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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
v-
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ct
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
IO04O4
100^99
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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
o -*
o
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