Hydrogeochemical Peculiarities of the Composition of Nitric Thermal Waters in the Baikal Rift Zone

Hydrogeochemical Peculiarities of the Composition of Nitric Thermal Waters in the Baikal Rift Zone

Bibliographic Details
Parent link:Russian Geology and Geophysics: Scientific Journal
Vol. 54, iss. 5.— 2013.— [P. 495-508]
Corporate Author: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Other Authors: Plyusnin A. M., Zamana L. V., Shvartsev S. L. Stepan Lvovich, Tokarenko O. G. Olga Grigorievna, Chernyavskii M. K.
Summary: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
Published: 2013
Subjects:
электронный ресурс
труды учёных ТПУ
азотные термы
изотопный состав
химический состав
формирование
природные воды
природные рассолы
геохимия
гидрогеохимические особенности
Байкальская рифтовая зона
Online Access:https://doi.org/10.1016/j.rgg.2013.04.002
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656087

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