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...

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Bibliographic Details
Published in:Marine Geophysical Researches
Main Authors: Marks, Karen M., Stock, Joann M.
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer Verlag 1995
Subjects:
Online Access:https://doi.org/10.1007/BF01227040