Forearc tectonics and volcanism during the Devonian–Carboniferous evolution of the North Patagonian segment, southern Chile (41,3°S)

Late Paleozoic to early Mesozoic subduction complexes formed during the evolution of southwestern Gondwana and extensively crop out along the Chilean continental margin. Recent findings in northern Patagonia (40°–43°S) revealed that accretionary processes were active since the Devonian when enhanced...

Full description

Bibliographic Details
Main Authors: C. Palape, P. Quezada, J. Bastías, F. Hervé, T. Reyes, M. Veas, F. Vildoso, M. Calderón, T. Theye, F. Fuentes, M. Chiaradia
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-09-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.873785/full