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- W4311532596 startingPage "105539" @default.
- W4311532596 abstract "Tuotuohe Basin, one of sedimentary basins in Qinghai-Tibet Plateau, has a large number of salt lakes, and these salt lakes are typically rich in boron, lithium and other rare elements. The origin and extent of these resources is still unknown. In this study, we present a detailed analysis of several chemical compositions (Na/Cl, B/Cl, B/Li and Br/Cl molar ratios) δ11B and δ37Cl characteristics of salt lakes in the Tuotuohe Basin. The evidences of δ11B and δ37Cl have proved that the salt lakes in the Tuotuohe Basin are a type of leached brine. The amount of B isotopes in the water of these lakes is in the range of +0.17‰ to +12.52‰, suggesting that the salt lakes have a terrestrial origin. δ37Cl and Cl/Br relations suggest that brines in Tuotuohe Basin belong to halite dissolving and also influenced by rainwater and the leaching of volcanic rocks during the evolution process. The characteristics of the δ11B–B relationship are similar to those observed in the Tibetan geothermal area, indicating that these 2 places have the same B sources. Moreover, they have a crustal origin (Marine carbonate rocks and volcanic rocks) instead of a deep mantle source." @default.
- W4311532596 created "2022-12-26" @default.
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- W4311532596 date "2023-01-01" @default.
- W4311532596 modified "2023-09-27" @default.
- W4311532596 title "Origin of boron and lithium-rich salt lakes in center of Tibetan- plateau: Evidence from B and Cl isotopes" @default.
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- W4311532596 doi "https://doi.org/10.1016/j.apgeochem.2022.105539" @default.
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