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New determinations of tin and tungsten in granites from south-west England
Published online by Cambridge University Press: 05 July 2018
Extract
Recent studies on the development of Sn-W mineralization in south-west England (Sheppard, 1977; Simpson et al., 1979; Jackson et al., 1979) indicate that the hydrothermal fluids dominantly consisted of local meteoric waters. These waters were heated up and drawn into the granite in a convective hydrothermal system. It is proposed that the fluids leached Sn and W from minerals such as the dark micas, during their passage through the granite. These metals were then deposited in veins at higher levels in the system.
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- Copyright © The Mineralogical Society of Great Britain and Ireland 1981
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