Deciphering climatic controls on sedimentation in a tectonically active area, Cyprus
The late Neogene to Quaternary of Cyprus is considered to be a tectonically active period coeval with major climatic change. Uplift, associated with the activities of the supra-subduction zone to south of island was concomitant with global cooling, the expansion of the Northern Hemisphere Ice Sheets...
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Durham University
2010
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Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.530184 |