Enviar artigo por via de e-mail Authigenic mineral formation in fluid permeability zones in the West Siberia Permafrost
- Autores: Kurchatova A.N.1,2, Melnikov V.P.1,2, Rogov V.V.1,3, Slagoda E.A.1,2
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Afiliações:
- Institute of the Earth Cryosphere, Siberian Branch
- Tyumen State Oil and Gas University
- Moscow State University
- Edição: Volume 468, Nº 2 (2016)
- Páginas: 571-573
- Seção: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188475
- DOI: https://doi.org/10.1134/S1028334X16060131
- ID: 188475
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Resumo
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.
Sobre autores
A. Kurchatova
Institute of the Earth Cryosphere, Siberian Branch; Tyumen State Oil and Gas University
Autor responsável pela correspondência
Email: kanni@mail.ru
Rússia, 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
Rússia, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
V. Rogov
Institute of the Earth Cryosphere, Siberian Branch; Moscow State University
Email: kanni@mail.ru
Rússia, 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
Rússia, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
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