The petrography of the mineralised dykes of W. Scotland
The epigenetic lead-zinc-barium-strontium mineralisation of the Loch Sunart area of Argyllshire has taken place along channels provided by dykes and faults. Dolerite and lamprophyre dykes of Permo-Carboniferous age constitute the most important structural controls. These were intruded along lines of...
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Durham University
1958
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.585639 |