Following the steps of CHIPA: Chilenia and Patagonia formed the same drift terrain that collided with the southwest Gondwana margin during the middle Paleozoic

Geological evidence indicates that the deformation along the southwest Gondwana margin began during the Middle-to-Late Devonian (the Acadian-Cháñica orogenic phase in Argentina). It has been interpreted that this deformation occurred as a consequence of the collision of Chilenia from the west and Pa...

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Bibliographic Details
Main Authors: Renata Nela Tomezzoli, Ernesto O. Cristallini, Hugo Tickyj, Guadalupe Arzadún, Juan Martín Calvagno, Giselle Choque, Belen Febbo, Eliana Saguas
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-11-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2023.1225271/full