Property Name |
Cunningham Creek
17114.pdf
|
Location |
NAD 83 |
52° 53' 00.00'' N, 121° 20' 05.00'' W
52.883333, -121.334722
UTM: Easting 612054, Northing 5860591, Zone 10 (North)
|
NAD 27 |
52° 53' 00.19'' N, 121° 20' 00.76'' W
52.883385, -121.333545
UTM: Easting 612137, Northing 5860381, Zone 10 (North)
|
NTS |
093A14W |
BCGS |
093A084 |
|
Mining Divisions |
Cariboo |
Mining Camp |
Cariboo - Barkerville Camp |
Title |
1987 Cunningham Creek Property Report |
Report Year |
1988 |
Number of Pages |
167 |
Statements of Work |
n/a |
Affidavit Date |
1987-07-09 |
Off Confidential |
1988-07-09 |
Claims |
Mineral Lease M32 |
General Work Categories |
Drilling, Geochemical, Geological, Geophysical, Physical |
Operators |
Cathedral Gold Corp.
|
Owners |
Cathedral Gold Corp.
|
Authors |
Delancey, Peter
|
MINFILE Nos |
093A 071,
093A 093
|
Commodities |
Gold |
Work Done |
Drilling |
Diamond surface |
12 hole(s); NQ; 1098.4 m; No. of maps: 7; Scale(s): 1:250 |
Geochemical |
Rock |
484 sample(s) |
|
Elements Analyzed For |
Multielement |
|
Soil |
940 sample(s); No. of maps: 5; Scale(s): 1:1000 |
|
Elements Analyzed For |
Multielement |
Geological |
Geological |
150.0 ha; No. of maps: 5; Scale(s): 1:1000, 1:5000 |
Geophysical |
Magnetic, ground |
9.1 km; No. of maps: 7; Scale(s): 1:1000 |
Physical |
Line/grid |
28.0 km |
|
Keywords |
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Related Report(s) |
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File(s) |
17114.pdf
|
Geological Summary |
Interbedded quartzites, sericite schists, limestones and chlorite schists striking northwest and dipping 70-80 degrees northeast are cut by several systems of auriferous quartz veins. The roughly parallel trending Shasta, Hudson and 605 veins occupy steeply dipping faults. Gold mineralization is associated with sulphides, mostly pyrite, and is concentrated along steeply plunging ore shoots. Preliminary results indicate that massive pyritic "replacement" deposits, similar to those at Wells, may occur along a limestone horizon.
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