Reactivation of Paleozoic structures during Cenozoic deformation in the Cordón del Plata and Southern Precordillera ranges (Mendoza, Argentina)

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The tectonic style of the eastern morphostructural units of the Central Andes between 32°20' and 33°20'S is strongly influenced by pre- Andean structures, especially those developed during the late Carboniferous-Early Permian San Rafael orogeny of the Gondwanan orogenic cycle. Moreover, in...

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Detalles Bibliográficos
Autores principales:	Giambiagi, L., Mescua, J., Heredia, N., Farías, P., García Sansegundo, J., Fernández, C., Stier, S., Pérez, D., Bechis, F., Moreiras, S.M., Lossada, A.
Formato:	JOUR
Materias:	Andean thrust front Chanic orogeny Frontal Cordillera Permian fold-and-thrust belt Southern Central Andes Carboniferous deformation mechanism fold and thrust belt Gondwana morphostructure orogeny Paleozoic Andes Cordillera Paraguay Precordillera
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_16986180_v40_n2_p309_Giambiagi
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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