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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Format: | Conference Object |
Language: | unknown |
Published: |
2005
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Online Access: | https://epic.awi.de/id/eprint/17110/ https://hdl.handle.net/10013/epic.26962 |