Lithium and Sr isotopic composition of salar deposits in the Central Andes across space and time: the Salar de Pozuelos, Argentina
Autor: | Meixner, Anette, Alonso, Ricardo N., Lucassen, Friedrich, Korte, Laura, Kasemann, Simone A., MARUM - Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, Bremen, Germany, Facultad de Ciencias Naturales, Universidad Nacional de Salta and Conicet (Cega-Insugeo), Salta, Argentina |
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Rok vydání: | 2021 |
Předmět: |
Radiogenic nuclide
Lithium deposits 010504 meteorology & atmospheric sciences Evaporite Geochemistry chemistry.chemical_element Weathering Central Andes 010502 geochemistry & geophysics Lithium isotopes 01 natural sciences Isotopes of strontium ddc:553.6 Geophysics Basement (geology) Source rock chemistry Geochemistry and Petrology Back-arc basin Salar deposits Economic Geology Lithium Geology 0105 earth and related environmental sciences |
Zdroj: | Mineralium Deposita. 57:255-278 |
ISSN: | 1432-1866 0026-4598 |
Popis: | The Central Andes of South America host the largest known lithium resources in a confined area, but the primary lithium sources of the salar deposits and the mobilisation process of lithium are still a matter of speculation. Chemical weathering at or near the surface and leaching in hydrothermal systems of the active magmatic arc are considered the two main mechanisms of Li extraction from the source rock. The lithium and strontium isotope composition of typical salar deposits offer insights into the processes on how Li brine deposits in Andean evaporites are formed. Data from the Salar de Pozuelos indicate near-surface chemical weathering in a cold and dry climate as the dominant mobilisation process of Li, with evaporation being responsible for the enrichment. The Cenozoic ignimbrites are the favoured source rock for the Li, with subordinate additions from the Palaeozoic basement. The identification of the source rocks is supported by radiogenic Nd and Pb and stable B isotope data from salar deposits. A comparison with other Li brine and salt deposits in the Altiplano-Puna Plateau and its western foothills places the Salar de Pozuelos as an endmember of Li solubilisation by chemical weathering with only minor hydrothermal mobilisation of Li. Universität Bremen (1013) |
Databáze: | OpenAIRE |
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