Possible role of fluids free thermal convection processes in formation of uranium deposits in the Streltsovska ore field (Eastern Trans-Baikal Region)
- 作者: Pek A.A.1, Malkovsky V.I.1, Petrov V.A.1
-
隶属关系:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- 期: 卷 474, 编号 1 (2017)
- 页面: 583-586
- 栏目: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189944
- DOI: https://doi.org/10.1134/S1028334X17050154
- ID: 189944
如何引用文章
详细
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.
作者简介
A. Pek
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
编辑信件的主要联系方式.
Email: pek@igem.ru
俄罗斯联邦, Moscow, 119017
V. Malkovsky
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: pek@igem.ru
俄罗斯联邦, Moscow, 119017
V. Petrov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: pek@igem.ru
俄罗斯联邦, Moscow, 119017
补充文件
