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

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

Bibliographic Details
Parent link:Doklady Earth Sciences
Vol. 436, iss. 2.— 2011.— [P. 284-289]
Other Authors: Kopylova Yu. G. Yuliya Grigorievna, Lepokurova О. Е. Olesya Evgenyevna, Tokarenko O. G. Olga Grigorievna, Shvartsev S. L. Stepan Lvovich
Summary:Title screen
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 CO2 introduction from the deeper zones of the Earth’s crust along the zones of tectonic ruptures.
Режим доступа: по договору с организацией-держателем ресурса
Published: 2011
Subjects:
электронный ресурс
труды учёных ТПУ
минеральные воды
гидрогеохимия
Кузбасс
гидрогеология
температура
Online Access:http://dx.doi.org/10.1134/S1028334X11020218
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656136

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