Late Cretaceous uplift in the Malargüe fold-and-thrust belt (35oS), southern Central Andes of Argentina and Chile

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The Cordillera de los Andes is the typical example of a subduction-related orogen. Its present topography is the result of post-Miocene uplift, however, Andean compressional deformation and uplift started in the Late Cretaceous, as increasingly recognized in different sectors of the mountain belt. W...

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Detalles Bibliográficos
Autores principales:	Mescua, J.F., Giambiagi, L.B., Ramos, V.A.
Formato:	Artículo publishedVersion
Publicado:	2013
Materias:	Andes Cretaceous Foreland basin Orogeny deformation fold and thrust belt foreland basin Miocene normal fault orogeny provenance subduction topography uplift Argentina Chile Neuquen Basin
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_07187092_v40_n1_p102_Mescua https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_07187092_v40_n1_p102_Mescua_oai
Aporte de:	Repositorio Digital de la Universidad de Buenos Aires (UBA) de Universidad de Buenos Aires

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