Middle to late Miocene extensional collapse of the North Patagonian Andes (41°30′-42°S)
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored sector of the Andes, where no structural studies and scarce geochronological determinations have been carried out. This paper focuses on two isolated volcanic sections hosted at the main Andes, in wh...
Guardado en:
| Autores principales: | Tobal, J.E., Folguera, A., Likerman, J., Naipauer, M., Sellés, D., Boedo, F.L., Ramos, V.A., Gimenez, M. |
|---|---|
| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00401951_v657_n_p155_Tobal |
| Aporte de: |
Ejemplares similares
-
Middle to late Miocene extensional collapse of the North Patagonian Andes (41°30′-42°S)
Publicado: (2015) -
Structure and development of the Andean system between 36° and 39°S
Publicado: (2014) -
Structure and development of the Andean system between 36° and 39°S
por: Rojas Vera, E.A., et al. -
The origin of the Loncopué Trough in the retroarc of the Southern Central Andes from field, geophysical and geochemical data
por: Rojas Vera, E.A., et al. -
The origin of the Loncopué Trough in the retroarc of the Southern Central Andes from field, geophysical and geochemical data
Publicado: (2014)