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Inclusions of Kîragit in topaz from pegmatites of the Mokrusha deposit (Urals, Russia). / Ponomareva, N. I.; Gordienko, V. V.; Antonov, A. V.; Krivovichev, S. V.; Nesterov, A. R.; Kazantseva, M. I.

в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 147, № 5, 01.01.2018, стр. 61-68.

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

Harvard

Ponomareva, NI, Gordienko, VV, Antonov, AV, Krivovichev, SV, Nesterov, AR & Kazantseva, MI 2018, 'Inclusions of Kîragit in topaz from pegmatites of the Mokrusha deposit (Urals, Russia)', Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том. 147, № 5, стр. 61-68. https://doi.org/10.30695/zrmo/2018.1475.04

APA

Ponomareva, N. I., Gordienko, V. V., Antonov, A. V., Krivovichev, S. V., Nesterov, A. R., & Kazantseva, M. I. (2018). Inclusions of Kîragit in topaz from pegmatites of the Mokrusha deposit (Urals, Russia). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 147(5), 61-68. https://doi.org/10.30695/zrmo/2018.1475.04

Vancouver

Ponomareva NI, Gordienko VV, Antonov AV, Krivovichev SV, Nesterov AR, Kazantseva MI. Inclusions of Kîragit in topaz from pegmatites of the Mokrusha deposit (Urals, Russia). Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2018 Янв. 1;147(5):61-68. https://doi.org/10.30695/zrmo/2018.1475.04

Author

Ponomareva, N. I. ; Gordienko, V. V. ; Antonov, A. V. ; Krivovichev, S. V. ; Nesterov, A. R. ; Kazantseva, M. I. / Inclusions of Kîragit in topaz from pegmatites of the Mokrusha deposit (Urals, Russia). в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2018 ; Том 147, № 5. стр. 61-68.

BibTeX

@article{8a690730f986427f8e1ded1b0d6a9c4a,
title = "Inclusions of K{\^i}ragit in topaz from pegmatites of the Mokrusha deposit (Urals, Russia)",
abstract = " The present communication is devoted to the study of inclusions in topaz from the Mokrusha pegmatite deposit field (Urals). Inclusions in topaz are represented by intergrowths of small crystals of manganocolumbite, cassiterite and a mineral corresponding to niobium tungstate with impurities of manganese, tantalum and iron. On the basis of microprobe and X-ray analyses it is confirmed the identity between the mineral and koragoite previously described by A. V. Voloshin and co-authors in granite pegmatites of south-western Pamirs, Tajikistan. The formula of the mineral is: (Mn 2.02 Fe 0.98 ) {\'O}3.00 (Nb 2.296 Ta 0.640 Ti 0.062 ) {\'O}3.00 (Nb 1.04 Mn 0.960 ) {\'O}2.00 (W 1.343 Nb 0.664 ) {\'O}2.00 O 20 . ",
keywords = "Koragoite, Mineral inclusions, Mokrusha deposits, Pegmatite, Topaz, Urals",
author = "Ponomareva, {N. I.} and Gordienko, {V. V.} and Antonov, {A. V.} and Krivovichev, {S. V.} and Nesterov, {A. R.} and Kazantseva, {M. I.}",
year = "2018",
month = jan,
day = "1",
doi = "10.30695/zrmo/2018.1475.04",
language = "English",
volume = "147",
pages = "61--68",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Inclusions of Kîragit in topaz from pegmatites of the Mokrusha deposit (Urals, Russia)

AU - Ponomareva, N. I.

AU - Gordienko, V. V.

AU - Antonov, A. V.

AU - Krivovichev, S. V.

AU - Nesterov, A. R.

AU - Kazantseva, M. I.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The present communication is devoted to the study of inclusions in topaz from the Mokrusha pegmatite deposit field (Urals). Inclusions in topaz are represented by intergrowths of small crystals of manganocolumbite, cassiterite and a mineral corresponding to niobium tungstate with impurities of manganese, tantalum and iron. On the basis of microprobe and X-ray analyses it is confirmed the identity between the mineral and koragoite previously described by A. V. Voloshin and co-authors in granite pegmatites of south-western Pamirs, Tajikistan. The formula of the mineral is: (Mn 2.02 Fe 0.98 ) Ó3.00 (Nb 2.296 Ta 0.640 Ti 0.062 ) Ó3.00 (Nb 1.04 Mn 0.960 ) Ó2.00 (W 1.343 Nb 0.664 ) Ó2.00 O 20 .

AB - The present communication is devoted to the study of inclusions in topaz from the Mokrusha pegmatite deposit field (Urals). Inclusions in topaz are represented by intergrowths of small crystals of manganocolumbite, cassiterite and a mineral corresponding to niobium tungstate with impurities of manganese, tantalum and iron. On the basis of microprobe and X-ray analyses it is confirmed the identity between the mineral and koragoite previously described by A. V. Voloshin and co-authors in granite pegmatites of south-western Pamirs, Tajikistan. The formula of the mineral is: (Mn 2.02 Fe 0.98 ) Ó3.00 (Nb 2.296 Ta 0.640 Ti 0.062 ) Ó3.00 (Nb 1.04 Mn 0.960 ) Ó2.00 (W 1.343 Nb 0.664 ) Ó2.00 O 20 .

KW - Koragoite

KW - Mineral inclusions

KW - Mokrusha deposits

KW - Pegmatite

KW - Topaz

KW - Urals

UR - http://www.scopus.com/inward/record.url?scp=85063753932&partnerID=8YFLogxK

U2 - 10.30695/zrmo/2018.1475.04

DO - 10.30695/zrmo/2018.1475.04

M3 - Article

AN - SCOPUS:85063753932

VL - 147

SP - 61

EP - 68

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 5

ER -

ID: 49249316