Seismic analysis of the Niger Delta gravitational detachment system
Ductile deformation of overpressured, fine-grained, argillaceous sediments (“mobile shale”) is commonly invoked to explain the deformation style at the base of thin-skinned, gravitational detachment systems. The usage of “mobile shale” arose as a consequence of poor imaging on seismic reflection dat...
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Durham University
2011
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.540825 |