hdl:10013/epic.27421
publisher:10.3133/of2007-1047.srp084
Differences in ice retreat across Pine Island Bay, West Antarctica, since the Last Glacial Maximum: Indications from multichannel seismic reflection data
Uenzelmann-Neben, Gabriele ORCID: https://orcid.org/0000-0002-0115-5923, Gohl, Karsten ORCID: https://orcid.org/0000-0002-9558-2116, Larter, R. and Schlüter, Philip
;
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Gabriele.Uenzelmann-Neben [ at ] awi.de
Abstract
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Article
Authors
Uenzelmann-Neben, Gabriele ORCID: https://orcid.org/0000-0002-0115-5923, Gohl, Karsten ORCID: https://orcid.org/0000-0002-9558-2116, Larter, R. and Schlüter, Philip
;
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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) > POL-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
Helmholtz Research Programs > MARCOPOLI (2004-2008) > MAR2-Palaeo Climate Mechanisms and Variability
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
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Published
Eprint ID
16538
DOI
10.3133/of2007-1047.srp084
Cite as
Uenzelmann-Neben, G.
,
Gohl, K.
,
Larter, R.
and
Schlüter, P.
(2007):
Differences in ice retreat across Pine Island Bay, West Antarctica, since the Last Glacial Maximum: Indications from multichannel seismic reflection data
,
U. S. Geological Survey Open-File Report, 2007, srp084 {http://pubs.usgs.gov/of/2007/1047/srp/srp084/} {doi:10.3133/of,
2007-1047}
.
doi: 10.3133/of2007-1047.srp084
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