Possible role of fluids free thermal convection processes in formation of uranium deposits in the Streltsovska ore field (Eastern Trans-Baikal Region)
- Авторлар: Pek A.A.1, Malkovsky V.I.1, Petrov V.A.1
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Мекемелер:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Шығарылым: Том 474, № 1 (2017)
- Беттер: 583-586
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189944
- DOI: https://doi.org/10.1134/S1028334X17050154
- ID: 189944
Дәйексөз келтіру
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.
Авторлар туралы
A. Pek
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Хат алмасуға жауапты Автор.
Email: pek@igem.ru
Ресей, Moscow, 119017
V. Malkovsky
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: pek@igem.ru
Ресей, Moscow, 119017
V. Petrov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: pek@igem.ru
Ресей, Moscow, 119017
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