The fate of the Farallon slab beneath Patagonia and its links to Cenozoic intraplate magmatism, marine transgressions and topographic uplift

The arrival and subsequent stagnation of the Farallon/Nazca slab at the mantle transition zone below southern South America triggered seemingly unrelated large-scale geological processes in the second half of the Cenozoic. During this period, three poorly understood regional events have characterize...

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Bibliographic Details
Published in:Earth-Science Reviews
Main Authors: Navarrete Granzotto, César Rodrigo, Gianni, Guido Martin, Massaferro, Gabriela Isabel, Butler, Kristina
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science
Subjects:
Online Access:http://hdl.handle.net/11336/120027