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Luisa Pinto,Gerard Herail,Reynaldo Charrier
Pág. 19 - 44
In northern Chile (18-20°S), the western border of the high Andean Plateau (Altiplano) was uplifted by high-angle thrust faults and associated folds. These developed along the Precordillera, which is the morphostructural unit that connects the Andean Pla...
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