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Birkhin Volcanoplutonic Association, Ol’khon Region, Western Baikal Area : Petrological Criteria of Comagmatic Origin. / Lavrenchuk, A. V.; Sklyarov, E. V.; Izokh, A. E. et al.

In: Petrology, Vol. 27, No. 3, 01.05.2019, p. 291-306.

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

Harvard

Lavrenchuk, AV, Sklyarov, EV, Izokh, AE, Kotov, AB, Vasyukova, EA, Fedorovskii, VS, Gladkochub, DP, Donskaya, TV & Mazukabzov, AM 2019, 'Birkhin Volcanoplutonic Association, Ol’khon Region, Western Baikal Area: Petrological Criteria of Comagmatic Origin', Petrology, vol. 27, no. 3, pp. 291-306. https://doi.org/10.1134/S0869591119030044

APA

Lavrenchuk, A. V., Sklyarov, E. V., Izokh, A. E., Kotov, A. B., Vasyukova, E. A., Fedorovskii, V. S., Gladkochub, D. P., Donskaya, T. V., & Mazukabzov, A. M. (2019). Birkhin Volcanoplutonic Association, Ol’khon Region, Western Baikal Area: Petrological Criteria of Comagmatic Origin. Petrology, 27(3), 291-306. https://doi.org/10.1134/S0869591119030044

Vancouver

Lavrenchuk AV, Sklyarov EV, Izokh AE, Kotov AB, Vasyukova EA, Fedorovskii VS et al. Birkhin Volcanoplutonic Association, Ol’khon Region, Western Baikal Area: Petrological Criteria of Comagmatic Origin. Petrology. 2019 May 1;27(3):291-306. doi: 10.1134/S0869591119030044

Author

Lavrenchuk, A. V. ; Sklyarov, E. V. ; Izokh, A. E. et al. / Birkhin Volcanoplutonic Association, Ol’khon Region, Western Baikal Area : Petrological Criteria of Comagmatic Origin. In: Petrology. 2019 ; Vol. 27, No. 3. pp. 291-306.

BibTeX

@article{0895d16b928d48caba8196b54e8c3d37,
title = "Birkhin Volcanoplutonic Association, Ol{\textquoteright}khon Region, Western Baikal Area: Petrological Criteria of Comagmatic Origin",
abstract = "Abstract: This paper reports the results of thermodynamic modeling of the formation of the Birkhin volcanoplutonic association by means of geochemical thermometry. The obtained liquid line of descent for the magma chamber of the Birkhin Massif indicates that the melt evolved into the field of subalkaline composition. The melts of the volcanics of the Tsagan-Zaba complex are identical to the melts in the magma chamber in both major components and REEs. It was concluded that the Birkhin and Tsagan-Zaba complexes are comagmatic. A scenario was proposed for the development of the Birkhin volcanoplutonic association involving multiple eruptions of volcanic rocks during its formation. It was shown that the intermediate rocks are not derivatives of basic magmas, but were produced by interaction of basic volcanic rocks with felsic intrusions cutting them.",
keywords = "basic magmatism, geochemical thermometry, thermodynamic modeling, Western Baikal area, CRYSTALLIZATION, PETROGENESIS, TERRANE, ROCKS, COMPLEXES, GEOCHEMISTRY",
author = "Lavrenchuk, {A. V.} and Sklyarov, {E. V.} and Izokh, {A. E.} and Kotov, {A. B.} and Vasyukova, {E. A.} and Fedorovskii, {V. S.} and Gladkochub, {D. P.} and Donskaya, {T. V.} and Mazukabzov, {A. M.}",
year = "2019",
month = may,
day = "1",
doi = "10.1134/S0869591119030044",
language = "English",
volume = "27",
pages = "291--306",
journal = "Petrology",
issn = "0869-5911",
publisher = "Springer Science + Business Media",
number = "3",

}

RIS

TY - JOUR

T1 - Birkhin Volcanoplutonic Association, Ol’khon Region, Western Baikal Area

T2 - Petrological Criteria of Comagmatic Origin

AU - Lavrenchuk, A. V.

AU - Sklyarov, E. V.

AU - Izokh, A. E.

AU - Kotov, A. B.

AU - Vasyukova, E. A.

AU - Fedorovskii, V. S.

AU - Gladkochub, D. P.

AU - Donskaya, T. V.

AU - Mazukabzov, A. M.

PY - 2019/5/1

Y1 - 2019/5/1

N2 - Abstract: This paper reports the results of thermodynamic modeling of the formation of the Birkhin volcanoplutonic association by means of geochemical thermometry. The obtained liquid line of descent for the magma chamber of the Birkhin Massif indicates that the melt evolved into the field of subalkaline composition. The melts of the volcanics of the Tsagan-Zaba complex are identical to the melts in the magma chamber in both major components and REEs. It was concluded that the Birkhin and Tsagan-Zaba complexes are comagmatic. A scenario was proposed for the development of the Birkhin volcanoplutonic association involving multiple eruptions of volcanic rocks during its formation. It was shown that the intermediate rocks are not derivatives of basic magmas, but were produced by interaction of basic volcanic rocks with felsic intrusions cutting them.

AB - Abstract: This paper reports the results of thermodynamic modeling of the formation of the Birkhin volcanoplutonic association by means of geochemical thermometry. The obtained liquid line of descent for the magma chamber of the Birkhin Massif indicates that the melt evolved into the field of subalkaline composition. The melts of the volcanics of the Tsagan-Zaba complex are identical to the melts in the magma chamber in both major components and REEs. It was concluded that the Birkhin and Tsagan-Zaba complexes are comagmatic. A scenario was proposed for the development of the Birkhin volcanoplutonic association involving multiple eruptions of volcanic rocks during its formation. It was shown that the intermediate rocks are not derivatives of basic magmas, but were produced by interaction of basic volcanic rocks with felsic intrusions cutting them.

KW - basic magmatism

KW - geochemical thermometry

KW - thermodynamic modeling

KW - Western Baikal area

KW - CRYSTALLIZATION

KW - PETROGENESIS

KW - TERRANE

KW - ROCKS

KW - COMPLEXES

KW - GEOCHEMISTRY

UR - http://www.scopus.com/inward/record.url?scp=85067071307&partnerID=8YFLogxK

U2 - 10.1134/S0869591119030044

DO - 10.1134/S0869591119030044

M3 - Article

AN - SCOPUS:85067071307

VL - 27

SP - 291

EP - 306

JO - Petrology

JF - Petrology

SN - 0869-5911

IS - 3

ER -

ID: 20587062