The climatic, eustatic and tectonic controls on the Mid Carboniferous (Visean and Namurian) strata of Northumbria, England
The Mid Caiboniferous (Viséan and Namurian) Yoredale cycles of Northumbria were deposited as a result of glacio-eustatic fluctuations, arising from waxing aid waning of Gondwanan ice sheets in the southern hemisphere. Each cycle contains a variety of Uthofacies, generally comprising carbonate platfo...
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Durham University
2006
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.550096 |