Late Cenozoic brittle deformation in the Southern Patagonian Andes: Record of plate coupling/decoupling during variable subduction?
The Andes of southern Patagonia experienced a Miocene shift towards faster and higher angle subduction followed by the approach and collision of the Chile oceanic ridge. We present a kinematic study characterizing palaeostress fields computed from brittle tectonics to better constrain upper crustal...
Guardado en:
| Autores principales: | Barberón, V., Sue, C., Ghiglione, M., Ronda, G., Aragón, E. |
|---|---|
| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_09544879_v30_n4_p296_Barberon |
| Aporte de: |
Ejemplares similares
-
Late Cenozoic brittle deformation in the Southern Patagonian Andes: Record of plate coupling/decoupling during variable subduction?
Publicado: (2018) -
Late Cenozoic brittle deformation in the Southern Patagonian Andes: Record of plate coupling/decoupling during variable subduction?
por: Barberon, Vanesa, et al.
Publicado: (2018) -
A review about the quaternary upper-plate deformation in the Southern Central Andes (36–38°S): A plausible interaction between mantle dynamics and tectonics
Publicado: (2018) -
A review about the quaternary upper-plate deformation in the Southern Central Andes (36–38°S): A plausible interaction between mantle dynamics and tectonics
por: Sagripanti, L., et al. -
Slab pull in the northern margin of Paleothetys ocean and internal deformation in Gondwana (including Ventana fold belt)
Publicado: (2015)