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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Veröffentlicht in:	Quaternary science reviews Jg. 78; S. 225 - 247
Hauptverfasser:	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
Sprache:	Englisch
Veröffentlicht:	Elsevier Ltd 15.10.2013
Schlagworte:	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-Zugang:	Volltext
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