Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea
Rui, L. . et al.-- Final Conference ARCA PROJECT : ARctic: present Climatic change and pAst extreme events, 11 October, 2016, Rome.-- 3 pages, 3 figures The development of high latitude continental margin has been mainly controlled by glacigenic processes during the glacial maxima. Superimposed to t...
Main Authors: | , , |
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Format: | Conference Object |
Language: | unknown |
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2016
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Online Access: | http://hdl.handle.net/10261/171441 |
Summary: | Rui, L. . et al.-- Final Conference ARCA PROJECT : ARctic: present Climatic change and pAst extreme events, 11 October, 2016, Rome.-- 3 pages, 3 figures The development of high latitude continental margin has been mainly controlled by glacigenic processes during the glacial maxima. Superimposed to these, there are both downslope and alongslope sedimentary processes (turbidites and contourites). [.] Peer Reviewed |
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