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File Created: 27-Mar-1987 by Allan Wilcox (AFW)
Last Edit:  14-Jul-2021 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name FRANK 63, PIM, RIO 10-14, BIN 6-8, NB Mining Division Kamloops
BCGS Map 092I035
Status Showing NTS Map 092I06E
Latitude 050º 22' 26'' UTM 10 (NAD 83)
Longitude 121º 04' 34'' Northing 5581972
Easting 636802
Commodities Copper Deposit Types L04 : Porphyry Cu +/- Mo +/- Au
Tectonic Belt Intermontane Terrane Quesnel
Capsule Geology

The Frank 63 (Bin 7) occurrence is located at an elevation of approximately 1630 metres on a south-facing slope of Spaist Mountain.

The area is underlain by Bethsaida phase granodiorites of the Upper Triassic to Lower Jurassic Guichon Creek Batholith.

Minor disseminated chalcopyrite and malachite staining occur in a hornblendite dike cutting diorite, and in narrow fracture zones in granodiorite to the east.

In 1969, drilling on the Bin 7 claim intercepted pale-green, (chlorite-?) altered quartz diorite with near vertical feldspar-calcite-quartz veinlets and disseminated chalcopyrite ± bornite ± chalcocite yielded intercepts of 0.12 per cent copper over 15 metres in hole NL-1 and 0.61 per cent copper over 3 metres in hole NL-3 (Property File - 10866).

Work History

In 1956 and 1957, Udd-Ramsey Syndicate completed programs of geological mapping, soil sampling and a 60.4 line-kilometre ground magnetic survey on the area as the Frank and Nord claims. In 1958, Northwestern Explorations Ltd. completed a program of geological mapping, soil sampling and a 45.5 line-kilometre ground magnetic and induced polarization survey on the area as the BJ claims.

In 1965 and 1966, Rio Tinto Exploration Ltd. completed programs of soil sampling, geological mapping and a ground magnetic survey on the area as the Rio claims. Also in 1966, T.C. Explorations Ltd. completed a program of soil sampling and a 47.4 line-kilometre ground magnetic survey on the IL, Oversight, PIM and PM claims. In 1969, Noranda Mining and Exploration Inc. completed a program of soil sampling, five diamond drill holes and a 41.0 line-kilometre induced polarization survey on the area as the Bin claims.

In 1971, Highland Star Mines Ltd. completed a soil sampling program on the area as the NB claims.

During late 2008 through 2012, Happy Creek Minerals completed programs of geochemical (rock, silt and soil) sampling, geological mapping, three diamond drill holes, totalling 740.9 metres, an induced polarization survey and a 1463.0 line-kilometre airborne gamma ray spectrometer and magnetic survey on the area as the West Valley property.

During 2013 through 2019, Happy Creek Minerals Ltd. completed programs of geological mapping, geochemical (rock, silt and soil) sampling, a 32.3 line-kilometre induced polarization survey and re-interpretation of historical airborne geophysical data on the area as part of the Rateria-West Valley property.

Bibliography
EMPR MAP *30
EMPR PFD *10866 811559
GSC MAP 1010A; 1386A; 42-1989
GSC MEM 262
GSC OF 980
GSC P 46-8; 47-10
CIM Spec. Vol. 15 (1976), pp. 85-104
Northcote, K.E. (1968): Geology and Geochronology of the Guichon Creek Batholith, British Columbia, Unpublished Ph.D. Thesis, The
University of British Columbia

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