Provenance changes between recent and glacial-time sediments in the Amundsen Sea embayment, West Antarctica: clay mineral assemblage evidence
about
Major advance of South Georgia glaciers during the Antarctic Cold Reversal following extensive sub-Antarctic glaciation.Evidence for a palaeo-subglacial lake on the Antarctic continental shelf.Sub-ice-shelf sediments record history of twentieth-century retreat of Pine Island Glacier.Influence of subglacial conditions on ice stream dynamics: Seismic and potential field data from Pine Island Glacier, West Antarctica
P2860
Provenance changes between recent and glacial-time sediments in the Amundsen Sea embayment, West Antarctica: clay mineral assemblage evidence
description
article
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wetenschappelijk artikel
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наукова стаття, опублікована в травні 2011
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name
Provenance changes between rec ...... ay mineral assemblage evidence
@en
Provenance changes between rec ...... ay mineral assemblage evidence
@nl
type
label
Provenance changes between rec ...... ay mineral assemblage evidence
@en
Provenance changes between rec ...... ay mineral assemblage evidence
@nl
prefLabel
Provenance changes between rec ...... ay mineral assemblage evidence
@en
Provenance changes between rec ...... ay mineral assemblage evidence
@nl
P2093
P2860
P1433
P1476
Provenance changes between rec ...... ay mineral assemblage evidence
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P2093
Alastair G.C. Graham
Claus-Dieter Hillenbrand
Gerhard Kuhn
James A. Smith
Robert D. Larter
Werner Ehrmann
P2860
P304
P356
10.1017/S0954102011000320
P577
2011-05-18T00:00:00Z