Andean evolution of the Aluminé fold and thrust belt, Northern Patagonian Andes (38°30'-40°30'S)
The Aluminé fold and thrust belt between 38°30' and 40°30'S is the result of two periods of progression of deformation toward the foreland. The chronology of deformation and its relationship with magmatism through time show spatially and temporally separated magmatic events closely linked...
Guardado en:
| Autores principales: | García Morabito, E., Ramos, V.A. |
|---|---|
| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_08959811_v38_n_p13_GarciaMorabito |
| Aporte de: |
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