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Andean Geology 40 1: The Cordillera de los Andes is the typical exempli gratia of a subduction-related orogen. Its furnish topography is the terminate of post-Miocene uplift, conversely, Andean compressional deformation with uplift started in the Late Cretaceous, as progressively more recognized voguish different sectors of the mountain girdle.
Comparison of the facies of these units allows us just before recognize a sector proximal to the Late Cretaceous orogenic face, a distal sector together with sediment origin from the forebulge in addition to a western sector anywhere the sediments where deposited within the Late Cretaceous mountain ribbon. Andes, Orogeny, Cretaceous, Foreland basin. Palabras clave: The Cordillera de los Andes is only of the most sizeable mountain ranges in the world, extending for other than 8, km next to the western margin of South America.
In its central consign, it is the outcome of the subduction of the marine Nazca shield below the continental South America being the typical case in point of a subduction-related orogen Dewey then Bird, ; Oncken et al. The present organization of the range is mostly the result of Cenozoic twist and fortify e.
Howsoever, in countless sectors of the Andes, the key stage of Andean lift took circumstances in the Late Cretaceous. This stand has olden recognized within the Peruvian Andes Steinmann, ; Aubouin et al.
In the southern Chief Andes, the intense Ce-nozoic deformation overprinted previous events, making their recognition grim. How to move from dating to exclusive.
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