Depositional environments and diagenesis of the Cenozoic sediments of the Almazan Basin, North-East Spain
The Almazan Basin is an half-graban, which formed between the Sierra de la Demanda and the Celtiberian Range. It is 30km-55km wide, 115km long and contains up to c.3.5km of Tertiary alluvial and lacustrine sediments. The spatial and temporal distribution of these deposits during the basin evolution...
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University of Cambridge
1989
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.596756 |