| Property Name |
Barb-Gusty
18092.pdf
|
| Location |
| NAD 83 |
53° 38' 00.00'' N, 125° 22' 06.00'' W
53.633333, -125.368333
UTM: Easting 343409, Northing 5945334, Zone 10 (North)
|
| NAD 27 |
53° 38' 00.31'' N, 125° 22' 01.17'' W
53.633420, -125.366991
UTM: Easting 343493, Northing 5945124, Zone 10 (North)
|
| NTS |
093F11W |
| BCGS |
093F064 |
|
| Mining Divisions |
Omineca |
| Mining Camp |
|
| Title |
Geological, Geochemical and Geophysical Report on the Barb-Gusty Claim Group |
| Report Year |
1988 |
| Number of Pages |
198 |
| Statements of Work |
n/a |
| Affidavit Date |
1988-09-09 |
| Off Confidential |
1989-09-09 |
| Claims |
Barb 1-4, Gus 2 Fr., Gus 3 Fr., Gus Fr., Gusty, Gusty 2-3 |
| General Work Categories |
Geochemical, Geological, Geophysical |
| Operators |
Newmont Ex. of Can.
|
| Owners |
Newmont Ex. of Can.
|
| Authors |
Bohme, D.M.
|
| MINFILE Nos |
093F 065
|
| Commodities |
Silver, Gold |
| Work Done |
| Geochemical |
Rock |
670 sample(s) |
|
Elements Analyzed For |
Multielement |
|
Silt |
15 sample(s) |
|
Elements Analyzed For |
Multielement |
|
Soil |
2366 sample(s); No. of maps: 9; Scale(s): 1:1000, 1:2500, 1:5000 |
|
Elements Analyzed For |
Silver, Arsenic, Gold, Molybdenum/Molybdenite, Antimony, Zinc |
| Geological |
Geological |
2500.0 ha; No. of maps: 3; Scale(s): 1:5000 |
|
Petrographic |
2 sample(s) |
| Geophysical |
Electromagnetic, ground |
VLF; 77.6 km; No. of maps: 4; Scale(s): 1:5000 |
|
Magnetic, ground |
77.6 km; No. of maps: 4; Scale(s): 1:5000 |
| Physical |
Line/grid |
77.6 km |
|
Road, local access |
0.5 km |
|
Trench |
11 trench(es); 525.0 m; No. of maps: 3; Scale(s): 1:250 |
|
| Keywords |
|
| Related Report(s) |
|
| File(s) |
18092.pdf
|
| Geological Summary |
The property is underlain predominantly by acid to intermediate composition volcanic rocks of the Upper Cretaceous-Eocene Ootsa Lake Group. Major fault lineaments and local zones of intense fracturing display a strong north-northeast trend. Several small, structurally- controlled gold-silver occurrences on the claims are associated with argillically altered rhyolite, local fracturing and faulting, and translucent quartz to grey chalcedonic quartz veinlets. Erratic gold-silver values persist over areas up to 3 by 5 metres in size.
|
