Onshore-offshore relationships and basin evolution along the west Greenland and conjugate Baffin-Labrador margins
The passive margins of west Greenland and Baffin/Labrador (sedimentary basins and onshore topography therein) developed mainly as a result of Late Mesozoic and Cenozoic rifting processes in the Davis Strait area. The origin and age of topography along the west Greenland margin is a matter of continu...
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University of Aberdeen
2013
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.600091 |