Evolution of the Murzuq Basin, southwest Libya, and surrounding region during the Devonian
During the Devonian the area currently delimited by the Murzuq Basin in SW Libya, was part of a slowly subsiding, extensive, low angle, platform cratonic margin, situated on northern Gondwana. Phases of tectonism occurred during the Gedinnian, Emsian, Frasnian and Fammenian which caused the localise...
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Aberystwyth University
1999
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.425850 |