The organic geochemistry and thermal maturity of the Pennine Carboniferous Basin, England
The Pennine Basin has undergone a complex geological history with major episodes of rifting, thermal subsidence and inversion, the pattern of which was largely controlled by the structure of the Caledonian basement. The resulting block and basin topography and differential subsidence led to major va...
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University of Aberdeen
1992
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.334734 |