Evolution of the Australian-Antarctic discordance since Miocene time

In this study we chronicle the development of the Australian-Antarctic discordance (AAD), the crenelated portion of the Southeast Indian Ridge between ∼120° and 128°E, since anomaly 6y time (19 Ma). We reconstruct satellite-derived marine gravity fields and depth anomalies at selected times by first...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Marks, Karen M., Stock, Joann M., Quinn, Katherine J.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 1999
Subjects:
Online Access:https://authors.library.caltech.edu/44959/
https://authors.library.caltech.edu/44959/1/jgrb11713.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20140415-124308456