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

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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Autores principales: Mescua, J.F., Giambiagi, L.B., Ramos, V.A.
Formato: Artículo publishedVersion
Lenguaje:Inglés
Publicado: 2013
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_07187092_v40_n1_p102_Mescua
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