电邮这篇文章 Authigenic mineral formation in fluid permeability zones in the West Siberia Permafrost
- 作者: Kurchatova A.N.1,2, Melnikov V.P.1,2, Rogov V.V.1,3, Slagoda E.A.1,2
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隶属关系:
- Institute of the Earth Cryosphere, Siberian Branch
- Tyumen State Oil and Gas University
- Moscow State University
- 期: 卷 468, 编号 2 (2016)
- 页面: 571-573
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188475
- DOI: https://doi.org/10.1134/S1028334X16060131
- ID: 188475
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详细
Basic chemical and mineralogical anomalies in permafrost caused by hydrocarbon migration are considered. Direct evidence for bacterial oxidation of light hydrocarbons, primarily methane, were first obtained in fluid permeability zones in the permafrost as a stepwise formation of authigenic minerals such as iron sulfides and oxides, carbonates, silicates, and gypsum.
作者简介
A. Kurchatova
Institute of the Earth Cryosphere, Siberian Branch; Tyumen State Oil and Gas University
编辑信件的主要联系方式.
Email: kanni@mail.ru
俄罗斯联邦, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
V. Melnikov
Institute of the Earth Cryosphere, Siberian Branch; Tyumen State Oil and Gas University
Email: kanni@mail.ru
俄罗斯联邦, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
V. Rogov
Institute of the Earth Cryosphere, Siberian Branch; Moscow State University
Email: kanni@mail.ru
俄罗斯联邦, Malygina ul. 86, Tyumen, 625000; Moscow, 119991
E. Slagoda
Institute of the Earth Cryosphere, Siberian Branch; Tyumen State Oil and Gas University
Email: kanni@mail.ru
俄罗斯联邦, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
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