Detailed Summary Report

Assessment Report: 17086

Property Name Bonaparte
17086a.pdf
17086b.pdf
17086c.pdf
Location
NAD 83
51° 00' 30.00'' N, 120° 26' 48.00'' W
51.008333, -120.446667
UTM: Easting 679122, Northing 5653855, Zone 10 (North)
NAD 27
51° 00' 30.21'' N, 120° 26' 44.04'' W
51.008391, -120.445568
UTM: Easting 679205, Northing 5653645, Zone 10 (North)
NTS 092P01W
BCGS 092P008
Mining Divisions Kamloops
Mining Camp
Title 1988 Geophysical Program on the Bonaparte Property West Geological, Geochemical and Geophysical Report on the Bonaparte Geological, Geochemical and Geophysical Report on the Bonaparte Property East Property West
Report Year 1988
Number of Pages 336
Statements of Work 0000029, 0000030, 0000031, 0000032
Affidavit Date 1988-03-24
Off Confidential 1989-03-24
Claims Bob 102-104, Bob 107-112, Bob 115, Bob 119, Bob 21-24, Bob 231-232, Bob 234, Bob 33, Bob 341, Bob 39-43, Bob 45-48, Stu 1-2
General Work Categories Geochemical, Geological, Geophysical
Operators Gabriel Resources Inc.
Gallant Gold Mines Limited
Inter-Pacific Resource Corp.
Owners MineQuest Exploration Associates Limited
Authors Gourlay, Andrew W.
McClintock, John A.
MINFILE Nos 092P 050, 092P 159
Commodities Gold
Work Done
Geochemical Heavy minerals 13 sample(s)
Elements Analyzed For Gold
Rock 170 sample(s)
Elements Analyzed For Gold
Soil 2350 sample(s); No. of maps: 7; Scale(s): 1:2500
Elements Analyzed For Silver, Gold, Copper
Geological Geological 5000.0 ha; No. of maps: 8; Scale(s): 1:10 000, 1:2500, 1:25 000, 1:5000
Geophysical Electromagnetic, ground VLF; 41.6 km; Scale(s): 1:10 000, 1:5000
Magnetic, ground 65.6 km; No. of maps: 1; Scale(s): 1:10 000, 1:5000
Keywords
Related Report(s) 16045, 15757, 15651, 15166, 13908
File(s) 17086a.pdf
17086b.pdf
17086c.pdf
Geological Summary
Argillaceous metasedimentary rocks, metamorphosed volcanic rocks and bedded greywacke and arkose form the basement rocks. The argillaceous metasedimentary rocks have been intruded by hornblende diorite correlated with Thuya-Takomkane Batholith intrusions resulting in hornfelsed contact zones. Basalt-andesite lavas, breccias and tuffs form the high ground. The hornblende diorite has been cut by late stage quartz veins that carry pyrite, chalcopyrite and rarely geochemically anomalous gold.