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...
Published in: | Journal of Geophysical Research: Solid Earth |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
1999
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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 |