Detailed Summary Report

Assessment Report: 14030

Property Name
14030.pdf
Location
NAD 83
58° 11' 59.00'' N, 128° 25' 06.00'' W
58.199722, -128.418333
UTM: Easting 534190, Northing 6451094, Zone 9 (North)
NAD 27
58° 11' 59.21'' N, 128° 25' 00.14'' W
58.199779, -128.416706
UTM: Easting 534287, Northing 6450891, Zone 9 (North)
NTS 104I01W
BCGS 104I028
Mining Divisions Liard
Mining Camp
Title
Report Year 1985
Number of Pages 0
Statements of Work n/a
Affidavit Date 1985-09-17
Off Confidential 1986-09-17
Claims JOSH 1-5
General Work Categories Geophysical, Physical
Operators Esso Min. Can.
Owners
Authors Holbek, Peter M.
Doborzynski, Z.
MINFILE Nos 104I 075
Commodities
Work Done
Geophysical Electromagnetic, ground 0.0 km
Physical Line/grid 0.0 km
Keywords
Related Report(s)
File(s) 14030.pdf
Geological Summary
POLYMETALLIC SULPHIDE DEPOSITS ARE HOSTED BY FELSIC PYROCLASTIC ROCKS OF THE TRIASSIC AGE KUTCHO FORMATION. THE LARGEST SULPHIDE LENS CONTAINS GEOLOGICAL RESERVES OF 17,000,000 TONNES GRADING 1.6% COPPER, 2.3% ZINC, 29.2 GRAMS/TONNE SILVER AND 0.3 GRAMS/TONNE GOLD. HOST ROCKS ARE ALTERED IN THE VICINITY OF THE SULPHIDE ZONES AND HAVE UNDERGONE REGIONAL GREENSCHIST FACIES META- MORPHISM AND SINGLE PHASE DEFORMATION. THREE SUB- CONTINUOUS CONDUCTORS WERE IDENTIFIED ALONG THE JOSH CREEK AREA GRIDS. CONTINUITY OF THE CONDUCT- ORS PARALLEL TO THE STRUCTURAL TREND SUGGESTS A LITHOLOGICALLY CONTROLLED LINEAR ANOMALY.