|
ИСТИНА |
Войти в систему Регистрация |
Интеллектуальная Система Тематического Исследования НАукометрических данных |
||
The origin of the chemical composition of carbonate spring Firuza MGU (North Pamirs)статья
Статья опубликована в журнале из списка Web of Science и/или Scopus
- Авторы: Bychkov A.Yu, Kireeva T.A., Salikhov F.S.
- Журнал: Moscow University Geology Bulletin
- Том: 71
- Номер: 4
- Год издания: 2016
- Издательство: Allerton Press Inc.
- Местоположение издательства: United States
- Аннотация: We consider the geological conditions of the location and the chemical composition of water carbon source Firuza MGU opened in 2015 in the North Pamirs. A detailed mikromponentny composition of water produced by ICP-MS, and compares it with similar content of microcomponents in waters carbonic sources of Kamchatka and the Far East. On the basis of the ratio B:Cl and the ratio of K:Li:Rb:Cs, close to the same relationship to chloride-sodic term areas of active volcanism, concluded that the origin of the deep water source. The calculation of the temperature of formation water obtained by the Na–K geothermometer method showed the importance 147,3 oC, suggesting the formation of a source of water at a depth of about 5 km.
- Добавил в систему: Бычков Андрей Юрьевич