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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Vydané v:	Quaternary science reviews Ročník 78; s. 225 - 247
Hlavní autori:	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.
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Elsevier Ltd 15.10.2013
Predmet:	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
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