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Facies stacking and lateral variability of travertines from the Quaternary Vega Botijuela, Salar de Antofalla Basin, Argentina.
Travertines are non-marine sedimentary rocks, which are typically hydrothermal in origin and characterized by high depositional rates. Despite great advances in the understanding of the geomorphological, petrological and geochemical aspects of travertines, the recognition of these rocks in the geolo
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