42C13SWet61 Z,7444 WABIKOBA LAKE 010

Geological Reporton the

BATTLE ENERGY CORPORATION PROPERTYHeralo Gold Area

District of Thunder Bay, Ontario

by

Nadia Caira, B.Se.

RECEIVED

NOV 2 7 1984

MINING UNOS SECTION

Robert S. Middleton Exploration Services Inc.P.O. Box 1637

Tinmins, OntarioP4N 7W8

August 15, 1984

42C13SW0161 2.7444 WABIKOBA LAKE 010C

TABLE OF CONTENTS

Page

INTRCDUCTICN. . . . . . . . . . . . . . . . . . . . . . lLocation and Access. . . . . . . . . . . . . . . . 2Property ..................... 2Topography and Vegetation. . , . . . . . . . . . . 3Previous Work. . . . . . . . . . . . . . . . . . . 3

REGIONAL GBOLOGY. . . . . . . . . . . . . . . . . . . . 5

PROPERTY GEOLOGY. . . . . . . . . . . . . . . . . . . . 6Table of Lithologies . . . . . . . . . . . . . . . 7Structural Geology and Metamorphism. . . . . . . . 10

CONCLUSIONS AND RBOOP.1^ENDATIONS . . . . . . . . . . . . 10

REFERENCES. . . . . . . . . . . . . . . . . . . . . . . 11

CERTIFICATIONS

LIST OF FIGURES

Figure l Property Location Map l" = 25 mi.

Figure 2 Claim Location Map 1:50,000

Figure 3 Regional Geology l" - 1/2 mi.

Figure 4 Detailed Property Geology l" = 200'

APPENDIX

Assay Certificate

- l -

INIKCPUCTIGN

A geological mapping survey was conducted between June 11 to

June 15, 1984 and on July 20, 1984 on the Battle Energy

Corporation Hemlo gold area property. Tlie property consists of

14 contiguous unpatented mining claims located in the northeast

corner of Map 2452, Hemlo Map Sheet, Molson Lake Area. The

property lies approximately 4 miles northeast of the presently

known Hemlo Gold deposit.

Geophysical examinations on the Battle Energy Corporation

property to date have consisted of magnetometer survey and a VLF

survey which were carried out during August, 1981. The

magnetometer and VLF survey was conducted by Mid-Canada

Explorations of Tinmins, Ontario.

The geological survey was conducted by lan Coster, B.Se.,

and Nadia Caira, B.Sc., and David Hurst, B.Se., who carried out

the mapping on a previously cut grid of approximately 11.5 miles.

A well-cut baseline extends from the east boundary of the claims

near the northeast corner of claim TB731202 westerly for 6400

feet with perpendicular lines, at 400 feet intervals which were

cut to the claim boundaries. Survey stations were established at

100 1 apart intervals along the picket lines.

It is the purpose of this report to discuss the findings ofi

the geological survey.

9 "*

Ix)cation and Access

The Battle Energy Corporation property is located in the

northeast corner of Map 2452, Hemlo Map Sheet (Muir (1980)). The

claims are located approximately 4 miles northeast of the Hemlo

gold deposit in the District of Thunder Bay, Thunder Bay Mining

Division, Ontario. Hemlo is a railway coomunity 16 miles east of

the town of Marathon on Lake Superior.

Indirect road access to the property is provided via Highway

614 that connects the mining community of Manitouwage with the

Trans Canada Highway (Highway 17) at the junction, approximately

6.25 miles east of Hemlo. Approximately 3.1 miles north of the

Highway 614 - Highway 17 junction a good all weather gravel road

leads west through a gravel pit for 1.06 mile to a left fork that

runs south for .625 miles then west for 0.62 miles where it ends

in a gravel pit approximately in the south central part of the

Battle property, on line 24W at approximately 21+OOS.

Property

The 14 contiguous mining claims included in the Battle

Energy Corporation claim group, encompass approximately 480 acres

of mining land in the northern part of Lecours Township. The

claims, which are registered with the Ministry of Natural

Resources, Recording Office, Thunder Bay are numbered as follows:

725140 - 725145 inclusive 731201 - 731208 inclusive

O N T A R l O'——— ———— ——'

100 miles

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for BATTLE ENERGYLocation Mop

JULY 1984Drawn:

SO ml.Approved:

N.T.S.: Fit*: M-61

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

BATTLE ENERGY CORPORATION

CLAIM LOCATION MAP

- 3 -

Topography and Vegetation

Topography in the area has very little relief with most of

the terrain comprising large flat-lying swampy areas. Bedrock is

not usually exposed in extensive flat-lying areas and a lichen

and moss cover is cannon on all rock surfaces. Some of the

property consists of low rolling ridges where outcrop does occur.

Valleys down to 100 feet have been eroded by the water courses

which eventually drain southwesterly into Lake Superior via Cedar

Creek and Philips Creek. In the northeastern part of the

property, Philips Creek flows westerly into Cedar Creek in the

west part of the property which then flows northerly into the

Black River and finally to the Pic River. In these drainage

valleys, overburden is thick and rock exposures are few.

Scattered outcrop comprises less than 5% of the property.

Outcrop areas are widely interspersed with swampy areas. A thick

forest of cottonwood, birch and aspen mixed with the younger

black spruce and balsam cover the property. Alders are thick in

the creek valleys and clearings.

Previous Exploration

Prior to the Hemlo staking rush, sporadic exploration

activity has been conducted in the Hemlo-Manitouage area, from

the early 1900's, until as recently as 1978. Ihe area was

included in a 1932 geological survey by J.E. Thomson for the

Ontario Department of Mines. V.G. Milne and assistants mapped

- 4 -

the area north of the south boundary of the property, in 1965 and

1966, for the Ontario Geological Survey. The area south of the

property was included in a 1978 survey by T.L. Muir and L.

Lafleur, for the Ontario Geological Survey.

In the 1920's, prospecting in the area resulted in J. Lecour

sinking a number of test pits on a mineralized shear zone

(currently the Bel-Air Resources Limited property).

Exploration activity in the area in 1945 indicated scattered

gold mineralization near Moose Lake, some 3 miles east, and a

little north of the hamlet of Hemlo.

Sporadic exploration continued for some 35 years until in

1981, when International Corona Resources Limited announced the

discovery of a significant gold deposit. This announcement

spurred the staking of over 7000 claims, in the area, twenty of

which encompass the property of Battle Energy Corp. Exploration

Diamond drilling over the last three years has shown the Hemlo

gold deposit to be more or less a stratabound deposit consisting

of over 75 million tons of ore grading at least 0.20 ounces of

gold per ton. There are no current assessment records available

to the writer concerning the nature or extent of any exploration

work undertaken prior to Battle Energy Corporation acquiring the

property.

In August, 1982, Mid Canada Exploration conducted a

magnetometer survey and a vertical loop electromagnetic survey

over the entire Battle Energy Corporation property. In the fall

of 1983, Corporate Oil and Gas Ltd. conducted a program of

- 5 -

geological mapping, soil geochemistry, and test IP surveying.

The results of this program are covered in reports by Wilson,

H.D.B., (1983).

RB3ICNAL GEOLOGY

The Battle Energy Corporation property is located within a

portion of the Schreiber - Marathon greenstone belt in the

Superior Province of the Canadian Shield. The property lies

within an Archean sequence of metavolcanic and metasedimSntary

rocks that extends from Lake Superior, near Heron Bay,

east-northeast across the Hemlo gold area. This sequence, called

the Heron Bay Sequence, is comprised mainly of metamorphosed,

intermediate to felsic calc-alkalic pyroclastic rocks, related

sedimentary rocks and high-iron tholeiitic basalt flows (Muir

1982). The property is situated within the Hemlo Map Sheet, Mapf

2452 (see enclosed portion, Figure 3), which was mapped by T.L.

Muir and associates for the Ontario Geological Survey in 1982.

The Heron Bay Sequence bends around the Cedar Lake Pluton to

the east-southeast and northeast. The northeast corner of the

property is intruded by this hornblende - biotite - granodiorite

pluton. Within the Heron Bay Sequence, a poorly defined lateral

facies change occurs from west to east from predominantly

pyroclastic rocks to mainly well-bedded and poorly-bedded

metasediments derived largely from unlithified volcanic and

epiclastic volcanic material (Muir 1982). Relatively large

"lenses" of mafic metavolcanics are present throughout the Heron

- 6 -

Bay Sequence.

Later granodiorite bodies have intruded all of the

aforementioned rocks. The Pukaskwa Gneissic Complex, which

consists of foliated trondhjemite, intrudes the southern and

southeastern parts of the map-area while Heron Bay and Cedar Lake

granodiorite bodies have intruded the southwest and northeast

parts of the map area respectively. The Gowan Lake Pluton

intrudes the northwest part of the map area which consists of

massive quartz monzonite.

All of the Early Precambrian rocks have been intruded by

later diabase dikes. Later lamprophyre dikes have locally

intruded the volcanic and sedimentary rocks.

PROPERTY GEOLOGY

The Battle Energy Corporation property is underlain by an

Archean metasedimentary rock complex which forms the hanging wall

sediments of the Hemlo gold deposit.

The Archean metasediment s have been intruded by diabase,

mafic and felsic dikes and/or sills. In the northeastern and

western part of the property they are intruded by the Cedar Lake

Pluton which is granodioritic in composition.

The bulk of the property is underlain by metasediments which

range from quartz wackes, (Unit 3d) to psammitic banded siltstone

and wacke, (Unit 3b). The quartz wacke (Unit 3d), occurs as

lenses or pods within the banded silstone-wacke, (Unit 3b), which

MIDDLE TO LATE PRECAMBRIAN (PROTEROZOIC)

MAFIC INTRUSIVE ROCKSJJ UnsubOmded Tie EQuigranutai diabase lib Porphyritic (plap&zase) tl' lie Ouam diabase

INTRUSlVl COH1ACT

CEDAR LAKE PLUTON

8 UnsubdvldedSa Hornblende-biotne granodiorite

INTERMEDIATE TO FELSIC METAVOlCANlCS

UnsubdividedFoliated Hows, lullsPillowed HowsJut!, lapilMufl, minor crystallullPyroclastic breccia, lull brecciaMigmstaed lullGarnet bearing

E J Unsubdividedle Dark green foliated Hows1b Dark green amphiboMaed. foliated

Howsle Pillowed HowsTd Variolitic Hows le Pyroclastic breccia, lull-breccia11 Jutl, lapitii-lullIp Laminated epidote layersl h Medium-tc-coarse-grained1j Garnet-bearingIk Migmal&edilows, lulls

TMnty-lammatec anilite* Tnickiy-laminates ic thinly-bedded e'KOsic wacke ana s/ftslone* Thickly-iaminatec to thinly-bedded arkosic wacke ami siltstone* Medium-bedded t'xosic wackef Massive lo poorfy-bedded wacke Ihinly-laminated to thinly-bedded siltstone, argillrte

3g Muostone siltstone, argillite 3h Very thinly-bedded, migmataed

wacke, siltstoneMagnetite-bearing (less than WU) Garnet-muscovtit-biotiie schist

3m GBrnet-stBurolrie-bioliie schist 3n Sillirriinite-andtiusiie-cordierite-

biotite schist Sp Gatnet-anlhophytie-biot'ite schist

3c

3d 3e 31

3j 3k

0,6 JmlH

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

forBATTLE ENERGY CORPORATION

Til k

REGIONAL GEOLOGY MAP

Date: July 1984Prawn: c.0.

l"'1/2 miteFIG. 3

N.T.S.:Fik: M-61

- 7 -

occurs throughout the property.

These rocks are crosscut by felsic, diabase and lamprophyre

dikes throughout the property.

Table of Lithologies

QuaternaryMiddle to Late Precambrian

Alkalic Intrusive Rocks

Unit 12a Biotite LamprophyreIntrusive Contact

Unit lla Equigranular DiabaseIntrusive Contact

Early Precambrian (Archean)Intermediate to Felsic Intrusive Rocks

Unit lOa Feldspar Porphyry Sill Unit lOb Aplitic Dike

Cedar Lake Pluton

Unit 9a Hornblende - Biotite Granodiorite

Metasediments

Unit 3d Quartz WackeUnit 3b Biotitic Siltstone and Wacke

Unit 12a Biotite Lamprophyre Dike?

This member outcrops in only one locality on the property.

The outcrop is weathered speckled dark grey to black. The matrix

is fine to medium-grained consisting of biotite and chlorite

flakes and fine-grained anhedral opaque minerals. Considerable

white carbonate (calcite) is also present.

Unit lla Equigranular Diabase

Throughout the property diabase dikes are found intruding

the metasediments. The diabase weathers a dark brown colour, and

- 8 -

on fresh surfaces, varies from dark grey black to greenish black.

In some of the more medium-grained varieties, sericitized

plagioclase imparts a lighter green colour to the rock.

The dikes range in width from 20 feet to 100 feet and within

the property can be followed for distances of up to 600 feet.

The dikes trend most commonly northwest.

Unit IQa Feldspar Porphyry Sill

This unit was seen in only a single outcrop at approximately

line 40W, 40 feet south of the baseline. The sill was

approximately three feet wide. The rock consists of

approximately 251 subhedral to euhedral feldspar phenocrysts set

in a pale green, felsic, aphanitic matrix. The phenocrysts were

moderately altered to sericite and epidote. Finely disseminated

pyrite, comprising S-4% of the rock, occurs in this unit. A

sample was taken at this location and was sent to Bell-White

Analytical Labs for geochemical analysis for gold. The rock

returned 3ppb in gold and is not considered anomalous.

Unit IQb Aplitic Dike

This unit was seen in only a single outcrop in the central

part of the property. This dike may be related to the local

pluton (Cedar Lake Pluton Unit 9a). The matrix is composed of

anhedral plagioclase phenocrysts in a finer-grained felsic

matrix. The plagioclase has been partly altered to hematite and

subsequently cause a pink weathered surface. Trace amounts of

biotite occurs as very fine flecks.

- 9 -

Unit 9a Hornblende Biotite Granodiorite

The Horneblende-biotite granodiorite (Cedar Lake Pluton) was

seen in the north eastern corner of the property and west of

Cedar Creek intruding the metasediments. The rock weathers light

grey to white to pink (where hematitic), and is generally medium

grained comprised of quartz and feldspar up to l-3rtm in size.

Hornblende and biotite which comprise lS-20% of the rock are the

main mafic constituents. Accessory magnetite is also present.

Unit 3d Quartz Wacke

This unit is seen as lenses throughout the property and is

interbedded with the banded siltstones (Unit 3b). The rock

weathers to a white grey colour and is fine to medium grained,

poorly bedded to massive. Fresh surfaces vary from a pale grey

to dark grey colour. The rock is composed of subrounded quartz

and feldspar grains with up to 5% fine biotite flakes. The rock

is quartz rich and weathers resistantly as a result. The rock

appeared to be slightly foliated in places, with biotite flakes

weakly aligned parallel to foliation. Trace amounts of pyrite

were seen within this unit.

Unit 3b Biotitic Siltstone and Wacke

This unit occurs as a fairly distinctive formation

throughout the property. It consists of a grey brown to dark

brown, well foliated biotitic siltstone interbedded with and/or

grading into, a slightly coarser-grained wacke. The rock varies

from massive to well laminated, with weathered surfaces dark grey

- 10 -

to light brown in colour. The siltstone is comprised

predominently of fine quartz and feldspar (up to 7(^ or 8(^) with

brown to black biotite comprising from 201 to 301 of the rock.

The rock is compact, even textured, with fine, dark and lighter

coloured laminae, due to different proportions of biotite. Thin

(less than l cm) felsic quartz and feldspar rich bands were seen

in several localitites. The siltstone was seen interbedded with

a coarser-grained wacke which is dark grey in colour with the

occassional quartz eye. Trace amounts of pyrite were seen within

this unit.

Structural Geology and Metamorphism

Few primary features were observed within the metasediments

on the Battle Energy property that could be used to interpret the

structural geology of the map area. The foliation (bedding?) was

cormonly between OSO0 and 0900 . Recrystallization in the finer

grained si 11stones, has obliterated, in part, any primary

structures indicative of stratigraphic tops.

CONCLUSIONS AND REOCMENDATICNS

The presence of metasediments similar to the Hemlo - type

metasediments and the general lack of outcrops make this property

worthy of a more complete program in search for economic gold

mineralization.

Due to the thick overburden cover, an extensive IP survey

over the existing lines using an "a" spacing of 100 feet with n s

- 11 -

1,2,3, should be conducted to explore to bedrock on all areas of

the property to test for areas of disseminated sulfide

mineralization. This type of mineralization hosts the large

Hemlo deposits to the south of the Battle Energy Corporation.

Evaluation of the IP data may lead to the recommendation of a

small drill program to test any anomalies considered to be

significant.

Respectfully Submitted,

Nadia Caira, B.Se.

- 12 -

tREFERENCES

CARLSON, H.D.1982 Report on Geophysical Survey on the property of

Battle Energy Corporation.

MILNE, V.G.1968 Geology of the Black River Area; Ontario Department

of Mines, Geological Report 72.

MUIR, T.L.1982 Geology of the Hemlo, District of Thunder Bay,

Ontario Geological Survey, Toronto, Report 217.

PATTERSON, G.C. ^ Exploration History in the Hemlo Area, Resident Geologist, Ontario Ministry of Natural Resources, Thunder Bay, Ontario.

TITTLEY, H.Z.1983 Report on Geophysical Surveys on the Property of Battle

Energy Corporation.

WILSON, H.D.R.1983 Report on Geochemical and Geological Survey of the

Battle Energy Corporation Option, Hemlo Area, District of Thunder Bay, Ontario.

WILSON, H.D.R.1983 Induced Polarization Survey of the Battle Energy

Corporation Option, Hemlo Area, District of Thunder Bay, Ontario for Corporate Oil and Gas.

CERTIFICATICN

I, Nadia M. Caira, B.Se., of Tinmins, Ontario, certify that:

1. I am a graduate of the University of British Columbia, Vancouver, B.C., with a B.Se. degree in Geology obtained in 1981.

2. I have been practising my profession in Canada since 1981.

3. I have no direct or indirect interest in the properties, leases or securities of Battle Energy Corporation nor do I expect to receive any.

Dated this August 15, 1984, Tinrnins, Ontario.

Nadia M. Caira, B.Se.

N D I

rv*~V'^. Y -*—*T y h ^

————————————————— ••••^^^^^^^•••••••^^•^^^^•^•^•••••il^l^MHMBHIM^HHII

^ BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HA1LEYBURY. ONTARIO TEL: 672-31O7

(flrriifirui? nf AnahjstflNO. B792-84

SAMPLE (S) OF:

SAMPLE (S) FROM:

Rock (1)

DATE: August 2, 1984

RECEIVED: July, 1584

Mr. IC.T' CcsterB. E. K: c c 2 e-L on Exruc r 5 tier, Services

GcJ 67rcb

G27053

IK * CCC-s;^* '-C t V.:TK l. CN'C--I 5T i E'.'FHtr KTRTH A^'fPlC**. C'.-no^. L"*lliS IT IS f *-C C i r 1C* LLV f.-**Et-f.-r'wii toi: *'-'- fi.vtfc \*.ivti ft'ct-rr cs'IhtSl I-.tCTi h*VT I-CT ft?N JT.'L'fltt TC CCM^t*.-l-Tl J Df LCltti *'-- f.k".l I'-r-tUNT H, 1HI t IRt

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5ELL-\VHITE ANALYTICAL LABORATORIES LTD.

42C13SW0161 2.7444 WABIKOBA LAKE 020

INDUCED POLARIZATION SURVEY

on the

BATTLE a^ERGY CORPORATION

Hemlo Area PropertyThunder Bay Mining Division

Ontario

RECEIVED:NOV 2 J J984

MINING LANDS SECTION

byR.Bruce Durham,

Consulting Geologist

Robert S. Middleton Exploration Services Inc.P.O. Box 1637

Timnins, OntarioP4N 7W8

September 11, 1984

42C13SWei61 2.7444 WABIKOBA LAKE

TABLE OF CONTENTS

Page

INBRODUCriCN. . . . . . . . . . . . . . . . . . . . . . l

LOCATION and ACCESS . . . . . . . . . . . . . . . . . . l

PROPERTY. . . . . . . . . . . . . . . . . . . . . . . . 2

TOPOGRAPHY and VEGETATION . . . . . . . . . . . . . . . 2

PREVIOUS EXPLORATION. . . . . . . . . . . . . . . . . . 2

PROPERTY GEOLOGY. . . . . . . . . . . . . . . . . . . . 4

SURVEY PROCEDURE, STATISTICS and INSTRUMENTATION. . . . 5

INTERPRETATION. . . . . . . . . . . . . . . . . . . . . 5

CONCLUSIONS and RECOMMENDATIONS . . . . . . . . . . . . 6

REFERENCES. . . . . . . . . . . . . . . . . . . . . . . 8

CERTIFICATION

LIST OF FIGURES

Figure l Property Location Map l" = 25mi.

Figure 2 Claim Location Map 1:50,000

Figure 3 Regional Geology l" - 1/2 mi.

Figure 4 Geology Showing IP Anomalies l" ~ 200'

APPENDIX

Specifications for IPR 11 IP Pseudosections

020C

- l -

INITOPUCTION

An Induced Polarization survey was completed during July and

August 1984 on the Battle Energy Corporation 14 claim property

located approximately 3 miles northeast of the Hemlo gold

deposit. This survey was undertaken as follow-up to a test

program of IP surveying which was done over two lines in January

1984 by Phoenix Geophysics of Toronto using a wide (200') "a"

spacing. Geological mapping and geochemical survey had been done

on the property prior to this survey.

The purpose of this IP survey was to attempt to locate

disseminated pyrite mineralization which might host gold

mineralization similar to the disseminated sulfide zones at the

Hemlo gold deposit south of the property.

LOCATION and ACCESS

The Battle Energy Hemlo area is located approximately 20

miles east of the town of Marathon in the Thunder Bay Mining

Division of Ontario.

The property which lies 2-3 miles northeast of the now well

known Hemlo gold deposit is accessible via a l mile bush road

which leads westerly from Highway 614 approximately 2 miles north

of the Highway 17 - 614 junction. Hie bush road ends in a gravel

pit near line 24W at 21S.

... O N TA RIO

T HUNDER y BAY Dist

Nip'jOfi

50 100 miles

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

tor BATTLE ENERGYLocation Mop

1984 N.T.S.:Approxd: File: M-61

xx-y^i

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

BATTLE ENERGY CORPORATION

CLAIM LOCATION MAP

- 2 -

PROPERTY

The 14 contiguous unpatented mining claims located in the

Thunder Bay mining division are numbered as follows:

TB 725140 - 725145 and

TB 731201 - 731208

TOPQGaRAPHY and VBGEIATION

The property lies in an area of low relief, varying only

between low lying swampy areas and low ridges and valleys along

creek beds.

The area is drained via a network of small creeks which flow

into the Black River which merges with the Pic River just above

-^ its entrance to Lake Superior, near the village of Heron Bay.

A thick forest of poplar, birch, spruce and balsam covers

the higher areas of the property while thick alders and spruce

dominate the swampy areas.

PREVIOUS EXPLCRATICN

The following is a brief summary of previous exploration in

the area from an August 15, 1984 Geological report on the

property (Caira, N., 1984).

"Prior to the Hemlo staking rush, sporadic exploration

activity has been conducted in the Hemlo-Manitouage area,

- 3 -

from the early 1900's, until as recently as 1978. The area

was included in a 1932 geological survey by J.E. Thomson for

the Ontario Department of Mines. V.G. Milne and assistants

mapped the area north of the property, in 1965 and 1966, for

the Ontario Geological Survey. The area was included in a

1978 survey by T.L. Muir and L. Lafleur for the Ontario

Geological Survey.

In the 1920's, prospecting in the area resulted in J.

Lecour sinking a number of test pits on a mineralized shear

zone (currently the Bel-Air Resources Limited property).

Exploration activity in the area in 1945 indicated

scattered gold mineralization near Moose Lake, some 3 miles

east, and a little north of the hamlet of Hemlo.

Sporadic exploration continued for some 35 years until

1981, when International Corona Resources Limited announced

the discovery of a significant gold deposit. This

announcement spurred the staking of over 7000 claims in the

area, fourteen of which encompass the property of Battle

Energy Corporation. Exploration diamond drilling over the

last three years has shown the Hemlo gold deposit to be more

or less a stratabound deposit consisting of over 75 million

tons of ore grading at least 0.20 ounces of gold per ton.

There are no current assessment records available to

the writer concerning the nature or extent of any

- 4 -

exploration work undertaken prior to Battle Energy

Corporation acquiring this property.

In January 1983, Mid Canada Exploration conducted a

magnetometer survey and a VLF electromagnetic survey over

the entire Battle Energy Corporation property. In the fall

of 1983, geological mapping, soil geochemistry, and test IP

surveying. TYie results of this program are covered in

reports by Wilson, H.D.B., (1983)."

PROPERTY GEOLOGY

Wilson (1983) describes the bedrock geology as consisting of

quartz-feldspar biotite metasediments with more sericitic

interbeds. One outcrop of granite gneiss and one outcrop of

diabase were also noted in the course of the survey.

Caira (1984) reports that the property is underlain by an

Archean metasedimentary complex which has been intruded by

diabase, mafic, and felsic dikes and/or sills.

A limited exploration program consisting of a soil

geochemistry, 2 lines of IP and cursory geological mapping was

carried out by Corporate Oil fc Gas between September 13 and

October 10, 1983. The results of these programs are discussed in

December 1983 reports by Harry D.B. Wilson.

! TO LATE PRECAMBRIAN (PROTEROZOIC)

MAFIC INTRUSIVE ROCKSINTERMEDIATE TO FELSIC

METAVOLCANICS

II UnsubdmdedTlc fQuiprenular diabaselib Porphyritic (piapoclase) ttioixtselie OuaW diabase

*."TRUS'Vf CCWIACT

CEDAR LAKE PLUTON

9 UnsubdMded9a Hornblende-Mottle granodiorite

? UnsubdivrdedIs Foliated Hows, tuffs2b Pillowed Hows2c Ti/ff. lapilli-Mt. minor crystaltutlid Pyroclastic breccia, lull brecciale MigmetitedtuttM Garnet bearing

IJBJbJc Id

•leII'C JhV J*

UnsubdhfideaDark green located HowsDark green amphiboMaed, MutedHowsPillowed HowsVenal/tic HowsPyroclastic breccia, lull-breccialull, lapiiii-tutlLaminated epidote layersMedium-lo-coarse-greinedGarnet-bearingMigmataed Hows, Mis

L'nsuJxJ'i'iOetfThinly-laminated argillite*

3b Jmckly -laminated to thinly-beddedt'Kosic wacke tne siltstone*

3c Thickly-iawine'ed to thinly-beddederkosic wacke and siltstone*

3d Medium-bedded arkosic wacke* 3e Massive to poorly-bedded wacke 31 Ihmly-laminaled to thinly-bedded

siltstone, argillite 3g Mudstone siltstone, argillite 3h Very thinly-bedded, migmatired

tucke. siltstone3i Magnetite-bearing (less then ID*,) 3k Garnet-musccvtt-biotite schist 3m Gtrnet-staurotrte-biotiie schist 3n Si/iimtnite-anoeiusite-cordierrle-

t-'Otiie schist Sp Cernet-anthoprtyUfie-biofite schrst

O.P J md*

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

tor BATTLE ENERGY CORPORATIONTitle

REGIONAL GEOLOGY MAP

Date: July 1964Drawn: e.g.

l"* l/SZmlteFIG. 5

N.T.S.:File: M -61

- 5 -

SURVEY PROCEDURE, STATISTICS, and INSTRUMENTATION

The Induced Polarization survey carried out by Robert S.

Middleton Exploration Services Inc. between July 20 and July 29,

1984 was undertaken to search for disseminated sulfide zones

which might be gold bearing.

A Scintrex IPR-11 receiver and a Scintrex TSQ-3 transmitter

were used to obtain the data. A pole - dipole array with an "a"

spacing of 100' was selected for this reconnaissance type survey.

Resistivity and chargeability values were obtained for 11=1,2,

and 3 and plotted in pseudo section form at a scale of l" = 100'.

The four man crew was comprised of David Hurst, John Scott,

Jim Bald and Francois Bonhormie. A total of 603 readings were

taken at 201 stations and 19,500' of grid line was covered by the

survey.

INTERPREEATICN

Rather high resistivity values encountered throughout the

property are probably a reflection of the effect of

mid-amphibolite facies grade metamorphism on the pelitic

metasediments which typically give rather low resistivity values.

The background chargeability values are also elevated as a

result. Only one zone of high chargeability is thought to be

caused by sulfide and/or graphite mineralization in bedrock.

- 6 -

This anomaly, which is located on line 40+OOW from 3+50S to 5+OOS

gave chargeability values three times background. The anomaly

appears to be located under less than 50' of overburden cover.

No estimate of the strike direction or length of the anomaly can

be determined as it was only detected on one line.

Since lines were read 800' east and west of line 40+OOW, the

maximum length of the anomaly would be somewhat less than 1600

feet assuming a more or less east west strike (i.e. parallel to

schistosity).

OCmJUSICNS and REOM1ENDATICNS

The work done to date on the Battle Energy Corporation

Property has consisted of a rather comprehensive program of

gephysics, soil geochemistry and geological mapping. While a

number of anomalous features were outlined by the preliminary

geophysical surveys, the only target which was detected by the

Induced Polarization survey, and considered to be significant,

was the one located on line 40+OOW between 3+50 and 5+OOS. While

no strong alteration zones were noted in this area in the course

of geological mapping there are no outcrops within several

hundred feet of the anomaly. In the area of the Hemlo deposit

alteration features are restricted to an area only a few tens of

feet strat igraphically above, and often less than 100 feet

stratigraphically below the ore zone. While it is thought that

- 7 -

the anonnalous IP response is caused by pyrite and/or graphite

mineralization within the metasediment s, the zone should be drill

tested at some time.

This drill test could be accomplished with one 500' diamond

drill hole collared at 6+OOS on line 40+OOW and drilled south at

509 . The total cost of such a hole and associated supervision,

assaying, core logging, mobilization, etc would be in the range

of S20,000. It would be advisable to try to co-ordinate the

drilling of this one hole with another small program in the area

to try to cut mobilization charges.

Respectfully Submitted,

R.Bruce Durham, Consulting Geologist

- 8 -

REFERENCES

CAIRA, Nadia1984 Geological Report on the Battle Energy Corporation

Property, Hemlo Gold Area, District of Thunder Bay, Ontario.

CARLSON, H.D.1982 Report on Geophysical Survey on the property of

Battle Energy Corporation.

MILNE, V.G.1968 Geology of the Black River Area; Ontario Department

of Mines, Geological Report 72.

MUIR, T.L.1982 Geology of the Hemlo Area, District of Thunder Bay,

Ontario Geological Survey, Toronto, Report 217.

PATTERSON, G.C.Exploration History in the Hemlo Area, Resident Geologist, Ontario Ministry of Natural Resources, Thunder Bay, Ontario.

TITTLEY, H.Z.1983 Report on Geophysical Surveys on the Property of Battle

Energy Corporation.

WILSON, H.D.R.1983 Report on Geochemical and Geological Survey of the

Battle Energy Corporation Option, Hemlo Area, District of Thunder Bay, Ontario.

WILSON, H.D.R.1983 Induced Polarization Survey of the Battle Energy

Corporation Option, Hemlo Area, District of Thunder Bay, Ontario for Corporate Oil and Gas.

CERTIFICATION

I, R. Bruce Durham of Timmins, Ontario certify that:

I am a graduate of the University of Western Ontario having obtained a Bachelor of Science degree in Geology in 1976.

I have been practising my profession primarily in Canada since 1976.

3. I have no direct or indirect interest in the properties, leases, or securities of Battle Energy Corporation, Hemlo Area Property, nor do I expect to receive any.

Dated this September 11, 1984 at Tinmu'ns, Ontario.

R.Bruce Durham, B.Se.

N D I

New from Scintrexff v"lj K- i b

Broadband Time Domain !P Receiver

Function

The IPR-11 Broadband Time Domain IP Receiver is principally used in electrical (EIP) and magnetic (MIP) induced polarization sur veys for disseminated base metal occurrences such as porphyry copper in acidic intrusives end lead-zinc deposits in carbonate rocks. In addition, this receiver Is used in geoelectrical surveying for deep groundwater or geothermal resources. For these latter targets, the induced polarization measurements may be as useful as the high accuracy resistivity results since It often happens that geological materials have IP contrasts when resistivity contrasts are absent. A third application of the IPR-11 is in induced polarization research projects such as the study of physical properties of rocks.Due to its integrated, microprocessor-based design, the IPR-11 provides a large amount of induced polarization transient curve shape information from a remarkably compact, relia ble and flexible format. Data from up to six potential dipoles can be measured simultane ously and recorded in solid state memory. Then, the IPR-11 outputs data as: 1) visual dig ital display, 2) digital printer profile or pseudo- section plots, 3) digital printer listing, 4) a cassette tape record or 5) to a modern unit for transmission by telephone. Using software available from Scintrex, all spectral IP and EM coupling parameters can be calculated on a desk top or mainframe computer.Because it can measure, record, calculate resistivity and output useful, broadband data in the field which are compatible with later computer processing using Scintrex software, the IPR-11 is the heart of a new, highly effi cient, integrated system for conducting spec tral induced polarization surveys.The IPR-11 is designed for use with the Scinr trex line of transmitters, primarily the TSQ ser ies current and waveform stabilized models. Scintrex has been active in induced polariza tion research, development, manufacture, consulting and surveying for over thirty years and offers a full range of time and frequency domain instrumentation as well as all accesso ries necessary for IP surveying.

Major Benefits

Following are some of the major benefits which you can derive through the key features of the l PR-11.Speed up survey*. The IPR-11 is primarily designed to save you time and money in gath ering spectral induced polarization data.For example, consider the advantage in gra dient, dipole-dipole or pole-dipole surveying with multiple 'n' or 'a' spacings, of measuring up to six potential dipoles simultaneously. If the specially designed Multidipole Potential Cables are used, members of a crew can pre pare new dipoles at the end of a spread while

measurements are underway. When the obser vation is complete, the operator walks only one dipole length and connects to a new spread leaving the cable from the first dipole for retrieval by an assistant.Simultaneous multidipole potential measure ments offer an obvious advantage when used In drillhole logging with the Scintrex DHIP-2 Drillhole IP/Resistivity Logging Option.The built-in, solid state memory also saves time. Imagine the time that would be taken to write down line number, station number, transmitter and receiver timings and other header Information as well as data consisting of SP, Vp and ten IP parameters for each dipole. With the IPR-11, a record is filed at the touch of a button once the operator sees that the measurement has converged sufficiently.The IPR-11 will calculate resistivity for you. Further time will then be saved when the IPR- 11 begins plotting your data in profile or - pseudo-section format in your base camp on a digital printer. The same printer can also be used to make one or more copies of a listing of the day's results. If desired, an output to a cassette tape recorder can be made. Or, the IPR-11 data memory can be output directly into a modem, saving time by transmitting data to head office by telephone line and by providing data which are essentially computer compatible.

If the above features won't save as much time as you would like, consider how the operator will appreciate the speed In taking a reading with the IPR-11 due to: 1) simple keyboard control, 2) resistance check of six dipoles simultaneously, 3) fully automatic SP buckout, 4) fully automatic Vp self ranging, 5) fully automatic gain setting, 6) built-in calibration test circuits, and 7) self checking programs. The amount of operator manipulation required to take a great deal of spectral IP data is minimal.

Compared with frequency domain measure ments, where sequential transmissions at dif ferent frequencies must be made, the time domain measurement records broadband information each few seconds. When succes sive readings are stacked and averaged, and when the pragmatic window widths designed into the IPR-11 measurement are used, full spectral IP data are taken in a minimum of time.Improved Interpretation of data. The quasi- logarithmically spaced transient windows are placed to recover the broadband information that Is needed to calculate the standard spec tral IP parameters with confidence. Scintrex offers its SPECTRUM software package which can take the IPR-11 outputs and generate the following standard spectral IP parameters: m, chargeability; T, time constant and C, exponent. :

Broadband Time Domain IP Receiver

Interpretability of spectral IP data are improved since time domain measurements are less affected by electromagnetic coupling effects than either amplitude or phase angle frequency domain measurements, due to the relatively high frequencies used in the latter techniques. In the field, coupling free data are nearly always available from the IPR-11, by simply using chargeability data from the later transient windows. Then, in the base camp or office, the Scintrex SPECTRUM computer program may be used to resolve the EM com ponent for removal from the IP signal. The electromagnetic induction parameters may also be interpreted in order to take advantage of the information contained in the EM component.A further advantage of the IPR-11 in interpret ing spectral IP responses is the amount of data obtainable due to the ability to change transmitted frequencies (pulse times) and measurement programs by keypad entry.Enhance signal/noise. In the presence of ran dom (non-coherent) earth noises, the signal /noise ratio of the l PR-11 measurements will be enhanced by JR where N is the number of individual readings which have been averaged to arrive at the measurement. The IPR-11 automatically stacks the information contained in each pulse and calculates a running aver age for Vp and each transient window. This enhancement is equivalent to a signal increase of JR, or a power increase of N. Since N can readily be 30 or more (a 4 minute observation using a 2 second on/off waveform), the signal /noise improvement realized by the IPR-11 cannot be practically achieved by an increase in transmitter power. Alternatively, one may employ much lower power transmitters than one could use with a non-signal enhancement receiver.The automatic SP program bucks out and cor rects completely for linear SP drift; there is no residual offset left in the signal as in some pre vious time domain receivers. Data are also kept noise free by: 1) automatic rejection of spheric spikes, 2) 50 or 60 Hz powerline notch filters, 3) low pass filters and 4) radio fre quency (RF) filters. In addition, the operator has a good appreciation of noise levels since he can monitor input signals on six analog meters, one for each dipole. Also, with the Optional Statistical Analysis Program, he can monitor relative standard error continuously on the digital display and then file these calcu lations in the data memory when the observa tion is complete.Noise free observations can usually be made using the self-triggering feature of the IPR-11. The internal program locks into the waveform of the signal received at the first dipole (near est a current electrode) and prevents mistrig- gering at any point other than within the final 2.5 percent of the current on time. In particu larly noisy areas, however, synchronization of

the IPR-11 and transmitter can be accomp lished either by a wire link or using a high sta bility, Optional Crystal Clock which fits onto the lid of the instrument.Reduce Errors. The solid state, fail-safe memory ensures that no data transcription errors are made in the field. In base camp, data can be output on a digital printer or a read-after-write cassette tape deck and played back onto a digital printer for full verification. The fact that the IPR-11 calculates resistivity from recorded Vp and l values also reduces error.

The self check program verifies program integrity and correct operation of the display, automatically, without the intervention of the operator. If the operator makes any one of ten different manipulation errors, an error, mes sage is immediately displayed.The Multidipole Potential Cables supplied by Scintrex are designed so there is no possibility of connecting dipoles to the wrong input ter minals. This avoids errors In relating data to the individual dipoles. The Internal calibrator assures the operator that the instrument is properly calibrated and the simple keypad operation eliminates a multitude of front panel switches, simplifying operation and reducing errors.

Features

Six Dipoles Simultaneously. The analog input section of the IPR-11 contains six identicaj,.dif- ferential inputs tc accept signals from up to six individual potential dipoles. The amplified"- analog signals are converted to digital form, multiplexed and recorded with header infor mation identifying each group of dipoles."; Custom-made multidipole cables are available for use with any electrode array.Memory. Compared with tape recording, the IPR-11 solid state memory is free from prob lems due to dirt, low temperatures, moving parts, humidity and mechanical shock. A bat tery Installed on the memory board ensures memory retention if main batteries are low or if the main batteries are changed. The following data are automatically recorded in the memory for each potential dipole: 1) receiver timing used, 2) transmitter timing used, 3) number df cycles measured, 4) self potential (SP), 5) primary voltage (Vp) and 6) ten transient IP windows (Mj). In addition, the operator can enter up to seventeen, four digit numerical headers which will be filed with each set of up to six dipole readings. Headers can include, for example, line number, station number, operator code, current amplitude, date, etc.In the standard data memory, up to 200 poten tial dipole measurements can be recorded. Optional Data Memory Expansion Blocks can be installed in the IPR-11 to increase memory capacity in blocks of about 200 dipoles each to a total of approximately 800 dipoles. Memory capacities will be reduced somewhat if the Optional Statistical Analysis Program is used.

Automatic SP Correction. The initial self potential buckout is entirely automatic - no adjustment need be made by the operator. Then, throughout the measurement, the IPR- 11 slope correction software makes continual corrections, assuming linear SP drift during a transmitted cycle. There is no residual SP offset included in the chargeability measure ment as in some previous time domain receivers.

Automatic Vp Self Ranging. There is no man ual adjustment for Vp since the IPR-11 auto matically adjusts the gain of its input amplifi ers for any Vp signal in the range 100 microvolts to 6 volts.Spheric Noise Refection. A threshold, adjusta ble by keypad entry over a linear range of O to 99, is used to reject spheric pulses. If a spheric noise pulse above the set threshold occurs, men the IPR-11 rejects and does not average the current two cycles of information. An alarm code appears on the digital display. If the operator continues to see this alarm code, he can decide to set the threshold higher.Powerilne and Low Pass Filter. An Internal switch is used to set the IPR-11 for either 50 or 60 Hz powerline areas. The notch filter is automatically switched out when the 0.2 second receive time is used since the filters would exclude EM signals.RF Filter. An additional filter in the input cir cuits ensures that radio frequency Interference is eliminated from the l PR-11 measurement.Input Protection. If signals in excess of 6 V and up to 50 V are applied to any input circuit, zener diode protection ensures that no dam age will occur to the input circuits.

Synchronization. In normal operation, the IPR- 11 synchronizes itself on the received wave form, limiting triggering to within Z.6% of the current on time. However, for operation in locations where signal/noise ratios are poor, synchronization can be done either by running a cable from the transmitter or by using the Optional Crystal Clock which can be installed . in the lid of the IPR-11.Optional Statistical Analysis. As an option, the IPR-11 can be provided with software to do statistical analysis of some parameters. The relative standard error is calculated, displayed on the LCD display and may be recorded in data memory. The total capacity of data memory will be reduced, depending on the extent of statistical data recorded. If the Optional Statistical Analysis Program is chosen, some thought should be given to pur chasing one or more blocks of Data Memory Expansion.Software for EM Coupling Removal. In tran sient measurements, the EM coupling compo nent occurs closest to the current off time (i.e. it is primarily in the early windows). Thus, it is

usually possible to obtain coupling-free IP data simply by using the later windows of the IPR-11 measurement program. If, however, full spectral information is desired, the data from the early windows must be corrected for the EM component. This can be done with confi dence using a desk top of mainframe compu ter and the Scintrex SPECTRUM program.

Software for Spectral IP Parameters. Using the chargeability data from the ten quasi- logarithmically spaced IPR-11 windows, a desk top or mainframe computer and the Scin trex SPECTRUM program, spectral IP parame ters can be calculated. The basis for this calcu lation as well as for the EM coupling removal calculation is discussed in a technical paper by H.O. Seigel, R. Ehrat and l. Brcic, given at the 1980 Society of Exploration Geophysicists Convention, entitled "Microprocessor Based Advances in Time Domain IP Data Collection and In-Field Processing".

OperationIn relation to the efficiency with which it can produce, memorize, calculate and plot data, the IPR-11 is quite simple to operate, using the following switches and keypad manipulations.Power On-Off. Turned on to operate the instrument.Reset. Resets the program to begin again in very poor signal/noise conditions.Function Switch. Connects either the potential dipoles or the internal test generator to the

input amplifiers or cotonecttthe external cir cuit resistance checkxciroAry to the potential dipoles.

Keypad. The ten digit andafc.fonction keys are used to: 1) operate ifoajpstrument, 2) ente information, 3) retrievB4ioUtyred data item for visual display, and4ty,jtfjjptrt data on to a digital printer, casseltiM|m^c4c or modem. Examples of some (rfM^f^i^nipulations, most of which are ecdHt^K^tfS by three key strokes, follow. Eis th*0ert*tt1 entry key.A concise card showing** keypad entry codes is attached insitfefieTfd Of the IPR-11Example 1. "keying 99E*omcnands the battery lest. The result is shovwnxjoBieitiigilal display

•*'Example 2. Keying 90E tells trW1PR-11 to use the 0.2 second receive ttrme. 9f i*2 and 04 co respond to the three otfhtertimtff:Example 3. Keying 12M resuttsTri the display of the chargeability of (he first dipole, window number 2, during the measurement Similarly, 6SP or 4 Vp would result in the display of the SP value In the sixth dipole or Vp in the fourth dipole respectively.Example 4. Keying NNMNH. where N is a vari able digit, records an item of header informa tion. Seventeen such Stems can be entered with each file of up to six dipotes of data. :

~":9i

Example 5.73E, 74E or 75E aroused to ou v .a the data from the memory to trve digital printer or modern at 110,300 ex 1200 baud respectively. **'

Nominal total receive time: 0.2,1,2,4 sec.

MQ M1 M2 M3 M4

t t t t 6t

IPR- 1 1 transient windows

6t 6t Windo Width

3 Broadband Time Domain IP Receiver

IPR-11 Options

The following options are available for pur chase with the IPR-11.

Multidlpole Potential Cables. These cables are custom manufactured for each client, depend ing on electrode array and spacings which are to be used. They are manufactured in sec tions, with each section a dipole in length and terminated with connectors. For each observa tion, the operator need only walk one dipole length end connect a new section, in order to read a new six dipole spread. There Is no need to move the whole spread. The connectors which join the cables are designed so that there is no possibility of connecting the wrong dipole to the wrong Input amplifier. The out side jacket of these cables is rubber which is flexible at low temperatures. About 5 percent extra length is added to each section to ensure that the cable reaches each station.Data Memory Expansion Blocks. The standard data memory of the IPR-11 allows for data for up to 200 dipole measurements to be recorded, assuming a common header for six dipotes. Up to three additional memory blocks can be installed in the instrument, each of about 200 dipole capacity.Statistical Analysis Program. Sclntrex can pro vide, in EPROM, a statistical program to give real time calculations of relative standard error of one or more parameters.Crystal Clock. Scintrex can provide a high stability clock to synchronize the IPR-11 with a similar clock in the transmitter. This option is, however, only required for work In extremely noisy and/or low signal environments.

Software. Scintrex offers its SPECTRUM pro grams for EM coupling removal, calculation of EM induction factors and calculation of the spectral IP parameters.Digital Printer. The Scintrex DP-4 Digital Prin ter is a modified Centronics Microprinter with an RS-232C, 7 bit ASCII serial port. It is a self contained module, including 110/230 V power supply, control electronics and printing mech anism. It produces copy on aluminum coated paper by discharging low voltages through tungsten styli. Characters are formed from the appropriate dots of a 5 x 7 dot matrix. All 96 standard ASCII characters are available, the paper width Is 120 mm and 80 characters can be printed per line at a rate of up to 150 lines per minute.Cassette Tape Recorder. The MFE Model 2500 with read-after-write verification is recom mended. It has an RS-232C, 7 bit ASCII serial Interface with a recording format compatible with the Texas Instruments 'Silent 700' terminals.Modern. A number of modern units are available on the market which are compatible with the IPR-11. Scintrex would be pleased to recom mend or supply such equipment if required.

The cassette tape recording format of the IPR-11 Is compatible with the Texas Instruments 'Silent 700' terminals which can be used lor printing out, editing, copying tapes or transmitting data to a similar termi nal using telephone lines.

The takeouts o! the Multidlpole Potential Cables allow lor connection to a porous pot or other elec trode as well as tor connection, ol the next section ot cable, usually one dipole in length.

Memory Recall. Any reading fn memory can be recalled, by simple keypad entry, for inspection on the visual display. For example, the operator can call up sequential visual dis play of all the data filed for the previous obser vation or for the whole data memory.Carefully Chown Transient Windows. TheIPR-11 records all the Information that is really needed to make full interpretations of spectral IP data, to remove EM coupling effects and to calculate EM induction parameters. Ten quasi- logarithmically spaced transient windows are measured simultaneously for each potential dipole over selectable total receive times of 0.2,1.0,2.0 or 4.0 seconds.After a delay from the current off time of t, the width of each of the first four windows Is t, of the next three windows Is 6t and of the last three windows is 12t. The t values are 3,15,30 or 60 milliseconds. Thus, for a given dipole, up to forty different windows can be measured by using all four receive times. The only restric tion is, of course, that the current off time must exceed the total measuring time. Since t is as low as 3 milliseconds and since the first four windows are narrow, a high density of curve shape information is available at short times (high frequencies) where It Is needed for confident calculation of the spectral IP and EM coupling parameters.Calculates Resistivity. The operator enters the current amplitude and resistivity geometry (K) factors In header with each observation. If the K factors remain the same, only a code has to be entered with each observation. Then, using the recorded Vp values, the IPR-11 calculates the apparent resistivity value which can be output to the printer or cassette tape recorder.Normalizes for time and Vp. The l PR-11 divides the measured area In each transient window by the width of the window and by the primary voltage so that values are read out in units of millivolts/volt (mils).Signal Enhancement. Vp and M values are continuously stacked and averaged and the display is updated for each two cycles. When the operator sees that the displayed values have adequately converged, he can terminate the reading and file all values in memory.

Vp Integration. The primary voltage is sampled over 50 percent or more of the current on (T) time (depending on receive time) and the result is normalized for time. This long integra tion helps overcome random noise. On stand ard Scintrex transmitters, T can be 1,2,4 or 8 seconds.Digital Display. Two, four digit LCD displays are used to display measured or manually entered data, data codes and alarm codes.Automatic Profile Plotting. When connected to a digital printer such as the Scintrex DP-4 hav ing an industry standard RS-232C, 7 bit ASCII serial data port, data can be plotted in a base camp. The IPR-11 Is programmed to plot any selected transient window and resistivity in pseudo-section or profile form. Line orienta tion is maintained consistent, that is station numbers on profiles are sorted in ascending number. In the profile plot, the scale for resis tivity is logarithmic with 1 to 10,000 ohmme- ters In four decades with another four decades of overrange both above and below. The char geability scale Is keypad selectable. In the pseudo-section plot, any one chargeability window can be presented in conventional pseudo-section form.Printed Data Listing. The same digital printer can be used to print out listings of all headers and data recorded during the day's operation. Several copies can be made for mailing to head office or for filing In case copies are lost. Baud rate is keypad selectable at 110,300 or 1200 baud, depending on the printer used.Cassette Tape Output. A cassette recorder having an industry standard RS-232C, 7 bit ASCII serial interface may be used for storing data directly from the IPR-11. If all six dipoles are used, then 16,80 character blocks of data per observation are transferred at a rate of 1200 baud. The storage capacity of one side of cassette tape is approximately 1400 blocks or about 90 six dipole observations. The MFE Model 2500 is recommended since It has a read-after-write feature for data verification.The recording format is compatible with the Texas Instruments 'Silent 700' terminals and records are made on standard digital grade cassettes. Once a cassette tape record is made, the tape can be played back onto the DP-4 Digital Printer for an additional verifica tion that the data on tape are correct.

Time domain IP transmitted waveform

Pseudo-section printout on DP-4 Digital Printer. Chargeability data are shown lor the sixth transient window (M,,) lor the dipole-dipole vray and six 'rt' spacings. Line number and station number ve also recorded. The contours have been hand drawn. Resistivity results can be plotted in a similar manner.

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Broadband Time Domain IP Receiver

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l: 8.2 6.3 5.2 4.6 3.4 2.3 1.7 13 9.9 -ft?728.2 -3. 5.71E+3 :. .

2: 8.5 6.4 5.2 4.6 3.3 2.3 l? 13 ft? 8.7M 6 e. 4.7E+3

3: 7. S 6.8 5.8 4.4 3.3 2.2 1.7 12 ft? 8.77155 -4. 3.46E+3

4: 7.7 59 4.9 4.3 3.2 22 1.7 13 9.9 9.744.57 4. 3.43Et3

5: 7.1 5.8 4.1 3.5 2.5 1.6 1.1 1,8 12 1.622.43 -2. 2.WE+3 ' :. -; ;-;'j-- , ;;\

6: 9.5 7.8 5.8 5.4 3.7 ; 2.7 );2.p' : 1/5^ 8.6 :4413.46 8. 2.2E+3 ' ' ' , "- -, '-- '-' - . . .

Modern. Data In the IPR-11 memory can be output directly into a modern near the field operation and transmitted by telephone through a modern terminal In or near head office, where data can be output directly onto a digital printer or tape recorder. In this way a geophysicist in head office can receive regular transmissions of data to improve supervision and interpretation of the data from field pro jects and no output device other than the modern is required in the field.External Circuit Check. Six analog meters on the IPR^II are used to check the contact res istance of Individual potential dipoles. Poor contact at any one electrode is Immediately apparent. The continuity test uses an AC sig nal to avoid electrode polarization.Self Check Program. Each time the Instrument is turned on, a check sum verification of the program memory is automatically done. TKte verifies program integrity and If any discre pancy is discovered, an error signal appears on the digital display. Part of the self check : program checks the LCD display by displaying eight ones followed sequentially by eight twos, eight fours and eight eights.Manipulation Error Checks. Alarm codes appear on the digital display if any of the fol lowing ten errors occur: tape dump errors, Illegal keypad entry, out of calibration or failed memory test, insufficient headers, header " buffer full, previous station's data not filed, r data memory full, Incorrect signal amplitude or excessive noise, transmit pulse time incorrect and receiver measurement timing incorrect?internal Calibrator. By adjustment of the func tion switch, an Internal slgnal.generator is ^ connected across the inputs to test the calibra tion of all six signal (inputs for SP, Vp and all M windows simultaneously. Then the software checks all parameters. If there is an error in one or more parameters, an alarm code appears on the display. The operator'can then push a key to scan all parameters of all input channels to determine where the error is.

Data listing output en DP-4 Digital Printer. Header information is shown in the first two lines. In this case, data are for Line 1. Station 3. Transmitted cur rent is 80 mA. Next are the resistivity K factors tor the six dipoles. 8292 Indicates that receive and transmit times are each Z seconds. The last header Itefn records that fact that 14 cycles were stacked. Following trie header are the geophysical data lor six dipoles which were measured simultaneously. For each dipole, the values tor the W transient windows tre shown on Ohfriinb. The next line shows Vp and SP in mV/V and resistivity. 5.71 B * 3 indicates that

- the calculated rttt&fWry* 5.71 Tt

Technical Description of the!PR-11 Broadband Time Domain IP Receiver

Industry standard cassette recorders such as this MFE-2500 can be connected directly to the IPR-11.

DP-4 Digital Printer

Input Potential Dipoles

Input Impedance

Input Voltage (Vp) Range

Automatic SP Bucking Range

Chargeability (M) Range

Absolute Accuracy of Vp, SP and M

Resolution of Vp, SP and M

IP Transient Program

Vp Integration Time

Transmitter Timing

Header Capacity

Data Memory Capacity

External Circuit Check

Filtering

Internal Calibrator

Digital Display

Analog Meters

Digital Data Output

Standard Rechargeable Power Supply

1 to 6 simultaneously4 megohms100 microvolts to 6 volts for measurement. Zener diode protection up to 50 V±1.5VO to 300 mV/V (mils or 0/00)

Ten transient windows per input dipole. After a delay from current off of t, first four windows each have a width*! t, next three windows each have a width of'6t and last three windows each have a width of 12t. The total measuring time is therefore 58t. t can be set at 3,15,30 or 60 milliseconds for nominal total receive times of 0.2,1,2 and 4 seconds.

In 0.2 and 1 second receive time modes; 0.51secIn 2 second mode; 1.02 secIn 4 second mode; 2.04 secEqual on and off times with polarity change each half cycle. On/off times of 1,2,4 or 8 seconds with MM stability are required.Up to 17 four digit headers can be stored with each observation.Depends on how many dipoles are recorded with each header. If four header Items are used with 6 dipoles of SP, Vp and 10 M windows each, then about 200 dipole measurements can be stored. Up to three Optional Data Memory Expansion Blocks are available, each with a capacity of about 200 dipoles.Checks up to six dipoles simultaneously using a 31 Hz square wave and readout on front panel meters, in range of O to 200 k ohms.RF filter, spheric spike removal; switchable 50 or 60 Hz notch filters, low pass filters which are automatically removed from the circuit in the 0.2 sec receive time.1000 mV of SP, 200 mV of Vp and 24.3 mV/V of M provided in 1 sec pulsesTwo, 4 digit LCD displays. One presents data, either measured or manually entered by the operator. The second display; 1) indicates codes identifying the data shown on the first display, and 2)'shows alarm codes indicating errors.Six meters for; 1) checking external circuit res istance, and 2) monitoring input signals.RS-232C compatible, 7 bit ASCII, no parity, serial data output for communication with a digital printer, tape recorder or modern.Eight Eveready CH4 rechargeable NiCad D cells provide approximately 15 hours of con tinuous operation at 25"C. Supplied with a battery charger, suitable for 110/230 V, 50 to 400 Hz, 10 W.

Technical DescriptionofthelPR-11Bros d ben d Time DomcinIP Receiver

Disposable Battery Power Supply

DimensionsWeightOperating Temperature RangeStorage Temperature RangeStandard Items

At 25* C, about 40 hours of continuous opera tion are obtained from 6 Eveready E95 or equivalent alkaline D cells.At 250 C, about 16 hours of continuous opera tion are obtained from 8 Eveready 1150 or equivalent carbon-zinc D cells.345 mm x 250 mm x 300 mm, Including lid.10.5 kg, including batteries.-20 to *55"C, limited by display.-40to*60e C.

Console with lid and set of rechargeable bat teries, 2 copies of manual, battery charger.

Optional Items Multidipole Potential Cables, Data Memory Expansion Blocks, Statistical Analysis Pro gram, Crystal Clock, SPECTRUM Program.

Shipping Weight 25 kg includes reusable wooden shippingcase.

222 Snidercroft Road Concord Ontario Canada L4K 1B5

Telephone: (416) 669-2280 Cable: Geoscint Toronto Telex: 06-964570

Geophysical and Geochemical Instrumentation and Services

IPR-11 LCD displays, actual size

RES

2DN I5N

24.62

235* 2350 g85o 3500

31570

C HA

25N 2DN 15N

RESISTIVITY (ohm/m)

5N

•itut

CHARGEABILITY (mv/v)

ISTIVITY(ohm7m)

ION B.L.O

RGB ABILITY (mv/v)

ION 5N B.L.O

B.L.O

5-745

B.L.O

f-* /.5 6.6 4*4 f*

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

l a ^Dp1^Dp2^Dp3\Dp4JDpS\Dp6\

\ ̂ ' x' x x 'f'

survey direction

PLOT

POINTS

Scintrex

Scintrex

TSQ-3 (3kw) Pu tee Scheme—^—2 SGC

IPR 11reading 7th slice

Total Line total

ROBERT S. MIDDLETON EXPLORATION SQWlCES INC.

for BATTLE ENERGYTitle

LI6W

Date: JULY 1984 Scale[Drawn: p.H. l c.G. {Approved

N.T.S.:

' 'T1* : --v --j-^-^;j.." ,-i-j&tof

File: M-61

B.L.O 5Srf*

B.L.O* ——————-i-

5S

RESISTIVITY (ohm/m)

IOSI5S

CHARGEABILITY (mv/v)

15 S

y. 4

RESISTIVITY (ohm/m)

4*27

K)S 155 2DS-4————

CHARGEABILITY (mv/v)

IOS I5S aos

20S

20S

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

00-fix

n1 /n2

survey direction

PLOT - x

POINTS n4 \

^ U2.3

'. Scintrex

: Scintrex

TSQ-3 (3kw) Pulse Scheme-2 sec-

\, V

v

ipR 11reading 7th slice

0)23 4 56 7 a 9

Total Line Total Readings

.REVISIONS ROBERT S. MIDDLETON

EXPLORATION SERVICES INCfor BATTLE ENERGYTitle

L I6W

B.L.O-20SDate: JULY I984DrawnrD.H/C.G.

Scale: i" sApproved

N.T.S.:File: M-61

Off

B.L.O

\5S

|jo/ /Ifcoeoj l \ W*

^ X* * V^ v v

JSto

r

B.L.O 5S

20S

8776

20S

4-4

6.3 ^

INDUCED POLARIZATION

00—— -——

Time Domain

POLE-DIPOLE ARRAY

^^^^^^ —a j Dp r lDp2 JDp 3 j Dp 4 f Dp5~fDp6}.- --^- --J..- — . .,.. . .r . - ——— ,^ . ^ . .

survey direction

PLOT POINTS

n4 -

n5^ KX) ^ 1,2,3

Scintrex TSQ-3 (3kw) Pulse Schemei ———— 2 sec

[2seci2 sec i

Scintrex l PR 11reading 7th slice

0123 45678 9

Total Line 'Tod Total Readings

.Off

REVIS1O6

11

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for

TitleBATTLE ENERGY

L24W

4S-2ISDate: JULY 1984 Scale: I'^ioo'

l y ^ (Drawn: D.H. 1 C.G. Approved :N.T.S.: 1File: M-61 1

25N 2DN 15 N

25N 2DN I5N

RESISTIVITY (ohm/m)

15 N

CHARGEABILITY (mv/v)

ION 5N

7/7

4.8

RESISTIVITY (ohm/m)

ION B.L.O

io i to i2.no m 60

CHARGEABILITY (mv/v)

ION 5N B.L.O.ri_______t—

10

\

B.L.O

74So

^

TJOO

7470

7*0 75JO 7310 11160

B.L.O

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

oo- Rx.——-i\/ 7

PLor"3 \ X .PO/A/rs n4 \X

survey direction

3=100"

TXT Scintrex TSQ-3 (3kw) Pulse Scheme———2 sec

: Scintrex IPR 11reading 7th slice

7 * 9

Total Line .2600!. Total Readings

Otf

1 REVISIONS11

i ———————

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for

Title

Date:Drawn

B/VTTLE ENERGY

L 24 W

25N-ISJULY ©84 Scale: i 11 s rao1: D.H. X C.G. Ap^proved:

N.T.S.:File: M -ei

--

F

5N B.L.O 5S

S j. s.\

6-4

5-3 S-S

t

RESISTIVITY (ohm/m)

B.L.O

B.L.O

.e

s-3

CHARGEABILITY (mv/v)

5S IOS

6-*

RESISTIVITY (ohm/m)

\0000 11000

HARGEABILITY (mv/v)

IOS

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

~\ a J Dp 1

n 1 ' .

PLOTn3'-

POINTSn4 '^.

n5

survey direction—————fr.

^ icx)'

T XI Scintrex

FxXI Scintrex

TSQ-3 (3kw) Pulse Scheme— 2 sec-

!KIPR 11reading 7th slice

L li,! i l --LJL---—.678

i 2 sec!2seC; i Of f

Total Line Total Readings

iREVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for BATTLE ENERGYTitle

L32W

N-I4SDate .JULY 1984 Scale: I'^ NT. S.Drawn: C.G. Approved File: M-61

F

5N B.L.O

17 Too

\8000

CI

5N B.L.O 5S

5 r-r

RESISTIVITY (ohm/m)

B.L.O

N\V \3250

CHARGEABILITY (mv/v)

B.L.O 58 10 S

3-3

RESISTIVITY (ohm/m)

I5S

HA RGE ABILITY (mv/v)

10 S I5S—i—

N3-4 J -3

15S

15 S

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

Rx

survey direction——————k.

PLOTPOINTS

n4 '

n5 ^ jpo1

Tx: Se in t rex TSQ-3 (3kw) Pulse Scheme

Scintrex IPR 11reading 7th slice

2 sec!4-

Off

Total Line Total Readings

1 REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for

Title

BATTLE ENERGY

L40W

B.L.O-I6SDate .JULY 1984 Scale: I'^IOO1Drawn: C.G. Approved :

N.T.S.:File: M-61^••^^•••••••^•i

5N

RE'

B.L.O 5S

Z Too

CH

B.L.O 5S

3-C, 3-0

3-t 3.fo

5

RESISTIVITY (ohm/m)

B.L.O 5S

CHARGEABILITY (mv/v)

B.L.O 5S KDS

S-o 5-3.

5 4

I'ill*lSTIVITY(ohm;m)

IOS

7730

7740

RGEABILITY(mvXv)

IOS

f- 3

5". i 5-4

oo~

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

j a*l a i Dp r iDp2lDp 3 4 Dp4 4 Dpslop 64—^——^ ^j——^——^———^——-i——— —————————

x' X survey direction

PLOTn3'

POINTSn4<

nS^ 100

l Scintrex TSQ-3 (3kw) Pulse Scheme2 sec

v*v :

: Scintrex IPR 11reading 7th slice

2 sec2 sec

OI23 * 5 678 9

Off

Total Line J3QQ1 Total Readings

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for BATTLE ENERGYTitle

L48MV

S-I4SDate .JULY I984 Scale: l" - KX) N.T.S.:

Aroved : File: M-61

RES

5.N B.L.O 5S

C HA

5N B.L.O 5S

z.-z.

3.8 3-5 3.^ 5. z.

3 -T 3'ft

z.* a

3.4 5-5 .3-8 3-8 3-7 3-5 3.5

RESISTIVITY (ohm/m)

CHARGEABILITY (mv/v)

5S K)S

3.8

3.1 3- T 3-fc 3-4

3-e

5".

;iSTIVITY(ohm7m)

15 s

RGEABILITY(mvXv)

f. t.

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

/of 7

Rx

"f

PLOT r

POINTS

a \Dp1\Dp2JfDp3^Dp4jDp5\Dp6\

^-, '' ,' ' ' ' ,'' ' Jsurvey direction

n6' i .2.3

Scintrex

Scintrex

TSQ-3 (3kw) Pulse Scheme———2 sec

2 sec

IPR 11reading 7th slice

2sec

O123 4 5 6 79

Total Line 20001 Total Readings

4-

Off

:1 REVISIONS

••••••••••••i

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for

Title

BATTLE ENERGY

L56W

2N-I8SDate: JULY I984 Scale: \ n **xf |N.T.S.:Drawn : D.H. /C.G Approved: (File: M-6I J

42C13SWei6t 2.7444 WABIKOBA LAKE 030

CORPORATE OIL b GAS LIMITED

REPORT ON

GEOCHEMICAL SURVEY

Si

GEOLOGICAL SURVEY

OF THE

BATTLE ENERGY CORP. OPTION

HEMLO AREA

DISTRICT OF THUNDER BAY,

ONTARIO

DECEMBER, 1983

Z 7 1984

LANDS SECTION

January 4, 1984

lr : ( H Aiml ;, D. B. WILSON;1 ^

'^.'.Hi" " ' vv^'?

l O N T A R l O'———~ ———— " ———"l

THUNDER 7 BAY Out

a t 0 S up e r f 4 r

KEY MAP

Showing

Property of

BATTLE ENERGY CORPORATION

SCALC

Km Ml

ISO

100\.\ l\ n O yi i r' i - : v j

LOCATION MAP

BATTLE ENERGY CORPORATION.

Memlo Gold AreaOMrlet of Thunder Bay

ONTARIO

i c ALC

Ml. Km

- l -

INTRODUCTION

A geochemical survey and a geological survey

have been done over the Battle Energy Corporation

Option in the Hemlo Area of northern Ontario (see

Key and Location Maps).

The geochemical samples were collected and

the geological mapping done by geologists in the employ

of Corporate Oil s Gas Limited as part of an agreement

whereby Corporate may earn an interest in the Battle

Energy Corp. Option.

The samples were assayed by Bell-White Analytical

Laboratories Ltd., of Haileybury, Ontario. The geological

mapping and geochemical soil sampling were done during

the period of September 13, 1983, to October 10, 1983.

Assays were received during December, 1983.

The presentation and evaluation of the data

is the purpose of this report.

HARRY YD. B. y,uxo?i !, ji

- 2 -

PROPERTY, LOCATION, AND ACCESS

The mineral property of the Battle Energy

Corp. Option consists of .14 contiguous unpatented

mining claims located in the Hemlo area, east of Lake

Superior in the Thunder Bay Mining District. The

claims are TB 731201 to TB 731208 inclusive, and TB

725140 to TB 725145 inclusive.

Hemlo is a station on the main line of the

CPR, approximately 200 miles east of Thunder Bay.

The Trans-Canada Highway (Ontario #17) runs more or

less along the railway and lies to the north of the

town.

The claims are situated 2^ miles northwest

of the junction between the Trans-Canada Highway and

Highway #614 to Manitouwadge, and two miles north

of the Golden Giant gold deposit currently being developed

for production. The northern .part of the property

is accessible via 6,000 feet of bush road, along

the north side of Phillips Creek. This bush road

joins Highway #614 two and one quarter miles to the.v - ! i:/:- ^

north of the junction of Highways #17 and #614. .-' .i?;'-W H A R RV^ ' D.;: V;,'^

i

.

- 3 -

TOPOGRAPHY

The dominant topographic features of the

property are the north-trending valley of Cedar Creek

and the northwesterly trending Phillips Creek. Drainage

along Cedar Creek is to the north and west into the

Pic River three miles above Lake Superior. Total

relief in the claims is approximately 70 meters from

the creeks to the tops of the rounded ridges.

The area is forest covered and bedrock exposures

are few.

HISTORY OF EXPLORATION

Previous mineral exploration on the property

has not been recorded, and evidence of such work was

not found during the present surveys, except for the

picket ling grid cut for Battle Energy Corp.

Dr. J. E. Thompson (1932) mapped the geology

of the area for the Ontario Department of Mines. vf-,\•'i "'^ .' "' ~ f

T. L. Muir (1978) (1982) published maps and reports l:; '~ jl' ' i

of the area for the Ontario Department of Mines. ;; ' D. 0. \Vii.lOM ,.

••''.•'.'•' 'il-",/ 'f'

l) . rnw r! A \\ R i

- 4 -

Other reports include those by T. W. Page (1957),

and V. G. Milne (1968). A report by H. D. Carlson

(1982) was not made available.

A report entitled "Geophysical Surveys of

the Property of Battle Energy Corporation in the Hemlo

Area, District of Thunder Bay, Ontario" (1983) by

H. Z. Tittley was made available to Corporate Oil

and Gas Limited. This report concerned magnetic

and VLF electromagnetic surveys that were carried

out over the claim area for Battle Energy Corporation.

J. W. Campbell (1983) reported on the property

for Corporate Oil S Gas Limited and estimated the

cost of an exploration program.

LINE CUTTING

A well-cut baseline extends from the east

boundary of the claims near the northeast corner of

claim TB 731202 as far as Cedar Creek approximately

3,600 feet to the westward. Cross lines from 00 to

3,600' are cut normal to the baseline at 400 foot

intervals and stations are marked at 100 foot intervals/.

ib--, D. B. KUSCfl ',

- 5 -

Evidence of base line or picket lines was not found

to the west of Cedar Creek so that flagged compass lines

were used to complete the survey west of Cedar Creek.

Geochemical samples were only taken where survey control was

considered satisfactory so that some of the extremities

and areas where it was difficult to maintain control

were not sampled at 100 foot intervals. ,

Unfortunately the work was planned and costs

estimated by both J. W. Campbell and Corporate Oil on the

basis of 100 foot spaced cross lines described in Tittleys

report (page 5). Tittley's maps, which show readings on

400 foot lines, were not made available until after the

geologists were in the field and had discovered the actual

spacing. The survey had to be adjusted to fit the actual

line spacing by reducing geochemical sample spacing to 100

feet from 200 feet.

The easternmost picket lines are well cut and

suitable for I.P. surveys. Picket lines approaching Cedar

Creek to the west are poorly cut, suitable for geologic ̂.^ifrV-^-vs.,

and geochemical surveys, but not for I.P. surveys. jy;-V/ """~ "^-x'' '.v'-,

GEOLOGY

'''i"' /' \ ' ' ''vir"i IIAUDY •••ffl\ ,,'', P-1. V.'iL'X'f! ; . ':-

\.-------..-,v'The geology of the claims was mapped using ''H,-'"' -V..; 'j V.''^''

. x ^;-i^A-~-^' traverses along the picket lines and the flagged lines

- 6 -

to the west of Cedar Creek.

Outcrops are rare, but the claims are apparently,

mainly underlain by quartz-feldapar-biotite metasediments,

which are interpreted as being derived from a predominantly

greywacke sequence. Sericitic metasediments occur

interbedded with the more common greywacke type, but

the sericitic bands are rare and narrow, reaching

only four feet in width.

Granite gneiss occurs on the claims as shown

on the map, but outcrop is too scarce to indicate any

contact. Granitic areas could probably be outlined

approximately by the composition of the surface deposits,

but this :conjectural information has not been included

on the map.

-Tittley's (1983) magnetic survey indicates

three anomalies whose shapes and magnitudes indicate

probable diabase dykes striking approximately N 700 W.

The largest of these diabases is confirmed by a diabase

outcrop as shown on the map.

Schistosity strikes N 45 W to west. Dips

are variable and range from 62 NE to 82 S. Bedding^: :.,'- l''..'l.' '' '.- X

; ' 11.";'? f? Y \ --'

\ - f ;.\)":; ;:v:

directions were not certain because of poor exposure,

but banding, which may represent bedding, dips approximately

parallel to schistosity.

Economic mineralization or evidence of hydrothermal

activity such as extensive silicification, chloritization,

or carbonatization were not observed on the small

outcrop. Minor, randomly oriented silicified fractures

occur in a few places. The greywacke environment

is not that of chemical sedimentation, which is associated

with some gold deposits, so that the sedimentary environment

exposed is not encouraging except for the thin sericitic

beds, which provide some hope that similar larger

beds may occur more extensively in the covered areas.

The probable northward dip of some of the

metasediments could result in deposits on claims to

the south dipping on to the Battle claims at depth.

The only exploration results reported (newspapers)

however, indicate the discovery of massive pyrite

with very low gold content.

GEOCHEMICAL SOIL SURVEY- - - - -- - -

,.- - . .Soil samples were collected and analyzed ; o ' \ -c J , ' ; ' f ' O 'i ' ' )

;, .' i l i . t . \ . i

for gold with the aim of locating soil areas that -t [). i,'. l,.;.jC '"

- 8 -

are anomolously rich in gold. The sampling began

by collecting, samples at 200 foot intervals on the

premise that picket lines were spaced 100 feet apart.

This sample spacing was reduced to 100 foot intervals

when the wider spaced picket lines were reported.

The 100 foot sample spacing was continued except for

the westernmost area of the claims where sample spacing

was increased because of the less accurate geographical

control.

A total of 442 samples were collected.

Analyses have been received for 419 of the samples.

The remaining 23 samples appear to be missing sometime

after shipment. The missing samples were from the

southwest portion of claim number TB 731205.

The samples were collected from the B soil

horizon except in swampy areas where only humus was

available. A few of the humus samples did not contain

enough mass for the desired analytical accuracy, but

show the results obtained.

The analytical results are reported in parts

per billion of gold. Analyses were made by Bell-White

using the fire assay concentration method, followed

- 9 -

by gold extraction and determination using the atomic

absorption method. Analytical results are considered

accurate to two parts per billion.

Anomolous gold values are normally considered

to be 10 ppb or greater in soils in the Precambrian

shield areas of Canada. Experience in the Hemlo Area

has shown that anomolous gold in soil values are more

commonly greater than 50 ppb, apparently due to local

geologic conditions where overburden is relatively

thin and bedrock weathering is somewhat deeper than

usual.*

was :

The mineral composition of the samples collected

Sand or silty sand

Silt or sandy silt

Humus

Gravel or sandy gravelClay or clay and humus

52%

20%

191

51

4%

Sands and silts may be white, red-brown,

or deep red-brown. Clays are either white or red.

A soil map was not prepared due to the lack of anomolous gold- i. J VW*** A.*.values. s'^Z :: "~

v- \ :.,'Ai HARHY V -f

. D D. V:ii.SON ;,,. j!- '

- 10 -

Overburden depths are not known but the

nature of the topography and the deposits indicated

that soil sampling might be successful.

The results of the survey were disappointing

from an economic standpoint because none of the samples

are more than 10 ppb gold resulting in a complete

lack of anomolous areas. Analyses for other possible

tracer elements do not appear warranted from these

gold results as well as from the geological provenance

of the metadediments.

CONCLUSION '

The geological mapping and the geochemical

soil sampling did not develop any targets for further

exploration. The I.P. results indicated a lack of

sulphide mineralization in the strongest and most

persistent V.L.P. anomaly.

These results indicate that further work

at the present time is not attractive.

: ; MARRY \ \\ J. D. li WLSOri

QUALIFICATIONS

The geological and geochemical work and

the appended geophysical work were supervised, and

the report written by H. D. B. Wilson, B. Se., M.S.,

Ph.D. who is also a Registered Engineer in the Province

of Manitoba. The project manager was Bernard Gaboury,

B. Se., and the geologist-geochemist was John Danko,

B. Se.* Paul Adamaitas, geophysicist, of Phoenix

Geophysics Limited operated the I.P. survey.

MARRY \' 0. P. IVIiSON ;'.

- 11 -

ADDRESSES

The claims are held by:

Mid Canada Exploration Services Ltd 251 Third Avenue Suite 81 Timmins, Ontario

The Claims are optioned to:

Battle Energy Corp.900 Bow Valley Square One202 - 6th Avenue S.W.Calgary, AlbertaT2P 2R9

The work was performed by

Corporate Oil and GAs Ltd, 201 - 52 Donald Street Winnipeg, Manitoba R3C 3Z6

- 12 -

REFERENCES

THOMPSON, J. E.1932 Heron Bay - White Lake Area

Ontario Department of Mines Annual Report, Vol. 41, Part 6

PAGE, T. w.1957 A GEOLOGICAL REPORT ON THE HEMLO AREA

THUNDER BAY DISTRICT, ONTARIO Department of Industrial Development Canadian Pacific Railway

MILNE, V. G. 1968 GEOLOGY OF THE BLACK RIVER AREA

Ontario Geological Survey Report G.R. 72

MUIR, T. L.1979 Hemlo Area, North Half

Ontario Geological SurveyGeological SeriesPreliminary Map P-2304, 1:15, 840

MUIR, T. L.1982 Geology of the Hemlo Area

Ontario Geological Survey Report 217

CARLSON, H. D. 1982 Report on the Property of

Battle Energy Corporation. District of Thunder Bay, Ontario Report to Battle Energy Corp.

CAMPBELL, J. W, 1983 Preliminary Geological Report on

Claims Held Under Option by Battle Energy Corporation in the Hemlo Area, Report to Corporate Oil and Gas Ltd.

DELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-31O7

Gterttfkate nf AnalysisNO. B985-B3

SAMPLE(S) OF: Soil (37)

SAMPLE(S) FROM: Mr. Bernard GabouryCorporate Oil S Gas Limited

DATE: December 9, 1983

RECEIVED: November, 1983

BE83S 050

051

052

053

BE83S 410

411

412

413

414

415

416

417

418

419

420

421

' 422

423

Gojkl/ppb

2

2

2

2

2

2

2

2

2

2

6

4

2

23*

2

2

2

S a{npljL.N o .

BE83S 424

425

426

427

428

429

430

431

432

433

434

435

436

437

438439440

441442

Gojd/ppb

2

2

2

2

2 4

24*

2

6

2

2

2

2

2 4

2

2 6*

Insufficient sample for accurate assay

ACCOROANCC WITH t,ONC.CSTABUSHCD NORTH cniCAN CUSTOM. UNLtM IT It tPCCiriCALLV (TATCO *mwiSC COLD AND IIIVCR VALUCI flfPORTCO ON LiC SMCCTS HAVC NOT BtCN ADJUSTCD TO COMPCN-

AAtO GAtKS tKHCKCnr tN THE flHC

ASSAY PHOCC&5.

BELL-WHITE ANALYTICAL LABORATORIES LTD.

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY, ONTARIO TEL: 672-31O7

Oterttfirat? nf AnahjataNO. * B954-83

*•t'

SAMPLE (S)-OF?' Soil (381)

SAMPLE (S) FROM:

Page 4 of 4 DATE: December 2, 1983

RECEIVED: October, 1983

Mr. Bernard Gaboury Corporate Oil S Gas Limited

Sample No.

BE-83S-317-318-319-320-321-322-323-324-325-326-327-328-329-330-331-332-333-334-335-336-337-338-339-340-341-342-343

. -344-345-346-347

Gold/ppb

24**2462264222622266224 4**4**46222242

Sample No.

BE-83S-348-349-350-351-352-353-354-355-356-357-358-359-360-361-362-363-364-365-366-367-368-369-370-371-372-373-374-375-376-377-378

Gold/ppb Sample No.2 . 2 2 4 2 2 2 2 4 2 2 4 2 2 2 2 2 2 2 2 2 2 46** 6 2 2 2 2 4**6**

BE-83S-379-380-381-382-383-384-385-386-387-388-389-390-391-392-393-394-395-396-397-398-399-400-401-402-403-404-405-406-407-408-409

Gold/ppb

224 4 4 4**842242282842426**226**2224**26** 6

** Insufficient sample for accurate assay

ACCORDANCE WITH LONO-ESTABLISHED NORTH 'CftlCAN CUSTOM. UNLESS IT It SPECIFICALLY STATED rr.CRWISE COLD AND SILVER VALUES REPORTED ON USE SHEETS HAVC NOT BEEN ADJUSTED TO COMPCN. TC FOR LOSSCS ANO CAINS INHCRCNT IN THE fIRE

BELL-WHITE ANALYTICAL LABORATORIES LTD.

DELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-3107

O. B954-83

AMPLE(S) OF:

nfPage 3 of 4

Soil (381)

DATE: December 2, 1983

RECEIVED: October, 1983

5AMPLECS) FROM:.. Mr. Bernard Gaboury•' Corporate Oil S Gas Limited

Sample No. Gold/ppbBE-83S-221

-222-223-224-225-226-227-228-229-230-231-232-233-234-235-236-237-238**-239-240-241-242-243-244-245-246-247-248-249-250-251-252

442244**22288**4**44224**8**4222226**6**224**222

Sample No.BE-83S-253

-254-255-256-257-258-259-260-261-262-263-264-265-266-267-268-269-270-271-272-273-274-275-276-277-278-279-280-281-282-283-284

Gold/ppb22242244222224422222422424222222

Sample No.BE-83S-285

-286-287-288-289-290-291-292-293-294-295-296-297-298-299-300-301-302-303-304-305-306-307-308-309-310-311-312-313-314-315-316

Gold/ppb4**6**4**22624222262224**222642442242244

CCORDANCC WITH LONG -ESTABLISH t D NORTH :*N CUSTOM, UNLESS IT IS SPECIFICALLY STATED WISE COLD AND SILVER VALUES REPORTED ON SHtCT* HAVE NOT BEEN ADJUSTED TO COHPEN.

OR t O*5 C* ANO GAINS INHCHCttT IN THE FIRE ASSAY PROCESS.

BELL-WHITE ANALYTICAL LABORATORIES LTD.

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-3107

Qfcrttfiratr nf AnalysisNO. B954-83 Page 2 of 4 DATE: December 2, 1983

SAMPLE(S) OF: Soil (381) RECEIVED: October, 1983

SAMPLE (S) FROM: Mr. Bernard GabouryCorporate Oil A Gas Limited

Sample No .

BE-83S-125-126-127-128-129-130-131-132-133-134-135-136-137-138-139-140-141-142-143-144-145-146-147-148-149-150-151-152-153-154-155-156

Gold/ppb

24224422422444422222444**242222422

Sample No.

BE-83S-157-158-159"-160-161-162^163-164-165-166-167-168-169-170-171-172-173-174-175-176-177-178-179-180-181-1B2-183-184-185-186-187-188

Gold/ppb

44222262284222222222442222282242

Sample No.

BE-83S-189-190-191-192-193-194-195-196-197-198-199-200-201-202-203-204-205-206-207-208-209-210-211-212-213-214-215-216-217-218-219-220

Gold/ppb

22222442222464882424**266**26**2224222

ACCORDANCE WITH LONG-tSTABLlEHED NORTHlliCAN CUtTOM. UNLEU IT 11 SPECIFICALLY ITATEO^RWISE COLD AND (ILVER VALUE* REPORTED ON

SHEETS HAVE NOT IEEN ADJUSTED TO COMPEN.'OX tOfiCf AftO QAINS INHERENT IN THE flKC

AttAV PROCEfS.

BELL-WHITE ANALYTICAL LABORATORIES LTD.

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-31O7

Otarttfkat? nf AnalgmaNO. B954-83

SAMPLE(S) OF: Soil (381)

SAMPLE (S) FROM:

Page l of 4 DATE: December 2, 1983

RECEIVED: October, 1983

Mr. Bernard Gaboury Corporate Oil St Gas Limited

Sample No. Gold/ppb Sample No.

BE-83S-001-002-003-004-005-006-007.-008-009-010-Oil-012-013-014-015-016-017-018-019-020-021-022-023-024-025-026-027-028-029-030-031-032

8 BE-83S-0336 -0342 -0352 -036 2 . -0372 -0382 -0394 -0402 -0412 -0422 -0434 -0444 -0452 -0462 -0474 -0488 -049 4 BE-83S-0764 -0772 -0784 -079 6** BE-83S-0824 -0832 -0842 -0852 -0862 -0874 -0882 -0894 -0902 -0914 -092

Gold/ppb

42422242224262262222242442444422

Sample No.

BE-83S-093-094-095-096-097-098-099-100-101-102-103-104-105-106-107-108-109-110-111-112-113-114-115-116-117-118-119-120-121-122-123-124

Gold/ppb

2224222242424664242226**422228**4224

ACCORDAMCC WITH LONG.CSTABUSHCD NORTH .ICRICAN CUSTOM. US.CSS IT IS SPCCIFICALLY tTATCO THtdWISC COLD ANC SILVCH VALUCS REPORTED ON

C SMtCTS HAVC "-CT BCtN ADJUSTtD TO COMPIN-

A&SAV PROCCSS.

BELL-WHITE ANALYTICAL LABORATORIES LTD.

42C13SW0161 a.7444 WABIKOBA LAKE 040

CORPORATE OIL 6 GAS LIMITED

INDUCED POLARIZATION SURVEY

OF THE

BATTLE ENERGY CORP. OPTION

HEMLO AREA,

DISTRICT OF THUNDER BAY,

ONTARIO

'-ir1.1 is P r? v \-- V- 111 \ . 1 1 1 i \ .-

January 4, 1984

- l -

LOCATION

An Induced Polarization survey was carried

out over a portion of the Battle Option of 14 contiguous

claims numbered: TB 721201 to TB 731208 inclusive,

and TB 725140 to TB 725145 in the Thunder Bay District,

Province of Ontario. This report is intended as an

addition to the report entitled "Geochemical Survey

and Geological Survey of the Battle Energy Corp. Option,

Hemlo Area," December 1983.

The Induced Polarization survey was designed

to give a two-line sample across the main portion

of the property, and in particular to test the A-B

VLP electromagnetic anomaly {Tittley 1983 ) at two of

its strongest crossovers. The lines chosen were 4 H- 00 W

and 8 * 00 W, where picket lines were suitable for

I.P. work.

SURVEY METHOD \ v.'-',-,s i'Xx.'1 *;-.^'c D

The I.P. survey was carried out by Phoenix

Geophysics Limited. The instruments employed consisted

of the Phoenix Spectial I.P. system MG-2 Motor Generator;

IPT - l Time/Frequency Domain Induced Polarization

Transmitter, with AC 3000 power module; IPV - 2 Receiver,

The survey was conducted in the Frequency Domain using

the dipole-dipole configuration with electrode spacing

at 200 feet using the receiver to measure phase shift.

INTERPRETATION

The very high resistivities and the lack

of any appreciable phase shift jrf is interpreted

as meaning that sulphide minerals are not present

in any interesting concentration on the two lines

measured. Both resistivity and phase shift indicate

a rock unit change at 6 * 00 N on line 8W f and 2 H- '00 N

on", line 4W. This is interpreted as being the contact

between granite to the north and metasedimets to the

south.

The decrease in resistivity at shallow depth

in the vicinity of 6 * 00 S on both lines 4W and 8W

is interpreted as due to swamp.

The two lines would be considered as blanks

in terms of sulphide or gold - pyrite deposits. •S/'jZ

RESU

25 S 20 S 15 S

3 b (r O

CHARi

25S 20S 15S

20 S

/o^y/o

J/ 4 00

RESlSTIVITY(ohm7m)

I5S IOS

X

?32.e?

CHARGEABILITY (mv/v)

20S I5S IOS

l

^TIVITYCohm/m)

ios

x

B.L.O

GEABILITY (mv/v)

ios 5S B.L.O

5.0 3 -5"

4 3

5S

5 -3

B.L.O

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

Rx

l a j Dp 1 \Dp2lbp 3 \ Dp4 \~Dp5\Dp 6\x ^ j--- -j . -. j -j -

nf-( y '' /' y /'survey direction

PLOT

POINTS n4n5

^ lOQ r^ l.2.3

Scinirex TSQ-3 (3kw) Pulse Scheme2 sea

Scintrex IPR 11reading 7th slice

2 sec l

O123 4 S 6 7

Total Line 2200' Total Readings ea

Off

1 REVISIONS

.

ROBERT S. MIDDLETON l EXPLORATION SERVICES INC. 1

for BATTLE ENERGY |Title L 4 w j

Date: AUG .1984Drawn: c G.

23S-INScale: I'^too1Approved:

I.KM \NT. S.: 1File: M-61 |]

RESIS1

B.L.O

CHARGE

B.L.O 5N

-3-0

1*2.

/-z.

- 3 2 .

/.z.

A/

AO o

(P-X

RESISTIVITY (ohm/m)

5N ION 15 N-l———————————————————L. Jl_______________L.

CHARGEABILITY (mv/v)

ION I5N

MVITYCohm/m)

ION I5N 20N

tocro *neo 697o

6-770 T&v

//fro (bC,o 6 wo ff8o o

;ABILITY(mvXv)

ION I5N

20N

6,970

20N

INDUCED POLARIZATIONTime Domain

POLE-DIPOLE ARRAY

Rx00-

a ^Dp1±Dp2^Dp3\Dp4{Dp5±Dp6\

n2*. PLOT "'

survey direction

\n5 '

n= 1.2.3

l Scintrex TSQ-3 (3kw) Pulse Scheme2 sec

K: Scintrex IPR 11

reading 7th slice

2 sec2seq

0123 45678 9

Total LinP 2200* Total Readings 66

REVISIONS

I

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for BATTLE ENERGYTitle

L 4 W

B.L.O-22N•

Date: AUG. 1984Drawn: c.G.

Scale:Approved

NT. S.:

•f Off

File: M-61

pMinistryof Natural Resources

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

42C13SWeH61 2.7444 WABIKOBA LAKE 900- Do not ut* shaded areas below.

owntnip er wee ^

.^tW-afe^ 'fi'ffffff 7V A/ ./ff-f/r -f r OCJ"-~^J / f~i ' O 7 Lf J-

Da'te 6t Survey (from A tor (Total Miles of line Cut

l Mo. l Yr. l Day l Mo. | Vr.

ACredits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Specie! Provisions

For first survey:

Enter 40 days. (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

- Megnetometer

- Radiometric

- Other fr*

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

t} f}

10Days per

Claim

m

Days per Claim

f.

Expenditures (excludes power stripping) ^-u, .^j-w-t* ISAType of Work Performed

Performed on Claim(s)

MINING D1V

S 1' f.jptJ r] H 'ixOv 1 y

A' 1

13!

ii.^

199Calculation of Expenditure Days Credits' ' " ' "!

Total Total Expenditures Days Credits

Is •i- [l5| - | "'

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

Date t , ;

//r/t,/^/' ',

T'.V"l •'"i

1

: l s

/;^^/ 0̂y^!xTJ

Mining ClaimPrefix

7/?.. .

' *B

J

i

Number

JJ^jr-'/t/Q

J 2 x? 4/IJL& y 37*3',**--yfrf/yi/Jff/y'tC73/2,0 s73/fof,7?/'?/??

f y r ~^ ' *

-31, f 9/v ̂f r* f r^f- ~*

7^/2 p "77?/ ?#A'

Expend. Days Cr.

po Office Use OnlvTotal Days Cr, Date Recorded J Recorded ^fjt^t J0 J Y if\'d

". " "^^ M^

Mining ClaimPrefix "

1

"

Number

——————————

Total number of mining claims covered by this report Of work.

Expend. Days Cr.

/'X

•C-iC^V^^y /Kf. 'jf,.(.g t s

ij&fl j^fa/wfhJt/yffi

/

CertificationVerifvinjfftepbrt 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 is true.

Name and Postal Address of

•^^,^^ f1362 181/9)

Person Certifying

i ' li / /i l ' '"* ^ f^~

^ / ̂ -~ r .0*^4^ . S s! /*S - -^ - ^ ^* f

*\,SS37Date Certified f

/k/8 jfa/sfacS ,C^o^Slgnatur^

' ' * ^ j/* l /US'.' " " J -7-*

;

f?-/ — — .

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

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 Township or Area ̂ Claim

MINING CLAIMS TRAVERSED List numericallyfa 9? KM #OV

Survey CompaAuthor of ReportAddress of Author Covering Dates of •^................/J^U.^.

7/3(BnecutttaB to offTotaLMiles of Line r.i.t AS f\

irtSe Ed* O

SPECIAL PROVISIONS CREDITS REQUESTED

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

DAYSGeophysical

AIRBORNE CREDITS (Special provision credit! do not apply to aliborne lurveyi)

Magnetometer. Electromagnetic . Radiometric(enter day* per claim)

SIGNATU

Res. Geol..Previous Surveys

File No. Type

_ Qualifications —————^——

Date Claim Holder

.,frff————

..tiS...,,.,....-JJf^sl.™.ZS/.^/.....

**j^*yvj*****t*****t

,^,,,.,,,,,,,z?./^^,

^.v.,,...,......^.^^^..,.

TOTAL CLAIMS

837 (5/79)

GEOPHYSICAL TECHNICAL DATA

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

Number of Stations x/0/ Station interval.Profile scale.

(

Contour interval_____jsq^ffyfo /Q-

* /nn ' (i famrj]/7A, - -—--*j

.Number of Readings -

.Line sparing Vfffiff ((/Q, W(1&r.

Instrument

Accuracy — Scale constant. Diurnal correction method.

Station check-in interval (hours). Base Station location and value ^—^—

Instrument

ELECTROMAGNETKCoil configuration

Toil separation

Accuracy

Method: D Fixed transmitter D Shoot back D In lineFrequency

1 (ipedfy V.L.F. nation) Parameters measured

d Parallel line

Instrument.Scale constant.

Corrections made.

O Base value and location.

accuracy.

\ S)Instrument Method J53 Time Domain Parameters — On time .

- Off time

requency Domain \ M\ fi.frequency

Ranges

— Delay time.i ( •Z '

PowerElectrode arrayElectrode spacing Type of electrode 7

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).

AIRBORNE SURVEYS Type of survey(s) ——— Instrument(s) —————

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

(specify for each type of lurvey) Aircraft used————————————————————————————————

Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude______________________________Line Spacing—. Miles flown over total area——————————————————————————Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples taken.

Total Number of Samples. Type of Sample.

(Nature of Material)Average Sample Weight——————— Method of Collection————————

Soil Horizon Sampled. Horizon Development. Sample Depth———— Terrain—————————

Drainage Development——————————— Estimated Range of Overburden Thickness.

ANALYTICAL METHODS Values expressed in: per cent

p. p. ra. p. p. b.

D Da

Cu, Pb, Zn,

Others————,

Ni, Co, Ag, Mo, As,-(circle)

Field Analysis (.Extraction Method. Analytical Method- Reagents Used——

Field Laboratory Analysis No.{———————.^

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

Mesh size of fraction used for analysis————

Extraction Method. Analytical Method - Reagents Used-.—

Commercial Laboratory (. Name of Laboratory.—. Extraction Method—— Analytical Method —— Reagents Used —-^^—

.tests)

.tests)

.tests)

General. General.

/j^jv Ministry ot lecnnicai AssessiWl Natura( i., ^ ~ .,-.VvJ sources Work Credits

Ontario ^f

*iem File2.7444bate Mining Recorder'4 Report of1984 12 17 Work *10 - 615

Recorded Holder MID-CANADA EXPLORATION SERVICES

Township or Area WABIKOBA LAKE AREA

Type ot survey and number of Assessment days credit per claim

Geophysical

oo

Other days

Section 77 (19) See "Mining Claims Attested" column

ftpnlngiral days

OeOChemiral ., . . days

Man days H Airborne di

Special provision Q Ground 0

D Credits have been reduced because of partial coverage of claims.

O Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

TB 725140 to 145 inclusive 731202 to 208 inclusive

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claims

K l not sufficiently covered by the survey l — l Insufficient technical data filed

TB 731201

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on

/J~x Ministry or Technical Assess) |\y) Natural taf . . ... r urces Work Credits '

™nl Fi "2.7444Date Mining Recorder's Report of

1984 12 17 Workk' ™

Recorded Holder

MID-CANADA EXPLORATION SERVICESTownship or Area

WABIKOBA LAKE AREA

Type of survey and number of Assessment days credit per claim

Geophysical

eiflcfomcgnetir days

Rariinmetric days

Other . days

Section 77 (19) Se* "Mining Claimi Allotted" column

40 Onlngiral days

13Geochemical.., -days

Man days Q Airborne CD

Special provision Q Ground Q

CB Credits have been reduced because of partial coverage of claims.

D Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claimi Assessed

TB 725140 to 145 inclusive 731201 to 208 inclusive

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claims

l — l not sufficiently covered by the survey l — l Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77(19)—60:828 (83/6)

/1^Z\ Ministry 01 Technical Assess * ^sources Work Credits

ment FH*2.7444

AMrwnrn ^•tt Winino Recorder's Report ofAMENDED ]QQS Q} ^ wc,kV 615

Recorded Holder MID-CANADA EXPLORATION SERVICES

Town,h (porAre, WABIKOBA LAKE AREA

Type ol survey and number of Assessment day* credit per claim

Geophysical

30lnrl,i r.ri polarization dayt

Oth.r days

Section 77 (19) S** "Mining Cltlmi Aliened" column

40R?0'AO'*"I day*

13Gporhemira| dav*

Man days Q Airborne CD

Special provision 0 Ground OD

09 Credits have been reduced because of partial coverage of claims.

O Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

TB 725140 to 145 inclusive 731201 to 208 inclusive

Special credits under section 77 (16) for the following mining claims

*

No credits have been allowed for the following mining claims

O not tufficiently covered by the survey - LJ Insufficient technical date filed

•.

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 60; Geological — 40; Geochemical — 40; Section 77(19)—GO:B38 IB3/6)

Mining Lands Section

Control Sheet

File NO j?. -7yy Y

TYPE OF SURVEY EOPHYSICAL

'LOGICAL

GEOCHEMICAL

EXPENDITURE

MINING LANDS COMMENTS:

f} , fi

Signature of Assessor

Date

1985 02 04 Your File: 615 Our File: 2.7444

Mining RecorderMinistry of Natural ResourcesP.O. Box 5000Thunder Bay, OntarioP7C 566

Dear Madam:

RE: Notice of Intent dated January 4, 1985.Geophysical (Induced Polarization) Geological and Geochemical Surveys on Mining Claims TB 725140 et al 1n the Wabikoba Lake Area.

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so Indicate on your records.

Yours sincerely,

S.t. Yundt01 rectorLand Management Branch

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

D. lsherwood:secc: 111 d Canada Exploration Services

189 Preston Street South Timmins, Ontario P4N 3N4

cc: Bruce Durham cc: Nadla Cal ra

c/o R. Middleton Exploration ServicesBox 1637Timmins, OntarioP4N 7U8

cc: Resident Geologist Thunder Bay, Ontario

cc: H. Wilsonc/o Corporate (011 A Gas Ltd 52 Donald Street Suite 901Winnipeg, Manitoba R3C 1L6

Inc

cc:Mr. G.H. FergusonMining ft Lands Commissioner Toronto, Ontario

ntano

Ministry ofNaturalResources

AMENDED

•1985 01 04 Your File: 615 Our File: 2.7444

r

Mining RecorderMinistry of Natural ResourcesP.O. Box 5000Thunder Bay, OntarioP7C 5G6

Dear Madam:

Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you may then change the work entries on the claim record sheets.For further information, if required, please contact Mr. R.J. Pichette at 416/965-4888.

iNurs sincerely,

Land Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3

D. Isherwood:mc

Ends.cc; Mid Canada Exploration Services

189 Preston Street South Timmins, Ontario P4N 3N4

cc;

845

Bruce Durham Nadia Caira c/o R. Middleton Exploration Services Inc Box 1637Timmins, Ontario cc: Mr. G.H P4N 7W8 Mining

Troonto

cc: H. Wilsonc/o Corporate Oil S Gas LtdSuite 90152 Donald StreetWinnipeg, ManitobaR3C 1L6

FergusonLands CommissionerOntario

Ministry ofNaturalResources

Ontario

AMENDED

Notice of Intent

for Technical Reports 1985 01 04

2.7444/615

An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.

846 (82/6)

V " Assessment Work Breakdown

Man Days are based on eight (8) hour Technical or Line-cutting days. Technical days include work performed by consultants, draftsmen, etc..

Type of Survey

Technical Technlcel Dayi Line-cutting No. of Dayi per Deyi Credit! Day! Total Credit! - Claim* Claim

| 5-9- x 7 * f/A? * - 1 V/3 +I /^' - saType of Survey

Technical Dayi Credit!

tint-cutting Di yi Total Cradlti

No. of Clalmi

Oayi par Claim

Technical Oayi Cradlti

Line-cutting Days Total Credit*

Dayi per Claim

Technical Dayi Credltl

Line-cutting Days Total Credlti

No. of Claim!

Dayi per Claim

ROBERT S. MIDDLETON EXPLORATION SERVICES INC.P.O. BOX 1637

TIMMINS. ONTARIOP4N 7W8

'HONE [705] 264-4246 [705] 264-4247

December 20, 1984

Mr. R. PichetteMinistry of Natural ResourcesWhitney Block, Room 6643Queen's ParkToronto, OntarioM7A 1W3

RE: File 2.7444

R;": c;: iLane! i;";: 1 .1 :^:'C!!;"; ; .

m;:/;.:!* in

i [ .: . . ..

l V/.;-. i.

As per our telephone conversation, I ami r enclosing duplicate copies of the 2 pseudo sections for Line 4 west which cover claim IB 731207. I apologize for any inconvenience this oversight has caused.

Yours truly,

RBD/mt End.

R.Bruce Durham, Consulting Geologist

DEC 2 7 1984

MINING

ario

Ministry ofNaturalResources

1984 12 17 Your File: 615 Our File: 2.7444

Mining RecorderMinistry of Natural ResourcesP.O. Box 5000Thunder Bay, OntarioP7C 5G6

Dear Madam:

Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you may then change the work entries on the claim record sheets.For further information, if required, please contact Mr. R.J. Pichette at 416/965-4888.

rs sincerely,

rundt :tor

Land Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3D. Isherwood:mcD

Ends.cc;

cc;

Mid Canada Exploration Services 189 Preston Street South Timmins, Ontario P4N 3N4Bruce DurhamNadia Cai rac/o R.Middleton Exploration Services IncBox 1637Timmins, Ontario P4N 7W8

H.Wilsonc/o Corporate Oil S Gas LtdSuite 90152 Donald StreetWinnipeg, ManitobaR3C 1L6

cc: Mr. G.H. FergusonMining b Lands Commissioner Toronto, Ontario

845

Ministry ofNaturalResources

Ontario

Notice of Intent

for Technical Reports

1984 12 17 2.7444/615

An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.

846 (82/5)

•*J*

Ik!

l/

v/

i/

v'

tf&t J/?

J?

\l

i/

\/20?lot

^

yi/

J3L

33

to

(7

y

2* T&fif

7-

(w.qfz.-chl. veins)

O 20 40 60 80 100

METERS

42C13SW&161 2.7444 WABIKOBA LAKE 200N)

LCP

**t

42CI3SWCI161 2.7444 WABIKOBA LAKE

725140

qfb——— —— (wqtz.-cW.veins)

725140 731206

~-D-

O 20 40 60 80 100

24S 225 20S IBS 165 14S l

125 105 85 65 45 25 2N l

4N 6N 8N l

ION l

12N

-ISM CO UJ CtL

LINE 4W

X s200 FEET

l Hz

U.Z

0 INDEX MAP

-N:2

-N*3

COZ ^O<Oi

.N=4 5

.. , -e^

TT? ANS-CANADA HW Y

CORPORATE OIL Se GAS LTD.

l. P SURVEY

BATTLE ENERGY GRID

i L

SCALE: r 2oo

DRAWN BY:W.A.W POWERS

DATE: OCTOBER, 1983

CHECKED BY:42C13SW8161 2.7444 WABIKOBA LAKE 220

18S 165l

145 125l

10 S 85l

65 45 25 l

O 2N l

4N 6N l

8N l

ION

l* K-

N=3

NM

CO UJ

uu

O

LINE 8W

X = 200 FEET

l Hz

INDEX MAP

H.*?O

-NO 9*

CORPORATE OIL ft GAS LTD.

l. R SURVEY

BATTLE ENERGY GRID

SCALE;

DRAWN BY ; WAW.POWERS

DATE: OCTOBER, 1983

CHECKED BY;

42C135W016I a.7444 WABIKOBA LAKE230

5N

B.L.O

10 S

15 S

T r^M, , ,-,r*

LEGENDLATE PRECAMBRIAN

Alkalic Intrusive RocksI2a Biotite Lamprophyre

MIDDLE TO LATE PRECAMBRIANMafic Intrusive Rocks

Ha Equigranular Diabase

EARLY PRECAMBRIAN (ARCHEAN)

BATTT-E tr^RoY C'jr.rO:iATION

LOCATION MAP

05 l rrv.le —-3

9a

Late Felsic Dikes or SillsFeldspar Porphyry Aplite

Cedar Lake PlutonHornblende-Biotite Granodiorite

Metasediments

42C13S*ai6t 2.7444 WABIKOBA LAKE

3d3b

"^

^^"~

OG

s- •r?:'-^^•' -.1—-'-

^^^

^^-^

C^———

nil li li *itlinn mi ^

E 240

Medium bedded Quartz WackeThickly laminated to thinly bedded Arkosic Wacke and Siltstone

X xfoliation attitude x

bedding attitude 27053

geological conlact

outcrop

geophysically inferred

gravel pit

gravel road

skidder road

edge of ridge

swamp

ladder silicification

small creek

carb

mt

bi

hem

pyAid

Asp

Bi

BISpr

Cot

ooulders

rock sample

carbonatization

magnetic

biotite

hematite

pyrite

Alder

Aspen 'D . , Indu Birch

arecBlack Spruce

Cotton wood

Induced Polarization area of line surveyed

LEGENDLATE PRECAMBRIAN

Alkalic Intrusive RocksI2a Biotite Lamprophyre

MIDDLE TO LATE PRECAMBRIANMafic Intrusive Rocks

lla Equigranular Diabase

EARLY PRECAMBRIAN (ARCHEAN)Late Felsic Dikes or SillsFeldspar Porphyry Aplite

Cedar Lake PlutonHornblende - Biotite Granodiorite

MetasedimentsMedium bedded Quartz WackeThickly laminated to thinly bedded Arkosic Wacke and Siltstone

foliation attitude

bedding attitude

geological contact

outcrop

geophysical!? inferred

gravel pit

gravel road

skid der road

edge of ridge

swamp

ladder silicification

small creek

boulders

rock sample

carbonatization

magnetic

biotite

hematite

pyrite

Aider

Aspen

Birch

Black Spruce

Cottonwood

•^Induced Polarization J" Anomaly

BATTLE ENERGY CORPORATION

UXATION MAPInduced Polarization area of line surveyed

42C13SW0161 2.7444 *ABIKOBA LAKE

D33 333333LCP

:;::; . qf b (w. sen)

LEGEND:

qfb BANDED QUARTZ FELDSPAR BIOTITE PARAGNEIS5(BANDED BY VIRTUE OF VARIABLE BIOTITE CONTENT/0-207.). SOME BIOTITE RICH LENSOID FRAGMENTS OF BIOTITE RICH MATERIAL RESEMBLING STRETCHEDCLASTS. SOME INTERBANDING WITH LEUCOCRATIC, SOMETIMES LIGHT GREENISH QUARTZO-FELDSPATHIC BANDS MINOR RANDOMLY ORIENTED SILICIFIED FRACTURES. FEW AREAS OF qfb CONTAIN INTERBANDS OF SERICITE RICH SCHIST.

gr- A MEDIUM GRAINED BIOTITE BEARING GNEISS OF gneiss GRANITIC COMPOSITION.

diab. A MEDIUM GRAINED MELANOCRATIC, MAFICINTRUSIVE ROCK WITH VERY MINOR PYRITE AND PYRRHOLITE.

INDEX MAP

BATTLE ENERGY CORP

48*45'

.LCP

SYMBOLS:

CUT TRAIL

SWAMP

OUTCROP OUTLINE

— CLAIM POST LOCATED (

DDDD ESKERan

FOLIATION STRIKE 8, DIP

SERICITE

QUARTZ VEINLETS

BIOTITE

CLAIM POST ASSUMED

set

qtZ.

biot

chl. CHLORITE

CORPORATE OIL ft GAS LTD.

GEOLOGICAL MAP

BATTLE ENERGY PROPERTY

SCALE: 1:2000

DRAWN BY: WA.W POWERS

DATE: OCTOBER, 1983

CHECKED BY :

(w qtz.+ li2

731202

-2 731206

LEGEND:

nfb BANDED QUARTZ FELDSPAR BIOTITE PARAGNEISS(BANDED BY VIRTUE OF VARIABLE BIOTITE CONTENT; Q-20%). SOME BIOTITE RICH LENSOID FRAGMENTS OF BIOTITE RICH MATERIAL RESEMBLING STRETCHED CLASTS. SOME INTERBANDING WITH LEUCOCRATIC, SOMETIMES LIGHT GREENISH QUARTZO-FELDSPATHIC BANDS MINOR RANDOMLY ORIENTED SILICIFIED FRACTURES. FEW AREAS OF qfb CONTAIN INTERBANDS OF SERICITE RICH SCHIST.

gr- A MEDIUM GRAINED BIOTITE BEARING GNEISS OFgneiss GRANITIC COMPOSITION.

didb A MEDIUM GRAINED MELANOCRATIC, MAFICINTRUSIVE ROCK WITH VERY MINOR PYRITE AND PYRRHOLITE.

•7-

INDEX MAP

BATTLE ENERGY CORP.

48'45'

86eOO' *fz^^^mmm

MILES

SYMBOLS:

or

•icpDDDD

t60

ser.

qtz.

biot

chl.

Au in

CUT TRAIL

SWAMP

OUTCROP OUTLINE

CLAIM POST LOCATED QCLAIM POST ASSUMED

ESKER

FOLIATION STRIKE S DIP

SERICITE

QUARTZ VEINLETS

BIOTITE '

CHLORITE

p.p.b.

CORPORATE OIL ft GAS LTD.

GOLD IN SOILSBATTLE ENERGY PROPERTY

r

SCALE: 1:2000

DRAWN BY: WA.W POWERS

DATE;OCTOBERJ983

CHECKED BY:

CVJ 00-J

o*-J

od

_.__ — r~[

25 N

20 N

15 N

ION

-B.L.O

20S

25S

2CO KX! O 200 400 feet

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for BATTLE ENERGYTitle GEOLOGY

Date: AUG. 1984Drawn: C G.

f MAP ^

FIO. 4

Scale: i'^200'Approved :

N.T.S.:File: M -61

x 10 CVIIj

ooO

*-J od

--a

25 N

20N

15 N

ION

B.L.O

20 S

25S

200 100 O 200 400 feel

ionayed

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for BATTLE ENERGYTitle GEOLOGY

SHOVING IP

Date: AUG. 1984Drawn: C.G.

r MAPANOMW.IES

O

Scale: r^aoo1Approved:

9 ^V 1/ 6/K

FIQ. 4

N.T.S.:File: M -61