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Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure. / Agakhanov, Atali A.; Kasatkin, Anatoly V.; Britvin, Sergey N.; Siidra, Oleg I.; Pautov, Leonid A.; Pekov, Igor V.; Karpenko, Vladimir Yu.

In: Canadian Mineralogist, Vol. 59, No. 1, 26.02.2021, p. 149-157.

Research output: Contribution to journalArticlepeer-review

Harvard

Agakhanov, AA, Kasatkin, AV, Britvin, SN, Siidra, OI, Pautov, LA, Pekov, IV & Karpenko, VY 2021, 'Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure', Canadian Mineralogist, vol. 59, no. 1, pp. 149-157. https://doi.org/10.3749/canmin.2000056

APA

Agakhanov, A. A., Kasatkin, A. V., Britvin, S. N., Siidra, O. I., Pautov, L. A., Pekov, I. V., & Karpenko, V. Y. (2021). Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure. Canadian Mineralogist, 59(1), 149-157. https://doi.org/10.3749/canmin.2000056

Vancouver

Agakhanov AA, Kasatkin AV, Britvin SN, Siidra OI, Pautov LA, Pekov IV et al. Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure. Canadian Mineralogist. 2021 Feb 26;59(1):149-157. https://doi.org/10.3749/canmin.2000056

Author

Agakhanov, Atali A. ; Kasatkin, Anatoly V. ; Britvin, Sergey N. ; Siidra, Oleg I. ; Pautov, Leonid A. ; Pekov, Igor V. ; Karpenko, Vladimir Yu. / Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure. In: Canadian Mineralogist. 2021 ; Vol. 59, No. 1. pp. 149-157.

BibTeX

@article{e4d2ac822dd24ad295c1fee9e273a6b8,
title = "Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure",
abstract = "Cesiokenopyrochlore is a new mineral belonging to the pyrochlore group. It was discovered in a specimen of granitic pegmatite collected at Tetezantsio, Betafo region, Madagascar. The mineral forms rough equant crystals up to 0.05 mm in size intergrown with b{\'e}hierite and rynersonite. Cesiokenopyrochlore is light-brown, translucent, with resinous luster. D calc. ¼ 5.984 g/cm 3. In reflected light it is light gray, isotropic, with strong light-brown internal reflections. The crystal structure was refined to R 1 ¼ 0.0212. The mineral is cubic, Fd -3m, a ¼ 10.444(1) A , V ¼ 1139.5(2) A 3, and Z ¼ 8. The strongest lines of the powder X-ray diffraction pattern [d, A , (I, %) (hkl)] are: 6.03 (37) (111), 3.70 (9) (220), 3.15 (100) (311), 3.02 (36) (222), 2.012 (17) (511, 333), 1.848 (19) (440), 1.576 (11) (622). The chemical composition is (wt.%; electron microprobe): Cs 2O 22.66, Na 2O 1.74, CaO 0.64, Nb 2O 5 20.87, Ta 2O 5 21.27, WO 3 30.67, H 2O (calc) 0.12, total 97.97. The empirical formula of the holotype specimen calculated on the basis of (Nb{\th}Ta{\th}W) ¼ 2 apfu and (O{\th}OH) ¼ 6 apfu and written according to the pyrochlore-supergroup nomenclature is Na 0.29Ca 0.06(Nb 0.81W 0.69Ta 0.50) R2[O 5.93(OH) 0.07] R6Cs 0.83. The simplified formula of the holotype specimen is A 2(Nb,W,Ta) R2O 6Cs. Cesiokenopyrochlore is the first natural niobate to adopt the inverse pyrochlore structure. ",
keywords = "Cesiokenopyrochlore, Cesium, Crystal structure, Granitic pegmatite, Inverse pyrochlore, Madagascar, New mineral, Niobate, Pyrochlore group, Tetezantsio",
author = "Agakhanov, {Atali A.} and Kasatkin, {Anatoly V.} and Britvin, {Sergey N.} and Siidra, {Oleg I.} and Pautov, {Leonid A.} and Pekov, {Igor V.} and Karpenko, {Vladimir Yu.}",
note = "Publisher Copyright: {\textcopyright} 2021 Mineralogical Association of Canada. All rights reserved.",
year = "2021",
month = feb,
day = "26",
doi = "10.3749/canmin.2000056",
language = "English",
volume = "59",
pages = "149--157",
journal = "Canadian Mineralogist",
issn = "0008-4476",
publisher = "Mineralogical Association of Canada",
number = "1",

}

RIS

TY - JOUR

T1 - Cesiokenopyrochlore, the First Natural Niobate with an Inverse Pyrochlore Structure

AU - Agakhanov, Atali A.

AU - Kasatkin, Anatoly V.

AU - Britvin, Sergey N.

AU - Siidra, Oleg I.

AU - Pautov, Leonid A.

AU - Pekov, Igor V.

AU - Karpenko, Vladimir Yu.

N1 - Publisher Copyright: © 2021 Mineralogical Association of Canada. All rights reserved.

PY - 2021/2/26

Y1 - 2021/2/26

N2 - Cesiokenopyrochlore is a new mineral belonging to the pyrochlore group. It was discovered in a specimen of granitic pegmatite collected at Tetezantsio, Betafo region, Madagascar. The mineral forms rough equant crystals up to 0.05 mm in size intergrown with béhierite and rynersonite. Cesiokenopyrochlore is light-brown, translucent, with resinous luster. D calc. ¼ 5.984 g/cm 3. In reflected light it is light gray, isotropic, with strong light-brown internal reflections. The crystal structure was refined to R 1 ¼ 0.0212. The mineral is cubic, Fd -3m, a ¼ 10.444(1) A , V ¼ 1139.5(2) A 3, and Z ¼ 8. The strongest lines of the powder X-ray diffraction pattern [d, A , (I, %) (hkl)] are: 6.03 (37) (111), 3.70 (9) (220), 3.15 (100) (311), 3.02 (36) (222), 2.012 (17) (511, 333), 1.848 (19) (440), 1.576 (11) (622). The chemical composition is (wt.%; electron microprobe): Cs 2O 22.66, Na 2O 1.74, CaO 0.64, Nb 2O 5 20.87, Ta 2O 5 21.27, WO 3 30.67, H 2O (calc) 0.12, total 97.97. The empirical formula of the holotype specimen calculated on the basis of (NbþTaþW) ¼ 2 apfu and (OþOH) ¼ 6 apfu and written according to the pyrochlore-supergroup nomenclature is Na 0.29Ca 0.06(Nb 0.81W 0.69Ta 0.50) R2[O 5.93(OH) 0.07] R6Cs 0.83. The simplified formula of the holotype specimen is A 2(Nb,W,Ta) R2O 6Cs. Cesiokenopyrochlore is the first natural niobate to adopt the inverse pyrochlore structure.

AB - Cesiokenopyrochlore is a new mineral belonging to the pyrochlore group. It was discovered in a specimen of granitic pegmatite collected at Tetezantsio, Betafo region, Madagascar. The mineral forms rough equant crystals up to 0.05 mm in size intergrown with béhierite and rynersonite. Cesiokenopyrochlore is light-brown, translucent, with resinous luster. D calc. ¼ 5.984 g/cm 3. In reflected light it is light gray, isotropic, with strong light-brown internal reflections. The crystal structure was refined to R 1 ¼ 0.0212. The mineral is cubic, Fd -3m, a ¼ 10.444(1) A , V ¼ 1139.5(2) A 3, and Z ¼ 8. The strongest lines of the powder X-ray diffraction pattern [d, A , (I, %) (hkl)] are: 6.03 (37) (111), 3.70 (9) (220), 3.15 (100) (311), 3.02 (36) (222), 2.012 (17) (511, 333), 1.848 (19) (440), 1.576 (11) (622). The chemical composition is (wt.%; electron microprobe): Cs 2O 22.66, Na 2O 1.74, CaO 0.64, Nb 2O 5 20.87, Ta 2O 5 21.27, WO 3 30.67, H 2O (calc) 0.12, total 97.97. The empirical formula of the holotype specimen calculated on the basis of (NbþTaþW) ¼ 2 apfu and (OþOH) ¼ 6 apfu and written according to the pyrochlore-supergroup nomenclature is Na 0.29Ca 0.06(Nb 0.81W 0.69Ta 0.50) R2[O 5.93(OH) 0.07] R6Cs 0.83. The simplified formula of the holotype specimen is A 2(Nb,W,Ta) R2O 6Cs. Cesiokenopyrochlore is the first natural niobate to adopt the inverse pyrochlore structure.

KW - Cesiokenopyrochlore

KW - Cesium

KW - Crystal structure

KW - Granitic pegmatite

KW - Inverse pyrochlore

KW - Madagascar

KW - New mineral

KW - Niobate

KW - Pyrochlore group

KW - Tetezantsio

UR - http://www.scopus.com/inward/record.url?scp=85110276188&partnerID=8YFLogxK

U2 - 10.3749/canmin.2000056

DO - 10.3749/canmin.2000056

M3 - Article

VL - 59

SP - 149

EP - 157

JO - Canadian Mineralogist

JF - Canadian Mineralogist

SN - 0008-4476

IS - 1

ER -

ID: 77683391