On Ash Mountain in the Cassiar Mountains of northern British Columbia, discontinuous skarn lenses occur in limestones within folded, faulted and metamorphosed argillites and quartzites of the Carboniferous Oblique Creek Formation, intruded by granites of the Late Cretaceous Parallel Creek Batholith. Disseminated scheelite occurs in various skarns, with grab sample assays running to 0.15 per cent WO3 (Assessment Report 8196).
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Map Reference: 59°19'N , 130°31'W
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Mineral List:4 entries listed. 4 valid minerals.
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