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...
Published in: | Journal of Sedimentary Research |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Society for Sedimentary Geology
1999
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/503526/ https://doi.org/10.2110/jsr.69.847 |