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...
Main Authors: | , , , , , , , , , , , , , , , , , , |
---|---|
Format: | Report |
Language: | unknown |
Published: |
Zenodo
2006
|
Subjects: | |
Online Access: | https://doi.org/10.13140/RG.2.2.16473.36961 |