Detailed Summary Report

Export Report

Assessment Report: 18251

Property Name

PDL
18251a.pdf
18251b.pdf
18251c.pdf

Location

NAD 83	49° 22' 00.00'' N, 119° 48' 04.00'' W 49.366667, -119.801111 UTM: Easting 296640, Northing 5471992, Zone 11 (North)
NAD 27	49° 22' 00.21'' N, 119° 48' 00.26'' W 49.366726, -119.800071 UTM: Easting 296709, Northing 5471776, Zone 11 (North)
NTS	082E05W
BCGS	082E032

Mining Divisions

Osoyoos

Mining Camp

Title

Geology, Geochemistry, Geophysics and Diamond Drilling on the PDL Property

Report Year

1988

Number of Pages

526

Statements of Work

0000059

Affidavit Date

1988-11-08

Off Confidential

1989-11-08

Claims

Akira I, Akira II Fr., Alalla 1-2, Astro 1, Astro 51-52, Astro 54-55, PDL, Shatford 1-2

General Work Categories

Drilling, Geochemical, Geological, Geophysical

Operators

QPX Minerals Inc.

Owners

QPX Minerals Inc.

Authors

Lee, L.J.

MINFILE Nos

082ESW190

Commodities

Silver, Gold

Work Done

Drilling	Diamond surface	3 hole(s); NQ; 524.0 m; No. of maps: 3; Scale(s): 1:250
Geochemical	Rock	301 sample(s); No. of maps: 2; Scale(s): 1:5000
	Elements Analyzed For	Multielement
	Sampling/assaying	165 sample(s)
	Elements Analyzed For	Multielement
	Soil	3005 sample(s); No. of maps: 6; Scale(s): 1:2500
	Elements Analyzed For	Multielement
Geological	Geological	1000.0 ha; No. of maps: 5; Scale(s): 1:10 000, 1:5000
	Petrographic	15 sample(s)
Geophysical	Electromagnetic, ground	VLF; 50.0 km; No. of maps: 5; Scale(s): 1:5000
	Magnetic, ground	50.0 km; No. of maps: 1; Scale(s): 1:5000

Keywords

Cherts, Conglomerates, Gold, Greenstones, Independence Formation, Lavas, Marron Formation, Massive sulphides, Old Tom Formation, Shoemaker Formation, Springbrook Formation, Stringers, Tertiary, Triassic

Related Report(s)

18527

File(s)

18251a.pdf
18251b.pdf
18251c.pdf

Geological Summary

The PDL property is underlain by Triassic or older cherts and greenstones (Old Tom, Independence and Shoemaker Formations), Tertiary conglomerates (Springbrook Formation) and lavas (Marron Formation). Minor gold bearing massive sulphides and pyrite/ arsenopyrite stringers occur in cherts of the Shoemaker Formation and anomalous gold values accompany alteration in Tertiary rocks.