Detailed Summary Report

Assessment Report: 16577

Property Name Byrl
16577.pdf
Location
NAD 83
50° 50' 57.00'' N, 120° 46' 20.00'' W
50.849167, -120.772222
UTM: Easting 656821, Northing 5635417, Zone 10 (North)
NAD 27
50° 50' 57.22'' N, 120° 46' 16.02'' W
50.849229, -120.771116
UTM: Easting 656903, Northing 5635207, Zone 10 (North)
NTS 092I15W
BCGS 092I087
Mining Divisions Kamloops
Mining Camp
Title Geochemical, Geological and Physical Work on the Byrl Claim Group
Report Year 1987
Number of Pages 42
Statements of Work n/a
Affidavit Date 1987-11-26
Off Confidential 1988-11-26
Claims BYRL 1-4
General Work Categories Geochemical, Physical
Operators Ward, David A.
Owners Ward, David A.
Authors Ward, David A.
MINFILE Nos 092INE037, 092INE058
Commodities Palladium, Nickel, Silver, Platinum, Copper, Arsenic
Work Done
Geochemical Soil 50 sample(s)
Elements Analyzed For Silver, Arsenic, Copper, Nickel, Palladium, Platinum
Physical Trench 83 trench(es); 518.2 m; No. of maps: 2; Scale(s): 1:1000
Keywords
Related Report(s) 15164, 13981, 13216, 2467, 1989, 1914, 1789
File(s) 16577.pdf
Geological Summary
A slice of variably altered and intruded Upper Triassic(?) calc-alkaline rocks about two kilometres wide trends northerly for at least three kilometres through the Byrl claims. Plutonic rocks of variable texture and composition, assumed to be Triassic-Jurassic, have intruded the Triassic volcanic rocks. Even though most of the intrusives are quartz deficient, two fine-grained felsic intrusives are present. Both the felsic intrusives and older volcanic rocks have been locally sheared, brecciated and mineralized to varying degrees with cinnabar, chalcedonic quartz, calcite and gypsum in some cases. Chalcedonic quartz is more commonly associated with the felsic intrusives while calcite is more commonly associated with the volcanic rocks.