hdl:10013/epic.31171
publisher:10.1016/j.margeo.2008.07.004
The present and past bottom-current flow regime around the sediment drifts on the continental rise west of the Antarctic Peninsula
Hillenbrand, C.-D., Camerlenghi, A., Cowan, E. A., Hernández-Molina, F. J., Lucchi, R. G., Rebesco, M. and Uenzelmann-Neben, Gabriele ORCID: https://orcid.org/0000-0002-0115-5923
;
Contact
Gabriele.Uenzelmann-Neben [ at ] awi.de
Abstract
Item Type
Article
Authors
Hillenbrand, C.-D., Camerlenghi, A., Cowan, E. A., Hernández-Molina, F. J., Lucchi, R. G., Rebesco, M. and Uenzelmann-Neben, Gabriele ORCID: https://orcid.org/0000-0002-0115-5923
;
Divisions
Programs
Helmholtz Research Programs > MARCOPOLI (2004-2008) > MAR-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > MAR2-Palaeo Climate Mechanisms and Variability
Helmholtz Research Programs > MARCOPOLI (2004-2008) > MAR2-Palaeo Climate Mechanisms and Variability
Publication Status
Published
Eprint ID
19082
DOI
10.1016/j.margeo.2008.07.004
Cite as
Hillenbrand, C. D.
,
Camerlenghi, A.
,
Cowan, E. A.
,
Hernández-Molina, F. J.
,
Lucchi, R. G.
,
Rebesco, M.
and
Uenzelmann-Neben, G.
(2008):
The present and past bottom-current flow regime around the sediment drifts on the continental rise west of the Antarctic Peninsula
,
Marine Geology,
255
(1),
pp. 55-63
.
doi: 10.1016/j.margeo.2008.07.004
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