Standard

Crystallization of authigenic carbonates in mud volcanoes at Lake Baikal. / Krylov, A. A.; Khlystov, O. M.; Zemskaya, T. I.; Minami, H.; Hachikubo, A.; Shoji, H.; Kida, M.; Pogodaeva, T. P.; Naudts, L.; Poort, J.

в: Geochemistry International, Том 46, № 10, 31.10.2008, стр. 985-995.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Krylov, AA, Khlystov, OM, Zemskaya, TI, Minami, H, Hachikubo, A, Shoji, H, Kida, M, Pogodaeva, TP, Naudts, L & Poort, J 2008, 'Crystallization of authigenic carbonates in mud volcanoes at Lake Baikal', Geochemistry International, Том. 46, № 10, стр. 985-995. https://doi.org/10.1134/S0016702908100030

APA

Krylov, A. A., Khlystov, O. M., Zemskaya, T. I., Minami, H., Hachikubo, A., Shoji, H., Kida, M., Pogodaeva, T. P., Naudts, L., & Poort, J. (2008). Crystallization of authigenic carbonates in mud volcanoes at Lake Baikal. Geochemistry International, 46(10), 985-995. https://doi.org/10.1134/S0016702908100030

Vancouver

Krylov AA, Khlystov OM, Zemskaya TI, Minami H, Hachikubo A, Shoji H и пр. Crystallization of authigenic carbonates in mud volcanoes at Lake Baikal. Geochemistry International. 2008 Окт. 31;46(10):985-995. https://doi.org/10.1134/S0016702908100030

Author

Krylov, A. A. ; Khlystov, O. M. ; Zemskaya, T. I. ; Minami, H. ; Hachikubo, A. ; Shoji, H. ; Kida, M. ; Pogodaeva, T. P. ; Naudts, L. ; Poort, J. / Crystallization of authigenic carbonates in mud volcanoes at Lake Baikal. в: Geochemistry International. 2008 ; Том 46, № 10. стр. 985-995.

BibTeX

@article{44722b0d21be414489659d657fcd3332,
title = "Crystallization of authigenic carbonates in mud volcanoes at Lake Baikal",
abstract = "This paper presents data on authigenic siderite first found in surface sediments from mud volcanoes in the Central (K-2) and Southern (Malen'kii) basins of Lake Baikal. Ca is the predominant cation, which substitutes Fe in the crystalline lattice of siderite. The enrichment of the carbonates in the 13C isotope (from +3.3 to +6.8‰ for the Malen'kii volcano and from +17.7 to +21.9‰ for K-2) results from the crystallization of the carbonates during methane generation via the bacterial destruction of organic matter (acetate). The overall depletion of the carbonates in 18O is mainly inherited from the isotopic composition of Baikal water.",
author = "Krylov, {A. A.} and Khlystov, {O. M.} and Zemskaya, {T. I.} and H. Minami and A. Hachikubo and H. Shoji and M. Kida and Pogodaeva, {T. P.} and L. Naudts and J. Poort",
year = "2008",
month = oct,
day = "31",
doi = "10.1134/S0016702908100030",
language = "English",
volume = "46",
pages = "985--995",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "10",

}

RIS

TY - JOUR

T1 - Crystallization of authigenic carbonates in mud volcanoes at Lake Baikal

AU - Krylov, A. A.

AU - Khlystov, O. M.

AU - Zemskaya, T. I.

AU - Minami, H.

AU - Hachikubo, A.

AU - Shoji, H.

AU - Kida, M.

AU - Pogodaeva, T. P.

AU - Naudts, L.

AU - Poort, J.

PY - 2008/10/31

Y1 - 2008/10/31

N2 - This paper presents data on authigenic siderite first found in surface sediments from mud volcanoes in the Central (K-2) and Southern (Malen'kii) basins of Lake Baikal. Ca is the predominant cation, which substitutes Fe in the crystalline lattice of siderite. The enrichment of the carbonates in the 13C isotope (from +3.3 to +6.8‰ for the Malen'kii volcano and from +17.7 to +21.9‰ for K-2) results from the crystallization of the carbonates during methane generation via the bacterial destruction of organic matter (acetate). The overall depletion of the carbonates in 18O is mainly inherited from the isotopic composition of Baikal water.

AB - This paper presents data on authigenic siderite first found in surface sediments from mud volcanoes in the Central (K-2) and Southern (Malen'kii) basins of Lake Baikal. Ca is the predominant cation, which substitutes Fe in the crystalline lattice of siderite. The enrichment of the carbonates in the 13C isotope (from +3.3 to +6.8‰ for the Malen'kii volcano and from +17.7 to +21.9‰ for K-2) results from the crystallization of the carbonates during methane generation via the bacterial destruction of organic matter (acetate). The overall depletion of the carbonates in 18O is mainly inherited from the isotopic composition of Baikal water.

UR - http://www.scopus.com/inward/record.url?scp=54849413386&partnerID=8YFLogxK

U2 - 10.1134/S0016702908100030

DO - 10.1134/S0016702908100030

M3 - Article

AN - SCOPUS:54849413386

VL - 46

SP - 985

EP - 995

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 10

ER -

ID: 47750428