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Riftogenic magmatism of western part of the Early Mesozoic Mongolian–Transbaikalian igneous province : Results of geochronological studies. / Yarmolyuk, V. V.; Kozlovsky, A. M.; Salnikova, E. B. и др.

в: Doklady Earth Sciences, Том 475, № 2, 01.08.2017, стр. 872-876.

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

Harvard

Yarmolyuk, VV, Kozlovsky, AM, Salnikova, EB, Travin, AV & Kudryashova, EA 2017, 'Riftogenic magmatism of western part of the Early Mesozoic Mongolian–Transbaikalian igneous province: Results of geochronological studies', Doklady Earth Sciences, Том. 475, № 2, стр. 872-876. https://doi.org/10.1134/S1028334X17080293

APA

Yarmolyuk, V. V., Kozlovsky, A. M., Salnikova, E. B., Travin, A. V., & Kudryashova, E. A. (2017). Riftogenic magmatism of western part of the Early Mesozoic Mongolian–Transbaikalian igneous province: Results of geochronological studies. Doklady Earth Sciences, 475(2), 872-876. https://doi.org/10.1134/S1028334X17080293

Vancouver

Yarmolyuk VV, Kozlovsky AM, Salnikova EB, Travin AV, Kudryashova EA. Riftogenic magmatism of western part of the Early Mesozoic Mongolian–Transbaikalian igneous province: Results of geochronological studies. Doklady Earth Sciences. 2017 авг. 1;475(2):872-876. doi: 10.1134/S1028334X17080293

Author

Yarmolyuk, V. V. ; Kozlovsky, A. M. ; Salnikova, E. B. и др. / Riftogenic magmatism of western part of the Early Mesozoic Mongolian–Transbaikalian igneous province : Results of geochronological studies. в: Doklady Earth Sciences. 2017 ; Том 475, № 2. стр. 872-876.

BibTeX

@article{30b705088e044a1ebcda0651e31d4c03,
title = "Riftogenic magmatism of western part of the Early Mesozoic Mongolian–Transbaikalian igneous province: Results of geochronological studies",
abstract = "Geochronological studies of rocks from a bimodal high-alkali volcanic–plutonic complex collected in the area of Kharkhorin zone of the Early Mesozoic Mongolian–Transbaikalian igneous province (MTIP) are made. The age of alkali granites from Olziit sum is 211 ± 1 Ma (U–Pb ID-TIMS on zircon) to 209 ± 2 and 217 ± 4 Ma (40Ar/39Ar on alkali amphibole); the age of alkali granite-porphyries from the area of Sant sum is 206 ± 1 Ma (U–Pb ID-TIMS on zircon). These rock series formed syncronously to the analogous magmatism episode in the Northern Gobi and Western Transbaikalian rift zones of the MTIP. The similarity of the age and composition of igneous associations of the MTIP suggests a common mechanism of its formation related to the effect of a mantle plume on the continental lithosphere at the base of the entire igneous zone having a zonal structure.",
author = "Yarmolyuk, {V. V.} and Kozlovsky, {A. M.} and Salnikova, {E. B.} and Travin, {A. V.} and Kudryashova, {E. A.}",
year = "2017",
month = aug,
day = "1",
doi = "10.1134/S1028334X17080293",
language = "English",
volume = "475",
pages = "872--876",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Riftogenic magmatism of western part of the Early Mesozoic Mongolian–Transbaikalian igneous province

T2 - Results of geochronological studies

AU - Yarmolyuk, V. V.

AU - Kozlovsky, A. M.

AU - Salnikova, E. B.

AU - Travin, A. V.

AU - Kudryashova, E. A.

PY - 2017/8/1

Y1 - 2017/8/1

N2 - Geochronological studies of rocks from a bimodal high-alkali volcanic–plutonic complex collected in the area of Kharkhorin zone of the Early Mesozoic Mongolian–Transbaikalian igneous province (MTIP) are made. The age of alkali granites from Olziit sum is 211 ± 1 Ma (U–Pb ID-TIMS on zircon) to 209 ± 2 and 217 ± 4 Ma (40Ar/39Ar on alkali amphibole); the age of alkali granite-porphyries from the area of Sant sum is 206 ± 1 Ma (U–Pb ID-TIMS on zircon). These rock series formed syncronously to the analogous magmatism episode in the Northern Gobi and Western Transbaikalian rift zones of the MTIP. The similarity of the age and composition of igneous associations of the MTIP suggests a common mechanism of its formation related to the effect of a mantle plume on the continental lithosphere at the base of the entire igneous zone having a zonal structure.

AB - Geochronological studies of rocks from a bimodal high-alkali volcanic–plutonic complex collected in the area of Kharkhorin zone of the Early Mesozoic Mongolian–Transbaikalian igneous province (MTIP) are made. The age of alkali granites from Olziit sum is 211 ± 1 Ma (U–Pb ID-TIMS on zircon) to 209 ± 2 and 217 ± 4 Ma (40Ar/39Ar on alkali amphibole); the age of alkali granite-porphyries from the area of Sant sum is 206 ± 1 Ma (U–Pb ID-TIMS on zircon). These rock series formed syncronously to the analogous magmatism episode in the Northern Gobi and Western Transbaikalian rift zones of the MTIP. The similarity of the age and composition of igneous associations of the MTIP suggests a common mechanism of its formation related to the effect of a mantle plume on the continental lithosphere at the base of the entire igneous zone having a zonal structure.

UR - http://www.scopus.com/inward/record.url?scp=85028752130&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17080293

DO - 10.1134/S1028334X17080293

M3 - Article

AN - SCOPUS:85028752130

VL - 475

SP - 872

EP - 876

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 9915896