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Tin and tungsten-bearing veins, breccias and skarns occur in a 60 km long belt trending west from Keno Hill to the Tintina Fault. The dataset likely contains geochemical and mineralogical data for occurrences hosted by mid-Cretaceous intrusions and older metasedimentary rocks. It was published by the Government of Yukon and last updated in April 2026.
License is OGL-CA-2.0. Data is provided in HTML and PDF formats, which may require extraction for analysis.