Tectonic evolution of the Southwest Indian Ocean since the Mid-Cretaceous: plate motions and stability of the pole of Antarctica/Africa for at least 80 Myr
The Southwest Indian Ridge is the boundary where seafloor is being created between the African and Antarctic plates. East of the newly-recognized Du Toit Fracture Zone at 27°E it trends north-easterly and is cut by a series of six deep near north-south clefts marking transform faults. This series st...
Published in: | Geophysical Journal International |
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Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
1983
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Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/73/2/553 https://doi.org/10.1111/j.1365-246X.1983.tb03330.x |