| Property Name |
Cliff Pick
18238.pdf
|
| Location |
| NAD 83 |
50° 37' 29.00'' N, 127° 27' 06.00'' W
50.624722, -127.451667
UTM: Easting 609517, Northing 5609238, Zone 9 (North)
|
| NAD 27 |
50° 37' 29.48'' N, 127° 27' 01.24'' W
50.624855, -127.450345
UTM: Easting 609614, Northing 5609036, Zone 9 (North)
|
| NTS |
092L11W |
| BCGS |
092L063 |
|
| Mining Divisions |
Nanaimo |
| Mining Camp |
Island Copper Area |
| Title |
Geochemical, Geophysical and Geological Report on the Pick and Cliff Mineral Claims |
| Report Year |
1988 |
| Number of Pages |
48 |
| Statements of Work |
0000123 |
| Affidavit Date |
1988-12-19 |
| Off Confidential |
1989-12-19 |
| Claims |
Cliff 1, Cliff 78, Cliff 79 Fr., Pick 1-2, Pick 5 Fr. |
| General Work Categories |
Geochemical, Geological, Geophysical, Physical |
| Operators |
McAndrew, John M.
|
| Owners |
McAndrew, John M.
|
| Authors |
McAndrew, John M.
|
| MINFILE Nos |
092L 113,
092L 159
|
| Commodities |
Gold, Zinc, Lead, Molybdenum/Molybdenite, Copper, Silver |
| Work Done |
| Geochemical |
Rock |
9 sample(s) |
|
Elements Analyzed For |
Gold |
|
Soil |
98 sample(s); No. of maps: 2; Scale(s): 1:2500, 1:5000 |
|
Elements Analyzed For |
Copper, Zinc |
| Geological |
Geological |
225.0 ha; No. of maps: 1; Scale(s): 1:2500 |
| Geophysical |
Magnetic, ground |
5.2 km; No. of maps: 1; Scale(s): 1:2500 |
| Physical |
Trench |
3 trench(es); 8.0 m |
|
| Keywords |
Bornite, Chalcopyrite, Contact zones, Galena, Intrusives, Limestones, Magnetite, Pyrite, Quatsino Formation, Skarns, Specularite, Sphalerite |
| Related Report(s) |
11407
|
| File(s) |
18238.pdf
|
| Geological Summary |
Karmutsen basalt and andesite flows, massive Quatsino limestone, Parson Bay Formation, argillaceous and carbonaceous sedimentary rocks, and Bonanza andesite flows and breccias are intruded by granodiorite, diorite, andesite and hornblende-porphyry (Jurassic to Tertiary). Skarn mineralization, containing chalcopyrite, bornite, sphalerite, ganlena, pyrite, magnetite and specularite, occurs along limestone contacts for over 2 kilometres. The mineralization strikes north- easterly, usually has a shallow dip to the southeast and has been block faulted. Some faults may have served as channelways for mineralizing solutions.
|
