malone gold prospect marmora township eastern …
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31C12SE8844 2 .11973 MARMORA
MIKING L':'? r
010
MALONE GOLD PROSPECT
MARMORA TOWNSHIP
EASTERN ONTARIO
REPORT ON A SELF-POTENTIAL SURVEY
r *~ r ! V E D
- by- I.SC.W -'
MINING LANDS HO**
C. R, Bowdldge, M.A., Ph.D.
December 1988
lINTRODUCTION
This report describes the results of a self-potential survey of a five-
claim property covering a series of occurrences of gold mineralization,
and referred to here as the Malone Gold Prospect, The survey work was
carried out in the fall of 1988.
PROPERTY
The property consists of five contiguous unpatented mining claims in lots
14 and 15 of concession X, Marmora Township, Hastings County, Southern
Ontario Mining Division. Details are as follows:
Claim no.
EO 840625
EO 840626
EO 840627
EO 840628
EO 898504
Fraction
NE/ 4
SE/ 4
SW/4
NW/4
NW/4
Lot
15
15
15
15
14
Con.
X
X
X
x
x
Each claim covers a quarter lot, for a nominal area of 50 acres, giving a
total property area of 250 acres, more or less.
LOCATION AND ACCESS
The property is situated approximately 4 km north of the village of Deloro
and l km south of the small community of Malone, in the eastern part of
Marmora Township. Deloro lies just north of Highway 7, approximately 200
km by road east-northeast of Toronto and 200 km west-southwest of Ottawa.
The Deloro-Malone road (Hastings County road No. 11) crosses the western
part of the property. The eastern quarter of the property lies east of
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fig. 3GEOLOGY AND GOLD DEPOSITS OF THE DELORO AREA, S.E. ONTARIO
Scale 1:63,360 After Wilson ( 1940)
2
the Molra River, and can be reached by crossing the river by the bridge at
Malone, and following the dirt road which circles the old marble quarries
in lot 16 of Concession XI. This road passes approximately 50 metres from
the north-east corner of the property.
HISTORY AND PREVIOUS WORK
A previous report by the writer has given a description of the history of
exploration and development of gold in the Deloro area/ and on the present
property. In summary, a modest amount of shallow shaft sinking and
pitting appears to have been done in the early 1870's and late 1880's, on
gold-bearing guartz-arsenopyrite veins on the property. No other work was
reported until 1986, when the author reported on geological mapping and
magnetic and VLF-electromagnetic surveys.
SELF-POTENTIAL SURVEY
The self-potential method, although not widely used in recent years, is a
simple and effective technique for finding near-surface occurrences of
sulphide mineralization. It depends on measuring low voltages produced In
the ground by oxidizing sulphide minerals. It does not depend on
detection of conductivity, and thus "massive sulphides" are not required
for the generation of a self-potential response. As with electromagnetic
methods, strong self-potential anomalies are produced by graphitic zones.
Self-potential readings are taken in millivolts, and local negative
deviations are anomalous.
3
The self-potential survey carried out In 1988 used the same grid as
previous surveys of the property in 1986. The line spacing was 100
metres, and the station Interval was 25 metres. Readings were taken at an
Interval of 12.5 metres.
The Instrument used was a Beckmann 310 voltmeter, with an input impedance
of 18 megohms. Ground contact was effected with porous pots filled with
saturated copper sulphate solution, and containing copper electrodes. The
pots were connected to each other and to the voltmeter by approximately l
kilometre of plastic-covered steel wire stored on a reel. Survey lines
were covered with one electrode stationary at the end of the line, and the
other electrode moved from station to station along the line. It was
necessary to stop the survey and move the stationary electrode and reel of
wire when lines crossed the road or the river.
The survey results are plotted on the accompanying map in numerical form,
with the voltage measured at each station expressed in millivolts, and
also as profiles. An anomaly will be a local negative deviation.
The readings in the survey seem to fluctuate around a background level of
about +250 millivolts. This background level represents an inherent
difference between the two porous pots being used, and illustrates the
importance of always using the same pot as the stationary electrode
throughout a survey.
4
The survey results show remarkably little variation across the grid.
Using a minimum anomaly amplitude of 50 millivolts, only two weak
anomalies can be defined. One lies at 2+05E on line 7N, and the other
lies at 2+25W on line 6N. Both of these anomalies lie in overburden-
covered areas/ but are close to outcrops and should be prospected in
detail.
CONCLUSIONS
The self-potential survey has defined only two single-line anomalies on
the property. Although they are of low amplitude, this is not significant
in assessing whether or not they are caused by sulphides. Both areas
should be prospected to search for unexposed mineralization.
The absence of self-potential anomalies from the rest of the survey area
indicates that any gold mineralization which may be present is not
necessarily associated with substantial accumulations of sulphide
minerals. Further exploration will have to rely on geological rather than
geophysical techniques.
Respectfully submitted,
C. R. Bowdldge
December 1988
e:s. G.co- "Min Nor
*
Ministry of Report of WorkNorthern Development
__pd Mines {Geophysical, Geological, Ontario^Br Geochemical and Expenditures)
DOCUMENT No
Wo~™. aoi. j
i
h, c. sf J C/
tructions: - Please type or print. ^~^'-f-^" - ' l — I f number of mining claims traversed
OType of Survey(s)
Claim
f* 9 3IC12SE8844 2.11973 MARMORA900
Addresf/J
Survey Company Date of Survey (from 6 to)
^x. *? ,^s5 z*r,/Day l Mo. | Yr. Day | Mo. | Yr.
Total Miles of line Cut
Name and Address of Author (of Geo-Technical report)
i f .L
Credits Requested per Each Claim in Columns at rightSpecial 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 credits do not apply to Airborne Surveys.
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other ?oTe:*^v Au
Geological
Geochemical
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Electromagnetic
Magnetometer
Radiometric
Days per Claim
20
Days per Claim
Days per Claim
Mining Claims Traversed (List in numerical sequence)
Expenditures (excludes power stripping)Type of Work Performed
Performed on Claim(s)
Calculation of Expenditure Days Credits
Total ExpendituresTotal
Days Credits
InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.
Date
17Recorded Holder or Agent (Signature)
Certification Verifying Report of Work
Total number of mining claims covered by this reporiiof work.
l hereby certify that l have a personal and intimate knowledge of the facts set forth i^/the Report of Work annexed hereto, having performed or witnessed same during and/or after its completion and the annexed report is true.
the work
Ministry ofNorthern Developmentand Mines
Geophysical-Geological-Geochemical Technical Data Statement
Ontario
TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT
TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.
l(d COD
lb O
Type of Survey(s) _ Township or Area — Claim Holder(s)^jZL
(C-1 S/V
Survey Company. Author of Report.
TP
Address of Author St.
Covering Dates of Survey-
Total Miles of Line
77/ Z2 M*(linecutting to office)
,*,,c/
SPECIAL PROVISIONS CREDITS REQUESTED
ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.
Geophysical—Electromagnetic.—Magnetometer.——Radiometric———Other—————
DAYSper claim
Geological.Geochemical.
AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)
Magnetometer. .Electromagnetic. . Radiometric
DATE:
(enter days per claim)
SIGNATURE:Author of Report or Agent
Res. Geol.. .Qualifications.Previous Surveys
File No. Type Date Claim Holder
MINING CLAIMS TRAVERSED List numerically
(prefix) (number)
i
TOTAL CLAIMS.
837 (85/12)
GEOPHYSICAL TECHNICAL DATA
GROUND SURVEYS — If more than one survey, specify data for each type of survey
Number of Stations ___________________________Number of Readings —
Station interval ____________________________Line spacing -————
Profile scale—————————————————————————^——.———-——-———.
Contour interval.
Instrument _
Bzl
Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours).
Base Station location and value ___
InstrumentCoil configuration
separation
Accuracy ——————————————————————————————————————————————————————————. Method: CD Fixed transmitter CD Shoot back CD In line D Parallel line
WJ W
Parameters measured.(specify V.L.F. nation)
Instrument.Scale constant.
tiso
Corrections made
Bas** stftion value anri loratinn
Elevation accuracy.
Instrument _________________———————————————————————————— Method CD Time Domain CD Frequency Domain
Parameters — On time __________________________ Frequency ————.— Off time ___________________________ Range ————————
— Delay time _________———————————————— Integration time.
Power.Electrode array.
Electrode spacing . Type of electrode
SELF POTENTIAL
Survpy Method ? T/) T/eV/?/?? iT^r/ZV^- /" ' /^Oi'/^ff *E^^
0r /M.^nm w,s?ir *v /-^^
Cnrrprtinnii maHp A/&&&
^^
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.
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 METHODSValues expressed in: per cent D
p. p. m. Dp. p. b. D
Cu, Pb,
Others_
Zn, Ni, Co, Ag, Mo, As.-(circle)
Field Analysis {.Extraction Method. Analytical Method- Reagents Used__
Field Laboratory AnalysisNo. ___________
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)
GeneraL General.
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LEGEND :
PROFILE SCALE l Cm s 200 Operator t D- Dmitrovic Instrument-. Beck man 310 Date : October 1986 2.11973
31C12SEM44 2.11973 MARMORA 210
MALONE GOLD PROSPECTMARMORA TOWNSHIP, ONTARIO
SELF POTENTIAL SURVEY
SCALE l : 2,500O 25 5O 75 IOO 50