. CANADA

DY- R T. M.

DATE MAR. 37SCALE l"*4milMRG. NO' l

t H

Metavolcanic rocks

Metasedirnentary rocks

Iron formation

Gold occurrence

Fault zone

OPAPIMISKAN LAKE

!Y\ 2\\\GOLD DISCOVERY

\

MUSSELWHITE DEPOSITS

Location

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861513 l 861514 IseiSlS l 861512 186I5M '16614241861423 l |——— —t —— — -p- — —\— ——-\~ —— ——F- —— -i--— 861422 .86142!""—L—i861516 .861517 '661518 861519 881520 .861425 861426 l l,-.,.,-——- .—— "T"~" "—— '—f" "—* *—"f '—— ——" l——- '——' -|—* — -- l__. t 0614 Z 7 . OD l ** 2 a

l l l l \ T ——*~ — — 1 l861525 861524 I86I52J 861522 861521

|66I4SI [8614^0 [861429

05 l mile

SANTA MAR(A RESOURCESZEEMEL LAKE PROPERJTY

Patricia M.D., Ontario

CLAIM SKETCH

OEOCAN6X LTD TORONTO. CANADA

DY: R.T. M.DATE MAR,

FlG. Ho-

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Claim Numbers Recording Date

Pa 861413 - 861432 inclusive

Pa 861501 - 861525 inclusive

Total

February 7, 1986

February 7, 1986

Claims

The claims are held by Santa Maria Resources Ltd. of 808-85

Richmond Street West, Toronto, Ontario, M5H 2C9.

The property is accessible by float or ski-plane onto Zeemel

Lake or by helicopter from Pickle Lake. It is also

accessible by foot or snowmobile about one mile east of a

winter road that connects Highway 808 with the Musselwhite

deposit.

4.0 TOPOGRAPHY AND VEGETATION

The property is dominated on surface by flat-lying, flooded

bog and swamp land on the southern side of Zeemel Lake. Very little outcrop exists.

5.0 PREVIOUS WORK

1950's Ben Ohmen and the Kovals

In the Libert Lake area, Ben Ohmen, a prospector working for

the Kovals of Pickle Lake, discovered gold in iron formation

and put down a number of trenches.

1962 The Musselwhite Brothers

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Gold was first discovered on the adjacent Musselwhite

propercy of the Dome et al consortium by the Musselwhite

brothers in 1962.

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1963 Kenpat Mines Ltd.

The property staked by the Musselwhite brothers in 1962,.was

optioned by Kenpat Mines Ltd., who in 1963, carried out

geological and geophysical surveys and diamond drilling. Two

gold zones were discovered with a number of ore grade inter

sections. However, work was suspended.

1962 - 1963 Inro Ltd.

Eighteen holes were drilled on the north and south sides of

Zeemel Lake for a total of 4,503 feet. Two of these holes

(115,800 and #23,107) were drilled along strike to the east

and west, respectively, of the Zeemel Lake property,

encountering chlorite schist and intermediate to mafic meta-

volcanics with up to 15% pyrrhotite and pyrite. Another

eight holes were drilled, for a total of 1,034 feet, in the

Karl Lake and Markop Lake areas east and southeast,

respectively, of the Zeemel Lake property.

1973 - 19B3 Pome Exploration (Canada) Ltd. et al

In 1973, the Musselwhite brothers formed a grub stake

financed and operated by Dome Exploration (Canada) Ltd., in

Joint Venture with Canico Ltd., Esso Minerals Canada and

Lacuna Mining Corp. Since that time, considerable

geophysical and geochrneical work has been done and a total of

180 holes were drilled as of 1980. This work culminated in

the announcement of the discovery of a major gold deposit

containing in excess of 1,000,000 tons, grading 0.20 ounces

of gold per ton (Northern Miner, March 5, L981).

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1976 John Reed

Prospecting/ trenching and diamond drilling were performed in

the Libert Lake property, by John Reed, an independent

prospector.

1981 - Present Various Companies

Since 1981, considerable amounts of work including geological

mapping, geophysics, geochemistry and diamond drilling have

been performed in the Libert Lake area by a number of

companies or individuals, some of whom include: H.J. Hodge;

493217 Ontario Ltd.; Van Horne Gold Exploration Inc. and

Legion Resources Ltd.; and G. Armstrong, A. Best, B. Reid

and S. Johnson.

1981 Dome Exploration (Canada) Ltd.

An airborne magnetic and electromagnetic survey, part of

which covered the Zeemel Lake property, was conducted by

Aerodat Ltd. over the area surrounding the Musselwhite

deposit.

1981 Canico (Inco Ltd.)

A geological survey and ground magnetic survey were carried

out, using a mapping scale of 1:2,500, in the Karl Lake area

east of the Zeemel Lake property.

1985 Ontario Geological Survey

An airborne magnetic and electromagnetic survey was carried

out by Aerodat Ltd. during the winter of 1985, and in early

1986, the results were released to the public on a set of 38

maps (scale 1:20,000). Maps 80743 and 80744 cover the Zeemel

Lake property.

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6.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION

The North Caribou Lake and Opapimiskan Lake greenstone belts

are comprised of Archean metavolcanic and metasedimenta(ry

rocks that belong to the Sachigo Subprovince of the Superior

Geological Province of the Canadian Shie-ld. Together, the

two belts form a narrow, arcuate, isoclinal syncline that

stretches for approximately 140 kilometers from end to end.

The metamorphic grade is upper greenshcist to middle

amphibolite facies. A. thick clastic metasedimentajry

sequence, known as the Eyapamikama Lake Metasediments occupy

the central and northwestern part of the North Caribou Lake

greenstone belt. This sequence is flanked to the north by

the North Rim Metavolcanics and to the south by the South Rim

Metavolcanics. The South Rim Metavolcanics contain mafic to

felsic metavolcanic flows and tuffs; the main lithol-jgiQs

being fine-to-medium-grained, massive and pillowed mafjic

flows. The North Rim Metavolcanics contain predominantly

mafic metavolcanic rocks. Both the North and South Rim

metavolcanic units host extensive zones of banded irpn

formation.

In the vicinity of Opapimiskan Lake, these two metavolcanicj

units pinch out and they are replaced by the Opapimiskafi-

Markop Metavolcanics. These rocks are mafic to ultramafic in

composition and are possibly older and geochemically mo^re

primitive. They are similar compositionally to the Keeyask

Lake Metavolcanics at the western end of Eyapamikama Lakb.

The metavolcanics are macroscopically intercalated with

clastic metHsediments between Opapimiskan and Markop Lake^.

At the eastern end of the Opapimiskan Lake greenstone belt,i a

sequence of pillowed and mafic metavolcanics exist, and a|re

known as the Forester-Neawagank Metavolcanics (Breaks et ajl,

1986).

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Chemical metasediments are extensive in the OpapinisKan-

Markop, Forester-Neawagank, North Rim and South Rim

Metavolcanic sequences. The presence of grunerite in banded

iron formation, correlates with zones of increased shearing

that commonly parallel iron formation banding and axial

planes of ?2 folds in banded iron formation at the

Musselwhite gold prope, ; { Breaks et al, 1985).

The main gold zones in the North Caribou Lake and Opapimiskan

Lake greenstone belts occur on the southern shore of

Opapimiskan Lake. The Musselwhite deposit was originally

discovered by the Musselwhite brothers in 1962. Between 1973

and 1980, the property was extensively explored and drilled

by a consortium of companies headed by Dome Exploration

(Canada) Ltd. This work culminated in the announcement of

the discovery of a major gold deposit containing in sxcess of

1,000,000 tons, grading 0.20 ounces of gold per ton (The

Northern Miner, March 5, 1981). Reserves currently stand at

3,200,000 tons grading 0.17 ounces of gold per ton in 4

zones. The discovery of the new Snoppy Lake gold deposit

located two miles to the east, was recently announced by Dome

Exploration (Canada) Ltd., (The Northern Miner, August 11,

986). It currently stands as a shallow dipping zone 4,300

feet in length grading 0.24 ounces of gold per ton over an

average width of 12 feet. Both of these deposits occur in

complexly folded banded iron formation.

7.0 PROPERTY GEOLOGY

No geological and prospecting survey has yet been undertaken

by Santa Maria on their Zeemel Lake property. However, from

the regional mapping done by the O.G.S. in 1986 (Breaks et

al, 1986), two units of multiple zoned iron formation hosted

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in mafic metavolcanics {Opapimiskan-Markop Metavolcanics) are

believed to cross the property in an east-west direction.

Clastic metasediment underlie the northern part of the

property and separate the two iron formation-mafic volcanic

units. The southern part of the property is underlain by

part of a biotite-hornblende tonalitic intrusion.

8.0 DESCRIPTION OF GEOPHYSICAL PROGRAM

During October and November, 1986, linecutting, magnetic

surveying and VLF-EM surveying were carried out on the land

portion of the Zeemel Lake property of Santa Maria. The

personnel involved were:

R.LeMay

C.Morin

R.Boone

F.Recoskie

C.Beggs

Val d'Or, Quebec

Val d'Or, Quebec

Val d'Or, Quebec

Val d'Or, Quebec

Toronto, Ontario

R.Carpenter Sioux Lookout,

Ontario

Linecutter Oct.

Linecutter Oct,

Linecutter Oct.

18-Nov. 5

18-Nov. 5

18-Nov. 5

30-Nov. 5Geophysical Oct

Operator

Geophysical Oct. 30-Nov. 5

Operator

Geophysical Oct. 30-Nov. 5

Operator

A total of 41.3 line miles were cut on the property. A base

line trending east-west was cut across the property, and

perpendicular survey lines were cut 400 feet apart with

pickets erected at 100-foot intervals.

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During February 1987, magnetic surveying and VLF-EM surveying

were carried out over the lake portion of the Zeemel Lake

property. Survey lines were set up across frozen Zeemel Lake

with pickets erected every 100 feet. The personnel involved

were:

F.Recoskie

G.Zimmer

D.Recoskie

R.Carpenter

Val d'Or, Quebec

Val d'Or, Quebec

Val d'Or, Quebec

Sioux Lookout, Ontario

GeophysicalOperatorGeophysicalOperatorGeophysicalOperatorGeophysicalOperator

Feb.15-20

feb.15-20

Feb.15-20

Feb.15-20

The magnetic survey was performed using a Scintrex Fluxgate

MF-2 magnetometer. Readings of the vertical magnetic field

were taken every 100 feet along the survey lines and in areas

of high magnetic gradient, readings were taken at 50-foot

intervals. Diurnal drift changes in the magnetic field were

estimated by taking repeat readings at previously established

stations at time intervals not exceeding 1.5 hours.

Corrections were made, accordingly, to the vertical magnetic

field value obtained at each station. The results of the

magnetic survey are presented in Drawings No. SMZ-1 and SMS-2

as vertical field readings and vertical field contours,

respectively.

The VLF-EM survey was carried out using a Geonics EM-16

receiver tuned to receive the 24.8 kHz signal transmitted

from Seattle, Washington (NLK). Readings of inphase (tilt

angle) and quadrature were taken every 100 feet along the

survey lines. The results are presented in profiled format

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and contoured, Eraser-filtered \nphase format in Drawings No.

SMZ-3 arid SMZ-4, respectively, located in back of the

report.

9.0 RESULTS AND INTERPRETATION

Refer to the magnetic, VLF-EM and compilation data presented^

in Drawings No. SMZ-1 to SMZ-5 inclusive, in back of the!

report.

l 9. l Lithology

Two units (1F-1 and IF-2) containing mafic metavolcanicS

hosting multiple zoned iron formation are interpreted, on th^

basis of contoured magnetic data, as crossing the property ih

an east-west direction. Both units contain several narrow

magnetic bands of high gradient. The iron formation zones

are probably relatively weak and/or thin since vertical field

magnetic values of only 3,100 gammas (IF-1) and 8,525 gammas

(IF-2) are the highest readings within both units.

A number of VLF-EM conductors occur within Units IF-1 and

IF-2 often concordant and coincident with magnetic bands a t

high gradient. These conductors may represent pyrrhotite-f

pyrite mineralization occurring as sulfide facies iroo

formation or as sulf ide-bear ing, concordant shear zones

within iron formation.

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North of Unit IF-1 is an .^rea of low magnetic gradient and

low background values which probably represents clastic

metasediments. A similar but more narrow unit exists betweeh

Units IF-1 and IF-2 and also probably represents clastic

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metasediments. A number of east-west trending VLF-EM

conductors occur within the clastic metasediments and may

represent stratabound sulfide and graphite zones, or

concordant shear zones.

The areas south, and possibly immediately east, of Unit IF-2

may represent part of a biotite-hornblende tonalitic

intrusion which has been mapped by the O.G.S. (Breaks et al,

1986), They are characterized by low magnetic gradient and

low background values.

Also noticeable from the magnetic contours is an intermediate

or mafic dyke that strikes across the property in a northeast

direction. It is more apparent from the regional airborne

magnetic contours (O.G.S., 1985).

9.2 Faulting and Shearing .

The property contains a complicated network of faulting and

shearing that probably represents more than one phase of

structural deformation. The most recent of these faults/

shears are believed to be north-northwest to north-northeast

structures that are easily discernible from the vertical

field magnetic contours. They are identified by

discontinuities alo'i linear magnetic trends and do not

possess VLF-EM conductive responses.

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An earlier fault/shear direction is identified by at least

three parallel, moderately strong, VLF-EM conductors that

trend east-northeasterly across the southeastern part of the

property. These conductors are subconcordant to the

east-west stratigraphic trend and appear to truncate Unit

IF-2 on the southeastern part of the property. Also, their

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VLF-EM conductive responses appear to be slightly offset in

spots by crosscutting structures/trending north-northwest to

north-northeast.

A number of east-west trending VLF-EM conductors occur on the

property and may represent conductive concordant shear zones

or primary stratabound sulfide and graphite zones.

9.3 Folding

Two areas of small scale folding may exist withiP Unit IF-2

associated with faulting/shearing. On the basis of contoured

magnetic data, these areas are defined by L36+OOW to L24+OOW,

12+OOS to 20+OOS and L16+OOE to L32+OOE, 18+OOS to 30+OOS.

9.4 Alteration

Five areas of possible hydrothermal alteration occurring

within iron formation Units IF-1 and IF-2, are outlined on

the basis of pronounced abatements in the magnetic intensity

along linear magnetic trends. These areas appear to exist

adjacent to or along fault/shear structures and t may reflect,

the hydrothermal alteration of magnetite to grunerite

sulfides.

10.0 CONCLUSIONS AND RECOMMENDATIONS

The Zeemel Lake property of Santa Maria is crossed by two

east-west striking units of multiple zoned iron formation

hosted in mafic metavolcanics . Clastic metasediments are

interpreted to underlie the northern part of the property and

to separate the two iron formation-mafic volcanic units.

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H The southern part of the property may be underlain by part of

a biotite-hornblende tonalitic intrusion.

H At least two generations of faults or shear zones cross the

property. The more recent ones trend north-northwest to

g north-northeast and appear to offset slighly an earlier

generation of conductive east-northeast trending faults/

[9 shears that cross the southeastern part of the property

subconcordantly to the stratigraphy. Small scale folding

H within the southern iron formation-mafic volcanic unit may be

related to these faults/shears.

The structures described above are especially significant

where they are associated with areas of abated magnetic

B response within iron formation zones. Such areas may reflect

the hydrothermal alteration of magnetite to grunerite ^

H sulfides and the possible disposition of gold. East-west

trending conductors occurring within or adjacent to areas of

H hydrothermally altered iron formation are favourable drilling

targets for gold.

0 The presence of grunerite ^ sulfides in the Akow-Eyapamikama

Lakes banded iron formation correlates with zones of

H increased boudinage and shearing. Also, conversion of

magnetite to grunerite is locally evident in progressing from

11 limbs to crests of F'2 folds in the banded iron formation at

at the Musselwhite gold property (Breaks et al, 1985). Using

SI these two examples as models for the Zeemel Lake property

five drill target fences have been selected:

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L44*OOW,28*OON to BLO+00Lse+ooWjio+oos to 24+oosL12+OOE,12+OOS to 32+OOS

L^S+OOEfS+OON to 6+OOS

L32+OOE,18+OOS to 32+OOS

iRespectfully submitted,

IfStephen B. Medd, B.Se.

Geocanex Ltd.

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B11.0 REFERENCES

Breaks, F.W., et al, 1985. Opapimiskan Lake Project:Precambrian and Quaternary Geology of the North Caribou Lake Area, District of Kenora, Patricia Portion; p268-276 in Summary of Field Work, 1985, O.G.S., Paper S54.

Breaks, F.W., et al, 1986. Opapimiskan Lake Project:Precambrian Geology of the Opapimiskan - Forester Lake Area, District of Kenora, Patricia Portion; p368-378 in Summary of Field Work, 1986, O.G.S., Paper 075.

Hodge, H.J., 1981. Report on Gold Properties adjacent to Dome-Inco-Esso-Lacana Discovery, Opapimiskan Lake Area, Patricia Division, Ontario; unpublished report of Geocanex Ltd.

Hodge, H.J., 1982. Report on Geological Mapping, Geochemical Sampling and Prospecting, Libert Lake Property of 493217 Ontario Ltd., District of Kenora, Patricia Portion, Patricia Mining Division, Ontario; unpublished report of Geocanex Ltd.

Ontario Geological Survey, Resident Geologist Files - Toronto! and Sioux Lookout, Various unpublished assessment reports.

O.G.S., 1985. Airborne Electromagnetic and Total Intensity Magnetic Survey, Opapimiskan Lake Area, District of Kenora, Patricia Portion; by Aerodat Limited for Ontario Geological Survey, Geophysical/Geochemical Series, Maps 80743 and 80744, Scale 1:20,000. Survey and Compilation March to July, 1985.

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APPENDIX A

CERTIFICATE OF QUALIFICATIONS

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CERTIFICATE OF QUALIFICATIONS

THIS IS TO CERTIFY THAT:

I have been a resident of Toronto, Ontario since 1984.

I have been actively engaged in Canadian and foreign mining and explorations since 1979.

I am a graduate of the University of Waterloo, Waterloo, Ontario, with an Honours B.Se. (1983) in the Co-op Program of Earth Sciences.

I am an associate member, in good standing, of the Geological Association of Canada.

I have disclosed, to the best of my knowledge, all relevant material, descriptive and interpretative, used in the compilation of this report.

DATED THIS DAY OF

/'Stephen B. Medd, B.Se, Geologist

APPENDIX B

TECHNICAL DATA STATEMENT

Ministry o lNorthern Developmentand Mines

Geophysical-Geological-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).

Township or Area.

Claim Holder(s)_

Ground magnetic and VLF-EM

Zeemel Lake_____ ^^^^

Santa Maria Resources Ltd.

808-85 Richmond S tree t , Wes t Toronto Survey company Geocanex Ltd. -^-—^-——-——- Author of Report Stephen B. Medd , B. Se. .-——————Address of A..thnr - 7 Crescent Place, Tor.Ont .

Covering Dates of S..rvgy October 18 , 1986-March 17. 198(linccutting to office)

Total Miles of Line rut ^1-3 miles _________________

SPECIAL PROVISIONSCREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

DAVS ~ , . . prr cliimGeophysical

— F.lrrtrnmflpnriir,. - ' .

-Mapnrtnmrirr 20

~ R^rliomrtrir. ., .......,.

-Olhrr

Grnlngir:il. . .,.

r.rnrhrmjca!

AIRBORNE CREDITS (Special provition crcdiu do nol *pply lo airborne lurvryi)

Magnetometer, .Electromagnetic , Radiometric(enter dayi per cUim)

DATE:. ..r.NATURP.

Res. Gcol.. .Qualifications.

\ - -~ t ' r - " ' t

i . 1 :

OFFICE USE ON1rrevious surveys

File No. Type Date Claim Holder

937 (85/12)

TOT A I.™ -A IMS ^5

MINING CLAIMS TRAVERSED List numerically

(prtfin) (number)

SEE ATTACHED LIST

GEOPHYSICAL TECHNICAL DATA

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

Number of Statinny 2.066-—-——————Station interval 1 00 feet (50 feet)Prnfiirsralf l JHCh "

.Number of Readings EM 2.068 Mat;.

.Line spacing .Jj 00 feet-——.———-—

Contour interval.100 gammas

W

s

Scintrex MF-2 Fluxgate magnetometer Instrument ___________________"——-M.r—^—————0 . Accuracy — Scale constant — n 10 gammas

n . . . . . . Looping methodDiurnal correction method ____ ______Base Station check-in interval (hours)———!™~——-

Base Station location and value Various

CJH w zo•a*

Instrument Geonics EM-16 VLF Receiver

Coil configuration Vertical———..——Coil separation Infinite_________

i p or Accuracy ————————±-Z————————————

Method: E) Fixed transmitter

Frequency.

D Shoot back KHz, Seattle, Washington (NLK)

D In line D Parallel !i;nc

Parameters measured.(•peafy V.L.r. xition)

Inphase (tilt angle) and Quadrature

Instrument.

Scale constant

Corrections made.

Base station value and location .

Elevation accuracy.

N2

Q ujC

C/300 UJf*

Instrument —————————— Method D Time Domain

Parameters — On time ———

- Off time —--

- Delay time ———

~ Integration time.

l l Frequency Domain

_ Frequency _____

_ Range -———————

Power.

Electrode array — Electrode spacing .

Type of electrode

iSANTA MARIA RESOURCES LTD. {Claim Holder)

ZEEMEL LAKE PROPERTY

List of Claims

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Claim No.

Pa 861413861414861415861416861417861418861419861420861421861422861423861424861425861426861427861428861429861430861431861432

Claim No.

Pa 861501861502861503861504861505861506861507861508861509861510861511861512861513861514861515861516861517861518861519861520861521861522861523861524861525

Total 45 claims

i

l

l

l

,, - ...

-- l

•- f 'f A ' f -

. ^

i:.-, ..

. ,- *-.f-^ ••i-. ^ i-~---

;.-

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...

Ministry ofNorthern Developmentand Mines

Ontario p /). /C - tt

Report of Work(Geophysical, Geological, Gcoclicniical and Expenditures)

f21-1 f

Type o*Mining Act

Instructions: — Please type or prim.— If number of mining claims Rraversed

exceeds space on this form, attach a list. Note: — Only days credits calculated .n the

"Expemjitures' 1 section may br? entered in the "Expend. Days C' " rcQlunins.

— Do not use shaded areas below.

Ground Magnetometer s VLF-EM SurveyClaim Holder(j)

William Masakeyash

Township o r Area

Zeemel Lake Area Q AM'B]r*f ospt'c tor ^ Licence No. ^ -

S-6130Auoroil

Survey Coru

Savant Lake, Ontario POV 2SOloiie ol Suivev il'orv i'lo) 'Toiai Miles oi lino CJ!

8|ljQ. : 8^. j 1,7,0,3..8,7 i 41.3..___._...— G.eo.canex.Ltd. . . . . . ..... .Name and Aaarcii of Auihor [of Gto-Tuc'intcai r e p O''J

S. B. Medd 3.Se., 1117 - 7 Crescent Place, Toronto, OntarioCredits Requested oer Each Claim in Columns ;it nqnt Minmc: Cljims Travel J (List m -iumeiic.ilSp*Cifll Provisions ! i n-w* nor

. G*0[)'\v*icai ,^jîv- Cla.m

For first survey: i , . ~ - Electromagnetic 4 (J

includes cine cutting) ; Magneto....-!,... 20

For each additional survey - Hicjiomoincusing the same grid:

Enter 20 days (for eacnl i

Geological

Gtfocnemic.ji :

Man Dayl 1 | O a s ( H,, ! Gcooi-yt.cai c,,, m

Comptete reverse side ' dna t'nier totoiisl here

MJyne,o,,,,,, l

. R^,o,,,.u,c

1

Geoiogicji

Geochointc ji j

A.rlJOfCly C'tfQiSS Ooyi pt'f: ci j ini

Note: SpeC'31 provisions ElectromagneticCÛHS 'l' i i|!"Ml —— " ——— .-.i.. ' i "| -

E \t (TU r -; '.'.i/ u .ri- ——— - IE, lâio.^.ri ib it l

poy.'tr^triDt^ngVpY ' — ' jType o' Work Pert rmed f-\\ i\ ^ ' t l

A.M- ' I '- rc^ ' ' r, .."i 1

Pcriorm.o on cud i,7(3|OilOilliT2r1i-iSi'7i'r ]6 Ji

i

Cjicuiatiun ol f.xoonaituie Davi Cf*atts Totjl

Total GxD^noituroi D^T, i Ctonui

S 4- 15 =

Toiol Days C.'ecits nuy bc JnponiOnt-M jl '.htj cuiiri hoioer -;

c

April 3, l?87 x v -NJ7'i^ -i-i^-' c /fCi'rtitication V'entvinn Report trr 'A'ink

M.n.nn Cla.cnPu* li x NurTM^Cf

Pa ; 861413

861414

' 861415

- . 861416

861417

' : 861418

861419

- 861420

861421•• ;; - : 861422

••''.'.y 861423

861424

861425

861426

861427

,, L 861428

861429

861430

861431

361432

-- - - - — - —

C. p c--, o D.ivs Gr.

-. ———— .

. ————— .

- —— - — -

.----——

Pa. 8WFor Orttco L'.ê Omv

7 Dim O.i v^ i." f . O.i t o tii*i:c'*'#o

1 /S fi f^- ^ '' '

\4 y ' ' ' ——

f.l-nmg CiJtrnP.,.1.. Nuftioor

c

'V™, :-

® "vv'v: '*'"'t, s

.. M .,.'v , ;.'.

|:;S':x A

.

' ," '-'

-

\ N

!v"S -C-iE-J-

^1121

—

V19

w

. — ...—.... —

c 'y mi covureWij-/ ^'S

\

^ ' ' (hereby certilv that 1 have a perion.T .mil inlim.iU' M'(.U\H-C . i! o! mi- Md 1 , VIM 1 1/ 1 M "i tl'f 'i.'t:,in oi tVoik. .nint-xi/n lunpn^-

or wil:U'4i,i'U SJMM' Uunnq .inj/oi .iltci its cjniiili'i on .nui tin- \ n i , 'VIM irm" l i-, l 'in'

^\

-^"^T^Nryfty^ /C

' - i^•"""••'*' m '

—

—

b ^ Denn

(Vi vt C'

p-0—

J7~-

.î.un

— - --

'

x 0

~-o-

-^.J ^d en,;, u,,,..

N.nnif .inci f'o^l.il Ailclirrnol rj vion Ccc c i' v"i|

G. G. Plaskett 808 - 85 Richmond Street West, Toronto, Ontario M5H ,2C9I n Ai3rii"'''3,1987 ' {'"/"l^'l

J \

Northern Dovelopmonl and Mines

deport ot W ork(Geophysical, Geological, Geochemical and Expenditures)

Type o l Su'

Mining A ct

— II number ol mining claims ir|aversod exceeds space on this form, ai!ac|h a list.

— Only days credits calculated lin theExpend,lures" section may belemered

in the "Expend. Pays Cr." cb'umns,— D o noi usi: shaded areas below.

Claim HolderU)

GroundTMagnetometer 6 VLF-EM Survey

Frank Recoskie

Zeemel Lake Area|"PrCiSpuc!0''t l..e*ncV"N

! K-19788

P.O. Box 186, Pickle Lake, Ontario POV 3AOSurvey Company 'D.ite o' "Survey "llr'oni ,'V :ol 'Toiai M.ias ot lire

^____^^ Gfocanex . Ltd - Nv i W 8,6 11:3, i 0,3 i 87 41.3Name and Aoortrss of Author (o' Gvo- Tticnmcai a:oouS

S. B. Medd B.Se., 1117 - 7 Crescent Place, Toronto, OntarioCredits Requested per Each Claim m Columns at mjht iMin.no Claims Traversed (List 'n numerical seui.ence)Socc.,1 P !0 v.,.on, Geonhv-ca, 1 C^'

For firsl survey: i - Elec'.r onMynet'C 40

includes .me cutting) Mi 9n,.|on.etcr 20

For eachaddition.il survey - Hjuion.euic using the same grid " "~"

- Oirn-rEnter 20 days dor each)

Geological

Geochun,.™.

Gl!O0h yS'*..H r* t , |nl

Complete reverse iide 1 and enter totJi(s) here

- Magnet O mt'U'f :

i - R joionittinc i

- Olfie' i

\ G ooiogic.il 1i i

' G,oc,,e,,,c,i i

A.ruorfiu CruUiI! OjyJ pe'

Note: SpeC'Ji provisions i Electromagnet..:

creoiU do not apply ' " ' IO Ai rUOine Surveys. J MiS"Cton'*lct

rpATft^wj "*'N 'Nfiniv.,lExoerauures !^\cludl!4p^v i) E.st (l'PPi6,!J) : li ^ \\ . -TypooiWorK Pertormc l j pA i vf're.zlci, rip r- V*^ I'-'J

7oD - Q 1937or 0'"MO on u.Ji.n,, ^^^ ^ ^ p^ ^

1Cjic i J t to" o' r. x UL'fui 1 1 u f o OXivi C'Oii'*

T o l .1 1Total EMOtnc.turm 13.n* G'^citi

S -:- 15 -Instruction!

TO131 03V* 0 CMtl* rnjy 1)0 J DOOr t uincO ,) l Ve f l.iirn (-yiufr ',

C no if*). Cnt**' MuiTiDor 01 1,1 is* v'ooit! pci ci.uni M.MrcU'ii in column* ji r ight.

^" l t 1Ooie Kt^mcO HOUI'^ ,;i 'Mjt'i'^ Sail 11 -)^!! C 1

Apr i 1 3 , 1987- "'^'.^ c - ^ '^ " '(CtTtiticauor1* Vonfvinq Ren^TrroT \Voi k

Min.nq Ci.l'M-.

;-.eln ' Numt-pr

Pa 861501

1 861502

' | 861S03

J 8615C4

861505

861506

"; 861507••'-•"i 8 61508

•' ,', : ! 861509

;. '.; j 861510"""'•I 861511

.-.j 861512

i 861513

861514

' --, 861515

' 861516

861517

861518

i 861519

861520

86.1521 ^

...861522..

t '61523

E x ne noDays Cr

——— -

li 86WIFor Oltico Uif Qnlv

Min.nq Oa.mPrel*. l Numne'

Pa

.

; ; : :

?.t;

MI;:

-

861524

861525

...

*ECliL-*Pft~2T~

—

yj196

NG-UNDSSE

U otai^x^'L'/' OP-'iimmq \ijiir.* c rXriHi t-'v uusrVpO' T J! -.V \' K , \

\tot.ii 15-ivi Cr.,C.ilO liccCTeo :Mirln^J*f o \ "' NocorOLHl /^ /T/OiS^ ( \t/har. Y //o/ SbkA~ .j.'r ~ . ....'.-..... ..... . -. ,. - ' f — H

/cfOO ^" " ," "'-" '( V-— ' /','<^^-^~~ i VJ7 --1 - ' ^ ^ /-^''f •^-

•/7**~* ———————— —— -r- —— ~7~

heieuv i:eMilv thai i have J ivrsonj ,iru] .nitm.ur knowu'tnio Ji i in- loctTî^'fh ,n mo iu'Ôft oi Work .in u*KCii I'-rfîo Of \viinL-ssctl s J f ut1 JuriMfj ono'oi .ittoi it-; coinoli'iuin .vui j ne ^nno VIM (Opm l i* uue

N'.iint? t)oi) Pr**.ii A.uiron of P**nc*n c*o f tiiV i( ^0

G. G. Plaskett 808 85 Richmond Street West, Toronto, Ontar

'April "3, 198 7 V'"'",^

/' |r^^'T/Tfy^î3v.no eeiiornir

io M5H 2;iniv'/

——

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25

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^^ld tt!i'jl\0it

C9 __ ..1

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SEE ACCOMPANYING MAP(S) IDENTIFIED AS

LOCATED IN THE MAP CHANNEL IN THEFOLLOWING SEQUENCE

(X)

536/015^-0038

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L.EGEND

Ci r i d , ' n e A i T n : O C"1 s ' c r :

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ZEEMEL LAKE PROPERTY Opapimiskan Lake Area, Ontario

Magnetometer Survey VERTICAL FIELD READINGS

GEOCANEX LTDTORONTO. CANADA

SCALE l 4BOODWG. No. S MZ-1

53B09SW0e0e 53Se9SWe*3S ZEEMEL LAKE

PROPERTY LOCATION9O 0 SO'

\i Skinner Lake

Kar/ '-7 Lake

Foresi~ , /. o K

BASE LINE 00

Instrument .............. . ..... ........ Scintrex MF-2

Contour interval ........ . .......... ...... 100 gammas

100 gamma contour

500 gamma contour

2500 g amma c ontour

Depression .............,.

5T3B CFI^^2.



Magnetometer Survey VERTICAL FIELD CONTOURS

GEOCANEX LTD rORONTO, CANADA

SCALE: I -48OODWG. No: SMZ-2

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PROPERTY LOCATION9O 0 I5'

..l0

Opop/mis/ton L ok e

Skinner Lake

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To PicKlfl Lake (50 miles)

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Fores'er

•JO M

COroCOr\j ^T

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20 N

ION

BASE LINE 00

iOS

20S

305

?

Instrument....................................Geonics EM-16

Transmitter .............NLK,Seottle,Wash.,24.8 kHz

Readings taken facing north .plotted...... IP -

Profiles at f'^40% ; plotted .............. -

Inphase profile ,........................... ———"

Quadrature profile ........................ — — ---

OP

-t-

400 feet

S3B89SWIW06 53B09SWM38 ZEEMEL LAKE



VLF EM SURVEY - Tx NLK

S^f"vfrGEOCANEX LTD

TORONTO, CANADA

BY;

DATE: December86SCALE: l 4800

No:

PROPERTY LOCATION

Tx NLK , 2266 kmsOpapimiskan , -

. . OK e

--•' i if Zeemel

Pickle Lake (50 milei )

Zeemel Lake

BASE LINE 00

Instrument ................................Geonics EM 16

Transmitter............NLK, Seattle,Wash., 24.8 kHz

Contours of Fraser filtered VLF EM inphase data

H-5% contour........................... -^—~~———"^

H-10% contour..........................

-f-50 *Vo con t our..........................

538*95*6*08 536098*0036 ZEEMEL LAKE 230



VLF EM Survey FILTERED INPHASE CONTOURS

GEOCANEX LTD TORONTO. CANADA

BY:DATE:December86SCALE: 1 = 4800DWG. No: SMZ-4

PROPERTY LOCATION

o Pickle Lake (60 Tii.es

F-1BASE LINE 00

20S

30S

00LO-l

EGEN

Gf id l ine witr .,'C' stations

Stream, sWarr^, G-e5": r e..

Claim, post end l,ne ........,.

Instrument .......................,......... .Scintrex MF-2

Contour interval ...,...... .......,......... 100 gammas

100 gamma contour

500 gamma contour

2500 gamma contour

Depression ...............

Fault or shear

Major geological boundary

Dyke

Area of alteration

VLF-EM conductor axis

5 - 30 *Jb

^ 5 "o

O500' 1000'

Scale l" * 4 00 feet

1500'

S3S09SWM3B ZEEI^L LAKE



COMPILATION MAP

GEOCANEX LTDTORONTO, CANADA

BY: S . MeddDATE: December 86SCALE: l 4800DWG. No: SMZ-5

MAG & VLF SUR ZEEMEL L PROP

Documents

Transcript of MAG & VLF SUR ZEEMEL L PROP