A sedimentologic-stratigraphic investigation of Marsdenian (Namurian R2A-B) sediments in the Central Pennines
The Marsdenian (R2a_b) sediments constitute the third major clastic influx into the Central Pennine Basin, following the first and second influxes during the Skipton Moor Grit (Elc) and Kinderscoutian (Ri) intervals respectively. The Marsdenian influx involves three distinct delta advances during th...
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Keele University
1982
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.240722 |