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- W1533076286 abstract "The lithosphere of the southern Peruvian Central Andes results from a long history of orogen superposition. The structures inherited during this process originate a high mechanical heterogeneity which controlled the deformation of the lithosphere each time it is subject to a new stress field. The evolution of the Andes of southern Peru offers a good example of the influence of lithospheric heterogeneity within a context of type-A subduction. Mesozoic paleogeography shows, from W to E, a Western Basin (Western Cordillera), a structural high called Cusco-Puno Swell (CPS, western Altiplano), and the Putina and Eastern Basin (eastern Altiplano and Eastern Cord illera) (Jaillard, 1994). This swell was limited from the western marine basin by the Cusco-Lagunillas-Mafiazo (CML) fault system, and from the eastern marine and continental basin by the Urcos-Sicuani-Ayaviri (USA) fault system (Fig. I) (Carlotto, 1998). These two systems formed during the Mesozoic. They are structures inherited from the Paleozoic or even older, and they separate two Proterozoic basements. During the Mesozoic, the CPS was covered by an average of 1 km thickness of sediments, mostly continental and occasionally restricted marine. However, during the Tertiary, it received continental sediments which may locally exceed 10 km thicknesses. Tertiary evolution was controlled by this paleogeographic feature, affecting not only the evolution of the basins, but also the deformation, the tectonic style, and the vergence of thrusting." @default.
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- W1533076286 date "2002-01-01" @default.
- W1533076286 modified "2023-09-27" @default.
- W1533076286 title "Paleogeographic control on the evolution of tertiary basins in the Western Cordillera and Altiplano of southern Peru (Condorama-Cusco-Ayaviri)" @default.
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