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...

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