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 |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Springer Verlag
1995
|
Subjects: | |
Online Access: | https://doi.org/10.1007/BF01227040 |