Cenozoic motion between East and West Antarctica

The West Antarctic rift system is the result of late Mesozoic and Cenozoic extension between East and West Antarctica, and represents one of the largest active continental rift systems on Earth. But the timing and magnitude of the plate motions leading to the development of this rift system remain p...

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Bibliographic Details
Published in:Nature
Main Authors: Cande, Steven C., Stock, Joann M., Müller, R. Dietmar, Ishihara, Takemi
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 2000
Subjects:
Online Access:https://authors.library.caltech.edu/44941/
https://resolver.caltech.edu/CaltechAUTHORS:20140415-074414969