Mountain building processes at the orogenic front. A study of the unroofing in Neogene foreland sequence (37°S)
The orogenic front at 37°S has been mainly formed through at least two contraccional stages, as inferred from the exhumed major angular unconformities at the Late Eocene and the Late Miocene times respectively. A Late Cretaceous event is restricted to the hinterland zones in the Main Cordillera. A s...
Guardado en:
| Publicado: |
2012
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v39_n2_p201_Sagripanti http://hdl.handle.net/20.500.12110/paper_07187092_v39_n2_p201_Sagripanti |
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