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Compositions of gabbro intrusions in the Krestovsky zone (western Baikal region) : A record of plume–suprasubduction mantle interaction. / Lavrenchuk, A. V.; Sklyarov, E. V.; Izokh, A. E. et al.

In: Russian Geology and Geophysics, Vol. 58, No. 10, 01.10.2017, p. 1139-1153.

Research output: Contribution to journalArticlepeer-review

Harvard

Lavrenchuk, AV, Sklyarov, EV, Izokh, AE, Kotov, AB, Sal'nikova, EB, Fedorovsky, VS & Mazukabzov, AM 2017, 'Compositions of gabbro intrusions in the Krestovsky zone (western Baikal region): A record of plume–suprasubduction mantle interaction', Russian Geology and Geophysics, vol. 58, no. 10, pp. 1139-1153. https://doi.org/10.1016/j.rgg.2017.09.001

APA

Lavrenchuk, A. V., Sklyarov, E. V., Izokh, A. E., Kotov, A. B., Sal'nikova, E. B., Fedorovsky, V. S., & Mazukabzov, A. M. (2017). Compositions of gabbro intrusions in the Krestovsky zone (western Baikal region): A record of plume–suprasubduction mantle interaction. Russian Geology and Geophysics, 58(10), 1139-1153. https://doi.org/10.1016/j.rgg.2017.09.001

Vancouver

Lavrenchuk AV, Sklyarov EV, Izokh AE, Kotov AB, Sal'nikova EB, Fedorovsky VS et al. Compositions of gabbro intrusions in the Krestovsky zone (western Baikal region): A record of plume–suprasubduction mantle interaction. Russian Geology and Geophysics. 2017 Oct 1;58(10):1139-1153. doi: 10.1016/j.rgg.2017.09.001

Author

BibTeX

@article{0073b89b45cb41a78a2efccb4adc870c,
title = "Compositions of gabbro intrusions in the Krestovsky zone (western Baikal region): A record of plume–suprasubduction mantle interaction",
abstract = "We provide new geochemical and isotope-geochronological evidence for gabbro intrusions of the Krestovsky zone in the Olkhon composite terrane. The intrusions belong to the Birkhin (similar to 500 Ma) and Ust'-Krestovsky (similar to 470 Ma) complexes, which underwent several pulses of magmatism. Rock structures and textures record magma crystallization in tectonically turbulent conditions. The compositions of gabbro are similar to those of subduction-related basalts, but the Ust'-Krestovsky gabbro is richer in incompatible elements than the Birkhin rocks. A similar composition trend of gabbro is observed in other areas of the Central Asian Orogenic Belt (CAOB): southeastern Tuva, Gornaya Shoria, and western Mongolia. We suggest a model of regular composition changes in parental magmas during the interaction of a mantle plume with suprasubductional lithospheric mantle. (C) 2017, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.",
keywords = "mafic magmatism, isotopic age, plume-lithosphere interaction, magma source, western Baikal region, TRACE-ELEMENTS, ISOTOPIC AGE, MAGMATISM, COMPLEX, ROCKS, PB, EVOLUTION, ZIRCON",
author = "Lavrenchuk, {A. V.} and Sklyarov, {E. V.} and Izokh, {A. E.} and Kotov, {A. B.} and Sal'nikova, {E. B.} and Fedorovsky, {V. S.} and Mazukabzov, {A. M.}",
year = "2017",
month = oct,
day = "1",
doi = "10.1016/j.rgg.2017.09.001",
language = "English",
volume = "58",
pages = "1139--1153",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "10",

}

RIS

TY - JOUR

T1 - Compositions of gabbro intrusions in the Krestovsky zone (western Baikal region)

T2 - A record of plume–suprasubduction mantle interaction

AU - Lavrenchuk, A. V.

AU - Sklyarov, E. V.

AU - Izokh, A. E.

AU - Kotov, A. B.

AU - Sal'nikova, E. B.

AU - Fedorovsky, V. S.

AU - Mazukabzov, A. M.

PY - 2017/10/1

Y1 - 2017/10/1

N2 - We provide new geochemical and isotope-geochronological evidence for gabbro intrusions of the Krestovsky zone in the Olkhon composite terrane. The intrusions belong to the Birkhin (similar to 500 Ma) and Ust'-Krestovsky (similar to 470 Ma) complexes, which underwent several pulses of magmatism. Rock structures and textures record magma crystallization in tectonically turbulent conditions. The compositions of gabbro are similar to those of subduction-related basalts, but the Ust'-Krestovsky gabbro is richer in incompatible elements than the Birkhin rocks. A similar composition trend of gabbro is observed in other areas of the Central Asian Orogenic Belt (CAOB): southeastern Tuva, Gornaya Shoria, and western Mongolia. We suggest a model of regular composition changes in parental magmas during the interaction of a mantle plume with suprasubductional lithospheric mantle. (C) 2017, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.

AB - We provide new geochemical and isotope-geochronological evidence for gabbro intrusions of the Krestovsky zone in the Olkhon composite terrane. The intrusions belong to the Birkhin (similar to 500 Ma) and Ust'-Krestovsky (similar to 470 Ma) complexes, which underwent several pulses of magmatism. Rock structures and textures record magma crystallization in tectonically turbulent conditions. The compositions of gabbro are similar to those of subduction-related basalts, but the Ust'-Krestovsky gabbro is richer in incompatible elements than the Birkhin rocks. A similar composition trend of gabbro is observed in other areas of the Central Asian Orogenic Belt (CAOB): southeastern Tuva, Gornaya Shoria, and western Mongolia. We suggest a model of regular composition changes in parental magmas during the interaction of a mantle plume with suprasubductional lithospheric mantle. (C) 2017, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.

KW - mafic magmatism

KW - isotopic age

KW - plume-lithosphere interaction

KW - magma source

KW - western Baikal region

KW - TRACE-ELEMENTS

KW - ISOTOPIC AGE

KW - MAGMATISM

KW - COMPLEX

KW - ROCKS

KW - PB

KW - EVOLUTION

KW - ZIRCON

UR - http://www.scopus.com/inward/record.url?scp=85032964258&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2017.09.001

DO - 10.1016/j.rgg.2017.09.001

M3 - Article

AN - SCOPUS:85032964258

VL - 58

SP - 1139

EP - 1153

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 10

ER -

ID: 9721848