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Granitoids of the Pozdnestanovoy Complex of the Dzhugdzhur–Stanovoy Superterrane, Central Asia Fold Belt : Age, Tectonic Setting, and Sources. / Larin, A. M.; Kotov, A. B.; Sal’nikova, E. B.; Kovach, V. P.; Ovchinnikova, G. V.; Savatenkov, V. M.; Velikoslavinskii, S. D.; Sorokin, A. A.; Vasil’eva, I. M.; Sergeeva, N. A.; Mel’nikov, N. N.; Wang, K. L.; Chun, S. L.

в: Petrology, Том 26, № 5, 01.09.2018, стр. 447-468.

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

Harvard

Larin, AM, Kotov, AB, Sal’nikova, EB, Kovach, VP, Ovchinnikova, GV, Savatenkov, VM, Velikoslavinskii, SD, Sorokin, AA, Vasil’eva, IM, Sergeeva, NA, Mel’nikov, NN, Wang, KL & Chun, SL 2018, 'Granitoids of the Pozdnestanovoy Complex of the Dzhugdzhur–Stanovoy Superterrane, Central Asia Fold Belt: Age, Tectonic Setting, and Sources', Petrology, Том. 26, № 5, стр. 447-468. https://doi.org/10.1134/S0869591118050041

APA

Larin, A. M., Kotov, A. B., Sal’nikova, E. B., Kovach, V. P., Ovchinnikova, G. V., Savatenkov, V. M., Velikoslavinskii, S. D., Sorokin, A. A., Vasil’eva, I. M., Sergeeva, N. A., Mel’nikov, N. N., Wang, K. L., & Chun, S. L. (2018). Granitoids of the Pozdnestanovoy Complex of the Dzhugdzhur–Stanovoy Superterrane, Central Asia Fold Belt: Age, Tectonic Setting, and Sources. Petrology, 26(5), 447-468. https://doi.org/10.1134/S0869591118050041

Vancouver

Larin AM, Kotov AB, Sal’nikova EB, Kovach VP, Ovchinnikova GV, Savatenkov VM и пр. Granitoids of the Pozdnestanovoy Complex of the Dzhugdzhur–Stanovoy Superterrane, Central Asia Fold Belt: Age, Tectonic Setting, and Sources. Petrology. 2018 Сент. 1;26(5):447-468. https://doi.org/10.1134/S0869591118050041

Author

Larin, A. M. ; Kotov, A. B. ; Sal’nikova, E. B. ; Kovach, V. P. ; Ovchinnikova, G. V. ; Savatenkov, V. M. ; Velikoslavinskii, S. D. ; Sorokin, A. A. ; Vasil’eva, I. M. ; Sergeeva, N. A. ; Mel’nikov, N. N. ; Wang, K. L. ; Chun, S. L. / Granitoids of the Pozdnestanovoy Complex of the Dzhugdzhur–Stanovoy Superterrane, Central Asia Fold Belt : Age, Tectonic Setting, and Sources. в: Petrology. 2018 ; Том 26, № 5. стр. 447-468.

BibTeX

@article{3bf4682e32154e48b5eee2bd5c1bd931,
title = "Granitoids of the Pozdnestanovoy Complex of the Dzhugdzhur–Stanovoy Superterrane, Central Asia Fold Belt: Age, Tectonic Setting, and Sources",
abstract = "The geochemistry, geochronology, and isotope geochemical systematics (Nd, Sr, Hf, and Pb) of the granitoids of the Pozdnestanovoy complex of the Dzhugdzhur–Stanovoy superterrane of the Central Asia fold belt were investigated. It was shown that their age is Mesozoic (142–138 Ma) rather than Early Precambrian, as was previously supposed. The main sources of parental melts for these granitoids were the Neoarchean and Paleoproterozoic rocks of the lower continental crust of the Dzhugdzhur–Stanovoy superterrane and the rocks of the Late Paleozoic–Early Mesozoic continental crust of the Amur microplate. They were formed at depths of >40 km and temperatures of 700–800°C, most likely through the melting of mafic feldspar granulites under the conditions of aqueous fluid infiltration without any significant contribution from a juvenile heat source. The granitoids of the Pozdnestanovoy complex were emplaced during the closure of the eastern segment of the Mongolia–Okhotsk Ocean owing to the collision of the Siberian and Sino-Korean continents.",
keywords = "adakite, Central Asia fold belt, collision, continental crust, crust formation, geochronology, geodynamic setting, granitoid, isotope geochemistry, Mongolia–Okhotsk Ocean, petrogenesis, Siberian craton, source",
author = "Larin, {A. M.} and Kotov, {A. B.} and Sal{\textquoteright}nikova, {E. B.} and Kovach, {V. P.} and Ovchinnikova, {G. V.} and Savatenkov, {V. M.} and Velikoslavinskii, {S. D.} and Sorokin, {A. A.} and Vasil{\textquoteright}eva, {I. M.} and Sergeeva, {N. A.} and Mel{\textquoteright}nikov, {N. N.} and Wang, {K. L.} and Chun, {S. L.}",
year = "2018",
month = sep,
day = "1",
doi = "10.1134/S0869591118050041",
language = "English",
volume = "26",
pages = "447--468",
journal = "Petrology",
issn = "0869-5911",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Granitoids of the Pozdnestanovoy Complex of the Dzhugdzhur–Stanovoy Superterrane, Central Asia Fold Belt

T2 - Age, Tectonic Setting, and Sources

AU - Larin, A. M.

AU - Kotov, A. B.

AU - Sal’nikova, E. B.

AU - Kovach, V. P.

AU - Ovchinnikova, G. V.

AU - Savatenkov, V. M.

AU - Velikoslavinskii, S. D.

AU - Sorokin, A. A.

AU - Vasil’eva, I. M.

AU - Sergeeva, N. A.

AU - Mel’nikov, N. N.

AU - Wang, K. L.

AU - Chun, S. L.

PY - 2018/9/1

Y1 - 2018/9/1

N2 - The geochemistry, geochronology, and isotope geochemical systematics (Nd, Sr, Hf, and Pb) of the granitoids of the Pozdnestanovoy complex of the Dzhugdzhur–Stanovoy superterrane of the Central Asia fold belt were investigated. It was shown that their age is Mesozoic (142–138 Ma) rather than Early Precambrian, as was previously supposed. The main sources of parental melts for these granitoids were the Neoarchean and Paleoproterozoic rocks of the lower continental crust of the Dzhugdzhur–Stanovoy superterrane and the rocks of the Late Paleozoic–Early Mesozoic continental crust of the Amur microplate. They were formed at depths of >40 km and temperatures of 700–800°C, most likely through the melting of mafic feldspar granulites under the conditions of aqueous fluid infiltration without any significant contribution from a juvenile heat source. The granitoids of the Pozdnestanovoy complex were emplaced during the closure of the eastern segment of the Mongolia–Okhotsk Ocean owing to the collision of the Siberian and Sino-Korean continents.

AB - The geochemistry, geochronology, and isotope geochemical systematics (Nd, Sr, Hf, and Pb) of the granitoids of the Pozdnestanovoy complex of the Dzhugdzhur–Stanovoy superterrane of the Central Asia fold belt were investigated. It was shown that their age is Mesozoic (142–138 Ma) rather than Early Precambrian, as was previously supposed. The main sources of parental melts for these granitoids were the Neoarchean and Paleoproterozoic rocks of the lower continental crust of the Dzhugdzhur–Stanovoy superterrane and the rocks of the Late Paleozoic–Early Mesozoic continental crust of the Amur microplate. They were formed at depths of >40 km and temperatures of 700–800°C, most likely through the melting of mafic feldspar granulites under the conditions of aqueous fluid infiltration without any significant contribution from a juvenile heat source. The granitoids of the Pozdnestanovoy complex were emplaced during the closure of the eastern segment of the Mongolia–Okhotsk Ocean owing to the collision of the Siberian and Sino-Korean continents.

KW - adakite

KW - Central Asia fold belt

KW - collision

KW - continental crust

KW - crust formation

KW - geochronology

KW - geodynamic setting

KW - granitoid

KW - isotope geochemistry

KW - Mongolia–Okhotsk Ocean

KW - petrogenesis

KW - Siberian craton

KW - source

UR - http://www.scopus.com/inward/record.url?scp=85053829860&partnerID=8YFLogxK

U2 - 10.1134/S0869591118050041

DO - 10.1134/S0869591118050041

M3 - Article

AN - SCOPUS:85053829860

VL - 26

SP - 447

EP - 468

JO - Petrology

JF - Petrology

SN - 0869-5911

IS - 5

ER -

ID: 52349651