Abstract
The JC deposit is a stanniferous skarn related to a ridge-like lobe of the mid-Cretaceous Seagull Batholith. Skarn replaces Mississippian carbonate sediments of the Yukon Cataclastic Complex along an elongate contact zone with a known strike length of 850 m. Tin mineralization was discovered at JC in 1977 and subsequent drilling has outlined estimated geologically inferred reserves of 1,250,000 t grading 0.54% Sn with a cut-off grade of 0.30%.
Cite
CITATION STYLE
Layne, G. D., & Spooner, E. T. C. (1988). The Geology and Mineralogy of the JC Tin Skarn, Yukon Territory, Canada. In Geology of Tin Deposits in Asia and the Pacific (pp. 163–184). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-72765-8_9
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