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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Bibliographic Details
Main Author: Mundy, D. J. C.
Published: University of Manchester 1980
Subjects:
560
Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.582167