Publication Date:
2009-03-04
Description:
The evolution of the East Antarctic Ice Sheet (EAIS) during the Late Quaternary is poorly known, partly because some regions, such as the Prydz Bay vicinity, indicate significant variability in the glaciation patterns (e.g. Domack et al. 1998, Zwartz et al. 1998, Hodgson et al. 2005).
Print ISSN:
0954-1020
Electronic ISSN:
1365-2079
Topics:
Biology
,
Geography
,
Geosciences
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