Tectonic segmentation across Patagonia controlled by the subduction of oceanic fracture zones
A set of fracture zones left by transform faults segmenting the active Chile Ridge that separates the Nazca and Antarctica Plates has been subducting beneath western Patagonia in the last 18 Myr. The subduction direction of these fractures zones has remained almost unaltered during this time lapse s...
Published in: | Journal of Geodynamics |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Pergamon-Elsevier Science Ltd
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Subjects: | |
Online Access: | http://hdl.handle.net/11336/147021 |