Kerogen variation in a Devonian half graben system
The Middle Devonian Rousay Flagstone Formation of Orkney is a 200m thick lacustrine succession that contains abundant preserved organic matter. It was deposited into a series of half graben formed by the collapse of over-thickened Caledonian crust. The 14 lake cycles that comprise the Rousay Flagsto...
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University of Southampton
1999
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.285663 |