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Strain Localization Along the Atlantis Bank Oceanic Detachment Fault System, Southwest Indian Ridge
Author(s):Miranda, E. A.; John, Barbara; Miranda, E. A.; John, Barbara
Microstructural observations and mineral thermometry from in situ samples collected from the Atlantis Bank oceanic core complex (SW Indian Ridge) indicate that detachment faulting was initiated under hypersolidus conditions ...
Evolution of the Southwest Indian Ridge from 55°45'E to 62°E: Changes in Plate-Boundary Geometry Since 26 Ma
Author(s):Baines, A. G.; Cheadle, Michael; Dick, H. J. B.; Scheirer, A. H.; John, Barbara; Kusznir, N. J.; Matsumoto, T.; Baines, A. G.; Cheadle, Michael; Dick, H. J. B.; Scheirer, A. H.; John, Barbara; Kusznir, N. J.; Matsumoto, T.
From 55°45'E to 58°45'E and from 60°30'E to 62°00'E, the ultraslow-spreading Southwest Indian Ridge (SWIR) consists of magmatic spreading segments separated by oblique amagmatic spreading segments, transform faults, and ...