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X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature. / Panikorovskii, T.L.; Mazur, A.S.; Bazai, A.V.; Shilovskikh, V.V.; Galuskin, E.V.; Chukanov, N.V.; Rusakov, V.S.; Zhukov, Y.M.; Avdontseva, E.Y.; Aksenov, S.M.; Krivovichev, S.V.

In: Physics and Chemistry of Minerals, 2017, p. 1-17.

Research output: Contribution to journal › Article

Harvard

Panikorovskii, TL, Mazur, AS, Bazai, AV, Shilovskikh, VV, Galuskin, EV, Chukanov, NV, Rusakov, VS, Zhukov, YM, Avdontseva, EY, Aksenov, SM & Krivovichev, SV 2017, 'X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature', Physics and Chemistry of Minerals, pp. 1-17. https://doi.org/10.1007/s00269-017-0885-2

APA

Panikorovskii, T. L., Mazur, A. S., Bazai, A. V., Shilovskikh, V. V., Galuskin, E. V., Chukanov, N. V., Rusakov, V. S., Zhukov, Y. M., Avdontseva, E. Y., Aksenov, S. M., & Krivovichev, S. V. (2017). X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature. Physics and Chemistry of Minerals, 1-17. https://doi.org/10.1007/s00269-017-0885-2

Vancouver

Panikorovskii TL, Mazur AS, Bazai AV, Shilovskikh VV, Galuskin EV, Chukanov NV et al. X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature. Physics and Chemistry of Minerals. 2017;1-17. https://doi.org/10.1007/s00269-017-0885-2

Author

Panikorovskii, T.L. ; Mazur, A.S. ; Bazai, A.V. ; Shilovskikh, V.V. ; Galuskin, E.V. ; Chukanov, N.V. ; Rusakov, V.S. ; Zhukov, Y.M. ; Avdontseva, E.Y. ; Aksenov, S.M. ; Krivovichev, S.V. / X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature. In: Physics and Chemistry of Minerals. 2017 ; pp. 1-17.

BibTeX

@article{eaa00e72e10144eaa08f060fd2a6d570,
title = "X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature",
abstract = "{\textcopyright} 2017 Springer-Verlag Berlin HeidelbergTwo wiluite samples from the Wiluy River, Yakutia, Russia have been investigated by means of single-crystal and powder X-ray diffraction, electron microprobe analysis, 1H, 27Al, 11B, and 29Si magic-angle spinning nuclear magnetic resonance (MAS NMR), thermogravimetric analysis (DSC/TGA), X-ray photoelectron spectroscopy (XPS) at the Si2p, Ca2p, Al2p, Mg1s, B1s and Fe2p core levels, 57Fe M{\"o}ssbauer spectroscopy, infrared (IR) spectroscopy and optical measurements. The crystal structures have been refined in the P4/nnc space group [a = 15.7027(3), c = 11.7008(3) {\AA}, V = 2885.1(1) {\AA}3 for 1 and a = 15.6950(2), c = 11.6787(4) {\AA}, V = 2876.9(1) {\AA}3 for 2] to R1 = 0.022 and R1 = 0.021, respectively. In the crystal structure of wiluite, five-coordinated Y1 site is predominantly occupied by Mg. IR spectra of wiluite substantially different from those of vesuvianite, in particular, by the presence of additional bands in the range 1080‒1415 cm−1, which correspond to symmetric B‒O stre",
author = "T.L. Panikorovskii and A.S. Mazur and A.V. Bazai and V.V. Shilovskikh and E.V. Galuskin and N.V. Chukanov and V.S. Rusakov and Y.M. Zhukov and E.Y. Avdontseva and S.M. Aksenov and S.V. Krivovichev",
year = "2017",
doi = "10.1007/s00269-017-0885-2",
language = "English",
pages = "1--17",
journal = "Physics and Chemistry of Minerals",
issn = "0342-1791",
publisher = "Springer Nature",

}

RIS

TY - JOUR

T1 - X-ray diffraction and spectroscopic study of wiluite: implications for the vesuvianite-group nomenclature

AU - Panikorovskii, T.L.

AU - Mazur, A.S.

AU - Bazai, A.V.

AU - Shilovskikh, V.V.

AU - Galuskin, E.V.

AU - Chukanov, N.V.

AU - Rusakov, V.S.

AU - Zhukov, Y.M.

AU - Avdontseva, E.Y.

AU - Aksenov, S.M.

AU - Krivovichev, S.V.

PY - 2017

Y1 - 2017

N2 - © 2017 Springer-Verlag Berlin HeidelbergTwo wiluite samples from the Wiluy River, Yakutia, Russia have been investigated by means of single-crystal and powder X-ray diffraction, electron microprobe analysis, 1H, 27Al, 11B, and 29Si magic-angle spinning nuclear magnetic resonance (MAS NMR), thermogravimetric analysis (DSC/TGA), X-ray photoelectron spectroscopy (XPS) at the Si2p, Ca2p, Al2p, Mg1s, B1s and Fe2p core levels, 57Fe Mössbauer spectroscopy, infrared (IR) spectroscopy and optical measurements. The crystal structures have been refined in the P4/nnc space group [a = 15.7027(3), c = 11.7008(3) Å, V = 2885.1(1) Å3 for 1 and a = 15.6950(2), c = 11.6787(4) Å, V = 2876.9(1) Å3 for 2] to R1 = 0.022 and R1 = 0.021, respectively. In the crystal structure of wiluite, five-coordinated Y1 site is predominantly occupied by Mg. IR spectra of wiluite substantially different from those of vesuvianite, in particular, by the presence of additional bands in the range 1080‒1415 cm−1, which correspond to symmetric B‒O stre

AB - © 2017 Springer-Verlag Berlin HeidelbergTwo wiluite samples from the Wiluy River, Yakutia, Russia have been investigated by means of single-crystal and powder X-ray diffraction, electron microprobe analysis, 1H, 27Al, 11B, and 29Si magic-angle spinning nuclear magnetic resonance (MAS NMR), thermogravimetric analysis (DSC/TGA), X-ray photoelectron spectroscopy (XPS) at the Si2p, Ca2p, Al2p, Mg1s, B1s and Fe2p core levels, 57Fe Mössbauer spectroscopy, infrared (IR) spectroscopy and optical measurements. The crystal structures have been refined in the P4/nnc space group [a = 15.7027(3), c = 11.7008(3) Å, V = 2885.1(1) Å3 for 1 and a = 15.6950(2), c = 11.6787(4) Å, V = 2876.9(1) Å3 for 2] to R1 = 0.022 and R1 = 0.021, respectively. In the crystal structure of wiluite, five-coordinated Y1 site is predominantly occupied by Mg. IR spectra of wiluite substantially different from those of vesuvianite, in particular, by the presence of additional bands in the range 1080‒1415 cm−1, which correspond to symmetric B‒O stre

U2 - 10.1007/s00269-017-0885-2

DO - 10.1007/s00269-017-0885-2

M3 - Article

SP - 1

EP - 17

JO - Physics and Chemistry of Minerals

JF - Physics and Chemistry of Minerals

SN - 0342-1791

ER -

ID: 7908176