Crustal and Sedimentary Structures and Geodynamic Evolution of the West Antarctic Continental Margin and Pine Island Bay

Since the last glacial maximum the West Antarctic Ice Sheet (WAIS) with a base mostly beneath the present-day sea-level has experienced dramatic volume changes within short periods of time. Studies are urgently required to show how these short-term variations are related to volume changes in the old...

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Bibliographic Details
Main Authors: Gohl, K., Uenzelmann-Neben, G., Eagles, G., Fahl, A., Feigl, T., Grobys, J., Just, J., Leinweber, V., Lensch, N., Mayr, C., Parsiegla, N., Rackebrandt, N., Schloter, P., Suckro, S., Zimmermann, K., Gauger, S., Bohlmann, H., Netzeband, G. L., Lemenkova Polina
Format: Report
Language:unknown
Published: Zenodo 2006
Subjects:
Online Access:https://doi.org/10.13140/RG.2.2.16473.36961