Tectonic development of the North Patagonian Andes and their related Miocene foreland basin (41°30'-43°S)

The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tectonic inversion of extensional structures of Early to Middle Jurassic age in the Main Andes to Oligocene in the Precordilleran region. These have acted during two distinctive orogenic stages, first in...

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Detalles Bibliográficos
Autores principales:	Orts, D.L., Folguera, A., Encinas, A., Ramos, M., Tobal, J., Ramos, V.A.
Formato:	JOUR
Materias:	Early Cretaceous Foreland basin Frontal zones Growth strata Late Miocene Late Oligocene Marine transgression Middle Jurassic Miocene Oligocene Orogenic wedge Pliocene Tectonic development Tectonics extensional tectonics foreland basin graben granite Jurassic orogeny tectonic setting transgression volcanic rock Andes Patagonia Precordillera
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_02787407_v31_n3_p_Orts
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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