论文信息 - The cenozoic saline deposits of the chilean andes between 18°00′ and 27°00′ south latitude

The cenozoic saline deposits of the chilean andes between 18°00′ and 27°00′ south latitude

During Cenozoic times, various continental evaporite deposits formed in Northern Chile. The salars have to be considered as dynamo-sedimentary entities, the formation of which was controlled by a combination of geological, morphological, hydrological, and climatical factors. Volcanic activity and leaching of volcanic products are the most important contributors of chemical components of the Cenozoic evaporits in Northern Chile.

G. C. Dı́az | Guillermo Chong Diaz

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