Detailed Summary Report

Export Report

Assessment Report: 18240

Property Name

Wayside
18240a.pdf
18240b.pdf

Location

NAD 83	50° 52' 00.00'' N, 122° 50' 05.00'' W 50.866667, -122.834722 UTM: Easting 511631, Northing 5635011, Zone 10 (North)
NAD 27	50° 52' 00.30'' N, 122° 50' 00.76'' W 50.866749, -122.833545 UTM: Easting 511714, Northing 5634802, Zone 10 (North)
NTS	092J15W
BCGS	092J086

Mining Divisions

Lillooet

Mining Camp

Bridge River Camp

Title

Group Physical, Geological, Geophysical and Drilling Report on the Wayside

Report Year

1988

Number of Pages

301

Statements of Work

n/a

Affidavit Date

1988-10-19

Off Confidential

1989-10-19

Claims

Alpha, Beta, Cabinet, Camp Denison, Commodore Fr., Counsel, Gamma, Helium, Lodge, Mineral Lease 57, Newport, Queen City Fr., Rodeo, Sun, Wayside

General Work Categories

Drilling, Geological, Geophysical, Physical

Operators

Chevron Minerals Ltd.

Owners

Chevron Minerals Ltd.

Authors

McAllister, S.G.
McArdy, D.
Getsinger, Jennifer S. PhD, PGeo

MINFILE Nos

092JNE030

Commodities

Gold

Work Done

Drilling	Diamond surface	13 hole(s); NQ; 2083.9 m
Geochemical	Rock	19 sample(s)
	Elements Analyzed For	Multielement
	Sampling/assaying	861 sample(s)
	Elements Analyzed For	Multielement
Geological	Geological	1825.0 ha; No. of maps: 13; Scale(s): 1:200, 1:2000, 1:5000
	Petrographic	5 sample(s)
Geophysical	Electromagnetic, ground	VLF; 34.9 km; No. of maps: 4; Scale(s): 1:2000
Physical	Trench	10 trench(es); 355.0 m

Keywords

Bralorne Intrusions, Cadwallader Group, Fergusson Group, Gold, Permian, Quartz veins, Triassic

Related Report(s)

16718

File(s)

18240a.pdf
18240b.pdf

Geological Summary

The area is underlain by volcano-sedimentary Fergusson Group of Permian to Triassic age and Triassic age 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.