Internal structure of a contourite drift generated by the Antarctic Circumpolar Current

We describe the internal structure and stratigraphy of a well-imaged contourite drift from the Southern Ocean. This drift, which we have named the South Falkland Slope Drift, lies on the northern flank of the Falkland Trough due south of the Falkland Islands. Drifts which occur directly in the path...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Koenitz, D., White, N. J., McCave, I. N., Hobbs, R. W.
Format: Article in Journal/Newspaper
Language:English
Published: AGU and the Geochemical Society 2008
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/457/
http://eprints.esc.cam.ac.uk/457/1/McCave_3G_9_6_2008.pdf
https://doi.org/10.1029/2007GC001799