rpt on mag & em sur of the mulliette - bell cl€¦ · 3. procedure ~ magnetic base stations...

42A10NE0S22 2.1535 CLERGUE

y 5"3 5-

010

REPORT

ON

MAfiNRTQMRTRR AND ELECTROMAGNETIC

SURVEYS

OF THE

MULLIETTE ~ BELL CLAIMS

CLERGUE AND STOCK TOWNSHIPS

PORCUPINE MINING DIVISION

AND

WALKER AND TAYLOR TOWNSHIPS

LARDER LAKE MINING DIVISION

ONTARIO

D. R. Bell, B.Se.

July 31, 1974.

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A McPhar vertical loop electromagnetic.and magnetometer ^ was comnio'Ce'd 'dUTing' the months of Aprii and Mav of 1974~ on Morley Mulliette - David Bell claims, sxtuatod in .Clergueand Stock yownships of the Porcupine Mining Division, and Walker and Taylor Townships of the Larder Lake Mining Division, Ontario.

The survey was performed by John J. Johnson, 112 Second Ave., Timmins, Ontario.

Location and Accessibility:

The claims are located on the mutual boundaries of Walker L TaylorL and Stock Townships. 42 miles east of Timmins, south of the village of Monteith, The claim group is cut in half by Highway 11 and access within this group is gained by numerous farm access roads and trails. The village of Monteith is one mile north of the property as is the Ontario Northland Railway.

3 * Property;

Total number of claims

Recorded Numbers

24 unpatented mining claims*

L372557-561 Inclusive


P372526-528 Inclusive

P372556


P372523-525 Inclusive

4. Ownership, and Title:

The 24 unpatented claims within this survey area are jointly held bv J'lorTeVfTuTrretTeahd David R, Bell on an equal sharingbasis; S ®* each.

Mineral rights held by: a) Morley Mulliette,Suite 201, 95 King St, East, Toronto, Ontario.

b) David R. Bell,672 Melrose Blvd., Timmins, Ontario,

-2-

l f i i i

Due largely to the area being overlain by clay, and . widespread outcrops, little exploration was carried out in thisarea until 1.9J8 when a landslide on the east bank of the DriftwoodRiver exposed an outcrop which assayed 0.13 ozs. gold per ton.

In the spring of J.939 the Montclerg Mines Limited was incorporated, The property was optioned to the following companies which carried

- out diamond-drill programmes and a limited magnetometer survey.

Companies - 1939 Newmont and Anglo-Huronian Ltd.

34 holes for a total of 20,335 feet.

~ 1941 Anglo-Huronian Ltd.

10 holes for a total of 6,672 feet.

- 1942 Howey Gold Mines Ltd.

l hole for a total of 776 feet a magnetometer survey.

This early work indicated an apparent gold bearing zone extend ing from 1500 feet west of the river to 2800 feet east of the river.

Subsequent to this work, the original company has been organized to Consolidated Montclerg Mines Limited, and no further work has been reported within this area.

The enclosed geophysical report covers the area immediately to the east and south of this previously explored ground.

6 * General .Geology:

Much of the claim area was mapped by H. D. Carlson, 1965 for the Ontario Department of Mines, and previously the general area was mapped by R. M. Ginn, 1959-1961 for the O.D.M. The map by H. D. Carlson, O.D.M. Preliminary Geological Map No. P.308, shows the claim area to be underlain by sheared and foliated light and dark weathering intermediate to mafic metavolcanics, cut by a wide east-west trending Pipestone fault zone of a composition essentially that of a talcose-chloritic matrix.

Previous assessment work on the Montclerg Group by diamond-drill ing has indicated North-South trending diabase dykes.

Structurally the metavolcanics have been isoclinally folded, with an east-west trending synclinal axis passing just south of Monteith. This has been structurally offset by a north-south fault. Extensive shearing, foliation and metamorphism has occurred with the schistocity following the general east-west trend*

-3-

ffhe gold in the Montclerg area is in arsenopyrite and appears to bc restricted in a silicified zone in the meta volcanics to the north of the talcose-chloritic Pipestone Fault Zone.

The picket lines were oriented in a north-south iliiiection. such that the~survey iines would be as near as possible at right angles to the formation.

Magnetometer Survey:

(a) Grid -

1. Baseline - bearing 090 E.

2. Crosslines - bearing 360N and 180S @ 400 ft. intervals

3. Total line/miles - 22.75 miles.

4. Stations ~ 2089.

5. Personnel - three (3) man crew supervised by John J. Johnson,112 Second Ave., Timmins, Ontario.

(b) Survey Method ~

1. Instrument - McPhar^M?00 Fluxgate magnetometer) a batteryoperated, ^TaTisTsveTizea, direct reading instrument which measures the vertical component of the earth's magnetic field.

Scale constant 20 gammas.

2. Theory of Method - the fluxgate magnetometer employs asaturable core system consisting of two highly permeable metallic strips about which primary coils have been wound. A low frequency field (1KH2) is applied to the coils through an oscillator. The field is sinusoidal and drives the strips into saturation during each half cycle resulting in an even change of permeability of these cores (at KH2). Any ambient magnetic field acting on this system yields a flux or phase variation which, when "gated" at the proper frequency (in this case the second harmonic), induces voltage pulses in an adjacent secondary winding. These pulses are amplified, fed into a phase doctor and emerge as a D.C. Signal. This

-4-

signal is directly proportional to the strength of the ambient field and, therefore the strength of the field can be read on a voltmeter cali brated in gammas. The accuracy of the McPhar instrument is generally within 1/2^ of full scale between 1000 and 10,000 gamma ranges and within 1# between the 10,000 and 30,000 gamma range.

3. Procedure ~ magnetic base stations were establised at 8+20 JSon nasa,

c;.: -ne J j+OQ Wa l kor Twp.. and Baseline 0+00,

Readings werethen taken at 50 ft. intervals on the crosslines, and check readings taken at a base station in order that a correction curve for the diurnal variation could be established. Using this curve, all readings were corrected for diurnal and instrument drift variations.

El e c t r om a gn e t i c, S ur y ey :

(a) Grid - same as for magnetic survey; Stations ~ 1060.

(b) Survey Method -

1. Instrument - McPhar SS-l.S Verticafl Loon EM t System; a dualTrequency fixed source, tilt angle method.

2. Operating Frequency - 1000 and 5000 C. P. S.

3. Operating Range - 2000 feet.

4. Transmitter Power - 300 watt supplied by gas-powered motorgenerator.

5. Transmitter - a mass-mounted, triangular cable loop about10' per side. The loop can be rotated about a vertical axis.

6. Receiver - a tuned pick-up coil assembly together with atransistorized amplifier with earphone outlet and a built-in clinometer for dip angle measurement.

7. Theory of Method - the basic principle is essentially that a horizontal electromagnetic field generated by passing an alternating through a wire loop will induce electrical "eddy" currents in any adjacent conductive media in the earth. The induced current in any conduc tor will in turn regenerate a secondary, electromagnetic field. The location and orientation of the principal axes of any secondary field and, hence, the location

-5-

and orientation of the source conductor can be determined by measuring tilt angles with a receiving coil. To do this the coil is rotated about a selected axis until a null position is obtained. This null position is essentially the orientation of the receiver coil producing minimum induction. The axis of orientation must be selected such that it is horizontal and lies in a direction parallel to the plane of the receiver coil and normal to the plane of the transmitting loop*

8, Procedure - Sites for the transmitter locations areselected at convenient points throughout the property. The transmitter is set up and current is applied. The plane of the loop must be kept as nearly as possible in a direction normal to the location of each receiver station. The person operating the receiver orients the coil about a vertical axes until a null point is established. The direction of the plane of the coil is now parallel to an axis which is normal to the plane of the transmitter loop. Next, the receiver coil is held in a horizontal position in this position.

If no secondary field is present a null will be obtained in the horizontal position, If such a field is present, its tilt angle is measured by rotating the coil until a null is received. The dip or tilt angle is read on a clinometer attached to the receiver apparatus.

The amount of tilt recorded at each station in plotted graphically on the line plane and connected by a curve.

A cross-over point is in theory, that point on the line where the curve changes from positive to negative, and in practice it is a point of inflection on the curve. This is due in part to distortion of the secondary field and to interference from other minor, conductors.

Results;

(a) Magnetometer Survey - the east-west magnetic trends reflect a general pattern which might be related to the trend of the metamorphic fabric superimposed by the intense regional talcose- chloritic Pipestone Fault Zone.

; -6-

/Intrusive diabase dykes exhibit a magnetic relief trending in a North-South direction and is sufficient in contrast to distinguish them from the older flows. This is exhibited on the Stock Twp. Group in claim P372525, and similarly on the Walker Twp. Group in claim L372754* This later magnetometer expression has been likely intensified within the Pipestone Fault, regionally metamorphosing the talc-chlorite schist along the diabase intrusive contact to a possible "magnetite- rich" serpentinized rock.

(b) Electromagnetic Survey, - only qne modnrate conductor of any magnitude is indicated. This is in the north-west corner of Claim L372753 in Walker Twp. between lines 4+00 E and 16+00 E; 24+00 N. This anomaly does not reflect any magnetic expression, and a small outcrop some 100 ft. south of the anomaly indicates fine stringers of pyrite in a rhyo-dacite. This small exposure might indicate that the anomaly is due to the presence of massive or stringer sulphides.

A couple of very weak conductors reflecting a trend east- west following the contact of the proposed Pipestone Fault. This is probably due to intense shearing and possible disseminated sulphides.

^10. Con c l u s ions :

The electromagnetic anomaly in the north-west corner of the Walker Township Group is in a geologically favourable environment for possible base metal potential. This area should be detailed with 200 ft. survey spacings. Due to the intense overburden and a local river passing over this area, diamond drilling would be recommended for this zone.

An induced polarization survey along the contact of the Pipestone Fault zone might further outline potential disseminated gold-sulphide horizones similar to those found on the adjoining Montclerg property.

It is recommended that following any successful results from the above conclusions, that diamond drill should be used to test the mineral potential of this property.

Respectfully submitted,

David R. Bell, B.Se.

July 31, 1974.

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PERFORMANCE 8c COVERAGE CREDITS

Township or

Type of Survey

ASSESSMENT WORK DETAILS

jf

each type of survey

Chief Line Cutter or Contractor

Party Chief

Address

Consultant. / Address

Name

Address'

COVERING DATES

Line Cnllint;

FieldInstrument work, g/ological mapping, sampling etc.

Office.

INSTRUMENT DATA

Make, Model and Type -Xx\

SScale Constant or Sensitivity___^?^Or provide copy of instrument data from Manufacturer's brochure.

Radiometric Background Count

Number of Stations Within Claim Group

Number of Readings Within Claim Group Z

Number of Miles of Line cut Within Claim Group

Number of Samples Collected Within Claim Group

CREDITS REQUESTED

Geological Survey

Geophysical Survey

Geochemical Survey,

20 DAYS per claim

a40 DAYS Includes per claim (Line cutting)

MINING CLAIMS TRAVERSED List numerically

372 -^

TOTAL

f'-eiul in duplicate to:

FRED W. MATTHEWSSUI'I K VISOK-PROJ ECr.S S ECTIONDEPARTMENT O l M INES gcNOUTHF.KN A F l" AIRSWHI'J'.Nl Y 151.0CKQL'I.1-,N'S I'ARK'fOROX'J'O, ONTARIO

anH r o vcra gf r rod i t s do not annlv to airborne survcvs

PERFORMANCE Se COVERAGE CREDITS

ASSESSMENT WORK DETAILS

Township or Ar

Type of Survey



Party Chief.

type of survey1~ S

Name

Address

Consultant.

Address

Name

/AAddrc/s

COVERING DATES

Line Cult ing

Field .

Office.

Instrument work, geological mapping, sampling etc.

JL- S*

INSTRUMENT DATA

Make, Model and Type

Scale Constant or Sensitivity____/O&& (2^r\ S.('r provide co/iy o / instrument data /rain Manufacturer's brochure,



Number of Readings Within Claim Group

Number of Miles of Line, cut Within Claim Groii]

Number of Samples Collected Within Claim Group

CREDITS REQUESTED

Geological Survey

Geophysical Survey

Geochemical Survey

DATE

20 DAYS ____^ Includes per claim (Line cutting)

n

L.

TOTAL

Send in duplicate to:

l- RED W. MATI'IHiM'SrROJECrS SECTION

DEPARTMENT OF MINKS fr . " .VORTflEX.N' AFFAIRS \V!!irXL'.V 11 LOCK Ql.'l i ;.\ r S 1'ARK TOKON'fO. ONTARIO

PERFORMANCE fc COVERAGE CREDITS

tfk .ASSESSMENT WORK DETAILS

Township or Area . .vy *z-ZfajJ tf^td ^^^/CT}^, -f— -t— Type of Survey—^—.


Parly Chief

Consultant

——— cacl) type oT survey

Address

Address x

COVERING DATES

Line Cutting

Field -—.—.

Office————

Instrument work, gcoiogi^l mapping, sampling etc.

AA - *?OQ

JNSTRUMEN'J' DATA

Make, Model and Type

Scale Constant or Sensitivity,Or jtroi'idc copy o/ instrument data /ram Manufacturer' 's brochure,



Number of Readings Within Claim Group

CREDITS REQUESTED

Geological Survey

Geophysical Survey

Geochemical Survey

gO DAYS [)cr claim

a

Number of Miles of Line cut Wilhin Claim Group—/4 Z*

Number of Samples Collected Within Claim Group ——

40 DAYS Includes per claim (Line cutting)

DAT


-&7Z-

X.

3.72

l. -3.72

TOTAL

Send in duplicau: lo:)"Ki;n \\r . MAI'TIJKVv'S SM'EUVISOR-l'ROIECTS SECTION' JU-.l'AUTMENT ()i MINES k NORTIIERN Al'EAlRS

QUKKX'S PARKXTO, ONTARIO

Calvert Twp.

Stock Twp.

Q.

(D .

••^

O

THE TOWNSHIP OF

CLERGUEDISTRICT OF COCHRANE

\PORCUPINE

MINING DIVISION SCALE 1 l-INCH-40 CHAINS

LEGENDPATENTED LAND CROWN LAND SALE LEASESLOCATED LAND LICENSE OF OCCUPATION MINING RIGHTS ONLY SURFACE RIGHTS ONLY ROADSIMPROVED ROADS KING'S HIGHWAYS RAILWAYSPOWER LINES MARSH OR MUSKEGMINES

NOTESSuffoc* h 9 M* r*S*rVA,tiork

all

- MINING LANDS lDATE O F ISSUE

AUGMINISTRY

OF NATURAL RESOURCES

ONTARIOMINISTRY OF NATURAL RESOURCES

SURVEYS AND MAPPING BRANCH

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0-.:

0101

42AI0NEeS22 2.1535 CLERGUE 200

Teefy Twp.

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Taylor Twp.

42A1®NE0522 2.1535 CLERGUE 210

THE TOWNSHIP OF

WALKERDISTRICT OF COCHRANE


SCALE: 1-INCH" 40 CHAINS

LEGENDPATENTED LAND CROWN LAND SALE LEASESLOCATED LAND LICENSE OF OCCUWTION MINING RIGHTS ONLY SURFACE RIGHTS ONLY ROADSIMPROVED ROADS KING'S HIGHWAYS RAILWAYS POWER LINES MARSH OR MUSKEGMINES

or C.S.

Loc.L.O.

M.R.O. S.R.O.

NOTES4-00 Surface rights reservation around all lakes and

.vers.

PLAN NO.- M-396ONTARIO

MINISTRY O F NATURAL R ESOURCESSURVEYS AND MAPPING BRANCH

Walker Twp.

373506 1573503

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42MWEK22 2.1535 CLERGUE 220

THE TOWNSHIP OF

TAY LO RDISTRICT OF COCHRANE


SCALE'1-INCH" 40 CHAINS

LEGENDPATENTED LAND

CROWN LAND SALE LEASES

LOCATED LAND

LICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINES

MARSH OR MUSKEGMINES

NOTES400' surface rights reservation along the shores of ail lakes S rivers

PLAN NO.-M39IONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

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42A10NE0522 2.1535 CLERGUE 330

THE TOWNSHIP OF

STOCKDISTRICT OF COCHRANE

PORCUPINEMINING DIVISION

SCALE'1-INCH=40 CHAINS

LEGENDPATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LINESMARSH OR MUSKEGMINES

NOTES

400 fcurtace rights rAserue^ion around all lake*

- MINING LANDS lDATE OF ISSUE

AUQ - 6 1974MINISTRY

OF NATURAL RESOURCES

PLAN NO.-M. 388ONTARIO

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

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MAGNETOMETER SURVEYBY

JOHN J. JOHNSON FOR

MULLIETTE AND BELLTAYLOR TOWNSHIP

LARDER LAKE MINING DIVISION, ONTARIO.

SC ALE: 1^200'

MAY, 1974.

LEGEND.

f Measure Station along Picket Lines

i Relative Value of the Vertical Component S of the Earths Magnetic Field in Gammas.4"*-

^,u-x' Magnetic Depression

/*" l / M agnetic Contour700-p

0 Claim Post

—— —— Claim Line

/•\ Main Magnetic Base Station

INSTRUMENT

McPhar M 7OO Fluxgate Magnetometer

Scale Constant 20 Gammas

Contour Interval 200 Gammas

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3

ELECTROMAGNETIC SURVEYBY

JOHN J. JOHNSON FOR

MULLIETTE AND BELLTAYLOR TOWNSHIP

LARDER LAKE MINING DIVISION, ONTARIO.SCALE *.i"s 200'

MAY, 1974.

LEGEND

Transmitter Location

Read from Transmitter LocationNo. 2

Conductor Axis

"NO 2 South Dip Angle 23^ North Dip Angle

O Claim Post

"—"—Claim Line

Vertical Scale l"-200

INSTRUMENT

McPhar Vertical Loop S S 15

Using 1000 C.P.S.

42A10WE9522 2.153S CLERGUE390

-d

V S. R. O.

ft.

J72527 372526

f i vy //t' (bKEY MAPSCALE^ 1 Inch: 40 Chain*

p l Pl

372524 l 372525 1372550^

rpt on mag & em sur of the mulliette - bell cl€¦ · 3. procedure ~ magnetic base stations...

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