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Olivine in a Coesite-bearing Eclogite from the Udachnaya Kimberlite Pipe. / Mikhailenko, D. S.; Rezvukhin, D. I.; Korsakov, A. V. и др.

в: Doklady Earth Sciences, Том 489, № 1, 01.11.2019, стр. 1358-1362.

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

Harvard

Mikhailenko, DS, Rezvukhin, DI, Korsakov, AV & Sobolev, NV 2019, 'Olivine in a Coesite-bearing Eclogite from the Udachnaya Kimberlite Pipe', Doklady Earth Sciences, Том. 489, № 1, стр. 1358-1362. https://doi.org/10.1134/S1028334X19110242

APA

Mikhailenko, D. S., Rezvukhin, D. I., Korsakov, A. V., & Sobolev, N. V. (2019). Olivine in a Coesite-bearing Eclogite from the Udachnaya Kimberlite Pipe. Doklady Earth Sciences, 489(1), 1358-1362. https://doi.org/10.1134/S1028334X19110242

Vancouver

Mikhailenko DS, Rezvukhin DI, Korsakov AV, Sobolev NV. Olivine in a Coesite-bearing Eclogite from the Udachnaya Kimberlite Pipe. Doklady Earth Sciences. 2019 нояб. 1;489(1):1358-1362. doi: 10.1134/S1028334X19110242

Author

Mikhailenko, D. S. ; Rezvukhin, D. I. ; Korsakov, A. V. и др. / Olivine in a Coesite-bearing Eclogite from the Udachnaya Kimberlite Pipe. в: Doklady Earth Sciences. 2019 ; Том 489, № 1. стр. 1358-1362.

BibTeX

@article{c3e09bc4194e4abcbf2f0758db66a19a,
title = "Olivine in a Coesite-bearing Eclogite from the Udachnaya Kimberlite Pipe",
abstract = "Abstract: Olivine (high-Fe forsterite; Fo# 69-76) and associated minerals have been studied in a coesite-bearing diamondiferous eclogite from the Udachnaya-East kimberlite pipe. Olivine was identified in the rock interstices together with K-feldspar, sodalite, phlogopite, and djerfisherite. The composition of individual olivine grains varies within the xenolith and is characterized by a consistent presence of P2O5, MnO, CaO, and Al2O3. The coexistence of olivine and coesite is uncommon for mantle xenoliths. The occurrence of olivine and K, Na, and Сl-bearing minerals in the studied sample is suggested to have been caused by the interaction of the eclogite with a protokimberlite melt enriched in alkali components and chlorine.",
keywords = "DIAMONDS, INCLUSIONS, YAKUTIA",
author = "Mikhailenko, {D. S.} and Rezvukhin, {D. I.} and Korsakov, {A. V.} and Sobolev, {N. V.}",
year = "2019",
month = nov,
day = "1",
doi = "10.1134/S1028334X19110242",
language = "English",
volume = "489",
pages = "1358--1362",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Olivine in a Coesite-bearing Eclogite from the Udachnaya Kimberlite Pipe

AU - Mikhailenko, D. S.

AU - Rezvukhin, D. I.

AU - Korsakov, A. V.

AU - Sobolev, N. V.

PY - 2019/11/1

Y1 - 2019/11/1

N2 - Abstract: Olivine (high-Fe forsterite; Fo# 69-76) and associated minerals have been studied in a coesite-bearing diamondiferous eclogite from the Udachnaya-East kimberlite pipe. Olivine was identified in the rock interstices together with K-feldspar, sodalite, phlogopite, and djerfisherite. The composition of individual olivine grains varies within the xenolith and is characterized by a consistent presence of P2O5, MnO, CaO, and Al2O3. The coexistence of olivine and coesite is uncommon for mantle xenoliths. The occurrence of olivine and K, Na, and Сl-bearing minerals in the studied sample is suggested to have been caused by the interaction of the eclogite with a protokimberlite melt enriched in alkali components and chlorine.

AB - Abstract: Olivine (high-Fe forsterite; Fo# 69-76) and associated minerals have been studied in a coesite-bearing diamondiferous eclogite from the Udachnaya-East kimberlite pipe. Olivine was identified in the rock interstices together with K-feldspar, sodalite, phlogopite, and djerfisherite. The composition of individual olivine grains varies within the xenolith and is characterized by a consistent presence of P2O5, MnO, CaO, and Al2O3. The coexistence of olivine and coesite is uncommon for mantle xenoliths. The occurrence of olivine and K, Na, and Сl-bearing minerals in the studied sample is suggested to have been caused by the interaction of the eclogite with a protokimberlite melt enriched in alkali components and chlorine.

KW - DIAMONDS

KW - INCLUSIONS

KW - YAKUTIA

UR - http://www.scopus.com/inward/record.url?scp=85077011990&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19110242

DO - 10.1134/S1028334X19110242

M3 - Article

AN - SCOPUS:85077011990

VL - 489

SP - 1358

EP - 1362

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 23054326