Upload
doantruc
View
215
Download
0
Embed Size (px)
Citation preview
CEOSERRCH CORSU1TRRTS limiTED
43AieNWe79S 2 .774 DUNDONALD 010
.17'
RECEIVED
FE6281972PROJECTS SECTION
TURAM ELECTROMAGNETIC AND
MAGNETOMETER SURVEYS
for
DOME EXPLORATION (CANADA) LIMITED
PROJECT No. 37
DUNDONALD TOWNSHIP, ONTARIO.
(To Accompany Maps 71-5^0 to
February 3, 1972,
INTRODUCTION
A Turain electromagnetic and magnetometer
survey was carried out for Dome Exploration (Canada)
Limited on Project 371 in November and December^ 1971*
The property is located in Dundonald Town
ship, Ontario, 24 miles northeast of Tinunins from where
it is accessible by road. Two grids were covered by
this survey. The east grid consists of portions of
Lots 1 to 3 in Con. III. The west grid consists of
portions of Lots 5 and 6 in Con. Ill and IV.
The purpose of this survey was to locate and
evaluate sub-surface geo-clectrical conductors which
might prove to be sulphide orebodies. No conductors
were located. The accompanying maps show the areas
surveyed ant] the results obtained.
- 2 ~
Magnetometer Survey
Method
The magnetometer survey was carried out with a
Scintrex model MF-2 fluxgate magnetometer which has a con
stant of 20 gammas per scale division on the most sensitive
range. The readings are a measure of the vertical component
of the earth's magnetic field, expressed in gammas.
Readings were t aken along lines ^00 feet apart
at 100 foot Intervals* A few readings were also taken at
50 foot intervti.ls in areas of high magnetic relief. Diurnal
and instrument-drif t^cprrjec tions were made by re-reading
previously established base stations at time intervals not
exceeding 60 minutes. The maximum correction was 1/2 a
gamma per minute.
The readings on the maps are expressed as being
above or below an arbitrarily selected base.
METHOD AND INTERPRETATION OF RESULTS
Turam Electromagnetic Survey
The model 2S Turam equipment was used for this survey. It
was manufactured and developed in Sweden by the ABEM Instrument
Group of the Craelius Company.
In common with other electromagnetic inductive systems the
Turam method is based on the fact that a secondary current is in
duced in an electrical conductor when the conductor is subjected
to an electromagnetic field. This secondary current creates its
own electromagnetic field which, together with the primary applied
field, produces a resultant electromagnetic field. This resultant
field, which can be detected and measured, differs both in phase
and amplitude from the calculated primary field; these differences
may indicate the presence of a conductor.
The primary alternating field is created by the use of a
large horizontal rectangular loop, energized by a current at 660
Hz or 220 Hz. The receiving system consists of two coils 100 feet
apart, connected to a compensator-amplifier which measures the
complex field-strength ratios and phase-differences between suc
cessive points on traverses outside and perpendicular to a long
side of the primary loop. Both the phase-difference readings and
the reduced field-strength ratios are plotted as curves at points
mid-way between the coil positions. The reduced ratios are the
measured ratios divided by the normal ratios. The normal ratios
may be calculated from the geometry of the primary loop and from
the location of the points at which the readings were taken in
relationship to the loop.
The conductivity c
mated from the followir
Ratio Anomaly > 1.00
Very small or nilSmallLargeLarge
)f steeply dipping conductor
lg chart i
Negative Phase-difference
Small to mediumMedium to largeMediumSmall
s may be esti-
Conduc t ivi ty
Very poorPoorGoodVery good
In areas of conductive overburden, the amplitudes of
anomalous readings, both the phase and the ratio, increase as
their distance from the primary loop increases.
- k .
Twelve primary loops wore employed, positioned to the north of tho areas surveyed, A frequency of 660 HZ was used exclusive]y along with a coil interval of 100 feet*
RESULTS
No conductors were located. A considerable portion of the east grjd was not adequately covered because of elect rical interference from the power line and telegraph line* These featxires caused anomalies w d th large amplitudes. Any bedrock conductor in these areas would not be identifiable*
The magnetometer survey over the west grid indicates a rather flat magnetic response with a gradual increase in mag netic intensity from the northeast corner to the southwest corner of the grid. A thickening of the overburden to the northeast could cause this effect.
The east grid j s dominated by two major magnetic anomalies which probably reflect basic iritrusives.
RECOjftlENDATIpNS
No further work on the two grids can be recommended from the results of this survey.
Respectfully submitted,
GEOSEARCH CONSULTANTS LTD.
J. A. Voodard, P. Eng., Consulting Geophysicist.
Project 37 - Turam b Mag.
42A1BNWe795 2 .774 DUNDONALD 900FACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
Typp nf Siirvpy., , , E!
Township ^^dcccas ^Xi
Claim holders)-, .-
Auth - "f Report, J tAHHrPSe Suite 111& -
Covering Pates of Survey.
Total Miles of Line cut .
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.
ENTER 20 days for each additional survey using same grid.
fir, tTomagrve tic f Maanetip
n^ona 1 d
A* Woodftpd100 University Ave., Torontt
Nnve. 1Q71 - Feb. T. 1972.(linecutting to office)
22.
1
DAYS Geophysical per^iena .
f j M^gnptnm^t w. J . .,,2,P -Oy
RaHinmptrir ^.^f^^^Or
-Hthpr ' "f
r.^h^n.1-
AIRBORNE CREDITS tSpecial provision credits do not apply to airborne gurvey*)
Magnetometer.,.,...,.. .Electromagnetic.,...., ,,.. Radiometric. ...- (enter days per claim)
PAT*. Feb. 17/7? sir.NATiTPR. Vs rf r^zZ**^-
PROJECTS SECTION
Res Genl. n r.
1 MPrevious Surveys fa 'Ju ,
s r.hprkpH hy
0 . wS GEOLOGICAL BRANCH
Sbfa ApprnvpH hy
GEOLOGICAL BRANCH
/^ Author of Report
Onalifiratinns fo&ill^"
Hatp
Annroved hv da tp *
. . ^ . :: ;
MINING CLAIMS TRAVERSED List numerically
-
(prefix) i (number)P 25571S
255720
2929^9
293649
.,,.......,:........m......,.....,....^.93^5.Q........
3134^5'326fcsb' ;
32i*59**f\4it Jif\............. ............................32,0^00........
" " " ' ' " ' f ^ojC i jfi^ ' i i fcO**OX
326^70
326^723^TO^6474j O/i. /T
32to622Z2| 6
TOTAL CLAIMS ... -gg
i
AJ1
a
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS Number of Stations—. Station interval——— Line spacing—————
Wag,1122 Number of
100 feet
400 feet.
Profile scale or Contour intervals Magi 50 gammas A 100 gammas
MAGNETIC InstrumentAccuracy - Scale Diurnal correction Base station location
(specify for each type of lurvey)E. M. Field Strength Ratio - 1 inc. to 20
Phase difference - 1,in? to 10rit e PI 1 1 -fr g
20 gainmas/div. on, most sensitive. range ______ . ____ Repeated base stations 60'ialn* or less time intervals along base lines - 400 feet apart*
ELECTROMAGNETIC InstrumentCoil configuration Coil separationArrurary
;Method: Frequency
ABEM Turatn 2SCo*-Planar
100 feet
I tO1 ( Phase l o
Parameters GRAVITY Instrument—— Scale constant.Corrections made.
B Fixed transmitter 660 Hz
D Shoot back D Inline O Parallel line
(specify V.L.F, rtation) .Fiftld Strenth ratio and haa difference
Base station value and location.
Elevation accuracy——^—^————^————. INDUCED POLARIZATION - RESISTIVITYInstrument ^-——^—.^-.———————.^—...
Time domainFrequencyPower
Frequency domain. Range ______ —
Electrode array^^ Electrode spacing. Type of electrode,
.fhx.
W
UJ
MCCART TWP - M.545
3260(83^.326084;
. - , v---
279048 ; ^9052,
279050 I Z79O54
333091 l 353092
P. ' P.
Frederick
332354)3330^3
326489 f 326437
/I "-'"
l 75887 .75886., t-p-Z58
H o u s ej (03586 i I035B9 |
J |78578fi"~lr jf~103587 j 103590 l 78576 | 78578 79451 79450 7945H
2657 12697- ®
l
I0558B . 103591 i 103592 ; 78579 i 79455 l 79432 n—r-L-~ir-f 103542 . 1035* l '03540 ' 103539 ! 101561 ' 101557 71015 7*016
M.H.Q
103551 i 103550 j (03549 I0354B i 101562 101560 101556 ' 101501 '10149(T~k e " "
l 103555 ! 103554 | 103553 l 103557 , 75818 -J -. - .
(D MAX), l -*W80 (C
I03S5B l 103557 ! 103556 ' 758Z3 l 75B22
103563 1103563; i I03S6I l 103560 ' 75S27 t-————--.--
L. T L. L. i LQ MHO .(y M.RO 217^*30, 217031
L il
03585 I035S2 103579 103576 103574
roPO
5
K
UJ
-jO
- 46 0 37 30
80 0 48 40"
GERMAN TWP - M.283
THF TOWNSHIP
OF
DUNDONALDDISTRICT OF
COCHRANE
PORCUPINEMINING DIVISION
SCALE: MNCH-40 CHAINS
LEGEND
PATENTED LAND
CROWN L'AND SALf
LEASES
LOCATED LARD
LICENSE O F OCCUPATIONMINING RIGHTS ONir"SUftfACE RIGHTS QNLY
ROADSIMPROVED ROADS
KING'S H IGHWAYS
RAILWAYS
POWER L INES
MARSH O R M USKEG
MINES
CANCELLED
S.R.O
C.S
LOC.
L, O
NOTES
POSTS FOR CLAIMS S T*KEO OWT LAMOS UMPiR WATERS Of FKtOt*tCK **OU9C; LAKt m OUMDOH*-D TWP SHOULD WOT SE ERECTED Oft **LA*TED tN EVCLVN
400' sjrfoc* rights reservation 010119 of all takes and
strores
LO.7128 - Flooding nghts on Frederick House take reserved TO H.Efr'C 10 contour elev. 903'
R(e 64516,11012
Area marked thus l Park Site.
1 SR.O reserved for Files 39684,51994
DATE OF ISSUE
MAR ^11972
ONT. DEPT. Of MINES AND NORTHERN AFFAIRS
ONTARIODEPARTMENT OF MINES
AND NORTHERN AFFAIRS
L:^v!
^frn
':ff -^r ,J f l '''tf--y'-;-:#p^ ; sij
,V'*i ^ i,, j**" "'-*
300
20 N
ION
205
FO
R K
B Y
MA
P - 5
EZ
MA
P 7
h 5
4-O
MflG
NETO
METE
R SU
RVEY
GEOSEflRCH C
ONSULTflNTS
LTD
(.52
0
DOME
EXPLORflTION
(Cfl
NRDf
l) LIMITED
PROJECT
37
WEST GRID
DUND0NRLD
TWP.
QUEBEC
SCRLE
: l
INCH
TO
200
FEET
NO
TE:
TOP
OF
CO
NTO
UR
IflB
EL
S
PO
INf
TOW
HRD
THE
HIG
HS
R
EH
DIN
GS
IN
G
RMM
RSDf
lTE:
DEC.
. 19
71MflP 7
1 - 5m
210
42A10NW8795 2.774 DUNDONALD
20 N
ION
—
IDS
20 S
20N
— I
ON
— 1
05
JL
FO
R
KE
Y M
AP
--S
EE
M
AP
71-5
-4-Z
.
MflG
NETO
MET
ER S
URVE
Y
GECJ
SERR
CH C
ONS
ULTf
lNTS
LTD
DOME EX
PLOR
RTIO
N (CRNRDR) LI
MITE
DPROJECT
37
ERST GRID
DUNDQNflLD TWP. QUEBEC
5CRLE
: i
INCH TO 200
FEET
NOTE:TOP OF CONTOUR
LRBELS POINT
TOWRRD THE
HIGHS
RERDING5 IN GflMMflS
DfiTE:
DEC..
1971
MflP 71 -
42M
8NW
8795
2
.774
DU
ND
ON
ALD
220
LJ
CO or
an o
o * o
20
N -
10
N
--e—-N-
-
10 s
—
20
S
r*e \J M
.c C
AR
T-
3264
60
xi-
n'
7 -
TUR
flM
SU
RV
EY
' SY
GEOSERRCH CQNSULTRNTS LTD.
/sort
DO
A/f
EX
PL
OR
AT
ION
(C
AN
AD
A)
LIM
ITE
D
DK
.,i?7
t42A10NW8795 2.774 DUNDONALD
PR
OJ
EC
T
37
PO
RTI
ON
OF
LO
TS
5, 6
, C
ON
. HI,
1 VD
UN
DO
NA
LD
TWP
., O
NTA
RIO
SC
ALE
: /IN
CH r
o 2O
O Ff
GTI/-
54
OS
30
X*t
i,f
Lik
r a
vb
fvfl
* P
vn
fli
So
wf
L
V M
| 5 C
AR
T
;
wnK
MO
UiW
Difc
W' -
Vfr
n^
^i
nt'f
'f,
) ,'
,\ *
f^5
3^
J
"^ ^
-i"
\ -
* --
^
' *
~ "
,~t
•*e.'
^-\
- '\
^ ^
A-
^^^.-w
./^
3^^-"
'v y
Vx
/- \
-r \x
'\
f *
n '
^ i
x
KE
Y M
AP
f
'*rc
# r
o 2
LOO
PSLE
GEN
D
R Z3W71 iaH40 ID
S 2N
B 23U71 10H40
2N
24N
C 8H
16E
MN
26N50
O 8H
16E
28N50 44N
E 16
E 43E
28NSO 44N5D
F 16
E 43E
14N
28N
-* RHTI0. 660 C-P.S,
- PHHSE. 660 C-P-S.
-*c Rf
lTIB
. 220 C.P-S.
K PH
fiSE
. 220 C.P-S.
TURRM SURVEY
BY
GEOSERRCH CQNSULTRNTS LTD.
/-o*
DO
ME
EX
PL
OR
AT
ION
(C
AN
AD
A)
LIM
ITE
D
42A10NWB795 2.774 DUNDONALD
DE
C-
PR
OJE
CT
3
7
PO
RT
ION
OF
LO
TS
/-
3,
CO
M III
DU
ND
ON
AL
D
TW
P.,
ON
TA
RIO
//N
CH
TO
Z
OO
71-5
42