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Brunovskyite, NaZrSi2O6(OH), a New Mineral from the Khibiny Massif. / Panikorovskii, T. L.; Yakovenchuk, V. N.; Bazai, A. V.; Bocharov, V. N.; Goychuk, O. F.; Antonov, A. A.; Kabanova, N. A.; Krivovichev, S. V.

In: Doklady Earth Sciences, Vol. 523, No. 1, 24, 01.10.2025.

Research output: Contribution to journal › Article › peer-review

Harvard

Panikorovskii, TL, Yakovenchuk, VN, Bazai, AV, Bocharov, VN, Goychuk, OF, Antonov, AA, Kabanova, NA & Krivovichev, SV 2025, 'Brunovskyite, NaZrSi2O6(OH), a New Mineral from the Khibiny Massif', Doklady Earth Sciences, vol. 523, no. 1, 24. https://doi.org/10.1134/s1028334x25607230

APA

Panikorovskii, T. L., Yakovenchuk, V. N., Bazai, A. V., Bocharov, V. N., Goychuk, O. F., Antonov, A. A., Kabanova, N. A., & Krivovichev, S. V. (2025). Brunovskyite, NaZrSi2O6(OH), a New Mineral from the Khibiny Massif. Doklady Earth Sciences, 523(1), [24]. https://doi.org/10.1134/s1028334x25607230

Vancouver

Panikorovskii TL, Yakovenchuk VN, Bazai AV, Bocharov VN, Goychuk OF, Antonov AA et al. Brunovskyite, NaZrSi2O6(OH), a New Mineral from the Khibiny Massif. Doklady Earth Sciences. 2025 Oct 1;523(1). 24. https://doi.org/10.1134/s1028334x25607230

Author

Panikorovskii, T. L. ; Yakovenchuk, V. N. ; Bazai, A. V. ; Bocharov, V. N. ; Goychuk, O. F. ; Antonov, A. A. ; Kabanova, N. A. ; Krivovichev, S. V. / Brunovskyite, NaZrSi2O6(OH), a New Mineral from the Khibiny Massif. In: Doklady Earth Sciences. 2025 ; Vol. 523, No. 1.

BibTeX

@article{c56bb7e675a148d48ff49e011effac93,
title = "Brunovskyite, NaZrSi2O6(OH), a New Mineral from the Khibiny Massif",
abstract = "Abstract: Brunovskyite, NaZrSi2O6(OH), is a new mineral from the pegmatites of Takhtarvumchorr Mountain, the Khibiny Massif, Russia. The mineral forms white powder-like aggregate rims around parakeldyshite, which it replaces. The mineral is triclinic, space group P-1. The unit-cell parameters refined from powder XRD data: a = 5.5472(4) {\AA}, b = 7.1960(6) {\AA}, c = 7.6177(5) {\AA}, α = 64.880(6)°, β = 81.509(8)°, γ = 89.048(7)°,V = 271.94(3) {\AA}3. The eight most intense lines of the powder XRD pattern (I-d[{\AA}]-hkl) are 94-6.50-010; 47-6.22-011; 73-3.94-1-1-1; 98-3.41-002; 100-3.03-121; 77-2.976-1-2-1; 36-2.744-200; 39-1.7961-042. Brunovskyite belongs to the group of zirconosilicates and is dimorphic with keldyshite. The mineral was named as a tribute to Bruno Karlovich Brunovsky (1900–1938), a Soviet crystallographer who solved the first crystal structure in the Soviet Union.",
keywords = "brunovskyite, new mineral, Khibiny massif, Arctic, zirconosilicate, secondary mineralization, Arctic, Khibiny massif, brunovskyite, new mineral, secondary mineralization, zirconosilicate",
author = "Panikorovskii, {T. L.} and Yakovenchuk, {V. N.} and Bazai, {A. V.} and Bocharov, {V. N.} and Goychuk, {O. F.} and Antonov, {A. A.} and Kabanova, {N. A.} and Krivovichev, {S. V.}",
year = "2025",
month = oct,
day = "1",
doi = "10.1134/s1028334x25607230",
language = "English",
volume = "523",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "1",

}

RIS

TY - JOUR

T1 - Brunovskyite, NaZrSi2O6(OH), a New Mineral from the Khibiny Massif

AU - Panikorovskii, T. L.

AU - Yakovenchuk, V. N.

AU - Bazai, A. V.

AU - Bocharov, V. N.

AU - Goychuk, O. F.

AU - Antonov, A. A.

AU - Kabanova, N. A.

AU - Krivovichev, S. V.

PY - 2025/10/1

Y1 - 2025/10/1

N2 - Abstract: Brunovskyite, NaZrSi2O6(OH), is a new mineral from the pegmatites of Takhtarvumchorr Mountain, the Khibiny Massif, Russia. The mineral forms white powder-like aggregate rims around parakeldyshite, which it replaces. The mineral is triclinic, space group P-1. The unit-cell parameters refined from powder XRD data: a = 5.5472(4) Å, b = 7.1960(6) Å, c = 7.6177(5) Å, α = 64.880(6)°, β = 81.509(8)°, γ = 89.048(7)°,V = 271.94(3) Å3. The eight most intense lines of the powder XRD pattern (I-d[Å]-hkl) are 94-6.50-010; 47-6.22-011; 73-3.94-1-1-1; 98-3.41-002; 100-3.03-121; 77-2.976-1-2-1; 36-2.744-200; 39-1.7961-042. Brunovskyite belongs to the group of zirconosilicates and is dimorphic with keldyshite. The mineral was named as a tribute to Bruno Karlovich Brunovsky (1900–1938), a Soviet crystallographer who solved the first crystal structure in the Soviet Union.

AB - Abstract: Brunovskyite, NaZrSi2O6(OH), is a new mineral from the pegmatites of Takhtarvumchorr Mountain, the Khibiny Massif, Russia. The mineral forms white powder-like aggregate rims around parakeldyshite, which it replaces. The mineral is triclinic, space group P-1. The unit-cell parameters refined from powder XRD data: a = 5.5472(4) Å, b = 7.1960(6) Å, c = 7.6177(5) Å, α = 64.880(6)°, β = 81.509(8)°, γ = 89.048(7)°,V = 271.94(3) Å3. The eight most intense lines of the powder XRD pattern (I-d[Å]-hkl) are 94-6.50-010; 47-6.22-011; 73-3.94-1-1-1; 98-3.41-002; 100-3.03-121; 77-2.976-1-2-1; 36-2.744-200; 39-1.7961-042. Brunovskyite belongs to the group of zirconosilicates and is dimorphic with keldyshite. The mineral was named as a tribute to Bruno Karlovich Brunovsky (1900–1938), a Soviet crystallographer who solved the first crystal structure in the Soviet Union.

KW - brunovskyite

KW - new mineral

KW - Khibiny massif

KW - Arctic

KW - zirconosilicate

KW - secondary mineralization

KW - Arctic

KW - Khibiny massif

KW - brunovskyite

KW - new mineral

KW - secondary mineralization

KW - zirconosilicate

UR - https://www.mendeley.com/catalogue/c2c09f72-7e3f-3405-b154-16b02875af57/

U2 - 10.1134/s1028334x25607230

DO - 10.1134/s1028334x25607230

M3 - Article

VL - 523

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

M1 - 24

ER -

ID: 138072627