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