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...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2017
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Subjects: | |
Online Access: | https://www.repository.cam.ac.uk/handle/1810/262906 https://doi.org/10.17863/CAM.8195 |