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...

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Bibliographic Details
Main Authors: González-Casado, J.M., Giner Robles, Jorge Luis, López-Martínez, J.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of America 2000
Subjects:
Online Access:https://hdl.handle.net/20.500.14352/102996