Late Cenozoic prograding wedges on the NW European continental margin : their formation and relationship to tectonics and climate
During late Pliocene to Pleistocene times, prominent prograding wedges were deposited along the continental margin of NW Europe, resulting in seaward shelf break migration of up to 150 km. Much of the sediment accumulation occurred marginal to the former mid- to high-latitude ice sheets. The geograp...
Published in: | Marine and Petroleum Geology |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
2005
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/18313/ http://www.sciencedirect.com/science/journal/02648172 |