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Paragenesis and complex zoning of olivine macrocrysts from unaltered kimberlite of the Udachnaya-East pipe, Yakutia : Relationship with the kimberlite formation conditions and evolution. / Sobolev, N. V.; Sobolev, A. V.; Tomilenko, A. A. et al.

In: Russian Geology and Geophysics, Vol. 56, No. 1-2, 01.01.2015, p. 260-279.

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

Harvard

Sobolev, NV, Sobolev, AV, Tomilenko, AA, Kovyazin, SV, Batanova, VG & Kuz'min, DV 2015, 'Paragenesis and complex zoning of olivine macrocrysts from unaltered kimberlite of the Udachnaya-East pipe, Yakutia: Relationship with the kimberlite formation conditions and evolution', Russian Geology and Geophysics, vol. 56, no. 1-2, pp. 260-279. https://doi.org/10.1016/j.rgg.2015.01.019

APA

Sobolev, N. V., Sobolev, A. V., Tomilenko, A. A., Kovyazin, S. V., Batanova, V. G., & Kuz'min, D. V. (2015). Paragenesis and complex zoning of olivine macrocrysts from unaltered kimberlite of the Udachnaya-East pipe, Yakutia: Relationship with the kimberlite formation conditions and evolution. Russian Geology and Geophysics, 56(1-2), 260-279. https://doi.org/10.1016/j.rgg.2015.01.019

Vancouver

Sobolev NV, Sobolev AV, Tomilenko AA, Kovyazin SV, Batanova VG, Kuz'min DV. Paragenesis and complex zoning of olivine macrocrysts from unaltered kimberlite of the Udachnaya-East pipe, Yakutia: Relationship with the kimberlite formation conditions and evolution. Russian Geology and Geophysics. 2015 Jan 1;56(1-2):260-279. doi: 10.1016/j.rgg.2015.01.019

Author

Sobolev, N. V. ; Sobolev, A. V. ; Tomilenko, A. A. et al. / Paragenesis and complex zoning of olivine macrocrysts from unaltered kimberlite of the Udachnaya-East pipe, Yakutia : Relationship with the kimberlite formation conditions and evolution. In: Russian Geology and Geophysics. 2015 ; Vol. 56, No. 1-2. pp. 260-279.

BibTeX

@article{e9ab9b6ccdb844139301ad2e44303e94,
title = "Paragenesis and complex zoning of olivine macrocrysts from unaltered kimberlite of the Udachnaya-East pipe, Yakutia: Relationship with the kimberlite formation conditions and evolution",
abstract = "Unaltered Mg-olivine (Fo=85-94) is a predominant mineral of the kimberlite block (serpentine-free) of the Udachnaya-East pipe, and it prevails in peridotite xenoliths and as inclusions in diamonds. The kimberlite of this pipe, like a series of hypabyssal kimberlites in other regions, contains two main types of olivine macrocrysts according to their size and morphology: those rounded or irregularly shaped (olivine I) and euhedral phenocrysts (olivine II), which are usually no larger than 0.5mm and very seldom reach 1mm in size. This study was focused on several thousand olivine samples assigned both to olivines I and to olivines II, with a gradual transition between them. Particular attention was paid to the search for mineral inclusions in olivine and for phenocrysts with a clear zoning. In the phenocryst cores of homogeneous composition, we have revealed orthopyroxene inclusions as well as clinopyroxene (chrome-diopside and chrome-omphacite) inclusions with wide variations in the Na2O and Cr2O3 contents, significantly higher than the previously established ones: up to 6.00wt.% Na2O and 4.23wt.% Cr2O3. Convincing evidence for the high-pressure origin of the olivine macrocryst cores is the presence of pyrope inclusions with 1.41-9.14wt.% &2O3, 4.64-6.61wt.% CaO, and Mg#=75.6-83.7 in six samples, which testifies to the high-pressure lherzolite paragenesis of the phenocrysts cores. The cores of the studied olivine phenocrysts are identical in the contents of Ni, Co, Ca, Cr, and Mn to olivines from diamonds and peridotite xenoliths. However, they differ significantly in the steady elevated Ti content, equal to 100-300ppm for the majority of the phenocrysts, including those containing pyroxene and pyrope inclusions.",
keywords = "Clinopyroxene, Diamond, Kimberlite, Olivine, Paragenesis, Pyrope, Trace elements",
author = "Sobolev, {N. V.} and Sobolev, {A. V.} and Tomilenko, {A. A.} and Kovyazin, {S. V.} and Batanova, {V. G.} and Kuz'min, {D. V.}",
year = "2015",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2015.01.019",
language = "English",
volume = "56",
pages = "260--279",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1-2",

}

RIS

TY - JOUR

T1 - Paragenesis and complex zoning of olivine macrocrysts from unaltered kimberlite of the Udachnaya-East pipe, Yakutia

T2 - Relationship with the kimberlite formation conditions and evolution

AU - Sobolev, N. V.

AU - Sobolev, A. V.

AU - Tomilenko, A. A.

AU - Kovyazin, S. V.

AU - Batanova, V. G.

AU - Kuz'min, D. V.

PY - 2015/1/1

Y1 - 2015/1/1

N2 - Unaltered Mg-olivine (Fo=85-94) is a predominant mineral of the kimberlite block (serpentine-free) of the Udachnaya-East pipe, and it prevails in peridotite xenoliths and as inclusions in diamonds. The kimberlite of this pipe, like a series of hypabyssal kimberlites in other regions, contains two main types of olivine macrocrysts according to their size and morphology: those rounded or irregularly shaped (olivine I) and euhedral phenocrysts (olivine II), which are usually no larger than 0.5mm and very seldom reach 1mm in size. This study was focused on several thousand olivine samples assigned both to olivines I and to olivines II, with a gradual transition between them. Particular attention was paid to the search for mineral inclusions in olivine and for phenocrysts with a clear zoning. In the phenocryst cores of homogeneous composition, we have revealed orthopyroxene inclusions as well as clinopyroxene (chrome-diopside and chrome-omphacite) inclusions with wide variations in the Na2O and Cr2O3 contents, significantly higher than the previously established ones: up to 6.00wt.% Na2O and 4.23wt.% Cr2O3. Convincing evidence for the high-pressure origin of the olivine macrocryst cores is the presence of pyrope inclusions with 1.41-9.14wt.% &2O3, 4.64-6.61wt.% CaO, and Mg#=75.6-83.7 in six samples, which testifies to the high-pressure lherzolite paragenesis of the phenocrysts cores. The cores of the studied olivine phenocrysts are identical in the contents of Ni, Co, Ca, Cr, and Mn to olivines from diamonds and peridotite xenoliths. However, they differ significantly in the steady elevated Ti content, equal to 100-300ppm for the majority of the phenocrysts, including those containing pyroxene and pyrope inclusions.

AB - Unaltered Mg-olivine (Fo=85-94) is a predominant mineral of the kimberlite block (serpentine-free) of the Udachnaya-East pipe, and it prevails in peridotite xenoliths and as inclusions in diamonds. The kimberlite of this pipe, like a series of hypabyssal kimberlites in other regions, contains two main types of olivine macrocrysts according to their size and morphology: those rounded or irregularly shaped (olivine I) and euhedral phenocrysts (olivine II), which are usually no larger than 0.5mm and very seldom reach 1mm in size. This study was focused on several thousand olivine samples assigned both to olivines I and to olivines II, with a gradual transition between them. Particular attention was paid to the search for mineral inclusions in olivine and for phenocrysts with a clear zoning. In the phenocryst cores of homogeneous composition, we have revealed orthopyroxene inclusions as well as clinopyroxene (chrome-diopside and chrome-omphacite) inclusions with wide variations in the Na2O and Cr2O3 contents, significantly higher than the previously established ones: up to 6.00wt.% Na2O and 4.23wt.% Cr2O3. Convincing evidence for the high-pressure origin of the olivine macrocryst cores is the presence of pyrope inclusions with 1.41-9.14wt.% &2O3, 4.64-6.61wt.% CaO, and Mg#=75.6-83.7 in six samples, which testifies to the high-pressure lherzolite paragenesis of the phenocrysts cores. The cores of the studied olivine phenocrysts are identical in the contents of Ni, Co, Ca, Cr, and Mn to olivines from diamonds and peridotite xenoliths. However, they differ significantly in the steady elevated Ti content, equal to 100-300ppm for the majority of the phenocrysts, including those containing pyroxene and pyrope inclusions.

KW - Clinopyroxene

KW - Diamond

KW - Kimberlite

KW - Olivine

KW - Paragenesis

KW - Pyrope

KW - Trace elements

UR - http://www.scopus.com/inward/record.url?scp=84925305849&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2015.01.019

DO - 10.1016/j.rgg.2015.01.019

M3 - Article

AN - SCOPUS:84925305849

VL - 56

SP - 260

EP - 279

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1-2

ER -

ID: 25763909