Glaciology and geological signature of the Last Glacial Maximum Antarctic ice sheet

Dynamical changes in contemporary ice sheets account for significant proportions of their current rates of mass loss, but assessing whether or not these processes are a natural part of ice-sheet evolution requires inference from palaeo-glaciological records. However, a robust mechanism for translati...

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Bibliographic Details

Published in:	Quaternary science reviews Vol. 78; pp. 225 - 247
Main Authors:	Golledge, Nicholas R., Levy, Richard H., McKay, Robert M., Fogwill, Christopher J., White, Duanne A., Graham, Alastair G.C., Smith, James A., Hillenbrand, Claus-Dieter, Licht, Kathy J., Denton, George H., Ackert, Robert P., Maas, Sanne M., Hall, Brenda L.
Format:	Journal Article
Language:	English
Published:	Elsevier Ltd 15.10.2013
Subjects:	Glacial geology Ice-sheet modelling Plio-Pleistocene Subglacial erosion PSE, Antarctica, Victoria Land, Arrival Heights, McMurdo Sound PS, Ross Sea Glacial geology Subglacial erosion Ice-sheet modelling Plio-Pleistocene
ISSN:	0277-3791, 1873-457X
Online Access:	Get full text
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