Property Name |
Lambda and Xi
16155.pdf
|
Location |
NAD 83 |
56° 18' 53.00'' N, 130° 09' 25.00'' W
56.314722, -130.156944
UTM: Easting 428433, Northing 6241709, Zone 9 (North)
|
NAD 27 |
56° 18' 53.40'' N, 130° 09' 19.21'' W
56.314833, -130.155337
UTM: Easting 428530, Northing 6241507, Zone 9 (North)
|
NTS |
104B08E |
BCGS |
104B040 |
|
Mining Divisions |
Skeena |
Mining Camp |
|
Title |
Assessment Report on Geochemical Work on the Lambda and Xi Claims |
Report Year |
1987 |
Number of Pages |
31 |
Statements of Work |
n/a |
Affidavit Date |
1987-04-22 |
Off Confidential |
1988-04-22 |
Claims |
Lambda |
General Work Categories |
Geochemical |
Operators |
Teuton Resources Corp.
|
Owners |
Foerster, J.V.
|
Authors |
Cremonese, Dino M.
|
MINFILE Nos |
104B 170
|
Commodities |
|
Work Done |
Geochemical |
Heavy minerals |
0 sample(s) |
|
Rock |
0 sample(s) |
|
Keywords |
|
Related Report(s) |
|
File(s) |
16155.pdf
|
Geological Summary |
Rocks of the Lower Jurassic Unuk River Formation consisting of volcanic breccia, conglomerate, sandstone and siltstone are exposed in the northern half of the property. These are in fault contact to the south with Middle Jurassic Salmon River Formation siltstone, greywacke and sandstone. Lead-zinc mineralization in the form of coarse to fine-grained galena and sphalerite occurs in both schists and quartz veins in altered volcanics. Gold and silver values are associated with base metal mineralization.
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