Asymmetric Seafloor Spreading and Short Ridge Jumps in the Australian-Antarctic Discordance
The crenulated geometry of the Southeast Indian ridge within the Australian-Antarctic discordance is formed by numerous spreading ridge segments that are offset, alternately to the north and south, by transform faults. Suggested causes for these offsets, which largely developed since ~ 20 Ma, includ...
Published in: | Marine Geophysical Researches |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Springer Verlag
1995
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Subjects: | |
Online Access: | https://authors.library.caltech.edu/49345/ https://resolver.caltech.edu/CaltechAUTHORS:20140908-114127033 |