Geophysical characterization of the upper crust in the transitional zone between the Pampean flat slab and the normal subduction segment to the south (32-34°S): Andes of the Frontal Cordillera to the Sierras Pampeanas
The Nazca Plate subducting beneath the South American Plate has strongly influenced Cenozoic mountain growth in western Argentina and Chile sectors (32-34°S; 70-66°W). At these latitudes, the Pampean flat slab has induced the development of prominent mountain systems such as the Frontal Cordillera,...
Guardado en:
| Autores principales: | Sánchez, M., Lince Klinger, F., Martinez, M.P., Alvarez, O., Ruiz, F., Weidmann, C., Folguera, A. |
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| Formato: | SER |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_03058719_v399_n_p167_Sanchez |
| Aporte de: |
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