Aspects of the palaeoecology of the Craven Reef Belt (Dinantian) of North Yorkshire
The Dinantian (largely Asbian) Craven Reef Belt of North Yorkshire was a marginal facies to the shelf limestones of the stable Askrigg Block, and bridged the transition to the deeper water facies of the more rapidly subsiding Craven Basin. The reef belt is thought to have consisted of an unbroken ma...
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University of Manchester
1980
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Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.582167 |