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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Bibliographic Details
Published in:Antarctic Science
Main Author: Gore, Damian B.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1997
Subjects:
Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Antarctic
East Antarctica
Amery
Larsemann Hills
Stillwell Hills
Taylor Islands
Antarc*
Antarctic Science
Antarctica
Ice Sheet
Online Access:http://dx.doi.org/10.1017/s0954102097000412
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102097000412

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