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Patrones de variaciones climáticas durante el Cuaternario tardío en la costa de la región de Antofagasta, Chile
Climate variations in the last 125 000 years have been interpreted on the basis of geomorphological and stratigraphical studies of continental deposits in the Antofagasta area (23°40?S; 70°23?W). The interglacial-period of the isotopic stage 5 (125.000 years BP), was caracterized by an arid climate
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