Influence of basin physiography on the evolution and sedimentation from flows transitional between turbidity current and debris flow
Hybrid event beds (HEBs) containing matrix (clay)-poor and overlying matrix-rich sandstone facies are increasingly recognised in deep-water systems and differ significantly from facies traditionally associated with sediment gravity flow deposition. HEBs are thought to reflect deposition from flows whose...
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University of Leeds
2015
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.665002 |