Bathymetry and geological structures beneath the Ross Ice Shelf at the mouth of Whillans Ice Stream, West Antarctica, modeled from ground-based gravity measurements-Reference-Cited by-同舟云学术

Bathymetry and geological structures beneath the Ross Ice Shelf at the mouth of Whillans Ice Stream, West Antarctica, modeled from ground-based gravity measurements

Published:2013-08 Issue:8 Volume:118 Page:4535-4546
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Muto Atsuhiro¹,Christianson Knut²,Horgan Huw J.³,Anandakrishnan Sridhar¹,Alley Richard B.¹

Affiliation:

1. Department of Geosciences and Earth and Environmental Systems Institute; Pennsylvania State University; Pennsylvania USA

2. Department of Physics; St. Olaf College; Northfield Minnesota USA

3. Antarctic Research Centre; Victoria University of Wellington; Wellington New Zealand

Funder

NSF

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference83 articles.

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2. Till beneath ice stream B: 3. Till deformation: Evidence and implications;Alley;J. Geophys. Res.,1987

3. Sedimentation beneath ice shelves - the view from Ice Stream B;Alley;Mar. Geol.,1989

4. Effect of Sedimentation on Ice-Sheet Grounding-Line Stability;Alley;Science,2007

5. Influence of subglacial geology on the position of a West Antarctic ice stream from seismic observations;Anandakrishnan;Nature,1998

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