Inversion tectonic in the Carboniferous basins of northern England : with special reference to Northumberland
The Northumberland basin is a member of the Carboniferous syn-orogenic complex that developed in the nonhern continental foreland of the Variscan orogeny. The basin occupies pan of the Iapetus province, forming a generalised half-graben between the Southern Uplands and the Alston block. It straddles...
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University of Leeds
1990
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.511982 |