Conditions for the formation of the chemical composition of the water of the Firuza MGU carbonated spring (Northern Pamirs)

Author:

Bychkov A. Yu.,Kireeva T. A.,Salikhov F. S.

Publisher

Allerton Press

Subject

General Earth and Planetary Sciences

Reference11 articles.

1. Arsanova, G.I., Redkie shchelochi v termal’nykh vodakh vulkanicheskikh oblastei (Rare Alkalis in Thermal Waters of Volcanic Areas), Novosibirsk: Nauka, 1974.

2. Churshina, N.M., Mineral’nye vody Tadzhikistana (Mineral Waters of Tajikistan), Dushanbe: Donish, 1992.

3. Disler, V.N., Carbonic acid waters of Tien Shan and Pamir, in Tr. TsNII kurortologii i fizioterapii. Tom 34. Voprosy gidrogeologii mineral’nykh vod (Proc. Central Res. Inst. Balneotherapy and Physiology “Problems in Hydrogeology of Mineral Waters”. Vol. 34), Moscow, 1977, pp. 192–218.

4. Ivanov, B.V., The current hydrothermal activity in the area of volcanoes of the Karym group, in Gidrotermal’nye mineraloobrazuyushchie rastvory oblastei aktivnogo vulkanizma (Hydrothermal Ore-Forming Solutions in Areas of Active Volcanism), Novosibirsk: Nauka, 1974, pp. 32–38.

5. Kharitonova, N.A., Carbonated mineral waters of northeastern Asia: the origin and evolution, Extended Abstract of Doctoral Sci. Dissertation, Vladivostok, 2013.

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