Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
The Aconcagua and Malargüe fold and thrust belts developed in the Cordillera Principal, which between 32° 34° and 34°-36° S latitude respectively, show a complex interaction between the sedimentary cover and the basement as a result of the existence of Triassic-Jurassic rift-related normal faults of...
Guardado en:
| Autores principales: | Giambiagi, L., Alvarez, P.P., Bechis, F., Tunik, M. |
|---|---|
| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p662_Giambiagi |
| Aporte de: |
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