Detailed Summary Report

Export Report

Assessment Report: 17091

Property Name

Wayside
17091a.pdf
17091b.pdf
17091c.pdf

Location

NAD 83	50° 52' 57.00'' N, 122° 49' 30.00'' W 50.8825, -122.825 UTM: Easting 512311, Northing 5636773, Zone 10 (North)
NAD 27	50° 52' 57.30'' N, 122° 49' 25.76'' W 50.882582, -122.823823 UTM: Easting 512394, Northing 5636564, Zone 10 (North)
NTS	092J15W
BCGS	092J086

Mining Divisions

Lillooet

Mining Camp

Bridge River Camp

Title

Physical, Geological, Geophysical, Geochemical and Diamond Drilling Work on the Wayside Group

Report Year

1988

Number of Pages

556

Statements of Work

n/a

Affidavit Date

1987-12-22

Off Confidential

1988-12-22

Claims

Alpha, Beta, Cabinet, Camp Denison, Commodore Fr., Counsel, Gamma, Helium, Lake 1, Lodge, Newport, Queen City Fr., Rodeo, Sun, Wayside Ext. 2

General Work Categories

Drilling, Geochemical, Geological, Geophysical, Physical

Operators

Chevron Canada Resources Ltd.

Owners

Chevron Minerals Ltd.

Authors

Dick, L.
McPherson, M.D.
Moffat, L.
Howell, William A.

MINFILE Nos

092JNE030, 092JNE121, 092JNE124

Commodities

Gold

Work Done

Drilling	Diamond surface	8 hole(s); HQ NQ; 924.8 m; No. of maps: 4; Scale(s): 1:1000, 1:5000
Geochemical	Rock	433 sample(s)
	Elements Analyzed For	Multielement
	Sampling/assaying	262 sample(s)
	Elements Analyzed For	Multielement
	Soil	1440 sample(s); No. of maps: 5; Scale(s): 1:2000, 1:5000
	Elements Analyzed For	Multielement
Geological	Geological	1870.0 ha; No. of maps: 10; Scale(s): 1:1000, 1:2000, 1:5000
Geophysical	Electromagnetic, ground	VLF; 30.4 km; No. of maps: 10; Scale(s): 1:2000, 1:5000
	Magnetic, ground	30.4 km; No. of maps: 5; Scale(s): 1:2000, 1:5000
Physical	Line/grid	35.0 km
	Trench	41 trench(es); 1077.0 m; No. of maps: 9; Scale(s): 1:100, 1:2000, 1:5000

Keywords

Related Report(s)

16718

File(s)

17091a.pdf
17091b.pdf
17091c.pdf

Geological Summary

The area is underlain by the Permo-Triassic volcano-sedimentary Bridge River Group and the Upper Triassic Cadwallader Group. In fault contact with these are the Bralorne Intrusions considered to be of Permian age. The area exhibits a high degree of faulting which seems to control the alteration and vein formation. Alteration takes the form of carbonatization and silicification. Mineralization is present as native gold in banded quartz veins.