Diagenesis of the oolite group between Blaen Onneu and Pwll Du, Lower Carboniferous, South Wales
The diagenetic history of the Oolite Group from Pwll du to Blaen Onneu has been unravelled. Cement types, solution events, dolomitisation, concretions and other authigenic minerals are described. The calcite cement crystals show chemical zonation through staining but cathodoluminescence (CL) has pro...
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University of Nottingham
1983
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.347713 |