| Property Name |
Shag
17814.pdf
|
| Location |
| NAD 83 |
50° 38' 20.00'' N, 115° 30' 44.00'' W
50.638889, -115.512222
UTM: Easting 605203, Northing 5610725, Zone 11 (North)
|
| NAD 27 |
50° 38' 20.06'' N, 115° 30' 40.70'' W
50.638907, -115.511305
UTM: Easting 605271, Northing 5610510, Zone 11 (North)
|
| NTS |
082J11W, 082J12E |
| BCGS |
082J063 |
|
| Mining Divisions |
Golden |
| Mining Camp |
|
| Title |
Geophysical Report on the Shag Creek Project |
| Report Year |
1988 |
| Number of Pages |
31 |
| Statements of Work |
0000018 |
| Affidavit Date |
1988-08-15 |
| Off Confidential |
1989-08-15 |
| Claims |
Shag, Shag 3-4 |
| General Work Categories |
Geophysical |
| Operators |
Graf, Chris
|
| Owners |
Graf, Chris
|
| Authors |
Hendrickson, Grant A.
|
| MINFILE Nos |
082JNW002
|
| Commodities |
Zinc, Lead, Silver |
| Work Done |
| Geophysical |
Induced Polarization |
12.0 km; No. of maps: 4 |
| Physical |
Line/grid |
12.0 km |
|
| Keywords |
|
| Related Report(s) |
11170,
10143,
9678,
8091,
7382,
7036
|
| File(s) |
17814.pdf
|
| Geological Summary |
A number of small lead-zinc showings occur in a thick, massive to well bedded limestone-dolostone unit of the Middle Cambrian Cathedral Formation. Massive sphalerite layers can be traced for 600 metres along strike.
|
