Aspects of the structural control of fluorite mineralisation in the South Pennine orefield with notes on the mining potential
The structural geology of the South Pennine Orefield is shown to be composed of an interference pattern of folds related in part to basement features. Folds are shown to have developed with varying trends during and after the deposition of the Carboniferous limestone. It is concluded that some of th...
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University of Leicester
1976
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.674106 |