Over the past two years Imperial has conducted a program of geological mapping, geochemical surveys, whole rock trace element studies and airborne and surface geophysical surveys over the
Hole CW-23-01B was drilled at 225° azimuth and a dip of -50° to a final depth of 408 metres. Veined and altered andesite volcanic and intrusive rocks associated with the Whiting Creek Stock were the primary lithologies encountered. Numerous mafic to intermediate post mineral dykes crosscut all lithologies in a northwest to southeast trend following a prominent structural trend on the property.
Copper, molybdenum, and silver mineralization occurs throughout hole CW-23-01B within every lithology except the post mineral dykes. Higher grade copper mineralization is concentrated in the veined and altered andesite volcanics. The hole intersected 316.8 metres grading 0.23% copper, 0.008% molybdenum and 0.89 g/t silver from 67.4 metres, including 52.6 metres grading 0.45% copper 0.006% molybdenum and 1.29 g/t silver starting from the top of bedrock at a depth of 67.4 metres to 120 metres and 37.5 metres of 0.32% copper, 0.005% molybdenum and 1.72 g/t silver from 320.0 metres to 357.5 metres. The highest-grade section, from 67.4 metres to 120 metres, was extremely fractured and contained chalcocite coatings on pyrite-chalcopyrite bearing veins along fracture planes, which may reflect a zone of supergene enrichment.
While historic drill holes in the
Mineralized intervals in hole CW-23-01B include:
Hole | From | To | Width | Cu% | Mo% | Ag g/t | CuEq% | |||||||
CW-23-01B | 67.4 | 384.2 | 316.8 | 0.23 | 0.008 | 0.89 | 0.29 | |||||||
including | 67.4 | 120.0 | 52.6 | 0.45 | 0.006 | 1.29 | 0.50 | |||||||
including | 320.0 | 357.5 | 37.5 | 0.32 | 0.005 | 1.72 | 0.37 | |||||||
CuEq% =Cu% +(6.84*Mo%)+(0.01*Ag g/t) based on insitu rock value, recoveries not included (Cu at
Cross section and plan view maps are available on https://imperialmetals.com/our-operations/huckleberry-mine/maps.
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