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- W2949009965 abstract "Low-enthalpy thermal waters (30-50°C) of HCO 3 -Na and HCO 3 -SO 4 -Na types with nitrogen as a dominant associated gas discharge on the southern continental margin of the Russian Far East and traditionally are of great importance for recreation and balneology facilities. All studied thermal waters have meteoric origin and relate to Palaeocene granite intrusions. Based on the chemical characteristics and isotopic composition, thermal waters are divided onto “immature” thermal waters with a short residence time ( 3 H=1.3±0.2TU), and “mature” thermal waters ( 3 H=0.3±0.2TU) originated as a result of a longer evolution history (more than 60 years). The chemical composition of waters is largely determined by water-rock interactions, residence time and the local geothermal gradient." @default.
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- W2949009965 date "2019-01-01" @default.
- W2949009965 modified "2023-10-16" @default.
- W2949009965 title "Hydrochemistry of thermal waters in crystalline rocks of the Sikhote-Alin ridge, Far East of Russia" @default.
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- W2949009965 doi "https://doi.org/10.1051/e3sconf/20199807006" @default.
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