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Isotope compositions of C and O of magmatic calcites from the Udachnaya–East pipe kimberlite, Yakutia. / Tomilenko, A. A.; Dublyansky, Yu V.; Kuzmin, D. V. и др.

в: Doklady Earth Sciences, Том 475, № 1, 01.07.2017, стр. 828-831.

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

Harvard

Tomilenko, AA, Dublyansky, YV, Kuzmin, DV & Sobolev, NV 2017, 'Isotope compositions of C and O of magmatic calcites from the Udachnaya–East pipe kimberlite, Yakutia', Doklady Earth Sciences, Том. 475, № 1, стр. 828-831. https://doi.org/10.1134/S1028334X17070297

APA

Tomilenko, A. A., Dublyansky, Y. V., Kuzmin, D. V., & Sobolev, N. V. (2017). Isotope compositions of C and O of magmatic calcites from the Udachnaya–East pipe kimberlite, Yakutia. Doklady Earth Sciences, 475(1), 828-831. https://doi.org/10.1134/S1028334X17070297

Vancouver

Tomilenko AA, Dublyansky YV, Kuzmin DV, Sobolev NV. Isotope compositions of C and O of magmatic calcites from the Udachnaya–East pipe kimberlite, Yakutia. Doklady Earth Sciences. 2017 июль 1;475(1):828-831. doi: 10.1134/S1028334X17070297

Author

Tomilenko, A. A. ; Dublyansky, Yu V. ; Kuzmin, D. V. и др. / Isotope compositions of C and O of magmatic calcites from the Udachnaya–East pipe kimberlite, Yakutia. в: Doklady Earth Sciences. 2017 ; Том 475, № 1. стр. 828-831.

BibTeX

@article{25524fd2706041ba95dc305c0208013e,
title = "Isotope compositions of C and O of magmatic calcites from the Udachnaya–East pipe kimberlite, Yakutia",
abstract = "It has been demonstrated for the first time that the isotopic compositions of carbon (δ13C) in magmatic calcites from the Udachnaya–East pipe kimberlite groundmass varies from–2.5 to–1.0‰ (V-PDB), while those of oxygen (δ18O) range from 15.0 to 18.2‰ (V-SMOW). The obtained results imply that during the terminal late magmatic and postmagmatic stages of the kimberlite pipe formation, the carbonates in the kimberlite groundmass became successively heavier isotopically, which indicates the hybrid nature of the carbonate component of the kimberlite: it was formed with contributions from mantle and sedimentary marine sources.",
keywords = "NORTHWEST-TERRITORIES, HYPABYSSAL KIMBERLITE, CANADA, CARBONATES, MINERALS, BEARING, GRAS",
author = "Tomilenko, {A. A.} and Dublyansky, {Yu V.} and Kuzmin, {D. V.} and Sobolev, {N. V.}",
year = "2017",
month = jul,
day = "1",
doi = "10.1134/S1028334X17070297",
language = "English",
volume = "475",
pages = "828--831",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Isotope compositions of C and O of magmatic calcites from the Udachnaya–East pipe kimberlite, Yakutia

AU - Tomilenko, A. A.

AU - Dublyansky, Yu V.

AU - Kuzmin, D. V.

AU - Sobolev, N. V.

PY - 2017/7/1

Y1 - 2017/7/1

N2 - It has been demonstrated for the first time that the isotopic compositions of carbon (δ13C) in magmatic calcites from the Udachnaya–East pipe kimberlite groundmass varies from–2.5 to–1.0‰ (V-PDB), while those of oxygen (δ18O) range from 15.0 to 18.2‰ (V-SMOW). The obtained results imply that during the terminal late magmatic and postmagmatic stages of the kimberlite pipe formation, the carbonates in the kimberlite groundmass became successively heavier isotopically, which indicates the hybrid nature of the carbonate component of the kimberlite: it was formed with contributions from mantle and sedimentary marine sources.

AB - It has been demonstrated for the first time that the isotopic compositions of carbon (δ13C) in magmatic calcites from the Udachnaya–East pipe kimberlite groundmass varies from–2.5 to–1.0‰ (V-PDB), while those of oxygen (δ18O) range from 15.0 to 18.2‰ (V-SMOW). The obtained results imply that during the terminal late magmatic and postmagmatic stages of the kimberlite pipe formation, the carbonates in the kimberlite groundmass became successively heavier isotopically, which indicates the hybrid nature of the carbonate component of the kimberlite: it was formed with contributions from mantle and sedimentary marine sources.

KW - NORTHWEST-TERRITORIES

KW - HYPABYSSAL KIMBERLITE

KW - CANADA

KW - CARBONATES

KW - MINERALS

KW - BEARING

KW - GRAS

UR - http://www.scopus.com/inward/record.url?scp=85026751875&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17070297

DO - 10.1134/S1028334X17070297

M3 - Article

AN - SCOPUS:85026751875

VL - 475

SP - 828

EP - 831

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 10069143