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...

Full description

Bibliographic Details
Main Authors: Rui, L., Urgeles, Roger, Accettella, Daniela
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Arctic
Barents Sea
Online Access:http://hdl.handle.net/10261/171441
Description
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

Similar Items