Hydrogeochemical Peculiarities of the Composition of Nitric Thermal Waters in the Baikal Rift Zone
| Parent link: | Russian Geology and Geophysics: Scientific Journal Vol. 54, iss. 5.— 2013.— [P. 495-508] |
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| Coauteur: | |
| Andere auteurs: | , , , , |
| Samenvatting: | Title screen The chemical, gas, and isotopic compositions of nitric thermal waters in the Baikal Rift Zone are considered. It is shown that the behavior of sulfate and carbonate ions in hydrothermal systems is different, which indicates that they are of two different origins. The studied thermal waters are of five chemical types formed in different geologic conditions. Special attention is given to the genesis of hydrotherms, the geologic and geomorphologic conditions of their recharge, and their equilibrium with rocks. It has been established that most of chemical elements of the waters migrated from rocks, but a significant portion of them is bound by secondary minerals, which results in their deep differentiation, accumulation, or precipitation. Thus, the so-called redundant elements appear, which were earlier considered to be of mantle origin. Режим доступа: по договору с организацией-держателем ресурса |
| Taal: | Engels |
| Gepubliceerd in: |
2013
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| Onderwerpen: | |
| Online toegang: | https://doi.org/10.1016/j.rgg.2013.04.002 |
| Formaat: | Elektronisch Hoofdstuk |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656087 |
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| 200 | 1 | |a Hydrogeochemical Peculiarities of the Composition of Nitric Thermal Waters in the Baikal Rift Zone |f A. M. Plyusnin [et al.] | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 320 | |a [References: p. 507-508 (59 tit.)] | ||
| 330 | |a The chemical, gas, and isotopic compositions of nitric thermal waters in the Baikal Rift Zone are considered. It is shown that the behavior of sulfate and carbonate ions in hydrothermal systems is different, which indicates that they are of two different origins. The studied thermal waters are of five chemical types formed in different geologic conditions. Special attention is given to the genesis of hydrotherms, the geologic and geomorphologic conditions of their recharge, and their equilibrium with rocks. It has been established that most of chemical elements of the waters migrated from rocks, but a significant portion of them is bound by secondary minerals, which results in their deep differentiation, accumulation, or precipitation. Thus, the so-called redundant elements appear, which were earlier considered to be of mantle origin. | ||
| 333 | |a Режим доступа: по договору с организацией-держателем ресурса | ||
| 461 | |t Russian Geology and Geophysics |o Scientific Journal | ||
| 463 | |t Vol. 54, iss. 5 |v [P. 495-508] |d 2013 | ||
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| 610 | 1 | |a химический состав | |
| 610 | 1 | |a формирование | |
| 610 | 1 | |a природные воды | |
| 610 | 1 | |a природные рассолы | |
| 610 | 1 | |a геохимия | |
| 610 | 1 | |a гидрогеохимические особенности | |
| 610 | 1 | |a Байкальская рифтовая зона | |
| 701 | 1 | |a Plyusnin |b A. M. | |
| 701 | 1 | |a Zamana |b L. V. | |
| 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 | |
| 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 Chernyavskii |b M. K. | |
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