Submarine landforms and the reconstruction of fast-flowing ice streams within a large Quaternary ice sheet: The 2500-km-long Norwegian-Svalbard margin (57°

Submarine landforms and the reconstruction of fast-flowing ice streams within a large Quaternary ice sheet: The 2500-km-long Norwegian-Svalbard margin (57°–80°N)

Published:2005 Issue:7 Volume:117 Page:1033
ISSN:0016-7606
Container-title:Geological Society of America Bulletin
language:en
Short-container-title:Geol Soc America Bull

Author:

Ottesen D.,Dowdeswell J.A.,Rise L.

Publisher

Geological Society of America

Subject

Geology

Reference66 articles.

1. Late quaternary sedimentation and glacial history of the western Svalbard continental margin

2. Three-dimensional seismic data from the Barents Sea margin reveal evidence of past ice streams and their dynamics

3. Antarctic ice streams: A review

4. Surface velocity and mass balance of Ice Streams D and E, West Antarctica

5. Till beneath ice stream B: 1. Properties derived from seismic travel times

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