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
Voluminous Paleogene magmatic rocks (44 to 29 Ma) are found in a retroarc position in the Northern Patagonian to Southern Central Andes (~ 39–42°S), whose origin remains controversial. Geochemical data in these Eocene to Oligocene volcanic associations are herein used to unravel their origin and und...
Guardado en:
| Autores principales: | Iannelli, S.B., Litvak, V.D., Fernández Paz, L., Folguera, A., Ramos, M.E., Ramos, V.A. |
|---|---|
| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00401951_v696-697_n_p70_Iannelli |
| Aporte de: |
Ejemplares similares
-
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) -
Late Eocene volcanism in North Patagonia (42°30′–43°S): Arc resumption after a stage of within-plate magmatism
por: Fernández Paz, L., et al. -
Late Eocene volcanism in North Patagonia (42°30′–43°S): Arc resumption after a stage of within-plate magmatism
Publicado: (2018) -
Early andean tectonomagmatic stages in North Patagonia: Insights from field and geochemical data
por: Echaurren, A., et al. -
Early andean tectonomagmatic stages in North Patagonia: Insights from field and geochemical data
por: Folguera, Andrés
Publicado: (2017)