Structure and breakup history of the rifted margin of West Antarctica in relation to Cretaceous separation from Zealandia and Bellingshausen plate motion
Geophysical data acquired using R/V Polarstern constrain the structure and age of the rifted oceanic margin of West Antarctica. West of the Antipodes Fault, the 145 km wide continent-ocean transition zone (COTZ) of the Marie Byrd Land sector resembles a typical Atlantic-type margin. New gravity and...
Published in: | Geochemistry, Geophysics, Geosystems |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Wiley
2012
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/25402/ https://epic.awi.de/id/eprint/25402/1/Wobbe-etal_breakup-rifting-West-Antarctic-margin_G3_2012.pdf https://hdl.handle.net/10013/epic.39211 https://hdl.handle.net/10013/epic.39211.d001 |