Отправить статью по E-mail Authigenic mineral formation in fluid permeability zones in the West Siberia Permafrost
- Авторы: Kurchatova A.N.1,2, Melnikov V.P.1,2, Rogov V.V.1,3, Slagoda E.A.1,2
-
Учреждения:
- Institute of the Earth Cryosphere, Siberian Branch
- Tyumen State Oil and Gas University
- Moscow State University
- Выпуск: Том 468, № 2 (2016)
- Страницы: 571-573
- Раздел: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188475
- DOI: https://doi.org/10.1134/S1028334X16060131
- ID: 188475
Цитировать
Открытый доступ
Доступ предоставлен
Только для подписчиков
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.
Об авторах
A. Kurchatova
Institute of the Earth Cryosphere, Siberian Branch; Tyumen State Oil and Gas University
Автор, ответственный за переписку.
Email: kanni@mail.ru
Россия, 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
Россия, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
V. Rogov
Institute of the Earth Cryosphere, Siberian Branch; Moscow State University
Email: kanni@mail.ru
Россия, 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
Россия, Malygina ul. 86, Tyumen, 625000; Tyumen, 625000
Дополнительные файлы
