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Rare-metal pegmatite deposits of the Kalba Region, Eastern Kazakhstan : Age, composition and petrogenetic implications. / Khromykh, Sergey V.; Oitseva, Tatiana A.; Kotler, Pavel D. и др.

в: Minerals, Том 10, № 11, 1017, 11.2020, стр. 1-15.

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

Harvard

Khromykh, SV, Oitseva, TA, Kotler, PD, D’yachkov, BA, Smirnov, SZ, Travin, AV, Vladimirov, AG, Sokolova, EN, Kuzmina, ON, Mizernaya, MA & Agaliyeva, BB 2020, 'Rare-metal pegmatite deposits of the Kalba Region, Eastern Kazakhstan: Age, composition and petrogenetic implications', Minerals, Том. 10, № 11, 1017, стр. 1-15. https://doi.org/10.3390/min10111017

APA

Khromykh, S. V., Oitseva, T. A., Kotler, P. D., D’yachkov, B. A., Smirnov, S. Z., Travin, A. V., Vladimirov, A. G., Sokolova, E. N., Kuzmina, O. N., Mizernaya, M. A., & Agaliyeva, B. B. (2020). Rare-metal pegmatite deposits of the Kalba Region, Eastern Kazakhstan: Age, composition and petrogenetic implications. Minerals, 10(11), 1-15. [1017]. https://doi.org/10.3390/min10111017

Vancouver

Khromykh SV, Oitseva TA, Kotler PD, D’yachkov BA, Smirnov SZ, Travin AV и др. Rare-metal pegmatite deposits of the Kalba Region, Eastern Kazakhstan: Age, composition and petrogenetic implications. Minerals. 2020 нояб.;10(11):1-15. 1017. doi: 10.3390/min10111017

Author

Khromykh, Sergey V. ; Oitseva, Tatiana A. ; Kotler, Pavel D. и др. / Rare-metal pegmatite deposits of the Kalba Region, Eastern Kazakhstan : Age, composition and petrogenetic implications. в: Minerals. 2020 ; Том 10, № 11. стр. 1-15.

BibTeX

@article{7993bafd58334441a92825563c238258,
title = "Rare-metal pegmatite deposits of the Kalba Region, Eastern Kazakhstan: Age, composition and petrogenetic implications",
abstract = "The paper presents new geological, mineralogical, and isotope geochronological data for rare-metal pegmatites in the Kalba granitic batholith (Eastern Kazakhstan). Mineralization is especially abundant in the Central-Kalba ore district, where pegmatite bodies occur at the top of large granite plutons and at intersections of deep faults. The pegmatites contain several successive mineral assemblages from barren quartz-microcline and quartz-microcline-albite to Li-Cs-Ta-Nb-Be-Sn-bearing cleavelandite-lepidolite-spodumene. Ar-Ar muscovite and lepidolite ages bracket the metallogenic event between 291 and 286 Ma. The pegmatite mineral deposits formed synchronously with the emplacement of the phase 1 Kalba granites during the evolution of hydrous silicate rare-metal magmas that are produced by the differentiation of granite magma at large sources with possible inputs of F and rare metals with fluids.",
keywords = "Ar-Ar isotope age, Eastern Kazakhstan, Kalba granite batholith, Rare-metal pegmatites",
author = "Khromykh, {Sergey V.} and Oitseva, {Tatiana A.} and Kotler, {Pavel D.} and D{\textquoteright}yachkov, {Boris A.} and Smirnov, {Sergey Z.} and Travin, {Alexey V.} and Vladimirov, {Alexander G.} and Sokolova, {Ekaterina N.} and Kuzmina, {Oxana N.} and Mizernaya, {Marina A.} and Agaliyeva, {Bakytgul{\textquoteright} B.}",
note = "Funding Information: Funding: This research was carried out on a government assignment to the V.S. Sobolev Institute of Geology and Mineralogy (Novosibirsk) and was supported by the Russian Foundation for Basic Research (Projects no. 20-35-70076, 20-05-00346). This research was funded by the Science Committee of the Ministry of Education and Science of the Republic of Kazakhstan (Grant No. AP08856325). Publisher Copyright: {\textcopyright} 2020 by the authors. Licensee MDPI, Basel, Switzerland. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.",
year = "2020",
month = nov,
doi = "10.3390/min10111017",
language = "English",
volume = "10",
pages = "1--15",
journal = "Minerals",
issn = "2075-163X",
publisher = "MDPI AG",
number = "11",

}

RIS

TY - JOUR

T1 - Rare-metal pegmatite deposits of the Kalba Region, Eastern Kazakhstan

T2 - Age, composition and petrogenetic implications

AU - Khromykh, Sergey V.

AU - Oitseva, Tatiana A.

AU - Kotler, Pavel D.

AU - D’yachkov, Boris A.

AU - Smirnov, Sergey Z.

AU - Travin, Alexey V.

AU - Vladimirov, Alexander G.

AU - Sokolova, Ekaterina N.

AU - Kuzmina, Oxana N.

AU - Mizernaya, Marina A.

AU - Agaliyeva, Bakytgul’ B.

N1 - Funding Information: Funding: This research was carried out on a government assignment to the V.S. Sobolev Institute of Geology and Mineralogy (Novosibirsk) and was supported by the Russian Foundation for Basic Research (Projects no. 20-35-70076, 20-05-00346). This research was funded by the Science Committee of the Ministry of Education and Science of the Republic of Kazakhstan (Grant No. AP08856325). Publisher Copyright: © 2020 by the authors. Licensee MDPI, Basel, Switzerland. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.

PY - 2020/11

Y1 - 2020/11

N2 - The paper presents new geological, mineralogical, and isotope geochronological data for rare-metal pegmatites in the Kalba granitic batholith (Eastern Kazakhstan). Mineralization is especially abundant in the Central-Kalba ore district, where pegmatite bodies occur at the top of large granite plutons and at intersections of deep faults. The pegmatites contain several successive mineral assemblages from barren quartz-microcline and quartz-microcline-albite to Li-Cs-Ta-Nb-Be-Sn-bearing cleavelandite-lepidolite-spodumene. Ar-Ar muscovite and lepidolite ages bracket the metallogenic event between 291 and 286 Ma. The pegmatite mineral deposits formed synchronously with the emplacement of the phase 1 Kalba granites during the evolution of hydrous silicate rare-metal magmas that are produced by the differentiation of granite magma at large sources with possible inputs of F and rare metals with fluids.

AB - The paper presents new geological, mineralogical, and isotope geochronological data for rare-metal pegmatites in the Kalba granitic batholith (Eastern Kazakhstan). Mineralization is especially abundant in the Central-Kalba ore district, where pegmatite bodies occur at the top of large granite plutons and at intersections of deep faults. The pegmatites contain several successive mineral assemblages from barren quartz-microcline and quartz-microcline-albite to Li-Cs-Ta-Nb-Be-Sn-bearing cleavelandite-lepidolite-spodumene. Ar-Ar muscovite and lepidolite ages bracket the metallogenic event between 291 and 286 Ma. The pegmatite mineral deposits formed synchronously with the emplacement of the phase 1 Kalba granites during the evolution of hydrous silicate rare-metal magmas that are produced by the differentiation of granite magma at large sources with possible inputs of F and rare metals with fluids.

KW - Ar-Ar isotope age

KW - Eastern Kazakhstan

KW - Kalba granite batholith

KW - Rare-metal pegmatites

UR - http://www.scopus.com/inward/record.url?scp=85096390321&partnerID=8YFLogxK

U2 - 10.3390/min10111017

DO - 10.3390/min10111017

M3 - Article

AN - SCOPUS:85096390321

VL - 10

SP - 1

EP - 15

JO - Minerals

JF - Minerals

SN - 2075-163X

IS - 11

M1 - 1017

ER -

ID: 26065154