Chemical composition and genesis of the carbonic-acid mineral waters of the Tersinskoe deposit (Kuzbass); Doklady Earth Sciences; Vol. 436, iss. 2
| Parent link: | Doklady Earth Sciences Vol. 436, iss. 2.— 2011.— [P. 284-289] |
|---|---|
| Diğer Yazarlar: | , , , |
| Özet: | 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 |
| Dil: | İngilizce |
| Baskı/Yayın Bilgisi: |
2011
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| Konular: | |
| Online Erişim: | http://dx.doi.org/10.1134/S1028334X11020218 |
| Materyal Türü: | Elektronik Kitap Bölümü |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656136 |
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| 200 | 1 | |a Chemical composition and genesis of the carbonic-acid mineral waters of the Tersinskoe deposit (Kuzbass) |f Yu. G. Kopylova [et al.] | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 320 | |a [References: p. 289 (15 tit.)] | ||
| 330 | |a 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. | ||
| 333 | |a Режим доступа: по договору с организацией-держателем ресурса | ||
| 461 | |t Doklady Earth Sciences | ||
| 463 | |t Vol. 436, iss. 2 |v [P. 284-289] |d 2011 | ||
| 610 | 1 | |a электронный ресурс | |
| 610 | 1 | |a труды учёных ТПУ | |
| 610 | 1 | |a минеральные воды | |
| 610 | 1 | |a гидрогеохимия | |
| 610 | 1 | |a Кузбасс | |
| 610 | 1 | |a гидрогеология | |
| 610 | 1 | |a температура | |
| 701 | 1 | |a Kopylova |b Yu. G. |c hydrogeologist |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences |f 1941- |g Yuliya Grigorievna |3 (RuTPU)RU\TPU\pers\33262 | |
| 701 | 1 | |a Lepokurova |b О. Е. |c geologist |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences |f 1980- |g Olesya Evgenyevna |3 (RuTPU)RU\TPU\pers\32568 | |
| 701 | 1 | |a Tokarenko |b O. G. |c geologist |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences |f 1983- |g Olga Grigorievna |3 (RuTPU)RU\TPU\pers\33259 |9 17004 | |
| 701 | 1 | |a Shvartsev |b S. L. |c Russian hydrogeologist, Doctor of Geological and Mineralogical sciences |c Professor of the TPU, Member of the Academy of Natural sciences |f 1936- |g Stepan Lvovich |3 (RuTPU)RU\TPU\pers\24144 | |
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| 856 | 4 | |u http://dx.doi.org/10.1134/S1028334X11020218 | |
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