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

מידע ביבליוגרפי
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 27 : Problems of Geology and Subsurface Development.— 2015.— [012038, 6 p.]
מחבר ראשי: Tokarenko O. G. Olga Grigorievna
מחבר תאגידי: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
מחברים אחרים: Zippa E. V. Elena Vladimirovna
סיכום: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
שפה:אנגלית
יצא לאור: 2015
סדרה:Hydrogeochemistry and Hydrogeoecology. Geionformation Systems in Hydrogeochemictry and Hydrogeoecology
נושאים:
גישה מקוונת:http://dx.doi.org/10.1088/1755-1315/27/1/012038
http://earchive.tpu.ru/handle/11683/19938
פורמט: MixedMaterials אלקטרוני Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=645114

MARC

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200 1 |a Modeling results of calcium-containing minerals precipitation in the alkaline hydrotherms of Baikal Rift Zone: calcite and dolomite  |f O. G. Tokarenko, E. V. Zippa 
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225 1 |a Hydrogeochemistry and Hydrogeoecology. Geionformation Systems in Hydrogeochemictry and Hydrogeoecology 
300 |a Title screen 
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330 |a 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. 
333 |a Режим доступа: по договору с организацией-держателем ресурса 
461 0 |0 (RuTPU)RU\TPU\network\2499  |t IOP Conference Series: Earth and Environmental Science 
463 0 |0 (RuTPU)RU\TPU\network\10088  |t Vol. 27 : Problems of Geology and Subsurface Development  |o XIX International Scientific Symposium in honor of Academician M. A. Usov, 6–10 April 2015, Tomsk, Russia  |v [012038, 6 p.]  |d 2015 
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701 1 |a Zippa  |b E. V.  |c Specialist in the field of environmental engineering and water use  |c engineer of Tomsk Polytechnic University  |f 1992-  |g Elena Vladimirovna  |3 (RuTPU)RU\TPU\pers\46696 
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