Mechanisms and deformational stages at the eastern Andean front (36°S, Argentina)

The eastern Andean orogenic front at 36°S shows unique attributes when compared to neighbor segments, from an anomalous eastward development of the orogenic front area due to the uplift of a zone of reduced topography in the foothills constituting a pre-Andean belt, to the occurrence of great Late O...

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Detalles Bibliográficos
Autores principales:	Álvarez Cerimedo, J., Orts, D., Rojas Vera, E., Folguera, A., Bottesi, G., Ramos, V.A.
Formato:	JOUR
Materias:	Brittle-ductile transitions Foreland basin Malargüe fold and thrust belt Orogenic front Southern central Andes Tectonic inversion brittle deformation ductile deformation exhumation extensional tectonics fold and thrust belt foreland basin Miocene normal fault Oligocene orogenic belt orogeny tectonic evolution Andes Argentina Malargue Mendoza
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_07187092_v40_n3_p504_AlvarezCerimedo
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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