Quaternary evolution of the northern North Sea margin through glacigenic debris-flow and contourite deposition

The Norwegian Channel Ice Stream of the Scandinavian Ice Sheet extended across the northern North Sea margin during the mid- to late Quaternary, eroding older sediment from the continental shelf. Consequently, little is known about early Quaternary sedimentation on this margin. We use two- and three...

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Bibliographic Details
Main Authors: Batchelor, C, Ottesen, D, Dowdeswell, JA
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:https://www.repository.cam.ac.uk/handle/1810/262906
https://doi.org/10.17863/CAM.8195