Bransfield Basin, Antarctic Peninsula: Not a normal backarc basin
The Bransfield Basin, a marginal basin located northwest of the Antarctic Peninsula, has been habitually considered as a backarc basin associated with the rollback process that took place along an inactive plate boundary, the South Shetland Trench, where the Antarctic and the Phoenix plates meet. Ne...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Society of America
2000
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Subjects: | |
Online Access: | https://hdl.handle.net/20.500.14352/102996 |