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Thermochronology of granitoid batholiths and their transformation into metamorphic core complexes (example of Song-Chai Massif, northern Vietnam). / Vladimirov, A. G.; Travin, A. V.; Anh, Phan Luu и др.

в: Geodynamics and Tectonophysics, Том 10, № 2, 01.01.2019, стр. 347-373.

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

Harvard

Vladimirov, AG, Travin, AV, Anh, PL, Murzintsev, NG, Annikova, IY, Mikheev, EI, Duong, NA, Man, TT & Lan, TT 2019, 'Thermochronology of granitoid batholiths and their transformation into metamorphic core complexes (example of Song-Chai Massif, northern Vietnam)', Geodynamics and Tectonophysics, Том. 10, № 2, стр. 347-373. https://doi.org/10.5800/GT-2019-10-2-0418

APA

Vladimirov, A. G., Travin, A. V., Anh, P. L., Murzintsev, N. G., Annikova, I. Y., Mikheev, E. I., Duong, N. A., Man, T. T., & Lan, T. T. (2019). Thermochronology of granitoid batholiths and their transformation into metamorphic core complexes (example of Song-Chai Massif, northern Vietnam). Geodynamics and Tectonophysics, 10(2), 347-373. https://doi.org/10.5800/GT-2019-10-2-0418

Vancouver

Vladimirov AG, Travin AV, Anh PL, Murzintsev NG, Annikova IY, Mikheev EI и др. Thermochronology of granitoid batholiths and their transformation into metamorphic core complexes (example of Song-Chai Massif, northern Vietnam). Geodynamics and Tectonophysics. 2019 янв. 1;10(2):347-373. doi: 10.5800/GT-2019-10-2-0418

Author

Vladimirov, A. G. ; Travin, A. V. ; Anh, Phan Luu и др. / Thermochronology of granitoid batholiths and their transformation into metamorphic core complexes (example of Song-Chai Massif, northern Vietnam). в: Geodynamics and Tectonophysics. 2019 ; Том 10, № 2. стр. 347-373.

BibTeX

@article{0b5eb9f1733d42c8bc26d1d421c42f91,
title = "Thermochronology of granitoid batholiths and their transformation into metamorphic core complexes (example of Song-Chai Massif, northern Vietnam)",
abstract = "Based on the reconstruction of the thermal evolution of granitoid batholith, represented by the Song-Chai gneiss-granite massif (Northern Vietnam), the long-term existence of granitoid magma at deep levels of the Earth's crust (H≥25 km, Δt~20–50 Ma) is established. The geodynamic analysis of the granitoid batholith and mathematical modeling of its thermal history shows that the magmatic chamber should be considered as a thermal trap at the lower level of the crust, which preserved residual granite melts for a long time. Activation of the magmatic chamber occurs in post-collisional strike-slip fault zones and is accompanied by tectonic exhumation of large crustal segments. As a result, the batholith is transformed into a Cordilleran-type metamorphic core complex, residual rare-metal melts are emplaced, and, commercial deposits are thus formed.",
keywords = "Geochronology, Granitoid batholith, Mathematical modeling, Metallogenic prediction, Metamorphic core complex, Song-Chai massif, Thermochronology, Vietnam, granitoid batholith, metamorphic core complex, geochronology, thermochronology, mathematical modeling, Vietnam, Song-Chai massif, metallogenic prediction, LATE PALEOZOIC GRANITOIDS, A-TYPE GRANITES, WESTERN TRANSBAIKALIA, CENOZOIC TECTONICS, MAGMATISM, CHINA, ISOTOPE, CRUSTAL, EVOLUTION, MANTLE",
author = "Vladimirov, {A. G.} and Travin, {A. V.} and Anh, {Phan Luu} and Murzintsev, {N. G.} and Annikova, {I. Yu} and Mikheev, {E. I.} and Duong, {Nguyen Anh} and Man, {Tran Thi} and Lan, {Tran Thi}",
note = "Владимиров А.Г., Травин А.В., Фан Лыу Ань, Мурзинцев Н.Г., Анникова И.Ю., Михеев Е.И., Нгуен Ань Зыонг, Чан Тхи Ман, Чан Тхи Лан. Термохронология гранитоидных батолитов и их трансформация в комплексы метаморфических ядер (на примере массива Шонгчай, Северный Вьетнам) // Геодинамика и тектонофизика. - 2019. - Т. 10/ - № 2. - С. 347-373",
year = "2019",
month = jan,
day = "1",
doi = "10.5800/GT-2019-10-2-0418",
language = "English",
volume = "10",
pages = "347--373",
journal = "Geodynamics and Tectonophysics",
issn = "2078-502X",
publisher = "Institute of the Earth's Crust",
number = "2",

}

RIS

TY - JOUR

T1 - Thermochronology of granitoid batholiths and their transformation into metamorphic core complexes (example of Song-Chai Massif, northern Vietnam)

AU - Vladimirov, A. G.

AU - Travin, A. V.

AU - Anh, Phan Luu

AU - Murzintsev, N. G.

AU - Annikova, I. Yu

AU - Mikheev, E. I.

AU - Duong, Nguyen Anh

AU - Man, Tran Thi

AU - Lan, Tran Thi

N1 - Владимиров А.Г., Травин А.В., Фан Лыу Ань, Мурзинцев Н.Г., Анникова И.Ю., Михеев Е.И., Нгуен Ань Зыонг, Чан Тхи Ман, Чан Тхи Лан. Термохронология гранитоидных батолитов и их трансформация в комплексы метаморфических ядер (на примере массива Шонгчай, Северный Вьетнам) // Геодинамика и тектонофизика. - 2019. - Т. 10/ - № 2. - С. 347-373

PY - 2019/1/1

Y1 - 2019/1/1

N2 - Based on the reconstruction of the thermal evolution of granitoid batholith, represented by the Song-Chai gneiss-granite massif (Northern Vietnam), the long-term existence of granitoid magma at deep levels of the Earth's crust (H≥25 km, Δt~20–50 Ma) is established. The geodynamic analysis of the granitoid batholith and mathematical modeling of its thermal history shows that the magmatic chamber should be considered as a thermal trap at the lower level of the crust, which preserved residual granite melts for a long time. Activation of the magmatic chamber occurs in post-collisional strike-slip fault zones and is accompanied by tectonic exhumation of large crustal segments. As a result, the batholith is transformed into a Cordilleran-type metamorphic core complex, residual rare-metal melts are emplaced, and, commercial deposits are thus formed.

AB - Based on the reconstruction of the thermal evolution of granitoid batholith, represented by the Song-Chai gneiss-granite massif (Northern Vietnam), the long-term existence of granitoid magma at deep levels of the Earth's crust (H≥25 km, Δt~20–50 Ma) is established. The geodynamic analysis of the granitoid batholith and mathematical modeling of its thermal history shows that the magmatic chamber should be considered as a thermal trap at the lower level of the crust, which preserved residual granite melts for a long time. Activation of the magmatic chamber occurs in post-collisional strike-slip fault zones and is accompanied by tectonic exhumation of large crustal segments. As a result, the batholith is transformed into a Cordilleran-type metamorphic core complex, residual rare-metal melts are emplaced, and, commercial deposits are thus formed.

KW - Geochronology

KW - Granitoid batholith

KW - Mathematical modeling

KW - Metallogenic prediction

KW - Metamorphic core complex

KW - Song-Chai massif

KW - Thermochronology

KW - Vietnam

KW - granitoid batholith

KW - metamorphic core complex

KW - geochronology

KW - thermochronology

KW - mathematical modeling

KW - Vietnam

KW - Song-Chai massif

KW - metallogenic prediction

KW - LATE PALEOZOIC GRANITOIDS

KW - A-TYPE GRANITES

KW - WESTERN TRANSBAIKALIA

KW - CENOZOIC TECTONICS

KW - MAGMATISM

KW - CHINA

KW - ISOTOPE

KW - CRUSTAL

KW - EVOLUTION

KW - MANTLE

UR - http://www.scopus.com/inward/record.url?scp=85076596356&partnerID=8YFLogxK

U2 - 10.5800/GT-2019-10-2-0418

DO - 10.5800/GT-2019-10-2-0418

M3 - Article

AN - SCOPUS:85076596356

VL - 10

SP - 347

EP - 373

JO - Geodynamics and Tectonophysics

JF - Geodynamics and Tectonophysics

SN - 2078-502X

IS - 2

ER -

ID: 22852023