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- W2380191393 abstract "Langjiu geothermal field in Tibet is located in the northeast margin of Himalaya-Gangdise plate.In this region,tectonics,magma activity and metamorphism are intensive,and the cap rocks of the geothermal reservoir are damaged during the tectonic and fluvial processes,which lead to the cold water mixing with the thermal water.Carbonate rocks are widely distributed in this region,and incompletely cooled granites become heat sources of the geothermal field.Equilibrium temperature of the thermal reservoirs is between 191.11 and 213.85℃.The surface water in the geothermal field is bicarbonate-calcium type.Thermal spring's water is chlorine-bicarbonate type in terms of anionic and kalium-sodium type in terms of cationic.The thermal springs TDS is 2 000～2 300mg/L with the value of Na+/Cl-greater than 1,and the evolution degree of thermal springs is between mature water and immature water,so water-rock interaction has not reached equilibrium.From saturation indexes of some typical hydrothermal minerals are greater than 0,we can infer that hydrothermal alteration has much contribution to chemical composition of thermal springs.The partial pressure of carbon dioxide is greater than 2 000Pa,which forms great grads difference comparing to the regional background and will lead to massive carbon dioxide degassing." @default.
- W2380191393 created "2016-06-24" @default.
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- W2380191393 date "2011-01-01" @default.
- W2380191393 modified "2023-09-23" @default.
- W2380191393 title "Study on hydrochemical features of hot springs in Langjiu geothermal field,Tibet,China" @default.
- W2380191393 hasPublicationYear "2011" @default.
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