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File Created: 13-Sep-1991 by Ron McMillan (RHM)
Last Edit:  21-May-2014 by Nicole Barlow (NB)

Summary Help Help

NMI
Name CUP, SECOND VEIN, BARBER BILL (SOUTH) Mining Division Omineca
BCGS Map 093M033
Status Prospect NTS Map 093M05E, 093M06W
Latitude 055º 21' 00'' UTM 09 (NAD 83)
Longitude 127º 30' 18'' Northing 6134758
Easting 594795
Commodities Silver, Lead, Zinc, Antimony Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Intermontane Terrane Overlap Assemblage, Plutonic Rocks
Capsule Geology

The Cup or Second vein is situated on the east rim of Silver Cup Basin, on the upper northern slope of Nine Mile Mountain, 14 kilometres northeast of Hazelton.

On the Cup property, quartz-filled fissure veins contain galena, sphalerite, jamesonite and pyrite in a gangue of quartz. The Second vein, situated at 1450 metres elevation on the Cup II claim, was exposed for more than 76 metres running east-west along the steep slope of the Silver Cup Basin. The vein occurs at the contact between hornfelsed tuffaceous sandstones and argillites of the Middle Jurassic to Lower Cretaceous Bowser Lake Group and granodiorite of the Late Cretaceous Bulkley Intrusions. The vein strikes east, dipping shallowly south, and ranges in thickness from 25 to 60 centimetres. The vein branches, pinches and swells, and is displaced by faults.

Another mineralized vein, situated 305 metres southwest of the peak of Nine Mile Mountain on the Cup I claim, was exposed for approximately 61 metres in two trenches. The vein consisted mainly of antimony or jamesonite, pyrite and minor galena and sphalerite.

The first discovery of silver-lead-zinc ore containing antimony was made on Nine Mile Mountain in 1908. In the years that followed, numerous other mineral-bearing veins were discovered in the area. Between 1910 and 1913, small shipments of high-grade silver-lead ore were made from 15 properties.

As of 1980, the Cup claims were owned by Short Staun Minerals Corporation. That year, a program of regional geological mapping and prospecting was carried out over the claims and surrounding areas.

By 1981, the area immediately to the east was held by Sunrise Metals Corporation. As part of a joint venture agreement with Sunrise Metals, Westmin Resources Limited began work on the Sunrise property. That year, exploration consisted of geological mapping, rock sampling, soil geochemical surveying and trenching. Exploration continued in 1982 with an induced polarization and resistivity geophysical survey over the central portion of the property.

The ground lay dormant until 2005, when Cadre Capital Incorporated staked new claims over the Nine Mile Mountain area and the Sidina Creek area to the north as part of their Hazelton project. The following year, Golden Sabre Resources optioned the claims and carried out a limited exploration program of rock sampling and soil grid geochemistry. Between 2006 and 2012, the claims appear to have been dormant.

By 2012, TAD Mineral Exploration Limited (formerly known as TAD Capital Corporation) expanded their Sidina property to include additional claims covering the Nine Mile Mountain area to the south, formerly held by Cadre Capital. That year, Rio Minerals Limited conducted grid surveys and soil sampling near the Silverton occurrence (MINFILE 093M 038).

A grab sample (N-9-3) from the Second vein assayed 602.8 grams per tonne silver, 7.08 per cent lead and 15.3 per cent zinc (Assessment Report 8706).

Bibliography
EMPR ASS RPT 5134, *8706, 10477, 10766, 28862, 31214, 31655, 33250
GSC MEM 110; 223
GSC OF 2322
EMPR PFD 681489

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