Ice-stream retreat and ice-shelf history in Marguerite Trough, Antarctic Peninsula: sedimentological and foraminiferal signatures

The timing, nature, and causes of grounded ice-sheet retreat following the Last Glacial Maximum (LGM) in Marguerite Trough, west Antarctic Peninsula, and subsequent early Holocene ice-shelf decay, are presented in this paper. We use sedimentological, foraminiferal, geotechnical, and accelerator mass...

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Bibliographic Details
Published in:Geological Society of America Bulletin
Main Authors: Kilfeather, A.A., Cofaigh, C.O., Lloyd, J.M., Dowdeswell, J.A., Xu, S., Moreton, S.G.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2011
Subjects:
Online Access:http://eprints.gla.ac.uk/70904/