MCKENZIE ENERGY CORP.

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PIC

MCKENZIE ENERGY CORP.

Geophysical Report On A

Magnetometer Survey and

Vector Pulse Electromagnetometer Survey Pic Township, Thunder Bay Mining Division Lat: 48 0 44'N Long: 86 O 18'W

Authors: Cliff Candy, B.Se. Geophysicist Glen E. White, B.Se., P.Eng.

Consulting Geophysicist Date of Work: Mar.l- 21, 1983

Date of Report: May 24, 1983

RECF1WED

OCT l 3 1983

MINING LANDS SECTION

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42D09NWee94 2 .5890 PIC TABLE OF CONTENTS PAGE INTRODUCTION . . . l

PROPERTY ... : :... !

LOCATION AND ACCESS . . . ! GENERAL GEOLOGY . . . 2 PREVIOUS WORK . . . 3 MAGNETOMETER SURVEY . . . 4 VECTOR PULSE ELECTROMAGNETOMETER SURVEY... 5 " 6 DISCUSSION OF RESULTS...7-9 SUMMARY AND CONCLUSIONS...9-10

INSTRUMENT SPECIFICATIONS...H-15

ASSESSMENT WORK DETAILS ... 16

STATEMENT OF QUALIFICATIONS...17-18

REFERENCES ...19

ILLUSTRATIONS

Figure 1- Location and Claims Map

2A- Composite Profile Map, Constant Gain Channel Three

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2B- Composite Profile Map, Primary Field Normalized Channel Three

I3A- Composite Profile Map, Total Field

Magnetic Intensity

3B- Contour Map, Total Field Magnetic Intensity

Figure 4-39 Component Profiles

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APPENDIX Data Listing

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Mckenzie Energy Cloims

MCKENZIE ENERGY CORPORATION

LOCATION AND CLAIMS MAP

l : 50,000

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INTRODUCTION

During the winter of 1983, Glen E. White Geophysical Consulting and Services Ltd. conducted a program of

vector pulse electromagnetometer surveying and detailed magnetometer surveying on fifteen claims for McKenzie Energy Corp. During the pulse E.M. survey 155 stations were occupied in some 7.2 kilometres of coverage from two transmitter loop setups. The magnetometer survey entailed the occupation of some 1420 stations. The objective of the survey is to delineate structure that would aid in the development of diamond drill targets

according to the Heralo type gold deposits.

PROPERTY

The property is situated in the Pic Township, Thunder Bay Mining Division, Ontario. The property

is shown on the Pic claim sheet G-630 and is comprised of 15 contiguous unpatented claims:

645822 to 645827, inclusive

655502

655510 to 655515, inclusive 655520 and 655521

LOCATION AND ACCESS

The claims are situated approximately 22 kilometres west of Hemlo, Ontario and some 6 kilometres east of Marathon Ontario, on the north shore of Lake Superior. The property is located at 48 O 44'N latitude by 86 O 18'W longitude on the Marathon Toposheet, Heron Bay Geological Map 2439 and Highway Geological Map 2440.

The property is accessible from Marathon via some 8 km southeasterly Highway 17 to a dirt road leaving the highway to the north, then approximately three kilometres into the property.

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GENERAL GEOLOGY

The geology of the McKenzie Energy Corp. is described by E. Amendolagine in his report of September, 1982 as

follows:

"The general geology of the area consists mainly of a belt of metasediments and metavolcanics lying between Early Precambrian-Archean-Heron Bay Pluton to the south, Gowan Lake Pluton to the north, and Proterozoic Port Coldwell Alkalic Complex to the west.

The Gowan Lake Pluton, the Heron Bay Pluton and the metavolcanics and metasediments are all intruded by the proterozoic mafic and felsic dikes and sills.

The eastern portion of the metavolcanics and sedi ments in which the Corona gold mineralization is found, lies between the Cedar Lake Pluton and the Pukaskwa

Gneissic Complex Formations. These are also intruded by the mafic and felsic dikes and sills. The relationship, origin and control of the gold mineralization is not ascertained. This is currently under study. The gold mineralization to date is associated with the metasediment-metavolcanic formations and contacts. The true con- . trols of the gold mineralization are not known. The metasediments are considered the favorable formation. These formations can be traced from east of the Hemlo area to Lake Superior in the west. At the western ex treme there is a metasediment belt striking north

easterly between the Port Coldwell Alkalic Complex and the Gowan Lake Pluton."

The Heron Bay geologic map, shown in the section, indicates that the geology consists of the projected contact of the intermediate and mafic metavolcanics and metasediments.

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PREVIOUS WORK

The history of the area is also described by E. Amendolagine in the above mentioned report:

"The mineral exploration within the Heron Bay area was sporadic.

The initial activity in search of gold dates back to 1872 near the Heron Bay Station. Assay results obtained from pits by Bell, 1873, returned values of 0.06 oz. Au and 7.03 oz. Ag. However, most of the early work was done in the 1920-1930's by J. Lecour. The first recorded assessment work was by Ollmann and Williams in 1945 on a property near Moose Lake. Since

that time, numerous medium and large companies have performed work in the area. Reference: Heron Bay Area report, Appendix I and Hemlo Area Geology report,

Appendix II, Economic Geology, pg. 50.

The current status is that the Corona property has some 1,000,000 tons of better than 0.20 oz. Au and that the adjoining ground held by the Long Lac Group has re- . ported some 1.8 million tons of 0.175 oz. Au minerali zation. This information was reported in the August 19th, 1982 NORTHERN MINER and in company reports.

There is no history of work done on the property covered by this report."

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PROTON PRECESSION MAGNETOMETER SURVEY

The magnetometer survey was carried out utilizing two GSM-8 proton precession magnetometers. One of these was operated in conjunction with a CMC MR-10 base magnetometer recorder to allow diurnal and

micropulsation variation removal. Operator precautions of demagnetization and consistancy were observed and field clock to base magnetometer timing skew was maintained within one second per day. Corrected, unfiltered data are plotted on each of the base maps.

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VECTOR PULSE ELECTROMAGNETOMETER SURVEY

The Crone pulse electromagnetometer system is a time domain E.M. system which can be used in the standard hor izontal loop mode, fixed source mode or in a downhole mode.

The primary field for the standard horizontal loop method is produced by a portable transmitter loop of 6, 10, or 50 metres diameter. A depth of search of approx imately 751 of separation is obtainable due to the high sensitivity of the receiver system. As measurements of the time derivative of the secondary field occur during primary field off time the method is relatively free from geometrical restrictions. Interpretation is accomplished with the aid of Slingram horizontal loop curves.

The primary field for the 2000 watt fixed source sys tem is provided by a 500 by 1000 metre transmitter loop. A 150 by 150 metre loop is utilized with the 500 watt sys tem. The time derivative of the secondary field resulting from the presence of a conductor is sampled at eight win dows on the decay curve, during primary field off time. These eight channels of secondary field information are equivalent to a wide spectrum of frequencies from approx imately 2 KHz to 16 Hz thus allowing conductor character and strength determination. The vertical and horizontal components are obtained at each station on the traverse, using the convention of vertical component positive upwards and horizontal component positive away from the transmitter loop. In areas of high surficial conductivity the primary field on time of 10.8 ms, and the receiver delay times may be doubled in order to obtain late time information. Time synchronization between transmitter and receiver is by radio or cable link.

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The apparent primary field information is recorded at each occupied station. Normalization of the data with respect to instrument gain produces a constant gain plot. In this format a vertical plate-like conductor anomaly would be symmetric. Normalization with respect to the

apparent primary field at each station provides a constant primary field plot that is useful in recognizing conductors present in the far primary field and in correlating ano maly amplitudes from line to line. The anomalies lose symmetry in this format but the condition of anomaly am plitude dependence on distance from the loop is relaxed. In the case of stacked profiles on plan maps it is prac tical to use the advantages of both of these methods and plot a constant gain profile normalized to the apparent primary field at a station near the conductor axis. This facilitates the correlation of conductors from line to line at varying distance in coverage from several trans mitter loops.

The vector focus method of data display is useful in some line source conductor conditions. A resultant vector can be obtained by the vector addition of the ver tical and horizontal components of the primary field. A perpendicular to this resultant indicates the apparent eddy current position.

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DISCUSSION OF RESULTS MAGNETOMETER SURVEY

The magnetometer survey consisted of 19 lines of coverage at 12.5 metre stations and is displayed on plan map Figures 3A and 3B. The former of these is a composite profile presentation and is most useful in displaying high spatial frequency anomaly effects and the latter is a data posting and contour map and dis plays large scale attributes of the data set. The

magnetics data has been corrected for diurnal variation but has had no filtering or other treatments applied.

The most obvious feature in the data is a strong northeast trending magnetics lineament. This lineament is a very high spatial frequency feature registering in as few as two stations data. This lineament is corre lated with a topographic feature which may represent a fault escarpment.

In the northwestern area of the grid an general increasing gradient to the northwest is evident. This may be associated with the approach to the Port Cold well Alkalic Complex in this direction. Also in this area a pronounced magnetics low is present at approxi mately SOON on lines 200E- 400E. This may be a magne tics minerals deficiency resulting from alteration within the metavolcanics.

Other areas of the grid show more minor isolated magnetic features without good line to line correlation. These minor features are most easily discerned on

composite profile map Figure 3A.

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Vector Pulse Electromagnetometer Survey The vector pulse E. M. data is presented in profile form in both constant gain and primary field normalized formats. In addition to this, the line to line anomaly relationships have been illustrated on composite profile maps, Figures 2A, 2B. These maps are comprised of channel three data plotted in both constant gain

field normalized formats. The former of emphasizes conductors present in the near transmitter loops and supports conductor depth interpretation. The latter allows anomalies present in the far field of the

loops. A second order polynomial fit has

and primary these formats field of the attitude and recognition of transmitter been removed from the data presented on the primary field normalized map in order to minimize the half space contribution to amplitude. On each of the four maps the_V*

ponent and the first deVivative filtered

horizontal vertical corn-ponents are plotted such that anomalous responses occur as minima, towards the grid east.

The pulse E. M. data in general does not show evi-dence of clearly defined plate-like conductors in the area of the grid. The responses obtained

very weak and are more likely results of ing effects across contact boundaries and continuities within the lithology. These are not strongly expressed and due to the line separation there exists an ambiguity to line to line correlation.

are generally current gather-other dis-lineaments 200 metre with respect

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geological mapping by G. Cavey indicates that correlation of these anomalies should be made with a northwesterly strike. These lineaments are illustrated on plan map Figures 2A and 2B and on component profile Figures

35-39.

The best correlated and longest strike length of these features are two parallel zones originating in the area of the strong magnetics low in the north east corner of the grid. These lineaments are of approx imately 800 metres strike length and would intersect the trace of the possible fault structure observed in the magnetics. A weaker flanking lineament is detected in the northeast area, also intersected by this possible fault zone. In addition, two isolated effects are

detected in the central area of the grid, on lines 600E and 1000E.

The possible fault interpreted from the magnetics data does not appear to have a clear conductive expres sion .

SUMMARY AND CONCLUSIONS

Glen E. White Geophysical Consulting and Services Ltd. conducted a program of vector pulse electromagnetometer and proton precession magnetometer surveying for McKenzie Energy Corp. on their fifteen claims in Pic Township, Ontario.

The magnetics survey shows a high spatial frequency lineament as its' most prominent feature. This feature is correlated with an escarpment and may be a north easterly trending fault zone. The areas of slight mag netics highs may be correlated with more mafic units within the metavolcanics and would thus be useful as an

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aid to mapping these rock types. A strong magnetics low is observed in the northeast area of the grid which may be related to alteration effects in these rocks. It is recommended that detailed geologic mapping be undertaken using the magnetics data as an aid.

The vector pulse E.M. survey shows a series of trends, interpreted as striking northwesterly, which probably result from current gathering effects across geologic contacts and other discontinuities. As a further aid to mapping these boundaries an additional rock property measure would be useful. Thus an induced polarization survey is recommended in areas where it would aid the geologic mapping of the property.

Analysis of these geophysical measures and the geology, according to the experience gained in the Hemlo Corona

area should allow the development of a diamond drill program to test for this type of deposit.

Respectfully submitted

/v//

Cliff Candy, B/Sc. Geophysicist

Vi n -* l l \ r - - ^r

Glen E. White, B.Se., P.Eng, Consulting Geophysicist

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PEM SPECIFICATIONS O S Time t Current On o O) o

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Prims * —— Current Off *

— ramp shut off time

t-"0" Time ii i ' M 8 secondary samples ry Pulse Sample

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Tx Loop r.irront Rx Coil Voltage

Current Off time: 9.4ms Current on time: 10.8 ms

Current shut off (ramp) time: 1.4 ms

Sample times (zero to centre of sample): .15ms, .45ms, .85ms, 1.45ms, 2.45ms, 3.75ms, 5.85ms, 8.85ms. Sample width: 100 us

Zero time set at drop off point of primary pulse

TRANSMITTER - Transmitter power and loop size may be increased to obtain increased penetration. Weight, portability and power capabilities of the control instrument are the limiting factors. The standard transmitter is designed to be carried by two men.

Loop diameter Loop current Loop applied voltage Loop output Loop weight Control unit weight Control unit dimensions Battery supply weight Battery supply

minimum 4 meters (13 feet) 15 to 20 amps

24 volts

minimum 4500 amps x meter 2 11.8 kilos (26 Ib)

10 kilos (22 Ib)

20.5cm x 25.5cm x 36.5cm (8" x 10' x 14.5") 18.1 kilos (40 Ib)

2 of 12 volt, 14 to 20 ampere hour Timing control by radio synchronization

RECEIVER

- Receive coil dimensions: 55cm x 15cm (22" x 6") - Receive coil weight: 4.5 kilos (10 Ib)

- Preamplifier in coil

- Preamplifier batteries: 2 of 9 volt - Receive coil tripod mounted

- Receiver measuring instrument dimensions: 28cm x 18cm x 21.5cm (11" x 7" x 9") - Receiver measuring instrument weight: 6.3 kilos (14 Ib)

- Timing control by radio synchronization - Primary sample width: 100 us

- Primary sample can be swept through primary pulse by means of a time calibrated pot - Zero time set at primary pulse drop-off

- Secondary samples (eight of them) width: 100 us

- Secondary samples time (zero to middle of sample): (1) .15ms (2) .45ms (3) .85ms (4) 1.45ms (5) 2.45ms (6) 3.75ms (7) 5.85ms (8) 8.85ms - Automatic sampling for 5 seconds then all samples automatically stored - Sample read out by means of meter

- Continuous sampling possible by switching function switch to "Continuous" - Noise can be monitored by switching function switch to "Noise"

- Battery supply: 24 volt rechargeable. 2 of 12 volt Gel GC 12-15

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VERTICAL COMPONENT HORIZONTAL COMPONENT

VPEM ANOMALY SHAPE

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VERTICAL COMPONENT

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GSM-8 PROTON PRECESSION MAGNETOMETER SPECIFICATIONS RESOLUTION: ACCURACY: RANGE: GRADIENT TOLERANCE; OPERATING MODES: OUTPUT: EXTERNAL TRIGGER: POWER REQUIREMENTS: POWER SOURCE: BATTERY CHARGER: OPERATING TEMPATURE; DIMENSIONS: WEIGHT: l gamma

il gamma over operating range

20,000-100,000 gamma in 23 overlapping steps

Up to 5000 gamma/metre

MANUAL PUSHBUTTON, new reading every 1.85 sec., display active between readings

CYCLING, pushbutton initiated, 1.85 sec. period

SELFTEST, pushbutton controlled, 7 sec. period

VISUAL: 5 digit l cm (0.4") high Liquid Crystal Display, visible in any ambient light

DIGITAL: Multiplied precession fre quency and gating pulse

ANALOG: Optional 0-99 or 0-999 gamma Permits externally triggered operation with periods longer than 1.85 sec.

(optional minimum period 0.9 sec.) 12V 0.7A peak, 5mA standby

INTERNAL: 12V 0.75Ah NiCd rechargeable battery 3,000 readings per full charge EXTERNAL: 12-32V

Input: 110/220V 50/GOHz; output: 14V 75mA DC

-35 to +55C

CONSOLE: 15x8xl5cm (6x3^x6") SENSOR: 14x7cm dia (5*5x3" dia) STAFF: 175cm (70") extended, 53cm

(21") collapsed

2.7kg (6 Ib) per standard complete with batteries

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ASSESSMENT WORK DETAILS

1. Type of Survey: 1) Proton Precession Magnetometer

Survey 2) Vector Pulse Electromagnetometer

Survey

2. Township or Area: Pic Township, Ontario 3 . Numbers

4 . Number D 2)

of Mining Claims traversed by Survey: 645822 to 645827, inclusive

655502

655510 to 655515, inclusive

655520 and 655521

of Stations established:

Magnetometer Survey: 1420 stations

VPEM Survey: 155 stations

5. Make and Type of Instrument Used: D

2)

Gem Systems GSM-8 Proton Precession Magnetometer Crone Pulse Electromagnetometer

6. Sensitivity — - 1) Magnetometer: 1 gamma

2) VPEM: 1 part per thousand of primary field

7. Frequency Used and Power Output: VPEM Survey; 8. Special l) 2) 0 8 channels, 2000 Watts Provision Credits:

Magnetometer Survey 40 days x 15 claims VPEM Survey 20 days x 15 claims

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STATEMENT OF QUALIFICATIONS Name : Profession: Education: Professional Associations : Experience: CANDY, Clifford, E. Geophysicist B.Se., Geophysics

University of British Columbia

Society of Exploration Geophysicists Six years Geophysicist with Glen E.

White Geophysical Consulting S Services Ltd. with work in B.C., Yukon, Saskatchewan,

Quebec, southwestern U.S.A. and Ireland.

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NAME : PROFESSION: EDUCATION: PROFESSIONAL ASSOCIATIONS: EXPERIENCE: 18 STATEMENT OF QUALIFICATIONS

WHITE, Glen E., P.Eng. Geophysicist

B.Se. Geophysicist - Geology University of British Columbia. Registered Professional Engineer, Province of British Columbia.

Associate member of Society of Explor ation Geophysicists.

Past President of B.C. Society of Mining Geophysicists.

Pre-Graduate experience in Geology - Geochemistry - Geophysics with Anaconda American Brass.

Two years Mining Geophysicist with Sulmac Exploration Ltd. and Airborne Geophysics with Spartan Air Services

Ltd.

One year Mining Geophysicist and Tech nical Sales Manager in the Pacific north-west for W.P. HcGill and Assoc iates.

Two years Mining Geophysicist and supervisor Airborne and Ground Geo physical Divisions with Geo-X Surveys Ltd.

Two years Chief Geophysicist Tri-Con Exploration Surveys Ltd.

Twelve years Consulting Geophysicist. Active experience in all Geologic pro vinces of Canada.

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M REFERENCES

Amendoligine, E. , Property Examination and Evaluation Report for McKenzie Energy Corp., Sept. 10, 1982

Muir, T.L. , Geology of the Heron Bay Area,

l District of Thunder Bay, Ontario

m Geological Survey, Open file Report

B 5261, 1979

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VECTOR PULSE ELECTROHRGNETOMETER COMPONENT PROFILES

GLEN E. NHITE

GE OPHYS3 Cfl L CON S ULTIN G J. SERVICE E LTD.

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INSTRUMENT: CRONE P.E.M,

METRES

i oa saa 400

MCKENZIE ENERGY CORP.

PIC TOWNSHIP RREfl VECTOR PULBE ELECTROMflGNETOMETER

HORIZQNTRL COMPONENT E

(37)

zzzzzzzz Ln 01 en in C'OHaE'EiClfi'Z IP El C3 C? 13 in d in O in D in O ® Z O D in o in 't t en m wry — -•inQin—•-•fj eg

LOOP

D O Q-^fe-q—D P D

-- 0

~ _ o c;_{C J} ^~ 50 ~-^- T C ~ 125 -- 150 BCRLE P. F, K. 4 OR

-GLEN E. WHITE

GEOPHYS3CRL CONSULTING *: SERVICES LTD. ..-l

PRIMRRY FIELD NORMRL3ZED DRTR NUMBER IN L3NE-CHRNNEL NUMBER INSTRUMENT: CRONE P.E.H,

METRES

l OB & 00 lift 4 DD

MCKENZIE ENERGY CORP.

PIC TOWNSHIP RRER VECTOR PULSE ELECTROMflGNETOMETER

HD8E S

(38)

2TZ z z z o tn in in in en en

LTO C" 13 O Z OTOQQEIEIOO

TJ-LOOP 2 -c* o q-^' -- 0 . __ o c _{— c j} ~ 50 ~ 7 5 • O 3 e— ~ 125 -- 159 ECflLE P. P. K. l OR -GLEN E. WHITE GEOPHYSICRL CONSULTING Se SERVICES LTD. CONS T RNT GRIN E RTR, G - ( l PC) "4 ) NUMBER IN L3NE-CHRNNEL NUMBER

INSTRUMENT: CRONE P.E.H.

METRES

ISO 3Q3 4DB

MCKENZIE ENERGY CORP.

PIC TONN9HIP RRER VECTOR PULSE ELECTROMflGNETOMETER

(39)

z z z in in en in in tn en d a GI z OToasBBrara d in o D Z G" O in Q in D in ® CJM OJ — — ITi GJ 10 — — O.) M n (O f LOOP 2 •d O O -q B P O '9 B •1^—-ou~ B 59 — 75 — 150 BCRLE P. P. K. 4- OR

-GLEN E. WHITE

GEOPHYSICflL CONSULTING. J, SERVICES LTD,

PRIMHRY FIELD NORMRLIZED DRTR NUMBER IH LINE-CHRNNEL NUMBER INSTRUMENT: CRONE P.E.M.

METRES

100 3QQ 40D

MCKENZIE ENERGY CORP.

PIC TOWNGHIP RREfl

VECTOR PULSE ELECTROMflGNETOMETER HORIZONTflL COMPONENT

16D0E 2

(40)

GJ C? E* C? C3 C3 in in in in tn inty ^3 I^J l^^l C? d o in GJ ID (D in — w w ci co * * LOOP 2 O-q Q- a- O O- q o—e 0 ~ 59 -•e—fr. ~ 125 ECRLE P. F. K. J OR -GLEN E. WHITE GECiPHYSICRL CONSULTING k SERVICES LTD. CONSTflNT GRIN DRTR,G-(

NUMBER IN LINE-CHRNNEL NUMBER INSTRUMENT: CRONE P.E.M.

METRES

ssf**

B l DO SOfl 3t*3 400

MCKENZIE ENERGY CORP.

HORIZONTRL COMPONENT 19D0E 2

(41)

zzzzzzz QC3C3QQE?E3 in CD in (3 in D in zz CktG3Z LO to Q d Z D _{-' — m O in} tnt/iu) ut en m en tn tn dn5) G) d Q Ip C3 Q (Scum O in d 10 O in ——-i w w en o ^ * LOOP 2 Od o o -D O O—B I~ H I— 25 I~ 5 0 - 75 ~ 125 -— 159 BCRLE P. P. K. 4 OR

-GLEN E. WHITE

GEOPHYSICRL CONSULTING *; SERVICES LTD. FIELD NORMFOZED DRTR NllMBHR IN LINE-CHRNNEL NUMBER

METRES

IDD 200 3Q3 4DD

MCKENZIE ENERGY CORP.

PIC TONNSHIP RRER VECTOR PULSE ELECTROMflGNETGMETER

HORIZONTRL COMPONENT 16D0E E

(42)

MCKENZIE ENERGY LTIJ.

PIC TOWNSHIP RRER

L i ne, Traniitfi i 11 er loop des i gnator , Coordi nat es of loop perimeter and Survey date

Table:

STRTION: FJeceiver station

l

Channel 1-8 sample times: .15, .45, .85, 1.45, 2.45, 3.75, 5.85, 8.8'

(43)

l

MCKENZIE ENERGY LTD.

PIC TOWNSHIP RRER

Page i

STfiTIOH VI V2 V3 V4 V5 V6 V7 V8 HI H2 H3 H4 H5 H6 H7 H8 G PP

Loop l, perimeter 660S,l166S,0W and 1666E, Survey date 13/3/83

1

1 sees

250S

2 e e s

150S 100S 50S 0N

sew

100N 150N 280N 25 ON 300N 35 6 H 400N 456H -36 -30 -23 -16 -13 -7 -3 e -13 ~8 -6 -4-1 66 -1 93 1 -43 -36 -27 -20 -16 -9 -3 -1 -16 -11 -8 -6 -2 -2 0 0 91 -48 -38 -28 -19 -15 -7 -5 -2 -13 -9 -7 -5 -5 -1 -1 0 77 -43 -36 -2f! -20 -16 -9 -3 -3 -12 -16 -7 -4 -4-20 1 53 -43 -35 -2(5 -19 -14 -8 -3 -1 -13 -10 -8 -4 -4 -2 -1 1 51 -40 -33 -24 -17 -15 -8 -3 -1 -14 -10 -8 -4 -3 -1 6 6 41 -37 -32 -24 -17-13-8-2 6-17-11-8-6-6-2 6 - 34 -34 -29 -24 -17 -13 -7 -5 -3 -12 -16 -8 -4 -3-26 1 24 -46 -33 -2J5 -17 -13 -7 -4 -2 -26 -12 -9 -8 -6 -5 -2 - 1 28 -37 -32 -24 -17 -13 -7 -2 -1 -19 -12 -8 -4 -4 -1 6 1 23 -32 -29 -22 -15 -13 -7 -4 -1 -16 -13 -9 -7 -6 -3 6 1 17 -34 -36 -24 -16 -12 -7 -3 -1 -26 -13 -9 -6 -5 -1 -1 1 18 -30 -28 -22 -16 -13 -7 -4 -1 -17 -13 -16 -6 -5 -2 6 1 15 -36 -28 -2:. -15 -13 -7 -3 6 -24 -16 -12 -7 -6 -4 -2 1 14 -29 -28 -22 -36-13 -7 -2 8 -17-15-10 -7 -6 -3 -1 6 1 13 -27 -26 -2:. -16 -12 -7 -4 6 -16 -13 -11 -8 -7 -6 -3 -1 1 11

Line 866E, Loop l, perimeter 666S,l166S,6W and 1000EE, Survey date 14/3/83

J

1

1 0

1

1 87 73 14 16 17 20 22 25 29 34 39 47 56 68 84 1 1 1 Line 660E, Loop l, perimeter 6668,11665,61*1 and 1666E, Survey date 15/3/S3

^^

1

450S 460S 350S 300S 250S 200S 150S 100S 50S -0N - 50N 100N 1 50N 260H 256H

1 11

(44)

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(45)

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CM 1 rt 1 O U j 1 1 rt Vjj V ID 1 1 CO rt 1 co ir 1 1 rt CO f-t f* t 1 t*— r^ 1 1 rv vjj CO CM 1 1 • : S 1 1 rt 05 rv vjj 1 1 oo co CO CO rt 1 1 z z CO CO OD b") ir ir CJ UJ 00 09 CO rt j CM CO 1 1 IT b"5 1 1 vjj CO 1 1 CO rt rt f i 1 1 ir or. 1 1 CO Or. co CM 1 1 00 CM 1 1 00 O5 1 1 or. cr. 1 1 Vjj Or. 1 1 ID CO CM co 1 1 •kAJ 1 \ f 05 T 1 1 rt 09 vi) rv 1 1 rt ID CO CO 1 rt 1 z z CD CD CD bj ID ID VII c* lil o LI Ol .,- —-(*. o lil w i. f-Oi 0 r- •*--* CO * fv lil s o ut tT b . '~ 3" VJ u o Oi s. U! 3 VI o •f f-IV Wl IDb") vi lil **- c o --*— 1 — •T) Cr. f o f c cc o

(46)

Mf-Ontario

Report of Work

(Geophysical, Geological, -n'JjO}. Geochemical and Expenditures)

The Mil 42D09NW8094 8.5690 PIC ₃₀₀

Type of Surveyls) _______ Claim Holder(s) Township or Ares ddress \ O y-* ^

Prospector's Licence Mo.

______ Survey Company

lcrn^ftiT

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

C.

O (\l\C_ C'V-OC vC^___XVC- .

[bate of Survey (from 81 to)

[A - *

Mo. | Yr. J Day j Mo. | Yr.

Total Miles of line Cut

Credits Requested per Each Claim in Columns at right

Special Provisions For first survey:

Enter,40 days. (This

includes line cutting) For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total (s) here

'

Airborne Credits

Note: Special provisions to Airborne Surveys. Geophysical - Electromagnetic - Magnetometer - Radiometric - Other Geological Geochemical Geophysical - Electromagnetic - Magnetometer - Radiometric - Other Geological Geochemical Electromagnetic Magnetometer Radiometric Days per Claim 'ko 2.0 —— — Days per Claim Days per Claim

Expenditures (excludes power stripping)

Mining Claims Traversed (List in numerical sequence)

Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total Expenditures Days CreditsTotal

Instructions

Total Days Credits may be apportioned at choice. Enter n umber of days credits in columns at right.

Certification VerifyrrT^Rep^rt of

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

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

fimrr arid Postal Address of Person Certifying

L.^.::.--J_..: ..:^ 13i;:' 'W 1/9 i

(47)

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

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.

Type of Survey(s) Ground Geophysical Survey_{i r}

Township c Claim Hold Survey Con Author of ] Address of Covering D Total Miles

r Area Pic Township

erM Murray Pezim, Arthur Clemis

ipany G leport .E. White Author Richmond B ates of Surv of Line Cut ey Geophysical Consultants 11 .C. March 1 to 21. 1983 (linecutting to office) 7.2 kilometers SPECIAL PROVISIONS CREDITS REQUESTED ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid. AIRBORNE CREDITS Magnetome DATE: Res. Geol. ter Previous Surveys

File No. Type

DAYS ~ , . . per claim Geophysical —p.WtrTr'agr"'ti'' 40 — MflgPPt^mptPr 20 — RfHi^nr'tr''' -Othf-r fipnlngiral ^ Gpnrhpfninil vt *** *

(Special provision credit! do not apply to airborne lurveyi) -X

Electromagi

(enter e

SIGN/!

\\V)

netir RaHinmptrir

lays per claim) ,

s-\ f . , .^\^~* ITIIRF.- (^ -'- JI 0^ \\^

Author of Report or Agent

Qualifications

Date Claim Holder

MINING CLAIMS TRAVERSED List numerically T. B. 645822 (prefix) (number) 645823 ... ..6.4582A... ...6A5825... ,...6A5826... ,...645827... ,...655502... ,...65551-0... 655511 . *^ ' 6 55512 cQ) 655513 ^ ^ 655514 ^' 6 55515

TOTAL CI, AIMS 1 "j

(48)

GEOPHYSICAL TECHNICAL DATA

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

Number of Stations Mao-1420 EH- 155___________Number of Readings —

Station interval———.. , _metres, —————————————————Line spacing———1QO metres i

Profile scale

Contour interval.

- ,, Accuracy — Scale constant _L

W '

c

2; O N f4

2

Q W U W

Instrument GSM - 8 proton precession magnetometer

Diurnal correction method CMfl - MR10 base magnetometer, record throughout day Base Station check-in interval (hours) fjft|d ftlork uaed

Base Station location and value —————.—^——.—^....——.

ECTROMAGNETIC Instrument Coil configurati Coil separation Accuracy Method: Freemen rv

Crone pulse EM system oft

1 8

part per thousand of primary field

D Fixed transmitter D Shoot back D In line channels 2000Watts

D Parallel line

...

Parameters measJBiMpndary field vertical component, Secondary field horleontal component

Instrument

Scale constant .— ^

Corrections made.

® Base station value and location.

Elevation accuracy.-.

Instrument ————————————————————————————————————————————————

Method D Time Domain D Frequency Domain

Parameters - On time ___________________________ Frequency ————— —Off time___________________________ Range.

— Delay time ———————————————————————— — Integration time ,———^^.————————-———^— Power. Electrode array — Electrode spacing . Type of electrode

(49)

SELF POTENTIAL Instrument-———-——-—-——-—-——-————-———-——-—-————^-——- 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)

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 survey) Aircraft used——————————-—-——-——^———.^^——^——^—-.— Sensor

altitude-Navigation and flight path recovery method.

Aircraft altitude-—————^——.—^-——-^—.——.————,.—.^—— Line Sparing Miles flown over total area^—-————^-—————————————Over claims only.

(50)

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. m. p.p. b. D O D Cu, Pb, Others —

Zn, 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) GcneraL General

(51)

s-1984 05 04 Your Filet 302

Our Filet 2.5890 Mrs. Audrey Hayes

Mining Recorder

Ministry of Natural Resources

P.O. Box 5000

Thunder Bay, Ontario P7C 5G6

Dear Madamt

RE} Notice of Intent dated April 9, 1984.

Geophysical (Electromagnetic S Magnetometer) Survey on Mining Claims TB 645822 et al in the Township of Pic.

The assessment work credits as listed with the

above mentioned Notice of Intent r 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.E. Yundt Director

Land Management Branch Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3 Phonei (416) 965-6918 M.E. Anderson:se ccj Murray Pezim Arthur Clemiss Suite 1550 605 Granville Street Vancouver, B.c,. V6C 1X5 cci Mr. G.H. Ferguson

Mining 6 Lands Commissioner Toronto, Ontario

cct Resident Geologist Thunder Bayi Ontario