Late Eocene volcanism in North Patagonia (42°30′–43°S): Arc resumption after a stage of within-plate magmatism
Mid-Cenozoic widespread arc magmatism in North Patagonia extends from the forearc to the retroarc zones, representing an anomalous large volume when compared to the present-day arc zone and even other past arc configurations. It represents a crucial stage in Andean arc evolution as was developed aft...
Autores principales: | Fernández Paz, L., Litvak, V.D., Echaurren, A., Iannelli, S.B., Encinas, A., Folguera, A., Valencia, V. |
---|---|
Formato: | JOUR |
Materias: | |
Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_02643707_v113_n_p13_FernandezPaz |
Aporte de: |
Ejemplares similares
-
Late Eocene volcanism in North Patagonia (42°30′–43°S): Arc resumption after a stage of within-plate magmatism
Publicado: (2018) -
Evolution of Eocene to Oligocene arc-related volcanism in the North Patagonian Andes (39–41°S), prior to the break-up of the Farallon plate
por: Iannelli, S.B., et al. -
Evolution of Eocene to Oligocene arc-related volcanism in the North Patagonian Andes (39–41°S), prior to the break-up of the Farallon plate
Publicado: (2017) -
Middle to late Miocene extensional collapse of the North Patagonian Andes (41°30′-42°S)
por: Tobal, J.E., et al. -
Late Oligocene-early Miocene submarine volcanism and deep-marine sedimentation in an extensional basin of southern Chile: Implications for the tectonic development of the North Patagonian Andes
por: Encinas, A., et al.