Detailed Summary Report

Export Report

Assessment Report: 17274

Property Name

White Pine
17274a.pdf
17274b.pdf
17274c.pdf
17274d.pdf

Location

NAD 83	50° 26' 17.00'' N, 125° 21' 35.00'' W 50.438056, -125.359722 UTM: Easting 332436, Northing 5589998, Zone 10 (North)
NAD 27	50° 26' 17.40'' N, 125° 21' 30.50'' W 50.438166, -125.358473 UTM: Easting 332520, Northing 5589789, Zone 10 (North)
NTS	092K06W
BCGS	092K044

Mining Divisions

Vancouver

Mining Camp

Title

Diamond Drilling Report on the White Pine Property Geological, Geochemical and Geophysical Report on the White Pine Property

Report Year

1988

Number of Pages

156

Statements of Work

n/a

Affidavit Date

1988-01-12

Off Confidential

1989-01-12

Claims

Bick 2, Electric, Stump Ranch, Union, White Pine

General Work Categories

Drilling, Geochemical, Geological, Geophysical, Physical

Operators

Rea Gold Corporation

Owners

Verdstone Gold Corporation

Authors

Windsor, Dwayne M.
Blanchflower, J. Douglas

MINFILE Nos

092K 036

Commodities

Silver, Copper, Gold

Work Done

Drilling	Diamond surface	13 hole(s); NQ; 1162.9 m; No. of maps: 14; Scale(s): 1:2500, 1:500
Geochemical	Rock	86 sample(s)
	Elements Analyzed For	Multielement
	Sampling/assaying	65 sample(s)
	Elements Analyzed For	Silver, Arsenic, Gold, Copper, Molybdenum/Molybdenite, Lead, Zinc
	Soil	531 sample(s); No. of maps: 14; Scale(s): 1:2500
	Elements Analyzed For	Multielement
Geological	Geological	164.0 ha; No. of maps: 2; Scale(s): 1:2500
Geophysical	Electromagnetic, ground	VLF; 20.2 km; No. of maps: 4; Scale(s): 1:2500
	Magnetic, ground	21.8 km; No. of maps: 2; Scale(s): 1:2500
Physical	Line/grid	21.8 km
	Road, local access	2.9 km
	Trench	3 trench(es); 100.0 m

Keywords

Related Report(s)

15589

File(s)

17274a.pdf
17274b.pdf
17274c.pdf
17274d.pdf

Geological Summary

The property is underlain by Paleozoic schists, greenstone, augite porphyry, gneiss of greenschist to amphibolite grade metamorphism and fine to coarse-grained quartz dioritic-granodioritic intrusive rocks of the Upper Cretaceous Coast Plutonic Complex. The gold and silver bearing mineralization is hosted by quartz-sulphide veins which are fracture controlled by northeasterly to northwesterly trending fault and shear structures.