Blanketing snow and ice; constraints on radiocarbon dating deglaciation in East Antarctic oases
Radiocarbon dating of marine, lacustrine or terrestrial biogenic deposits is the main technique used to determine when deglaciation of the oases of East Antarctica occurred. However, at many of the oases of East Antarctica, including the Schirmacher Oasis, Stillwell Hills, Amery Oasis, Larsemann Hil...
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Format: | Article in Journal/Newspaper |
Language: | English |
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1997
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Online Access: | https://researchers.mq.edu.au/en/publications/4ce56ab8-2f2e-473f-92a1-944f6dd38df1 http://www.scopus.com/inward/record.url?scp=0030793788&partnerID=8YFLogxK |