Megaturbidites and the late Quaternary regional sedimentology of the eastern and central Mediterranean Sea
The late Quaternary sedimentology of the Mediterranean is controlled primarily by fluctuations in global climate and sea level, and by an overriding compressive regime between the Eurasian and African plates. Local variations in this convergence have led to marked differences in the two regions stud...
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University of Southampton
2000
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.481697 |