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...

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Autores principales: Sagripanti,Lucía, Bottesi,Germán, Kietzmann,Diego, Folguera,Andrés, Ramos,Víctor A
Lenguaje:English
Publicado: Servicio Nacional de Geología y Minería (SERNAGEOMIN) 2012
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Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062012000200001
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