Property Name |
Kael
15423.pdf
|
Location |
NAD 83 |
55° 14' 48.00'' N, 124° 45' 18.00'' W
55.246667, -124.755
UTM: Easting 388431, Northing 6123645, Zone 10 (North)
|
NAD 27 |
55° 14' 48.22'' N, 124° 45' 13.06'' W
55.246727, -124.753627
UTM: Easting 388515, Northing 6123434, Zone 10 (North)
|
NTS |
093N02E, 093N02W, 093N07W |
BCGS |
093N027 |
|
Mining Divisions |
Omineca |
Mining Camp |
|
Title |
Lithogeochemical Survey of the Kael #2 Mineral Claim |
Report Year |
1986 |
Number of Pages |
28 |
Statements of Work |
n/a |
Affidavit Date |
1986-09-26 |
Off Confidential |
1987-09-26 |
Claims |
Kael 2 |
General Work Categories |
Geochemical, Geological |
Operators |
Campbell, Colin J.
|
Owners |
Campbell, Colin J.
|
Authors |
Campbell, Colin J.
|
MINFILE Nos |
093N 101
|
Commodities |
|
Work Done |
Geochemical |
Rock |
60 sample(s) |
|
Elements Analyzed For |
Multielement |
Geological |
Petrographic |
3 sample(s); thin |
|
Keywords |
|
Related Report(s) |
10971,
3384,
3383,
2933,
2932,
2714
|
File(s) |
15423.pdf
|
Geological Summary |
The claim is underlain by syenite and monzonite of the Hogem Batholith in contact with Upper Triassic Takla Group volcanic rocks. Mineralization consists of quartz lenses with locally abundant bornite and as disseminated bornite and lesser chalcopyrite in altered potash feldspathized mesocratic monzonite. Gold up to 1680 ppb is associated with the best bornite mineralization.
|