Resumé
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).
Originalsprog | Engelsk |
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Sider (fra-til) | 299-300 |
Antal sider | 2 |
Tidsskrift | Antarctic Science |
Vol/bind | 21 |
Udgave nummer | 3 |
DOI | |
Status | Udgivet - jun. 2009 |
Programområde
- Programområde 5: Natur og klima