Bedrock platforms within the Ross Embayment, West Antarctica: Hypotheses for ice sheet history, wave erosion, Cenozoic extension, and thermal subsidence

[1] Ice-penetrating radar (mostly airborne) and marine seismic surveys have revealed plateaus and terraces about 100–350 m below sea level beneath parts of the Ross Embayment, including the West Antarctic ice sheet, the Ross Ice Shelf, and the eastern Ross Sea. These surfaces cover many thousands of...

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Bibliographic Details
Main Authors: Douglas S. Wilson, Bruce P. Luyendyk
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.506.4730
http://www.geol.ucsb.edu/faculty/luyendyk/Luyendyk_pdf/Wilson%26Luyendyk2006Gcubed.pdf