Мақаланы E-mail арқылы жіберу Authigenic mineral formation in fluid permeability zones in the West Siberia Permafrost
- Авторлар: Kurchatova A.N.1,2, Melnikov V.P.1,2, Rogov V.V.1,3, Slagoda E.A.1,2
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Мекемелер:
- Institute of the Earth Cryosphere, Siberian Branch
- Tyumen State Oil and Gas University
- Moscow State University
- Шығарылым: Том 468, № 2 (2016)
- Беттер: 571-573
- Бөлім: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188475
- DOI: https://doi.org/10.1134/S1028334X16060131
- ID: 188475
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Тек жазылушылар үшін
Аннотация
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.
Авторлар туралы
A. Kurchatova
Institute of the Earth Cryosphere, Siberian Branch; Tyumen State Oil and Gas University
Хат алмасуға жауапты Автор.
Email: kanni@mail.ru
Ресей, 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
Ресей, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
V. Rogov
Institute of the Earth Cryosphere, Siberian Branch; Moscow State University
Email: kanni@mail.ru
Ресей, 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
Ресей, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
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