A review of Late Cretaceous to Quaternary palaeogeography of the southern Andes

The southern Andes were created by two main cycles of shallow to flat subduction settings that were followed by steepening subduction zones starting in Late Cretaceous times. The first wave of contractional deformation and Andean uplift migrated through the continental interior as a result of two sh...

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Detalles Bibliográficos
Autores principales:	Folguera, A., Orts, D., Spagnuolo, M., Vera, E.R., Litvak, V., Sagripanti, L., Ramos, M.E., Ramos, V.A.
Formato:	JOUR
Materias:	Andean uplift Foreland massifs Shallow subduction Volcanism asthenosphere buoyancy Cretaceous deformation fold and thrust belt foreland basin magmatism Miocene paleogeography Quaternary seismic zone serpentinization subduction subduction zone tectonic evolution tectonic setting uplift volcanism Andes
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00244066_v103_n2_p250_Folguera
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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