Low-temperature hydrothermal mineralisation in the St. Austell Pluton, Cornwall, England
The St. Austell pluton is part of the large Hercynian batholith of south-west England. The pluton exhibits a complex sequence of mineralisation events, which occur as distinct hydrothermal vein generations associated with characteristic alterations of the host granites. Geological and petrographic o...
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University of Manchester
1996
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.602490 |