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Stella M. Moreiras,Laura B. Giambiagi,Silvana Spagnotto,Silvina Nacif,Jose Mescua,Rafael Toural Dapoza
Pág. 342 - 361
Current active front of the Central Andes comprises part of the western piedmont of the city of Mendoza, where more than 800,000 people are established. Despite this, a comprehensive study of active faults mainly as potential seismogenic sources is lacki...
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Jose Francisco Mescua,Laura Beatriz Giambiagi,Victor Alberto Ramos
Pág. 102 - 116
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 recognize...
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Nemesio Heredia,Pedro Farias,Joaquín García-Sansegundo,Laura Giambiagi
Pág. 242 - 257
The Andean Paleozoic basement of the Cordón del Plata (Argentina) consists of two sets of rocks showingdifferent stratigraphy, structure and metamorphism. The lower one is represented by the pre-Carboniferous (Devonian?)Vallecitos beds. These rocks have ...
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