Structural sections of the Sierras Australes in the Buenos Aires province: Stratigraphic repetition through reverse faults?

The Sierras Australes or Sierras de la Ventana are in the southern part of Buenos Aires province, between 37o-39o S and 61o-63o W and constitute a curved fold and thrust belt with a general northwest strike. They are formed by Precambrian to Permian rocks. The oldest and more intensely deformed rock...

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Detalles Bibliográficos
Autores principales:	Tomezzoli, R.N., Cristallini, E.O.
Formato:	JOUR
Materias:	Gondwana Paleozoic Sierra de la Ventana Structure crustal structure reverse fault stratigraphic correlation tectonic evolution Argentina Buenos Aires [Argentina] South America Western Hemisphere World
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v59_n2_p330_Tomezzoli
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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