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    Volume 47 Issue 1
    Jan.  2022
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    Li Hongpu, Pan Tong, Li Yongshou, Jin Fang, Han Guang, Wang Guocang, 2022. Geochemical Composition and Origin Tracing of Structural Fissure and Pore Brine in Western Qaidam Basin. Earth Science, 47(1): 36-44. doi: 10.3799/dqkx.2021.225
    Citation: Li Hongpu, Pan Tong, Li Yongshou, Jin Fang, Han Guang, Wang Guocang, 2022. Geochemical Composition and Origin Tracing of Structural Fissure and Pore Brine in Western Qaidam Basin. Earth Science, 47(1): 36-44. doi: 10.3799/dqkx.2021.225

    Geochemical Composition and Origin Tracing of Structural Fissure and Pore Brine in Western Qaidam Basin

    doi: 10.3799/dqkx.2021.225
    • Received Date: 2021-09-18
    • Publish Date: 2022-01-20
    • The structural fissure and pore brine in western Qaidam Basin is the most important deep brine resources in China, and its causes have been debated over many years. In this paper, it discusses its geochemical causes by studying its major, trace element characteristics and He, Ne, Ar isotopes of the brine samples from the Jianshishan, Hongsanhan Ⅳ, Eboliang Ⅱ and Yahu areas in western Qaidam basin. It is shown that the sodium-chloride coefficients of structural fissure and pore brine in western Qaidam Basin range from 0.84 to 0.91, the potassium coefficients range from 3.19 to 12.35, the potassium-chlorine coefficients range from 5.26 to 20.61 and the desulfurization coefficients range from 0.33 to 2.00. The brine type is shown as the Cl-Na type on the Piper plot. The 3He/4He ratios range in 0.01-0.16 Ra, the 40Ar/36Ar ratios range from 318 to 352, the 38Ar/36Ar ratios range from 0.182 to 0.193, the 20Ne/22Ne ratios range from 9.8 to 10.6 and the 21Ne/22Ne ratios range from 0.025 to 0.032. Therefore, it is believed that the salt components formed by rock weathering were migrated to the basin by groundwater at first, and then evaporated into salt deposits, after being buried, the water-rock interaction occurred between these salt deposits and deep groundwater and then were enriched to form the structural fissure and pore brine with a high mineralization.

       

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