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PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia). / Ilyina, O. V.; Tychkov, N. S.; Agashev, A. M. et al.

In: Doklady Earth Sciences, Vol. 467, No. 2, 01.04.2016, p. 408-411.

Research output: Contribution to journal › Article › peer-review

Harvard

Ilyina, OV, Tychkov, NS, Agashev, AM, Golovin, AV, Izokh, AE, Kozmenko, OA & Pokhilenko, NP 2016, 'PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia)', Doklady Earth Sciences, vol. 467, no. 2, pp. 408-411. https://doi.org/10.1134/S1028334X16040176

APA

Ilyina, O. V., Tychkov, N. S., Agashev, A. M., Golovin, A. V., Izokh, A. E., Kozmenko, O. A., & Pokhilenko, N. P. (2016). PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia). Doklady Earth Sciences, 467(2), 408-411. https://doi.org/10.1134/S1028334X16040176

Vancouver

Ilyina OV, Tychkov NS, Agashev AM, Golovin AV, Izokh AE, Kozmenko OA et al. PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia). Doklady Earth Sciences. 2016 Apr 1;467(2):408-411. doi: 10.1134/S1028334X16040176

Author

Ilyina, O. V. ; Tychkov, N. S. ; Agashev, A. M. et al. / PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia). In: Doklady Earth Sciences. 2016 ; Vol. 467, No. 2. pp. 408-411.

BibTeX

@article{4f2771c9af4f456392dfef24eb765f4b,
title = "PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia)",
abstract = "The results of the first study of the PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia) are presented here. The complex character of evolution of the PGE composition in the Deformed lherzolites is assumed to be the result of silicate metasomatism. At the first stage, growth in the amount of clinopyroxene and garnet in the rock is accompanied by a decrease in the concentration of the compatible PGE (Os, Ir). During the final stage, the rock is enriched with incompatible PGE (Pt, Pd) and Re possible due to precipitation of submicron-sized particles of sulfides in the interstitial space of these mantle rocks.",
author = "Ilyina, {O. V.} and Tychkov, {N. S.} and Agashev, {A. M.} and Golovin, {A. V.} and Izokh, {A. E.} and Kozmenko, {O. A.} and Pokhilenko, {N. P.}",
year = "2016",
month = apr,
day = "1",
doi = "10.1134/S1028334X16040176",
language = "English",
volume = "467",
pages = "408--411",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia)

AU - Ilyina, O. V.

AU - Tychkov, N. S.

AU - Agashev, A. M.

AU - Golovin, A. V.

AU - Izokh, A. E.

AU - Kozmenko, O. A.

AU - Pokhilenko, N. P.

PY - 2016/4/1

Y1 - 2016/4/1

N2 - The results of the first study of the PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia) are presented here. The complex character of evolution of the PGE composition in the Deformed lherzolites is assumed to be the result of silicate metasomatism. At the first stage, growth in the amount of clinopyroxene and garnet in the rock is accompanied by a decrease in the concentration of the compatible PGE (Os, Ir). During the final stage, the rock is enriched with incompatible PGE (Pt, Pd) and Re possible due to precipitation of submicron-sized particles of sulfides in the interstitial space of these mantle rocks.

AB - The results of the first study of the PGE distribution in deformed lherzolites of the Udachnaya kimberlite pipe (Yakutia) are presented here. The complex character of evolution of the PGE composition in the Deformed lherzolites is assumed to be the result of silicate metasomatism. At the first stage, growth in the amount of clinopyroxene and garnet in the rock is accompanied by a decrease in the concentration of the compatible PGE (Os, Ir). During the final stage, the rock is enriched with incompatible PGE (Pt, Pd) and Re possible due to precipitation of submicron-sized particles of sulfides in the interstitial space of these mantle rocks.

UR - http://www.scopus.com/inward/record.url?scp=84971254484&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16040176

DO - 10.1134/S1028334X16040176

M3 - Article

AN - SCOPUS:84971254484

VL - 467

SP - 408

EP - 411

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25488988