Antarctic circumpolar deep water:A Quaternary paleoflow record from the northern Scotia Sea, South Atlantic ocean
In the northern Scotia Sea, the main pathway of Circumpolar Deep Water (CPDW) flows north to pass through a deep gap in the North Scotia Ridge before turning east into the Falkland Trough. A sediment drift has developed on the seabed since the Early-Middle Miocene, coincident with the opening of Dra...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1999
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Subjects: | |
Online Access: | https://pure.uhi.ac.uk/en/publications/4bb90f7c-a8be-461e-a489-d3da563bbc99 |