Property Name |
PF
16029.pdf
|
Location |
NAD 83 |
48° 50' 17.00'' N, 123° 38' 05.00'' W
48.838056, -123.634722
UTM: Easting 453425, Northing 5409648, Zone 10 (North)
|
NAD 27 |
48° 50' 17.79'' N, 123° 38' 00.35'' W
48.838275, -123.633432
UTM: Easting 453518, Northing 5409452, Zone 10 (North)
|
NTS |
092B13E |
BCGS |
092B082 |
|
Mining Divisions |
Victoria |
Mining Camp |
|
Title |
1986 Geological Report on the PF Option |
Report Year |
1987 |
Number of Pages |
283 |
Statements of Work |
n/a |
Affidavit Date |
1987-03-02 |
Off Confidential |
1988-03-02 |
Claims |
Beatrice I-IV, Crof 1, John Travers, John Travers I-IV, P.F. III, P.F. V, PF, Peggy I-IV |
General Work Categories |
Geochemical, Geological, Physical |
Operators |
Falconbridge
|
Owners |
Postuk, P.
|
Authors |
Booth, Ken
|
MINFILE Nos |
092B 038,
092B 039
|
Commodities |
|
Work Done |
Geochemical |
Rock |
203 sample(s) |
|
Elements Analyzed For |
Multielement |
|
Soil |
349 sample(s) |
|
Elements Analyzed For |
Silver, Copper, Lead, Zinc |
Geological |
Geological |
0.0 ha; Scale(s): 1:2500, 1:5000 |
Physical |
Line/grid |
8.0 km |
|
Keywords |
|
Related Report(s) |
2397
|
File(s) |
16029.pdf
|
Geological Summary |
The claims are underlain by mafic volcaniclastics with minor felsic flows and ash tuffs of the Upper Devonian Myra Formation which is part of the Paleozoic Sicker Group. These rocks are intruded by the Paleozoic Saltspring Intrusion and Jurassic gabbro. Schistosity is moderately developed and has a strike ranging from 110-130 degrees and dips steeply to the north and south. One analysis of a quartz vein yielded 0.35 per cent copper. Two pyritic zones occur on the property. The zones contain up to 7 per cent pyrite and up to 0.09 per cent copper. The rocks on this property have been affected by regional low-grade greenschist metamorphism.
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