Standard

Pyroxenite veins in spinel peridotites of the Unnavayam sheet, Kuyul ophiolite terrane (Koryak Upland) : Origin and setting of formation. / Ledneva, G. V.; Bazylev, B. A.; Kuzmin, D. V. et al.

In: Geochemistry International, Vol. 55, No. 4, 01.04.2017, p. 330-340.

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

Harvard

Ledneva, GV, Bazylev, BA, Kuzmin, DV & Kononkova, NN 2017, 'Pyroxenite veins in spinel peridotites of the Unnavayam sheet, Kuyul ophiolite terrane (Koryak Upland): Origin and setting of formation', Geochemistry International, vol. 55, no. 4, pp. 330-340. https://doi.org/10.1134/S0016702917020045

APA

Ledneva, G. V., Bazylev, B. A., Kuzmin, D. V., & Kononkova, N. N. (2017). Pyroxenite veins in spinel peridotites of the Unnavayam sheet, Kuyul ophiolite terrane (Koryak Upland): Origin and setting of formation. Geochemistry International, 55(4), 330-340. https://doi.org/10.1134/S0016702917020045

Vancouver

Ledneva GV, Bazylev BA, Kuzmin DV, Kononkova NN. Pyroxenite veins in spinel peridotites of the Unnavayam sheet, Kuyul ophiolite terrane (Koryak Upland): Origin and setting of formation. Geochemistry International. 2017 Apr 1;55(4):330-340. doi: 10.1134/S0016702917020045

Author

Ledneva, G. V. ; Bazylev, B. A. ; Kuzmin, D. V. et al. / Pyroxenite veins in spinel peridotites of the Unnavayam sheet, Kuyul ophiolite terrane (Koryak Upland) : Origin and setting of formation. In: Geochemistry International. 2017 ; Vol. 55, No. 4. pp. 330-340.

BibTeX

@article{0223d767da584e83acb65f944ef1b019,
title = "Pyroxenite veins in spinel peridotites of the Unnavayam sheet, Kuyul ophiolite terrane (Koryak Upland): Origin and setting of formation",
abstract = "Pyroxenite veins in mantle peridotites of the Unnavayam sheet of the Kuyul ophiolite terrane (Koryak—Kamchatka folded area) are composed of clinopyroxenite and websterite crystallized from a boninite-like melt. The host clinopyroxene-bearing spinel harzburgites are moderately depleted residues, whose mineral compositions and conditions of formation correspond to those of peridotites from mid-oceanic and back-arc spreading centers. Mantle peridotites of the Unnavayam sheet may have formed a part of the mantle wedge above a subduction zone and have been intruded by boninitic melts at a certain stage of their evolution.",
keywords = "boninites, Koryak–Kamchatka folded area, Kuyul terrane, ophiolites, pyroxenites, spinel harzburgites",
author = "Ledneva, {G. V.} and Bazylev, {B. A.} and Kuzmin, {D. V.} and Kononkova, {N. N.}",
year = "2017",
month = apr,
day = "1",
doi = "10.1134/S0016702917020045",
language = "English",
volume = "55",
pages = "330--340",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "PLEIADES PUBLISHING INC",
number = "4",

}

RIS

TY - JOUR

T1 - Pyroxenite veins in spinel peridotites of the Unnavayam sheet, Kuyul ophiolite terrane (Koryak Upland)

T2 - Origin and setting of formation

AU - Ledneva, G. V.

AU - Bazylev, B. A.

AU - Kuzmin, D. V.

AU - Kononkova, N. N.

PY - 2017/4/1

Y1 - 2017/4/1

N2 - Pyroxenite veins in mantle peridotites of the Unnavayam sheet of the Kuyul ophiolite terrane (Koryak—Kamchatka folded area) are composed of clinopyroxenite and websterite crystallized from a boninite-like melt. The host clinopyroxene-bearing spinel harzburgites are moderately depleted residues, whose mineral compositions and conditions of formation correspond to those of peridotites from mid-oceanic and back-arc spreading centers. Mantle peridotites of the Unnavayam sheet may have formed a part of the mantle wedge above a subduction zone and have been intruded by boninitic melts at a certain stage of their evolution.

AB - Pyroxenite veins in mantle peridotites of the Unnavayam sheet of the Kuyul ophiolite terrane (Koryak—Kamchatka folded area) are composed of clinopyroxenite and websterite crystallized from a boninite-like melt. The host clinopyroxene-bearing spinel harzburgites are moderately depleted residues, whose mineral compositions and conditions of formation correspond to those of peridotites from mid-oceanic and back-arc spreading centers. Mantle peridotites of the Unnavayam sheet may have formed a part of the mantle wedge above a subduction zone and have been intruded by boninitic melts at a certain stage of their evolution.

KW - boninites

KW - Koryak–Kamchatka folded area

KW - Kuyul terrane

KW - ophiolites

KW - pyroxenites

KW - spinel harzburgites

UR - http://www.scopus.com/inward/record.url?scp=85018477341&partnerID=8YFLogxK

U2 - 10.1134/S0016702917020045

DO - 10.1134/S0016702917020045

M3 - Article

AN - SCOPUS:85018477341

VL - 55

SP - 330

EP - 340

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 4

ER -

ID: 12692515