A fluid inclusion and geochemical investigation of the fluorite deposits of the Southern Pennine Orefield
The fluorite deposits of the Southern Pennine Orefield occur in vein fillings and metasomatic replacements. Primary and secondary fluid inclusions define five discrete phases of fluorite mineralization or remobilization. Homogenization temperature ranges for the five events are; (1) 100-171°C; (2) 6...
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University of Leicester
1983
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.347846 |