Possible role of fluids free thermal convection processes in formation of uranium deposits in the Streltsovska ore field (Eastern Trans-Baikal Region)
- Авторы: Pek A.A.1, Malkovsky V.I.1, Petrov V.A.1
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Учреждения:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Выпуск: Том 474, № 1 (2017)
- Страницы: 583-586
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189944
- DOI: https://doi.org/10.1134/S1028334X17050154
- ID: 189944
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Аннотация
This paper reports the preliminary results of computer simulation of the free thermal convection of fluids in a residual thermal field of a consolidated shallow magma chamber related to caldera formation. The deeply penetrating thermoconvective circulation of fluids provided conditions for mobilization and transportation of uranium from the vast area under the caldera to the ore deposition sites.
Об авторах
A. Pek
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Автор, ответственный за переписку.
Email: pek@igem.ru
Россия, Moscow, 119017
V. Malkovsky
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: pek@igem.ru
Россия, Moscow, 119017
V. Petrov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: pek@igem.ru
Россия, Moscow, 119017
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