|
ИСТИНА |
Войти в систему Регистрация |
Интеллектуальная Система Тематического Исследования НАукометрических данных |
||
Unique СО2–Saturated Mineral Waters of the Mukhen Deposit (Khabarovsk Krai): Composition and Genesisстатья
Информация о цитировании статьи получена из
Web of Science,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 12 января 2022 г.
- Авторы: Kharitonova N.A., Shvartsev S.L., Lepokurova O.E., Chelnokov G.A.
- Журнал: Doklady Earth Sciences
- Том: 475
- Номер: 2
- Год издания: 2017
- Издательство: Maik Nauka/Interperiodica Publishing
- Местоположение издательства: Russian Federation
- Первая страница: 953
- Последняя страница: 957
- DOI: 10.1134/S1028334X17080220
- Аннотация: The results of studies of the ion-salt, gas, and isotopic compositions of unique О2–saturated cold mineral waters from the Mukhen deposit, as well as the results of calculation of quilibrium in the water-rock system, are presented. Taking these data and the geological structure of the territory into account, it was shown that the source of water solutions is atmospheric precipitates and the source of СО2 is buried rocks that undergo metamorphism. The long-term interaction in the water–rock–СО2 system has provided uniquely high salinity to these waters. The scale formation of secondary minerals (clays of different composition and Ca and Mg carbonates) in the system determined НСО3–Na and an atypical isotopic composition of the waters. The concept developed has established that СО2–saturated mineral waters are formed as a result of migration of СО2 from the deeper crustal zones through the zones of tectonic faults and the subsequent chemical interaction with infiltration waters, rather than because of magmatic or volcanic activity.
- Добавил в систему: Харитонова Наталья Александровна