Tectonics and glacial-marine sedimentation in Pine Island Bay: Survey plan of an upcoming RV Polarstern cruise

Pine Island Bay forms the third-largest outflow area for the West Antarctic ice-shield. The main ice streams from the WAIS into Pine Island Bay flow through the Pine Island and Thwaites Glacier systems, through which most of the glacial-marine sediments onto the shelf of Pine Island Bay and across t...

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Bibliographic Details
Main Author: Gohl, Karsten
Format: Conference Object
Language:unknown
Published: 2005
Subjects:
Online Access:https://epic.awi.de/id/eprint/17110/
https://hdl.handle.net/10013/epic.26962