Carbonate facies on a Lower Carboniferous storm influenced ramp in SW Britain
The Lower Carboniferous ('mid'-Courceyan to early Chadian) Black Rock Limestone ramp succession of SW Britain, accumulated along the southern margin of the Welsh-Brabant Massif during the early stage of development of the SW European foreland basin. Two depositional cycles are recognized w...
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University of Bristol
1989
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.232918 |