Clastic diagenesis and porefluid evolution : an isotopic study, Magnus oilfield, North Sea
The Upper Jurassic Magnus Sandstone is a medium-grained feldspathic submarine fan sandstone, which was derived from the northwest and deposited in the East Shetland Basin as four stacked lobes. These formed a reservoir up to 200m thick within the Kimmeridge Clay oil source rocks. The oilfield was fo...
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University of Strathclyde
1990
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303271 |