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Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia) : Petrogeochemical features of magmatism and ore-forming processes. / Kovalev, K. R.; Kalinin, Yu A.; Turkina, O. M. и др.

в: Russian Geology and Geophysics, Том 60, № 6, 06.2019, стр. 583-601.

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

Harvard

Kovalev, KR, Kalinin, YA, Turkina, OM, Gimon, VO & Abramov, BN 2019, 'Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia): Petrogeochemical features of magmatism and ore-forming processes', Russian Geology and Geophysics, Том. 60, № 6, стр. 583-601. https://doi.org/10.15372/RGG2019078

APA

Kovalev, K. R., Kalinin, Y. A., Turkina, O. M., Gimon, V. O., & Abramov, B. N. (2019). Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia): Petrogeochemical features of magmatism and ore-forming processes. Russian Geology and Geophysics, 60(6), 583-601. https://doi.org/10.15372/RGG2019078

Vancouver

Kovalev KR, Kalinin YA, Turkina OM, Gimon VO, Abramov BN. Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia): Petrogeochemical features of magmatism and ore-forming processes. Russian Geology and Geophysics. 2019 июнь;60(6):583-601. doi: 10.15372/RGG2019078

Author

Kovalev, K. R. ; Kalinin, Yu A. ; Turkina, O. M. и др. / Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia) : Petrogeochemical features of magmatism and ore-forming processes. в: Russian Geology and Geophysics. 2019 ; Том 60, № 6. стр. 583-601.

BibTeX

@article{e1bee927fe9c4d26ae64802578e1a2a9,
title = "Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia): Petrogeochemical features of magmatism and ore-forming processes",
abstract = "The Kultuminskoe deposit is located within the Gazimur metallogenic zone in eastern Transbaikalia. Mineralization is associated with the Middle–Upper Jurassic Kultuma pluton composed of subalkaline rock series ranging from quartz monzonites and quartz syenites to granites and of monzodiorite dikes. Dikes of Late Jurassic age are composed of subalkaline gabbro. Analysis of fractionation trends of major and trace elements suggests that the monzonitoids prevailed in the Kultuma pluton and the dike complex formed through the differentiation of subalkaline basaltic melt from an enriched mantle source. The formation of the gold–copper–iron–skarn and medium-temperature veinlet-disseminated polysulfide and epithermal Ag–Te–Bi mineralization as well as iron–magnesia and silica–alkaline metasomatites was a long multistage process during the general evolution of the ore-magmatic system.",
keywords = "Au–Cu–Fe skarns, Eastern Transbaikalia, Kultuminskoe deposit, Magmatism, Petrogeochemistry, Polysulfide and epithermal Ag–Te–Bi mineralization",
author = "Kovalev, {K. R.} and Kalinin, {Yu A.} and Turkina, {O. M.} and Gimon, {V. O.} and Abramov, {B. N.}",
note = "Publisher Copyright: {\textcopyright} 2019, V.S. Sobolev IGM, Siberian Branch of the RAS. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.",
year = "2019",
month = jun,
doi = "10.15372/RGG2019078",
language = "English",
volume = "60",
pages = "583--601",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "6",

}

RIS

TY - JOUR

T1 - Kultuminskoe gold–copper–iron–skarn deposit (Eastern Transbaikalia, Russia)

T2 - Petrogeochemical features of magmatism and ore-forming processes

AU - Kovalev, K. R.

AU - Kalinin, Yu A.

AU - Turkina, O. M.

AU - Gimon, V. O.

AU - Abramov, B. N.

N1 - Publisher Copyright: © 2019, V.S. Sobolev IGM, Siberian Branch of the RAS. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.

PY - 2019/6

Y1 - 2019/6

N2 - The Kultuminskoe deposit is located within the Gazimur metallogenic zone in eastern Transbaikalia. Mineralization is associated with the Middle–Upper Jurassic Kultuma pluton composed of subalkaline rock series ranging from quartz monzonites and quartz syenites to granites and of monzodiorite dikes. Dikes of Late Jurassic age are composed of subalkaline gabbro. Analysis of fractionation trends of major and trace elements suggests that the monzonitoids prevailed in the Kultuma pluton and the dike complex formed through the differentiation of subalkaline basaltic melt from an enriched mantle source. The formation of the gold–copper–iron–skarn and medium-temperature veinlet-disseminated polysulfide and epithermal Ag–Te–Bi mineralization as well as iron–magnesia and silica–alkaline metasomatites was a long multistage process during the general evolution of the ore-magmatic system.

AB - The Kultuminskoe deposit is located within the Gazimur metallogenic zone in eastern Transbaikalia. Mineralization is associated with the Middle–Upper Jurassic Kultuma pluton composed of subalkaline rock series ranging from quartz monzonites and quartz syenites to granites and of monzodiorite dikes. Dikes of Late Jurassic age are composed of subalkaline gabbro. Analysis of fractionation trends of major and trace elements suggests that the monzonitoids prevailed in the Kultuma pluton and the dike complex formed through the differentiation of subalkaline basaltic melt from an enriched mantle source. The formation of the gold–copper–iron–skarn and medium-temperature veinlet-disseminated polysulfide and epithermal Ag–Te–Bi mineralization as well as iron–magnesia and silica–alkaline metasomatites was a long multistage process during the general evolution of the ore-magmatic system.

KW - Au–Cu–Fe skarns

KW - Eastern Transbaikalia

KW - Kultuminskoe deposit

KW - Magmatism

KW - Petrogeochemistry

KW - Polysulfide and epithermal Ag–Te–Bi mineralization

UR - http://www.scopus.com/inward/record.url?scp=85079499151&partnerID=8YFLogxK

U2 - 10.15372/RGG2019078

DO - 10.15372/RGG2019078

M3 - Article

VL - 60

SP - 583

EP - 601

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 6

ER -

ID: 23291503