Grounding-zone wedges on Antarctic continental shelves
Author:
Affiliation:
1. Department of Earth Sciences, Rice University, 6100 Main Street, Houston, Texas 77005, USA
2. Department of Geological Sciences, Stockholm University, Svante Arrhenius väg 8, 106 91 Stockholm, Sweden
Publisher
Geological Society of London
Subject
Geology
Reference13 articles.
1. Till beneath Ice Stream-B: 4. A coupled ice-till flow model;Journal of Geophysical Research,1987
2. Discovery of Till Deposition at the Grounding Line of Whillans Ice Stream
3. Bart P.J. & Anderson J.B. 1995. Seismic record of glacial events affecting the Pacific Margin of the northwestern Antarctic Peninsula. In: Cooper A.C. , Barker P.F. & Brancolini G. (eds) Geology and Seismic Stratigraphy of the Antarctic Margin, Antarctic Research Series. American Geophysical Union, Washington, DC, 75–96.
4. Early stall of West Antarctic Ice Sheet advance on the eastern Ross Sea middle shelf followed by retreat at 27,500 14C yr BP;Palaeogeography, Palaeoclimatology, Palaeoecology,2012
5. The seismic architecture and geometry of grounding-zone wedges formed at the marine margins of past ice sheets
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