KORDOL EXPLORATIONS LIMITED

MAGNETOMETER SURVEY

HYMAN TWP. PROPERTY

ONTARIO

LEGEND

. 1450

BASE STATION a Control Stations

Vertical Magnetic intensity at Stations in GAMMAS

Interpreted Lines of equa magnetic intensity

Scale l2400 or l Inch to 200 Feet

Gammas

-8000 - O

O - 1000

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BASE LINE BASE LINE

' N^lnJto.^i!Lloc a*ion of Patented Land

1520 1520 1550

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99461

99462

100397

100391

99460

99459

100398

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IO04OO

CLAIM NUMBERS

Magnetometer by W.Murray - Map 8k Interpretation by K.L Reading, October, 1959.

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KORDOL

Suite 407, 19 Melinda Strtat ; T*rohto l, Ontario*'• ' * * ' -

HAOHCTOMBTES SURVEY, SUDBURY AREA PROPERTY

r-,

itEFKRKNCESl

1.2.3.

Kordol Report and nap by Ogdon, April, 1959 291A, Espanola Sheet, 0. S.C. 1928 Claim map, Hyman Township.

IKTRODUCTJoN* *

During the period June 10 to August 28, 1959, a

Kagnotoaetor Survty vas conducted orcr the entiro property of

Kordol Explorations Limited in Hyxtan Township, Sudbury Mining

District, Ontario*

One cone of heavy sulphide mineralization with copper

and nickel was known to exist in the southwest corner of the

property. Other vhowings of sulphide mineral i sat i on were

suspected out their locations were not defined* A Magnetometer

Survey was therefor* tonducted for two specific reasons) first,

in order to see whether or not the mineralisation itself vas';\ . ^

detectable by magnetic survey, and secondly to discover if the

HALIT. BMOAOHUMT a OOOEN

. .rdcks which oncloited the Bineralleation vere

-t . . , , -different froi other ro!Bk't7pea ; i^ch''ttpierlay the property

PROPERTT .-* " . . ' .' " ' . ; t * r "'*. "- .vw /' 'J ".: 'v.

The property tennist* of 15 unpatested olaina ini1 f

Tpvnihip, a one 40 ail ea V4at of Sudbury, Ontario*

ssioh 1| KB quarter of H^ii;i.i;i*x.

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clain 3*100391t?NHttttttttnMNHHNtt

S- 994615- 99460S- 99462S- 99459S-1003973-1003983-108459S-108460S-108462S-108461S -10 846 3S-108464S-108466S-108465

ACCRKSSt

The property nay be reached by boat, from the small

town of Turbine at the east ond of Agnev Lake* The cross-

voter distance is about tvo miles. Aircraft may also bo used,

landing in a long marrov bay of Agnev Lake \t the northeast

corner of the property* The transportation 6f heavy equip

ment to andfroro the property is best done b/ road or rail

frora Nairn, vhich is on Highway 17 and the C.P.R. A good

gravel road leads f rota Nairn across the Spanish River by

ferry, to within tvo miloa of the southwest corner of the

Kordol property* A bush road connects the gravel road with

the property*

CSOLOOTl

A geological *UTT*y hi* b t ea dono/laa*

following the na^tteto^ter survey. Although''the final results

are not plotted, tbe distribution of rock types in the Kordol

property is quite obrious. Sills or dykes of nipissing-type

diabase underlie the northern half and the Southern quarter of

the Kordol ground* The remaining quarter is underlain by

Ramsay-Lake-type conglomerate. The strike of the formations

is east-northeast with oteep dips to the south* four occurrences

of sulphide mineralisation have been located and all of then

are within the Xipisaing-typo diabase rock* The mineralisation

is mostly pyrite and pyrrhottite vivh s^o chalcopyrite and a

little pentland* :e.

METHOD OF S URVEY

A Sharpe A-2 magnetometer was used, aerial niwber 102,

with a sensitivity of 22*0 eanr.as per scale division*

A base lino vas cut east And west through the north

central part of the property and picket linns vere run north

and south at 200 foot intervals from the base line*

Magnetometer readings vere taken at every 100 foot interval

along each picket lino and if anomalous readings were

encountered, thainterval vaa shortened to 50 foet and

occasionally to 23 foot intervals. A total of 16*6 nilcs of

lin* vere surveyed by vagnetoneter* for a total of 904 station

readings*

HALCY. BMOAOHUMST ft OOOCN

Th* nain base station in l ocated on line sasro at bat*

line* Its arbitarily a*ci^*(t Value is 1500 gaauuu. All ,'

readings vere calculated so that their value is what it would11 ' .' ' ' p f '

have been had the whole 904 readiugs been taken simultaneously

vith that of the Main base station* The calculations remove

most of tho effect of the hour to hour, day to day and veek

to week variations in the earth*s mugnetic field, plus jars

and shakos to the instrunent that wight alter its ability to

measure magnetic intensity* Subsidiary stations,or control

stations, were set up at convenient locations about the

property and were very accurately tied to the base st&tien*

During the coume of tho survey, readings were taken on a

control station or the mainbase station at least every tvo

hours in order to determine the diurnal variations*

MAGNETIC TEXTDRESI

Tho magnetometer readings as shown contoured on the

accompanying plan of thf property display two distinct

textures* The northern half and southern quarter of the

property are smooth toxturod with the occasional b imp or

hollow* tfhoreas t IK* spath central quarter is rough textured

with frequent nagnetic bunps, nounds, hills and a few hollows.*' ^ f

The general tuagnetic intensity of tho smooth textured area is.-4V .i '

1500 gauuabs and the rough area averages 1600 gannas*!

A

These results vere not aa expected, for the smooth

texturod magnetic results overlie areas that have been found

to bo underlain by diabase, which would be expected to be

quite variable ttagne,ticVlly.

tke rfcxifcb. texture va* found to refleet the ftamsay^laljce type

conglomerate, vith the excepti

vhich is underlain by diabase*

?KK/•: 5'--.V ; ^Bk' ' ! - ".- . ', - ,- ,.' ..' . i - -.- ' ' ",- ^ ' . :' '"' .- ,' -

h.\ : " conglomerate, vith the exception of the moat easterly 400

AKOMALIBS WITHIN THE TKXTORAL DIVISIOHSl 7 ,

Sulphide mineral! tatjon has nerer been fotrnd in the

edintnts outlined by the rough textnredmagnetice. Therefore

the numerous tiuill./ magnetic anomaliee in thi* area way be

considered insignificant^

All the known Bulphide deposit* on the property are in

the diabase as reflected by tho smooth tcxtured magnetic*.

Thus it is within this area that the significant anomalies exist*

1. Main showing, at 2900 feet south on line 32 vest*

Here, a very sharp magnetic negative (lainus 7410 gammas) vas

encountered on top of the mineralisation.

2* Shaft shoving. On line scro at 900 feet south.' *

Here, considerable sulphides vrere exposed near the erratic

magnetics on tho line*' . i , - .

3* A small shoving of sulphide mineral x* titin on line**~- " ' ' -- - -- - ^ . ,,^

2 vest at 700 feet south. Fifty feet south of the exposure,

there is a 6710 gamma reading and immediately north of it, an

1150 g a rana result.

4t An 1800 gamma anomaly on line IB vest at 400 feet

south. This anomaly is on A large outcrop where no significant

mineralization vao noticed* It is therefore unlikely to be

productire.

HALKT. BNOADHUMVT ft OOOCN

mY*x\ ; .;-.'

5. A 600 gaana anonaly on line 24 vest 100 feet south

taken in conjunction With e. 100 to 200 gwaiaa depression on

line 28 vest at 100 feet south. As botfc these mild anomalous

conditions are in areas of heavy overburden the rock cannot be

examined. They should bo further investigated. If the

overburden is quite thick, it could dampen the magnetic results.

6. A 500 gncuBt anonaly on line 36 vest at 2300 feet south.

Thisis a small anomaly, close enough to the nain No* l shoving

that there might be none connection And therefore it should

be investigated along with the nuxin shoving.

7. A 400 gara^a depression in one location on line 10

west at 3000 feet south. This Anomaly is at the contact

between diabase on the north and grcyvackcs to tho souuh, and

is unlikely to be productive, but vould bear somo further

investigation.

GCKCLUSIONSj

1. Tho nain shoving should be drilled at close

intervals vith a series of short holes in order to properly

establish its tenure and trend.

2* If significant mineralisation is encountered in

the above drilling,programme, anomalous areas 2,3,4,3,6 and

7 should be investigated by geophysical means in order to

establish the direction of any concentrated mineralization

nearby* f ,- ,

i ' f ' ' iHALBT. BROADHUMT

1. Brill 6 holes into the main showing froa north

to south* Sach hele to be 30 feet apart. The holes to be

drilled in tvo series of 3 holes each, the second xsr deeper

series to be 30 feet beneath the first series* . '•',. f̂ .'"

2. Electrical-Geophysical wark could boat bo done

by tho Boleden type nurvcy vh.Qr0. a *rev. cpiild'go onto the*'"" : ' ' . ' -

property for one or tvo days'aiiti qtoickly check the vicinity

of the magnetically anonalous areas.

r" ' . , -

' .' ', , ' ' ' ' '' ' - -, ' '^~

Roopcctfulljr submitted)

'•li^

Michael

•-VV;':'';'-';";'- '. . ', , HALCT, BNOAOHUMCT ft OOOKN

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Ktrdol Validations Lioitod

.

Township 1'roporty, Ontario*

Line CuttJpgt Period froo Jun* 10 to July IS, 1959. dnys

Murray - 97 Duneden Or*, Toronto 35 George Popoviob - Sudbury, Ontario 30

Period from July 16 to Aug. 28, 1SS9.

Wallace Hurray * 87 Uuneden t-rive, Toronto 42

Technical Assistants to L .opera tor i July 16 to Aug. 2t, 1S59.

George popcvich - Sudbury, Ontario 20S* E, Armstrong - Sudbury, Ontario 13

preparatipn and consulting- June 10 to Aug. 28, 1959,

Hlohael Ogden ~ Bay Htroet, Toronto 10

Total 150

factor of 4 600

Hichael Ogden*

HALCT. BMOAOHURVT a OODCN

\

KORDOL EXPLORATIONS LIMITED

MAGNETOMETER SURVEY

HYMAN TWP. PROPERTY

ONTARIO

LEGEND

o BASE STATION a Control Stations

1450

1610'

Vertical Magnetic Intensity at Stations in GAMMAS

Interpreted Lines of equa magnetic intensity

Scale l2400 or l Inch to 200 Feet

Gammas

--8000 - O

O - 1000

1000 - 1300

V-ot o

tt

BASE LINE

1300 - 1500

Approx. N. Bndry. due location of Patented••"•"••B* ^*ri^. .^ JW^T4^^ VBK4A|MhflAiflH J - -

\7O0 - 1660

LINE

Col or t d

99461

99462

100397

100391

99460

99459

100398

/0 ̂ X)f

160395

'ST

I6O399

—100394

IOW03

IOO4OO

CLAIM N UMBERS

Magnetometer by W.Murray - Map ft Interpretation by K. L Reading, October, 1959.

41I05NE0088 0025B1 HYMAN 300