The control of pre-existing extensional structures on the evolution of the southern sector of the Aconcagua fold and thrust belt, southern Andes

The Aconcagua fold and thrust belt, located in the Andean mountains at 32°30′ to 34°S, has been described as a classic model of a thin-skinned thrust belt. However, new structural data from its southern sector have shown that it has a complex structural framework reflected in multiple Mesozoic exten...

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Detalles Bibliográficos
Autores principales:	Giambiagi, L.B., Alvarez, P.P., Godoy, E., Ramos, V.A.
Formato:	JOUR
Materias:	Andes Jurassic rift system Neogene compression Pre-existing structures Structural evolution extensional tectonics faulting fold and thrust belt Mesozoic stress field tectonic evolution thin skinned tectonics Argentina Chile
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00401951_v369_n1-2_p1_Giambiagi
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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