LOWER DETOUR L AREA - Geology Ontario

32E13NEM79 2.4786 LOWER DETOUR LAKE 010

GEOPHYSICAL REPORT

ON THE

MIDLAND ENERGY PROPERTY

LOWER DETOUR LAKE AREA

PORCUPINE MINING DIVISION

DISTRICT OF COCHRANE, ONTARIO

Arrx l 9 1982

MINING LANDS

March 23, 1982 Mary Greer

Geophysical Technician

32E.3NE0e79 2.-1706 LOWER DETOUR L "E "

010C

TABLE OF CONTENTS

INTRODUCTION . . . . . . .......... ..... .. . . . . 1

PROPERTY DESCRIPTION .. . .. ... .. . ........ 2

LOCATION 4 ACCESS . . . . . . . . . . . . . . . . . ..... 2, 3

PREVIOUS WORK .................. . . . . . . . . 3, 4

SURVEY PROCEDURE . . . . . . . .. . . . . .. . . . . . . . . 4

TOPOGRAPHY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4

GEOLOGY ................................ 4, 5

ECONOMIC GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . 5, 6, 8

SURVEY METHODS . . . . . . . . . . . . . . . . . . . . . . . . . 8

ELECTROMAGNETIC SURVEY . . . . . . . . . . . . .. . . . 8, 9

PRESENTATION A DISCUSSION OF RESULTS ... 10, 11, 12

CONCLUSIONS A RECOMMENDATIONS .......... 12, 13

ILLUSTRATIONS

LOCATION MAP . . . . .. . . . . . . . . . . . . . . . .. . . . . 2 a)

GENERAL GEOLOGY . .. . . . . .. . . . . . .. . . . . . . . . 4 a)

GROUND VLF-EM SURVEY (1"r100 m)

VLF PROFILE ...................... back pocket

FRASER CONTOUR .......... ...... ... back pocket

GEOPHYSICAL REPORT

ON THE

MIDLAND ENERGY PROPERTY

LOWER DETOUR LAKE AREA


DISTRICT OF COCHRANE, ONTARIO

INTRODUCTION;

The Midland Energy Group was recorded by Ingamar

Explorations Limited on February 19, 1981.

A geophysical grid at 100 meter line spacing was

subsequently established by Ingamar Explorations Limited in

November 1981. During February 1982, a geophysical survey

(electromagnetic) was completed over the entire thirty-seven

claims. The instrument used for this survey was a Geonics

VLF-EM16 unit.

This work was conducted by and under the active

supervision of Daryl Bremner with assistance by Ivan

Bellemore. Preparation of the data was prepared by Mary

Greer. The purpose of this report is to briefly describe

the results attained in the said survey.

The anomalies detected are shown on the

accompanying map at a scale of 1 inch to 100 meters that

form an integral part of this report.

- 2 -

PROPERTY DESCRIPTION;

The Midland Energy claims consists of a

contiguous block of thirty-seven (37) 40 acre, unpatented

mining claims located in the Lower Detour Lake Area,

Porcupine Mining Division, District of Cochrane, and are

further described as follows:-

CLAIM NO. NO. OF CLAIMS

P 597077 - 083 7

P 609501 - 530 22

Total number of claims -- 37

The forementioned claims have been attested to by

Ingamar Explorations Limited, Cedar Hill, Connaught, Ont.

to be held in trust for Midland Energy Corporation,

463 - 1155 West Georgia Street, Vancouver, B.C. V6E 3H9.

LOCATION AND ACCESS;

The Midland Energy property is located approx

imately 130 miles northeast of the city of Timmins, Ontario,

at latitude 50 0 N and longitude 70O 36'W. The property can be

found between Sunday Lake and Lower Detour Lake, (two miles

north - northeast of Lower Detour Lake). The nearest town

is La Sarre, Quebec, located ninety (90) miles to the

southeast.

The property is accessible by float equipped

aircraft on Lower Detour Lake, then direct access to the

rtour take Project

Detour Lake ProjectLocation and Access Figure 1

- 3 -

property via boat down Detour River. Access is also

X possible via a winter road located three (3) miles west of

the property. This road services the Amoco property and

its Detour Lake Camp, which is found six (6) miles northwest

of the Midland Energy property,

(see location Map 1) .

PREVIOUS WORK;

The Ontario Department of Mines carried out a

aeromagnetic survey in 1964. These surveys indicated an

east-west strike over the general area of Midland Energy.

Further airborne geophysical surveys were carried

out by Questor Surveys Ltd. in 1980. This survey indicated

a strong conductor found with a strike length of .8 miles,

dipping 70 0 north. The best response is 2000 feet long

with a five (5) and six (6) channel anomalies. The conduc

tivity thickness is 12 mho and the magnetic correlation is

flanking 15 nT.

This conductor was found on the western end of a

string of en echelon conductors, possibly separated by some

faulting, however there is no data to further define this

observation. There is no magnetic correlations but a magnetic

high trends parallel on the down dip side of the found

conductor. The width of this response suggests the presence

of a wide source.

Surrounding the immediate vicinity of the Midland

- 4 -

Energy group a number of geophysical surveys were conducted,

inclxding vertical loop and induced polarization. These

surveys outlined a sulphide-bearing cherty tuff horizon

and main concentrations of sulphides.

To the east a ground magnetometer and a vertical

loop electromagnetic survey was carried out. This vertical

loop survey indicated east-west striking conductors.

SURVEY PROCEDURE;

An east-west baseline was established from the

#1 claim post of claim P-609515. This point was subsequently

called 0+00 and the baseline was extended for 1185 meters

east and 1330 meters west.

A grid system of picket lines at 100 meters spacing

with stations every 100 meters was established at right angles

to the baseline.

TOPOGRAPHY;

The Midland Energy property consists primarily of

spruce bog, which is found on dry flat topography with a few

infrequent outcrops located on the property.

GENERAL GEOLOGY;

The Detour Lake Area has not been well defined due

to the inaccessibility of the area, infrequent outcrops and

also because of the covering of glacial overburden which

varies between 10 - 100 feet thick.

GENERAL GEOLOGY

FELSIC INTRUSIVE ROCKS6a Massive granitic rocks. 6b Foliated granitic rocks.

Scale 1 inch to 4 miles

METASEDIMENTS3a Greywacke. 3c Quartzite.

FELSIC TO INTERMEDIATE METAVOLCANICS2a Rhyolite, dacite, trachyte:

2 l massive to foliated.2b Pyroclastic rocks, agglomerates

tuffs.

INTERMEDIATE TO MAFIC METAVOLCANICS 1a'Andesite, basalt: massive to

folliated.1o A mriuih~n4-Q omû-i, i u - i. Amphibolite, amphibole schist,

amphibole-pyroxene-plaqioclase gneiss

- 5 -

The regional geology appears to be mafic vol-/ -

canics with mino;^ felsic tuffs and graphitic siltstones.

This area is found along the northwest margin of the

Abitibi greenstone belt, lying between Timmins, Ontario

to the west and Val D'Or, Quebec to the east. The

greenstone belt is composed of mafic, ultramafic and

felsic tuffs, flows and intrusions along with volcan-^

iclastic rocks and sediments.

Local aeromagnetic maps indicated the area is under

lain predominently by mafic and felsic volcanics with a

few local ultramafic and felsic intrusives, infrequent

sulphide bearing horizons are also indicated.

More research from the Geological Compilations

Series, Coral Rapids - Cochrane sheet, Map 2161, indicates

that the area is .underlain by felsic intrusive rocks

consisting mainly of folliated granitic rocks.

The Midland property is found on clastic metased-

iments and felsic to intermediate metavolcanics of Archean

age. The general strike of this bedrock is east-west,

dipping steeply to the north and south. The dip is north

and south because the area is located on the axis of an

anticline.

ECONOMIC GEOLOGY:

Recent geological interest in the Detour Lake

area has resulted by the discovery of the Detour Lake

- 6-

gold deposit, presently being examined by Dome - Amoco -/ ,

Campbell - Red Lake joint venture.

This gold deposit lies just six (6) miles

northwest of the Midland Energy property and both

properties have basicly the same underlying bedrock.

The gold mineralization of the Detour Lake gold

deposits are found in three primary zones| the main zone

or chert zone, the quartz factor zone or hanging wall

zone and the footwall zone or talc-carbonate zone.

The main zone consists of narrow disseminated gold

veins with 10 - 15& sulphides, all associated with a narrow

cherty tuff horizon lying on the north limb of an east-

west striking anticline. This is all within a sequence

of fine grained arkosic and graphitic sediments, inter

bedded with basaltic or ultramafic flows and tuffs.

The main zone strikes at 75 - 80 O , dips 70 0

north and plunges 40 - 45 to the west. The quartz veins

are usually less than six (6) inches wide but has a high

sulphide and quartz content, therefore a high gold

content.

The depth of the main zone is approximately

1800 feet and is open at depth. It has a strike length

of 1400 feet (average) and averages 29 feet in horizontal

width down to the 900 foot level.

From the 900 foot level down to the 1800 foot

level the strike length varies from 700 - 100 feet and

the width (average) is 50 feet.

- 7 -

The hanging wall or quartz fracture zone consistsx .

of basalt and andesite volcanics. The quartzxfsecture zone

tends to have the same mineralization as the main zone

found within quartz veins with pyrrhotite and chalcopyrite

association while the gold occurs in tight smears

along slips and lenses.

Within 300 feet of the main zone lie three (3)

of the gold zones while one zone is found 900 feet above.

The average width of these zones are 10 - 15 feet but are

found to have a slightly higher grade than the main zone.

These zones are not continuous and do not extend from the

surface to the 1800 foot level.

The footwall zone consists of a sulphide bearing

chlorite-talc-carbonate rocks. The sulphides are mainly

pyrrhotite and chalcopyrite, and the mineralizations occurs

as specks or leafs within fractures, and are closely assoc

iated by varing directly with the chlorite and chalcopyrite

content. These talc-carborate zones occur along the plunging

hinge of the fold and run parallel to the main zone. It is

not essential to have quartz veinsin order to have some

mineralization.

The mining reserves are reported as follows:-

MAIN ZONES TONNES GRAM PER TONNE

(oz l tonne)

Main zone 16,000,000 4.36 (0.140)

Other zones 11,700,000 3.22 (0.104)

TOTAL RESERVES - 27,700,000 3.88 (0.125)

These figures include 15 percent dilution for open pit

- 8 -

and 5 percent dilution for underground ore.s

S

SURVEY METHODS;

The instrument used for this EM survey was a

Geonics VLF-EM16 unit. The sensitivity of this unit is

t l?o for the in-phase and - 185 for the quadrature. The

operating frequency for the EM 16 is from 15 - 25 kHz and

station selection is made by plug-in units.

For the purpose of this EM survey the station

used was Cutler, Maine, which has a frequency of 17.8 kHz.

All the readings were taken facing north at 25 meter

intervals along the grid and the topography was noted for

future use in the interpretation of the EM results.

ELECTROMAGNETIC SURVEY;

The VLF-EM method uses as a source one of the

many submarine communication transmitters in the 15 to 25 kHz

band found throughout the world. These communication radio

waves travel in a single mode parallel to the surface of the

earth along the earth-air interface.

Without vertical conductors and travelling over

flat .ground the magnetic field component of this radio or

surface wave is horizontal and perpendicular to its

direction of travel.

VLF instruments are capable of picking up

structures that change the direction of the waves by

measuring the tilt angle of the major axis of the

- 9 -

polarization eclipset This is illustrated by the tilt

angle being zero on flat ground, but when a conductor is

present the tilt angle will aquire a finite value. The

direction of tilt indicates the direction of the conductor}

however calculations of depth, depth extent, dip and width

of the conductor is very minimal.

The VLF shows the location of the upper limit

of dipping structures which can be seen on VLF profiles as

areas of greatest change in tilt angle per unit of

distance.

(10)

PRESENTATION AND DISCUSSION OF RESULTS

Using the orthogonal station NAA, frequency

17.8 kHz, six (6) conductors were found. They are

further described as follows:-

CONDUCTOR NO. TREND OF CONDUCTOR APPROXIMATE INTENSITY

82-A east-west

LOCATION

L11W 6+50S veryto

L3W 7+OOS good

82-B east-west L12W 0+50Nto

L4W 0+50N

good

82-C northwestto

southeast

LOOO 6+50Sto

L10E 11+OOS

fair

82-D northwestto

southeast

L12W 10+OOS goodto

L5W 12+50S

82-E east-west L6E 9+OONto

L11E 9+OON

poor

82-F east-west L6E 3+OONto

L11E 2+75S

poor

(see accompanying plan map - drawing 82-A)

(11)

Conductor 82-A shows a positive inphase cross

over with a negative quadrature anomaly. The overburden

may txe moderately conductive but the negative response of

the quadrature indicates possible association with local

sulphide concentrations. The strongest response is found

between L10W and L8W.

Conductor 82-B has a strong positive inphase

response. This response follows a flat, low negative

inphase which is followed by a stronger low negative

response. This may indicate a horizontal conductor of a

tabular form. The negative quadrature indicates further

association with some type of sulphide concentrations.

Conductor 82-C also shows a low positive

inphase cross-over with a negative quadrature anomaly.

This possibly indicates a conductor found under weakly

conductive ground and may have some sulphide association.

The main response lies between L2E and L4E.

Conductor 82-D has a weak positive quadrature

suggesting a poor conductor with a fairly non-conductive

overburden. The positive profile of the inphase has a very

strong response, the flat positive quadrature may indicate a

surrace conductor. This is noticeable between L9W and L6W.

Conductor 82-E has a very weak positive inphase

response and a very weak negative quadrature response. It

does indicate a favourable response, although the conductor

may be small and very shallow.

(12)

Conductor 82-F has a slightly stronger response

than conductor 82-E. The negative quadrature anomaly indi

cates the presence of possible sulphide mineralization.

CONCLUSIONS AND RECOMMENDATIONS

According to the Geological Survey of Canada,

Aeromagnetic Series, sheet 32 13, Detour Lake Map 2369C,

the area of the Midland Energy Property is flat with no

magnetic anomalies present. A strong magnetic anomaly,

trending northwest-southeast is found to the south of the

property but would have no influence from the conductors

found on the property. These conductors have no known

magnetic association.

The response of Conductor 82-A indicates the

need for further detailed work. This conductor has a

strong association with sulphide mineralization and is

the same conductor detected, (and previously described in

this report), by the airborne geophysical survey conducted

by Questor Surveys in 1980.

Conductor 82-C has the same characteristics as

82-A, only weaker and may be the easterly strike extension

of conductor 82-A, possibly separated by some sort of

faulting although this is not clearly indicated.

Conductor 82-B may possibly be a topographic

boundary of a low lying swamp or a buried swamp, since the

profile does indicate a horizontal tabular sheetlike conductor.

(13)

Conductor 82-D may also indicate a topo

graphic boundary but because of the positive quadrature

response may not necessarily indicate a swamp boundary,

since it is non-conductive.

Conductors 82-E and 82-F indicate a weak

response to a sulphide mineralization and can be further

investigated with more geophysical work.

Recommended, in the cases of possible sulphides,

would be a detailed grid across the anomalies and then read

with an Inductive Vertical Loop System with a fixed trans

mitter. This would give a detailed description of the said

conductors. Since there are few outcrops and the magnetic

suceptability of the local bedrock is low, rather than

recommending a geological or magnetic survey one recommend

ation would be the Induced Polarization Method. However,

a Magnetic Survey might be attempted to try and pick up

any sulphide mineralization. This would vary with the

depth of the overburden and sulphide concentrations. Once

the conductors are further described by the vertical loop

system or a magnetic survey the I.R. could be used to find

any possible sulphides, found in conductors 82-A,B,C,D,E &F,

especially 82-E and 82-F, which may only be indicating

disseminated sulphides.

Respectfully submitted,

March 23, 1982 Mary Gre\er


CERIIFICAJE

I, Mary Maureen Greer, of Lynden, Ontario, certify with

respect to this Geophysical Report:-

1. That I am a Geophysical Technician and reside at Site 3, R.R. #2, Box 9, Swastika, Ontario

2. That I graduated from Sir Sandford Fleming College at Lindsay, Ontario in 1978, with a diploma as a Geological Technician.

3. That I was employed as a Geophysical Technician by H.E. Neal 4 Associates Ltd., of Suite 607, 55 Queen Street East, Toronto, Ontario, for eighteenmonths.

4. That I have been employed as a private Geological Consultant for the past four months.

5. That I have been practising my profession for a period of three years and I am qualified to write this report,

March 20, 1982 Mary Gr* er\


EM16 VLF Electromagnetic Unit

I Pioneered and patented exclusively by Geonica Limited. the) VLF method of electromagnetic surveying has been proven to be a major advance in exploration geophysical instrumentation

Since the beginning of 1965 a large number of mining companies have found the EM16 system to meet the need for a simple, light and effective exploration tool for mining geophysics.

The VLF method uses the military and time standard VLF transmissions as primary field. Only a receiver is then used to measure the secondary fields radiating from the local con* ductlve targets. This allows a very light, one-man Instrument to do the job. Because of the almost uniform primary field, good response from deeper targets is obtained.

The EM16 system provides the in-phasa and quadrature components of the secondary field with the polarities indicated.

interpretation technique has been highly developed particularly to differentiate deeper targets from the many surface indications.

Principle of OperationThe VLF transmitters have vertical antennas. The magnetic signal component is then horizontal and concentric around the transmitter location.

i -M-r: l,

K .^Specifications

Source of primary field

Transmitting stations used

Operating frequency range

Parameters measured

VLF transmitting stations.

Any desired station frequency can be supplied with the instrument m the form of plug-in tuning units. Two tuning units can be plugged in at one time. A switch selects either station.

About 15-25 kHz.

d) The vertical in-phase component (tangent of the tilt angle of the polarization ellipsoid). (2) The vertical out-of-phase (quadra* lure) component (the short axis of the polarization ellipsoid compared to the long axis).

Reading time 10-40 seconds depending on signal strength.

Operating temperature range -40 to SO* C.

Operating controls

' 'ethod of reading

Scale range

Readability

from a mechanical Incline- "eterandauadraturefroma calibrated-i a' SuMi-g by audio !one.

in-phase ISO'%; quadrature

Power Supply

Dimensions

Weight

Instrument supplied with

Shipping weight

ON-OFF switch, battery testing pus button, station selector, switch, volume control, quadrature, dial 40S, inclinometer dial ̂SO%.

6 size AA (penlight) alkaline cells. Life about 200 hours.

42 x 14 x 9 cm (16 x 5.5 x 3.5 in.)

1.6 kg (3.5lbs.)

Monotonic speaker, carrying case, manual of operation. 3 station seie( olug-in tuning units (additional fre quencies are optional), set o) batte

4.5xg(10lbs.)

LIMITED LimilCL-r Designers 4 manufacturers oi geophysical instruments

2 Thorncliffe Park Drive, Toronto/Ontario/Canada

ouriesy ol Newfoundland A Labrador Corp. Ltd.

Aree* of VLF Signal* -. Coverage thown only lor will-known stations. Othe* reliable, tully operational station! a*itt. For lull information regarding VLF tignalt In your ara* eontult Geon/ca Limited. Extensive 11*14 experience hat proved that In* circlat ol coverage thown ara vary conservative and ere actually much largar In extent.

t

* 16 Profile over Lockport Mine Property, Newfoundland ditional cas* histories on request.

l l

vertical coil T T ITT to - o * io

'lion St lector3 tuning units can be plugged t ona lima. A switch salacts er station.

Receiving Coll* Vertical receiving coil circuit In instrument picks up any vartical signal present. Horizontal receiv ing coil circuit, after automatic 90* signal phase shift, leada signal into quadrature dial in sarias with the receiving coll.

In-Phate Dialshowa the tilt-angle ol the) instru~ man! lor minimum tlgntl. This angle it the measure ol the vertical in-phtsa signal expressed In percentage whan compared lo (ne horizontal Held.

Quadrature Dialit calibrated in percentage mark'ings and nulls the vartical quad'ratura signal in the vertical collcircuH.

selecting a suitable transmitter station as a source, the 16 user can survey with the most suitable primary field

muth.

j EM 16 has two receiving coils, one for the pick-up of the zo^'.ai (primary) field and the other for detecting any ""2 c -s vertical secondary field The coils are thus ortho-3 :"d 3'e mounted ins'de t.ê instrument "handle".

1 ac'.ai measurement is done by first tilting the coil e~::'y to minimize the signal in the vertical (signal) coil and ^ further sharpening the null by using the reference signal )uck out the remaining signal. This is done by a calibrated ladrature" dial.

The tangent of the tilt angle is the measure of the vertical in-phase component and the quadrature reading is the signal at right angles to the total field. All readings are obtained in per centages and do not depend on the absolute amplitude of the primary signals present.

The "null" condition of the measurement is detected by the drop in the aud ; 0 sigral emitted 'ro-n the patented resonance loudspeaker. A jack is provided for those preferring the use of an earphone instead.

The power for the instrument is from 6 penlight cells. A battery tester is provided.

r. S

Ontario

Report of Work

(Geophysical, Geological, Geochemical and Expenditures)

4 63 The Min 32EI3NE8879 3.4706 LOWER DETOUR LAKE 900Type of Survey(s)

Linecutting and E.M. 16 SurveyClaim Holder(s)

Ingamar Explorations Limited\V,l\

Township or Area

Lower Detour AreaProspector'1 Licence No.

T-836O rJT .Survey Company

Ingamar Explorations LimitedSurvey Dates (llntcuttlng to office)

as life ffi.Total Miles of line Cut

61.1?Name and Address of Author (of Geo-Technlcal report)

Mary Greer___Gen* Del,. Kirkland Lake OntarioSpecial Provisions Credits RequestedInstructions

For first survey:Enter 40 dayt, (Thli Inoludn Mm cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Geophysical

- Electromagnetic

- Mignttomittr

- Radiometric

- Other

Geological

Geochemical

Dayt per Claim

40

Man DaysInstructions

Complete reverse side and enter total (s) here

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Days per CI afm

Airborne Credits

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

Electromagnetic

Magnetometer

Radiometric

Expenditures (excludes power stripping)

Days per Claim

Type of Work Performed

Performed on.Clalm(s) '

Calculation of Expenditure Days.Credits. --!..'i , ,. - : ] .... ! :.|- l.' l'

Total Expenditures - - - -v--Total

Days Credits

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

Report CompletedDate of Report

, 24/82Recorded HoW^r or,Asent (Siflfiature)

K ffCertification Verifying Report of Work

Mining Claims Traversed (List in numerical sequence)Mining Claim

Prefix

P

illWmW* tw*'*

'•1 '^P"'*t,1Ev ij^jp^"^

IIIf'-S.*-sV; -vSiW-rtr •i- f'.", -im*,',;y^vj?liWMi•- *.,.^5 Vi--i 'J"j.

'̂îk4fKVf;'.^'*'•y'"'.- 'f **:,'f. •ii','-." ,. ,''r Vff^", :C\-'K

''i'*"*'y V'v-W'^V'

:,V:'^':fr

v'-.-iJ;-./'

^•'•'h

: 'V ;*;Q:

,'S^V'^'* *V;t v,- '

W&' •'4'iA: -i?^'Vj.f-r,..'

ill4•J?M-i-?Vn'.' 14,-." 1' i

'^",*4-/' ^ ^

Number

609501609502609505609504609505609506609507609508609509609510609511fe)9512s60951 3609514609515609516609517609518609519609520609521C.r*QCOObuy?cc60952360952460Q525

Expend. Days Cr.

4040404040404040404040404040404040404040404-O

40

40

40

N

Mining ClaimPrefix

P"';v'A'y#J^•vps.-:.^fV."J••V'r-j'O'*L s, ? *-i^jV-UW^v^;;'

-i'.;. ,,T( i, i t ,••',-j'"'-r^, ,-,'M: i ,;W'ti

V-V'^-;'?i",- .'' : '-'.'

" '* '"' ; ''

,V' ' .-, " k'

:! *if'-':' ' '

' ''; "*\ ''•."'^'h.(•'•i, ''-. -!-'i .'''".r'",'.'

mw

INING

R

Roco

Number

609526609527609528609529609530S97077S97078&97079B97080.597081597082.697083/^ p. f \ f f 'CE Fi3 1 ft *nooKit) 19o^ —

LANDS SECT

iCOftD

['EG 25 198

•f^No........

Expend. Days Cr.

404040404040404040404040

y—

ON

ED i)

(

0

Total number of mlnlnfl claims covered by this report of work.

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

Name and Postal Address of Person CertifyingM* Hibbard- President- Ingamar Exploration Limited

hereto, having performed the work

i(Date Certified . . .-— 1 CertHied'by /Signature) S

Cedar Hill , Connaught, Ontario | Feb., 24/82 Xsjp&ff /,/^^J

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

F

Type of Survey (s

Township or Are;

Claim Holder(s)

Survey Company

Author of Reporl

Address of Authc

Covering Dates oi

Total Miles of Lir

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

) GEOPHYSICAL SURVEY (ELECTROMAGNETIC)

i Lower Detour Lake Area

MIDLAND RESOURCES LIMITED (VANCOUVER)

INGAMAR EXPLORATIONS LIMITED

\ Mary Maureen Greer

,r Site 3. RR# 2, Box 9; Swastika, Ontario

FSiirvfiy 10/11/81 to 23/3/82

ie Cut 36

1 SPECIAL PROVISIONS CREDITS REQUESTED

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

ENTER 20 days for each additional survey using same grid.

(linecutting to office)

miles approx. :

DAYS~, i - i per claim Geophysical

-Electromagnetic., .40

r,fn\n ira i

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

Magnetometer F.lprrrrimacrnetir RaHinmptrir

HATF; mwf(Af\

Res. Geol.

Previous Surveys

(enter days per claim)

to kl SIRNATITBR. Mcl/frl tfatf' "Author (of Report or Agent

( ) ('iV - V'-"7Qualifications f, ! ^ '"

File No. Type Date

l................... ................. .................

Claim Holder

i

MINING CLAIMS TRAVERSED List numerically

w

(prefix)

P

PP

...............P.............D

P

P

P

P

P

P

...............R.............P

P ...............R.............

P

P...............B.............

P...............B............

P...............B............

P ...............P.............

P

P ..............P.............

(number) 609501

609503609504

,,,,,60?505.............oU x ̂ UoX OQCOT1

609508

609510

609512

609514

609516 .........6025.17.............

609518

609520 .. .... .60352.1.............

609522y'riQCO'Z Q ̂ fffnr

609524 609525 i***t***tfTr*rtnr*****t*******i*609526

..........6..Q9.5.2I........... 609528

.........6D2522..............

697078 697079**t***tt*rtr*r*rtr*r*t************

697080

697082 .........692QB3.............

TOTAL CLAIMS? ?7

i

i

ia

837 (5/79)

GEOPHYSICAL TECHNICAL DATA

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

Number of Stations. Station interval ——Profile scale ————.

Contour interval.

636

inn

1 inch = -

.Number of Readings 2619 approx.

..Line sparing 100

c Instrument.Accuracy — Scale constant.

Diurnal correction method.

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

uH

O

SsGwW:

Instrument,Coil configuration

Coil separation ——

Accuracy .————

Method:

Frequency-————

Parameters measured.

GEONICS VLF-EM16

Vertical and Horizontal

Infinity

Fixed transmitter O Shoot back Q In line Cutler. Maine (frequency 17.8 kHz)

O Parallel line

(specify V.L.F. nation)

In-phase and Quadrature

Instrument.

Scale constant.Corrections made.

O Base station value and location.

Elevation accuracy.

< Nh-*

o4

O o*Q tJ O P Qz;

Instrument —————————— Method D Time Domain Parameters — On time ———

- Off time ———

\ l Frequency Domain _ Frequency _____

_ Range ————.——

— Delay time.

Integration time.

Power —

Electrode array— Electrode spacing , Type of electrode

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

Corrections made.

RADIOMETRIC Instrument^——.Values measured.

Energy windows (levels)——.^^———-—————————-—————^^^^—^^————Height of instrument____________________________Background Count. Size of detector.^—^———————-..—.—.——-—-.^-—-—————^———^—...^——.—.Overburden —————————-.^—-—————-————^——-——————.————.-————

(type, depth - include outcrop map)

,S (SEISMIC, DRILL WELL LOGGING ETC.) of survey_________________________

Instrument ̂ ———^—^———.———————.^^^^—. Accuracy__________________________Parameters measured.

Additional information (for understanding results).

Type of survey(s) Instrument(s)

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

(specify for each type of survey)

Aircraft used—————-————-——————^^^—-——————.Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude______________________________Line Sparing Miles flown over total area________________________Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD

Numbers of claims from which samples 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.

GeneraL

ANALYTICAL METHODS

Values expressed in: per cent p.p. m. p.p. b.

D D D

Cu, Pb,

Others—.

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

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

Field Laboratory Analysis No.(__________ .tests)

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)

General.

Appioval FILE,

Mining landi Commcnu

Fb: Geophysia

Comments

lwiihio *** o*ln with coricctlonsl D*1*

J JTo: Geology- Expenditures

Comnrxnn

ApfMOvtd With to ict *p*1n with correction!

ITo: Geochemistry

T

With lo willh eon*cliix**

j J To: Mininp Lantk Scciion, Room G462, Whiiney Block. (Tel: 5-13BO)

1982 04 26 2.4706

Mining RecorderMinistry of Natural Resource*60 Wilson AvenueTimmins, OntarioPAN 2S7

Dear Sir:

We have receive* reports and maps for a Geophysical (Electromagnetic) Survey submitted under Special Provisions (credit for Performance and Coverage) on Mining Claims P 609501 et al in the Area of Lower Detour Lake.

This material will be exaalned and assessed and a statement of assessment work credits will be issued.

Yours very truly.

E.F. AndersonDirectorLand Management Branch

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

J. Skura/amc

cct Ingamar Explorations Limited Connaught, Ontario

INGAMAR EXPLORATIONS LIMITEDCEDAR HILL CONNAUGHT. ONTARIO RON 1AO

TEL (705) 433-3551 or (705) 433-3521

TELEX 067-81502

March 24, 1982 RECEIVED

APK l g mMINING LANDS SECTION

Ministry of Natural Resources Land Management Branch Whitney Block, Room 6450 Queen's Park Toronto, Ontario M7A 1W3

ATTENTION; MR. FRED MATTHEWS

Dear Mr. Matthews,

Please find enclosed three geophysical assessment reports for the following properties:-

Midland Energy Property

Award Resources Property

Kenar Property

The above properties are all located in the Detour Lake Area, Porcupine Mining Division, District of Cochrane.

In accordance with the Mining Act we are filing these properties for assessment.

Thank you for your cooperation.

Sincerely,INGAMAR EXPLORATIONS LIMITED

Mary Greer, Geophysical Technician

MG/ab

Enc .

SUNDAY LAKE M-3003

50000-uu—n IP IP 421402

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1595702 \395709 595714 . 595721'595726 f 595733 5957-39 595699JL

156B71593586)595668 l 885B47 5a5840 ' 585e 37 , 583830 '383627563820 3 3 854,885855 l 5957SS 586517 5865161 586515 566313 566573,586574-.^J..-. — -J_________L

43 4241' 40 39 38

37' 36' 35 34 33 32 3179 0 45'

ATKINSON LAKE M-2622

326I3NEM79 2.4706 LOWER DETOUR LAKE 300

n—500 00'

59

56

55

54

53

79b 30

AREA OF

LOWER DETOUR LAKE

DISTRICT OFCOCHRANE


SCALE: 1-INCH 4O CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINESCANCELLED

CS.© LocL.O.

MR.O SRO

NOTES400' Su' face rights reservation arouna all lakes and rivers

HL'"" f - ffif.'; Aroa* withdrawn from staking under Section

.13 of the Mining Act ( R.s.o.1970). ? vi4*\ No. FiU Dot* Disposition

'iJNR.W. 1/BI IBB5I1 15/t/ei S.R.O,

DATE OF ISSUE

JAN 1 1 1983

ResourcesTOfiONTO

498793

NATIONAL TOPOGRAPHIC SERIES 32EI3

PLAN NO -M. 2603

ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

32E13NEW79 2.4706 LOWER DETOUR LAKE210

M

0*MT U** Protect

SYMBOLS

inpn ase '

Claim post : *

Claim line —

INSTRUMENT

eonics VLF-EM16

Station used: NAA

Cutler j Mair\e

-. 17.8 kHz

Vertical Scale-- l"- t 4 OV,

V L F Conductors

M mor :

MIDLAND ENERGY CORPORATION

LOWER DETOUR LAKE PROJECT

GROUND VLF-EM SURVEYDETOUR LAKE AREA

PORCUPINE MINING DIVISIONDISTRICT OF COCHRANE

l 00 l 00 Z.OO 300 METERS

t INCH TO 100 METERS

INGAMAR EXPLORATIONS LTD.CONNAUGHT ONTARIO

DRAWN BY. M.M.Xi. APPROVED BY; K.H

DRAWING No DATE: MARCH 1983,

O (O O N m OD

- zoos

//CO S

/200S

32E13NE9079 2.4706 LOWER DETOUR LAKE 220

ff

LOWER DETOUR L AREA - Geology Ontario

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