Morphology and architecture of confined-to-unconfined flow transitions in modern and ancient deep-marine systems
Confined-to-unconfined flow transitions in deep-marine systems occur in areas where either a submarine channel passes into a depositional sheet/lobe or a submarine canyon passes into a submarine channel or basin plain. Transition zones are areas of complex interplay between erosive and depositional...
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University of Leicester
1995
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.737545 |