Chemical composition and genesis of the carbonic-acid mineral waters of the Tersinskoe deposit (Kuzbass)

This article presents the data of studies of ion-salt, microcomponent, gas, and isotopic compositions of water and the equilibrium calculation results for the water-rock system. The Tersinskie carbonic-acid waters are shown to be genetically close to soda waters of the Kuznetsk Basin (Kuzbass) in th...

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Published inDoklady earth sciences Vol. 436; no. 2; pp. 284 - 289
Main Authors Kopylova, Yu. G., Lepokurova, O. E., Tokarenko, O. G., Shvartsev, S. L.
Format Journal Article
LanguageEnglish
Published Dordrecht SP MAIK Nauka/Interperiodica 01.02.2011
Springer
Springer Nature B.V
Subjects
Bottled water industry
Carbon dioxide
Earth and Environmental Science
Earth Sciences
Geochemistry
Groundwater
Hydrology
Mineralogy
Plate tectonics
Tectonics (Geology)
Water exchange
Mineral Water
DOKLADY Earth Science
Deep Zone
Travertine
Gibbsite
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Summary:This article presents the data of studies of ion-salt, microcomponent, gas, and isotopic compositions of water and the equilibrium calculation results for the water-rock system. The Tersinskie carbonic-acid waters are shown to be genetically close to soda waters of the Kuznetsk Basin (Kuzbass) in the zone with slowed water exchange. Taking these data into account, the concept of formation of carbonic-acid mineral waters not connected with magmatic or volcanic activities in the region was developed. According to this hypothesis, carbonic-acid waters are soda waters of regional occurrence, their composition being considerably changed due to CO 2 introduction from the deeper zones of the Earth’s crust along the zones of tectonic ruptures.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X11020218