British Columbia Ministry of Energy, Mines and Natural Gas and Responsible for Housing
News | The Premier Online | Ministries & Organizations | Job Opportunities | Main Index

MINFILE Home page  ARIS Home page  MINFILE Search page  Property File Search
Help Help
File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  12-Feb-2020 by George Owsiacki (GO)

Summary Help Help

NMI 104O9 W1
Name BLUE LIGHT, BLULITE Mining Division Liard
BCGS Map 104O068
Status Prospect NTS Map 104O09W
Latitude 059º 38' 59'' UTM 09 (NAD 83)
Longitude 130º 28' 06'' Northing 6613318
Easting 417240
Commodities Tungsten, Tin Deposit Types K05 : W skarn
K06 : Sn skarn
Tectonic Belt Omineca Terrane Dorsey, Cassiar
Capsule Geology

The Blue Light occurrence is located 12 kilometres east of Jennings Lakes in northwest British Columbia, about 137 kilometres north of the community of Dease Lake.

The main showing occurs in the Upper Paleozoic Dorsey Complex in an embayment on the west side of the Early Cretaceous Cassiar batholith. Scheelite occurs as disseminations and coarse aggregates in quartz-amphibole and diopside-garnet skarn lenses up to 1.5 metres thick within a 15-metre-wide sheeted zone of augen gneiss and pelitic hornfels. Late pegmatite dikes crosscut the metasediments and intrusive phases. The mineralization is associated with an Eocene granitic intrusion (Nelson et al., Fieldwork 1987). The dikes contain fluorite, fluorapatite and minor beryl. The zone of discontinuous tungsten mineralization is exposed for a length of 30 metres. South of this, magnetite-quartz-pyrite lenses up to 3 metres thick occur in a quartzitic hornfels, roughly parallel to bedding. These contain up to 0.89 per cent tin (Fieldwork 1987).

Initially the property was explored for magnetite-chalcopyrite mineralization which had been discovered by Mr. Andy Zborovazky prior to 1962. In the fall of 1962, under an agreement between Mr. Zborovazky and E.P. Chapman, Jr., a re-examination of the claims resulted in the discovery of scheelite mineralization. This initiated an exploration program consisting of trenching, channel and bulk sampling, geological mapping, and diamond drilling under the direction of Chapman, Wood and Griswold Ltd. Encouraging results were obtained in this work.

Mr. G.C. Singhai, in a report on the property in 1977, describes the location of six drillholes which explored the creek showing. Two BQ size diamond-drill holes were undertaken by Pacific Cypress Minerals Ltd. in 1979 as a further exploration of this zone. The holes were located near the south end of the main showing but generally only trace values in tungsten were obtained except for a narrow section in drillhole 79-2. A 1.53 metre width in drillhole 79-2 (from 5.91-7.44 metres) assayed 0.26 per cent WO3 (Assessment Report 7937).

Bibliography
EMPR PF (*Smith, C.L. (1969): Bulldozer trenching report on Blue Light Claims, Spartan Explorations Ltd. Report)
EMPR AR 1968-33
EMPR EXPL 1980-506
EMPR ASS RPT *7937
EMPR FIELDWORK 1987, pp. 525-527
EMPR OF 1991-17; 1992-16; 1996-11; 2000-4
EMPR BULL 83
GSC P 66-2, pp. 48,49; *68-55, p. 35; *68-70, p. 9
GSC EC GEOL *28, pp. 80,81
GSC MAP *18-1968
GSC OF 561; 2779
EMR MP RESFILE (MR-W-301.000)
EMR MP CORPFILE (Spartan Explorations Ltd.)
EMPR PFD 881134

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY