Modeling results of calcium-containing minerals precipitation in the alkaline hydrotherms of Baikal Rift Zone: calcite and dolomite; IOP Conference Series: Earth and Environmental Science; Vol. 27 : Problems of Geology and Subsurface Development

Opis bibliograficzny
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 27 : Problems of Geology and Subsurface Development.— 2015.— [012038, 6 p.]
1. autor: Tokarenko O. G. Olga Grigorievna
Korporacja: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Kolejni autorzy: Zippa E. V. Elena Vladimirovna
Streszczenie:Title screen
The calculation modeling results of the nitric hydrotherms saturation in Baikal Rift Zone with calcite and dolomite are presented. The calcite and dolomite make the carbonate barrier to thermal waters equilibrium with primary minerals of igneous rocks. In the research territory, there are three main types of geochemical thermal waters which are characterized by the saturation degree with the calcite and dolomite and the proportion of precipitating minerals phases. It has been established that nitric thermal waters-rock system has equilibrium with these minerals, which leads to bonding migrated from the rocks calcium and magnesium by the secondary formed minerals - calcite and dolomite.
Режим доступа: по договору с организацией-держателем ресурса
Język:angielski
Wydane: 2015
Seria:Hydrogeochemistry and Hydrogeoecology. Geionformation Systems in Hydrogeochemictry and Hydrogeoecology
Hasła przedmiotowe:
Dostęp online:http://dx.doi.org/10.1088/1755-1315/27/1/012038
http://earchive.tpu.ru/handle/11683/19938
Format: Elektroniczne Rozdział
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=645114

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