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Late Paleozoic anorogenic magmatism in Southern Mongolia : Evolutionary stages and structural control. / Yarmolyuk, V. V.; Kozlovsky, A. M.; Travin, A. V.

в: Doklady Earth Sciences, Том 475, № 1, 01.07.2017, стр. 753-757.

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

Harvard

Yarmolyuk, VV, Kozlovsky, AM & Travin, AV 2017, 'Late Paleozoic anorogenic magmatism in Southern Mongolia: Evolutionary stages and structural control', Doklady Earth Sciences, Том. 475, № 1, стр. 753-757. https://doi.org/10.1134/S1028334X17070200

APA

Yarmolyuk, V. V., Kozlovsky, A. M., & Travin, A. V. (2017). Late Paleozoic anorogenic magmatism in Southern Mongolia: Evolutionary stages and structural control. Doklady Earth Sciences, 475(1), 753-757. https://doi.org/10.1134/S1028334X17070200

Vancouver

Yarmolyuk VV, Kozlovsky AM, Travin AV. Late Paleozoic anorogenic magmatism in Southern Mongolia: Evolutionary stages and structural control. Doklady Earth Sciences. 2017 июль 1;475(1):753-757. doi: 10.1134/S1028334X17070200

Author

Yarmolyuk, V. V. ; Kozlovsky, A. M. ; Travin, A. V. / Late Paleozoic anorogenic magmatism in Southern Mongolia : Evolutionary stages and structural control. в: Doklady Earth Sciences. 2017 ; Том 475, № 1. стр. 753-757.

BibTeX

@article{3565d3d6e57c49c2aff6008d0492a6ac,
title = "Late Paleozoic anorogenic magmatism in Southern Mongolia: Evolutionary stages and structural control",
abstract = "Geochronological studies of anorogenic magmatic complexes in the South Mongolian Hercinide have been carried out. Series of the massifs composed of alkaline and subalkaline granitoids with some monzonite formed during the interval of 318–316 Ma have been found. Taking into account previously obtained data, two groups of Late Paleozoic A-type granitoids different in age have been identified in the region: Late Carboniferous and Early Permian. These two occupy different structural positions. The location the early magmatic massifs is controlled by the extended Trans–Altai fault zone of northwest strike: the massifs cluster in areas of the fault intersection with boundaries of structural blocks formed by the pull-apart mechanism. The later Early Permian igneous complexes are associated with the Gobi–Tienshan rift zone of sublatitudinal strike.",
author = "Yarmolyuk, {V. V.} and Kozlovsky, {A. M.} and Travin, {A. V.}",
year = "2017",
month = jul,
day = "1",
doi = "10.1134/S1028334X17070200",
language = "English",
volume = "475",
pages = "753--757",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - Late Paleozoic anorogenic magmatism in Southern Mongolia

T2 - Evolutionary stages and structural control

AU - Yarmolyuk, V. V.

AU - Kozlovsky, A. M.

AU - Travin, A. V.

PY - 2017/7/1

Y1 - 2017/7/1

N2 - Geochronological studies of anorogenic magmatic complexes in the South Mongolian Hercinide have been carried out. Series of the massifs composed of alkaline and subalkaline granitoids with some monzonite formed during the interval of 318–316 Ma have been found. Taking into account previously obtained data, two groups of Late Paleozoic A-type granitoids different in age have been identified in the region: Late Carboniferous and Early Permian. These two occupy different structural positions. The location the early magmatic massifs is controlled by the extended Trans–Altai fault zone of northwest strike: the massifs cluster in areas of the fault intersection with boundaries of structural blocks formed by the pull-apart mechanism. The later Early Permian igneous complexes are associated with the Gobi–Tienshan rift zone of sublatitudinal strike.

AB - Geochronological studies of anorogenic magmatic complexes in the South Mongolian Hercinide have been carried out. Series of the massifs composed of alkaline and subalkaline granitoids with some monzonite formed during the interval of 318–316 Ma have been found. Taking into account previously obtained data, two groups of Late Paleozoic A-type granitoids different in age have been identified in the region: Late Carboniferous and Early Permian. These two occupy different structural positions. The location the early magmatic massifs is controlled by the extended Trans–Altai fault zone of northwest strike: the massifs cluster in areas of the fault intersection with boundaries of structural blocks formed by the pull-apart mechanism. The later Early Permian igneous complexes are associated with the Gobi–Tienshan rift zone of sublatitudinal strike.

UR - http://www.scopus.com/inward/record.url?scp=85026768708&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17070200

DO - 10.1134/S1028334X17070200

M3 - Article

AN - SCOPUS:85026768708

VL - 475

SP - 753

EP - 757

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 10069109