MINFILE Mineral Inventory

MINFILE Record Summary

MINFILE No 092INW027

File Created:	24-Jul-1985	by	BC Geological Survey (BCGS)
Last Edit:	25-Sep-1998	by	George Owsiacki (GO)

SUMMARY


Capsule Geology	The Raf 16 showing is located in the Late Triassic-Early Jurassic Guichon Creek batholith. Minor disseminated bornite occurs in a chlorite-sericite alteration zone in Chataway variety, Highland Valley phase granodiorite. About 450 metres to the east of the showing, a few malachite-bearing quartz veinlets cut granodiorite. See Mer, 092INW028 for a detailed work history of the area.

Bibliography

EMPR AR 1965-148; 1966-154; 1967-153,154; 1968-182,183

EMPR ASS RPT 2117, 2474, *2602, 4708, 4897

EMPR BULL 56; 62

EMPR FIELDWORK 1974, pp. 27-34; 1981, pp. 270,271

EMPR GEM 1969-264,265; 1970-348,351,352; 1971-342; 1973-206

EMPR MAP 7; 30

GSC MAP 1010A; 1386A; 42-1989

GSC MEM 262

GSC OF 165; 866; 980

GSC P 46-8; 47-10; 69-23; 73-1A, p. 212; 74-49; 82-1A, pp. 293-297; 85-1A, pp. 349-358

CJES Vol.15, No.1 (January 1978), pp. 99-116

Northcote, K.E. (1968): Geology and Geochronology of the Guichon Creek Batholith, British Columbia, Ph.D. Thesis, University of British Columbia