Detailed Summary Report

Export Report

Assessment Report: 18129

Property Name

Ticker Tape
18129a.pdf
18129b.pdf

Location

NAD 83	56° 49' 59.00'' N, 131° 00' 07.00'' W 56.833056, -131.001944 UTM: Easting 377852, Northing 6300589, Zone 9 (North)
NAD 27	56° 49' 59.41'' N, 131° 00' 01.03'' W 56.833170, -131.000285 UTM: Easting 377949, Northing 6300386, Zone 9 (North)
NTS	104B14E, 104B15W
BCGS	104B085

Mining Divisions

Liard

Mining Camp

Title

Geological, Geochemical and Diamond Drilling Report on the Ticker Tape Property

Report Year

1988

Number of Pages

285

Statements of Work

n/a

Affidavit Date

1988-09-19

Off Confidential

1989-09-19

Claims

Ice 1-2, Ice 6-11, New 7-8, Ver 3-4

General Work Categories

Drilling, Geochemical, Geological

Operators

Ticker Tape Resources Ltd.

Owners

Ticker Tape Resources Ltd.

Authors

Hudson, K.
Cavey, George

MINFILE Nos

Commodities

Lead, Silver, Gold, Zinc

Work Done

Drilling	Diamond surface	9 hole(s); 975.0 m; No. of maps: 4; Scale(s): 1:500
Geochemical	Rock	254 sample(s); No. of maps: 4; Scale(s): 1:500
	Elements Analyzed For	Multielement
	Sampling/assaying	739 sample(s)
	Elements Analyzed For	Multielement
	Silt	19 sample(s)
	Elements Analyzed For	Multielement
	Soil	270 sample(s); No. of maps: 5; Scale(s): 1:10 000
	Elements Analyzed For	Multielement
Geological	Geological	750.0 ha; No. of maps: 5; Scale(s): 1:10 000, 1:2000, 1:500
Physical	Line/grid	23.0 km

Keywords

Related Report(s)

File(s)

18129a.pdf
18129b.pdf

Geological Summary

The property is possibly underlain by Unik River-Betty Creek Formation rocks. Two styles of mineralization are developed. Native gold +/- bismuth bearing quartz veins which are shallow dipping and vary in width from 0.1 to 1.3 metres along a 150 metre surface exposure are hosted by granodiorite which has been pervasively chloritized and locally silicified with vein envelopes and microveinlets. Local argillic, potassic and chlorite-magnetite alteration is also present. The second style of mineralization developed on the property consists of fine-grained lead-zinc mineralization which is hosted in carbonates.