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File Created: 05-May-2023 by Karl A. Flower (KAF)
Last Edit:  06-Jun-2023 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name LUCKY, DEE, JOAB Mining Division Liard
BCGS Map 104P022
Status Prospect NTS Map 104P05W
Latitude 059º 17' 30'' UTM 09 (NAD 83)
Longitude 129º 46' 03'' Northing 6572782
Easting 456279
Commodities Gold, Silver, Copper Deposit Types I01 : Au-quartz veins
I06 : Cu+/-Ag quartz veins
Tectonic Belt Omineca Terrane Slide Mountain, Cassiar
Capsule Geology

The Lucky occurrence is located at an elevation of approximately 1690 metres on an east-west–trending ridge, north of Troutline Creek and approximately 5 kilometres east of the historical community of Cassiar.

The area is underlain by the Upper Paleozoic Sylvester Allochthon located on the northeastern margin of the Lower Cretaceous Cassiar Batholith. The Sylvester Allochthon is a fault bound imbricate assemblage of Mississippian to Upper Triassic Slide Mountain Complex regionally metamorphosed (greenschist) oceanic rocks thrust over the sediments of autochthonous North America. The assemblage contains basaltic to andesitic flows, pyroclastics, argillites, limestones, greywacke, chert, listwanite and quartz veins.

Locally, a quartz vein with tetrahedrite, sphalerite and trace chalcopyrite and pyrite mineralization is hosted at the contact between black, carbonaceous limestone in the hangingwall and black argillite. The vein averages between 1.0 and 1.5 metres in width and strikes approximately 160 degrees with a dip of 50 degrees northeast. The vein has been exposed for 15 metres along strike. The quartz-carbonate alteration of a parent ultramafic has produced listwanite which is associated with increased mineralization in the quartz veins. A trench located 20 metres north has exposed the possible northwest extension of the vein but is barren of sulphides at this location.

In 1984, a chip sample over a highly mineralized zone of the vein assayed 5.97 grams per tonne gold and 1662.6 grams per tonne silver (Assessment Report 14375). The following year, two chip samples (8053 and 8054) yielded 3.0 and 1.3 grams per tonne gold with 103.1 and 82.5 grams per tonne silver, respectively, whereas a grab sample (6178) taken from another quartz vein, located approximately 150 metres to the northeast, assayed 68.1 grams per tonne silver (Assessment Report 14375).

In 1986, diamond drilling yielded intercepts of up to 0.22 gram per tonne gold and 3.8 grams per tonne silver over 7.7 metres, including 0.94 gram per tonne gold over 1.0 metre in hole E86-1 (Assessment Report 15396).

In 2018, two samples (Z1012 and Z1042) from the Lucky vein yielded 0.55 and 0.32 gram per tonne gold, 2690 and 973 grams per tonne silver with 1.25 and 1.09 per cent copper, respectively, whereas an outcrop sample (CH007) of iron-carbonate–altered basalt with quartz veins and disseminated pyrite, located downslope to the south of the Lucky vein at an elevation of approximately 1620 metres, assayed 1.06 grams per tonne gold (Assessment Report 38310).

Work History

The area has been explored in conjunction with the nearby Elan (MINFILE 104P 075) and Boomerang (MINFILE 104P 112) occurrences and a complete exploration history can be found there.

Bibliography
EMPR BULL 83
EMPR EXPL 1980-517; 1982-410; 1983-560; 1986-C467
EMPR FIELDWORK 1980, pp. 55-62; *1981, pp. 156-161; 1987, pp. 245-248; 1988, pp. 323-337
EMPR MP MAP 1992-13
EMPR OF 1989-9; 1996-11
GSC MAP 381A; 1110A
GSC MEM 194; 319, p. 138
GSC OF 2779
Dussell, E. (1986): Listwanites and Their Relationship to Gold Mineralization at Erickson Mine, British Columbia, Canada, M.Sc. Thesis, Western Washington University
Harms, T.A. (1986): Structural and Tectonic Analysis of the Sylvester Allochthon, Northern British Columbia, Implications for Paleogeography and Accretion, Ph.D. Thesis, University of Arizona

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