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The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean. / Yarmolyuk, V. V.; Kozakov, I. K.; Kozlovsky, A. M. и др.

в: Doklady Earth Sciences, Том 480, № 1, 01.05.2018, стр. 559-563.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Yarmolyuk, VV, Kozakov, IK, Kozlovsky, AM, Kudryashova, EA, Travin, AV, Kirnozova, TI, Fugzan, MM & Plotkina, YV 2018, 'The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean', Doklady Earth Sciences, Том. 480, № 1, стр. 559-563. https://doi.org/10.1134/S1028334X18050094

APA

Yarmolyuk, V. V., Kozakov, I. K., Kozlovsky, A. M., Kudryashova, E. A., Travin, A. V., Kirnozova, T. I., Fugzan, M. M., & Plotkina, Y. V. (2018). The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean. Doklady Earth Sciences, 480(1), 559-563. https://doi.org/10.1134/S1028334X18050094

Vancouver

Yarmolyuk VV, Kozakov IK, Kozlovsky AM, Kudryashova EA, Travin AV, Kirnozova TI и др. The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean. Doklady Earth Sciences. 2018 май 1;480(1):559-563. doi: 10.1134/S1028334X18050094

Author

Yarmolyuk, V. V. ; Kozakov, I. K. ; Kozlovsky, A. M. и др. / The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean. в: Doklady Earth Sciences. 2018 ; Том 480, № 1. стр. 559-563.

BibTeX

@article{c970092284c0459088e43f48a96a3148,
title = "The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean",
abstract = "Within the northern fringe of the western (Khangai) flank of the Mongol–Okhotsk fold belt, magmatic complexes of intermediate to moderately acidic rocks occur. They comprise widely distributed gabbro–diorites, diorites, tonalites, and granodiorites. Geochronological studies have demonstrated that these rocks were formed in the time span of 437 to 375 Ma. The geochemical affinities of the rocks suggest their formation in subduction tectonic settings; hence, their paleotectonic position corresponds to the continental margin of the Mongol–Okhotsk paleoocean. It has been concluded that this Middle Paleozoic igneous activity occurred in the active continental margin settings, formed by subduction of the paleooceanic plate under the Siberian continent.",
author = "Yarmolyuk, {V. V.} and Kozakov, {I. K.} and Kozlovsky, {A. M.} and Kudryashova, {E. A.} and Travin, {A. V.} and Kirnozova, {T. I.} and Fugzan, {M. M.} and Plotkina, {Yu V.}",
year = "2018",
month = may,
day = "1",
doi = "10.1134/S1028334X18050094",
language = "English",
volume = "480",
pages = "559--563",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean

AU - Yarmolyuk, V. V.

AU - Kozakov, I. K.

AU - Kozlovsky, A. M.

AU - Kudryashova, E. A.

AU - Travin, A. V.

AU - Kirnozova, T. I.

AU - Fugzan, M. M.

AU - Plotkina, Yu V.

PY - 2018/5/1

Y1 - 2018/5/1

N2 - Within the northern fringe of the western (Khangai) flank of the Mongol–Okhotsk fold belt, magmatic complexes of intermediate to moderately acidic rocks occur. They comprise widely distributed gabbro–diorites, diorites, tonalites, and granodiorites. Geochronological studies have demonstrated that these rocks were formed in the time span of 437 to 375 Ma. The geochemical affinities of the rocks suggest their formation in subduction tectonic settings; hence, their paleotectonic position corresponds to the continental margin of the Mongol–Okhotsk paleoocean. It has been concluded that this Middle Paleozoic igneous activity occurred in the active continental margin settings, formed by subduction of the paleooceanic plate under the Siberian continent.

AB - Within the northern fringe of the western (Khangai) flank of the Mongol–Okhotsk fold belt, magmatic complexes of intermediate to moderately acidic rocks occur. They comprise widely distributed gabbro–diorites, diorites, tonalites, and granodiorites. Geochronological studies have demonstrated that these rocks were formed in the time span of 437 to 375 Ma. The geochemical affinities of the rocks suggest their formation in subduction tectonic settings; hence, their paleotectonic position corresponds to the continental margin of the Mongol–Okhotsk paleoocean. It has been concluded that this Middle Paleozoic igneous activity occurred in the active continental margin settings, formed by subduction of the paleooceanic plate under the Siberian continent.

UR - http://www.scopus.com/inward/record.url?scp=85048474261&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18050094

DO - 10.1134/S1028334X18050094

M3 - Article

AN - SCOPUS:85048474261

VL - 480

SP - 559

EP - 563

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 14047741