Hostname: page-component-78c5997874-4rdpn Total loading time: 0 Render date: 2024-11-19T05:22:20.376Z Has data issue: false hasContentIssue false

A highly hydrated variety of elpidite from the Khibiny alkaline complex, Kola Peninsula, Russia

Published online by Cambridge University Press:  27 November 2020

Natalia V. Zubkova*
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991Moscow, Russia
Igor V. Pekov
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991Moscow, Russia Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Kosygina str. 19, 119991Moscow, Russia
Nikita V. Chukanov
Affiliation:
Institute of Problems of Chemical Physics, Russian Academy of Sciences, 142432 Chernogolovka, Moscow region, Russia
Vasiliy O. Yapaskurt
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991Moscow, Russia
Anna G. Turchkova
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991Moscow, Russia
Tatiana S. Larikova
Affiliation:
Institute of Problems of Chemical Physics, Russian Academy of Sciences, 142432 Chernogolovka, Moscow region, Russia
Dmitry Yu. Pushcharovsky
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991Moscow, Russia
*
*Author for correspondence: Natalia V. Zubkova, Email: [email protected]

Abstract

An unusual highly hydrated and Na-depleted variety of elpidite was identified in a hydrothermally altered peralkaline pegmatite at Mt. Yukspor in the Khibiny alkaline complex, Kola Peninsula, Russia. It differs from ‘ordinary’ elpidite, ideally Na2ZrSi6O15⋅3H2O, in its crystal chemical features, infrared spectrum and optical characteristics. The chemical composition (wt.%, electron microprobe, H2O by TGA) is: Na2O 5.45, K2O 0.67, CaO 0.05, SiO2 60.32, TiO2 1.34, ZrO2 18.43, Nb2O5 0.65, H2O 12.80, total 99.71. The empirical formula calculated on the basis of 6 Si and 15 O atoms is [(Na1.05K0.08Ca0.01)Σ1.14(H3O)0.74]Σ1.88(Zr0.89Ti0.10Nb0.03)Σ1.02Si6O15⋅3.47H2O; the H2O:H3O ratio was calculated from the charge balance requirement, taking into account the results of crystal structure refinement. The highly hydrated variety of elpidite is orthorhombic, Pma2, a = 14.5916(6), b = 7.3294(3), c = 7.1387(2) Å, V = 763.47(5) Å3 and Z = 2. The crystal structure was solved from single-crystal X-ray diffraction data, R1 = 3.43%. The structure is based upon an elpidite-type heteropolyhedral Zr–Si–O framework with Na+ and H3O+ cations and H2O molecules in the zeolitic channels. Hydronium cations substitute for water molecules in one of the extra-framework sites. This variety of elpidite could be considered as an intermediate product of natural ion-exchange reaction between ‘ordinary’ elpidite and a low-temperature hydrothermal fluid.

Type
Article – Gregory Yu. Ivanyuk memorial issue
Copyright
Copyright © The Author(s), 2020. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

Associate Editor: Sergey V Krivovichev

This paper is part of a thematic set ‘Alkaline Rocks’ in memory of Dr Gregory Yu. Ivanyuk

References

Agakhanov, A.A., Pautov, L.A., Karpenko, V.Yu, Sokolova, E., Abdu, Y.A., Hawthorne, F.C., Pekov, I.V. and Siidra, O.I. (2015) Yusupovite, Na2Zr(Si6O15)(H2O)3, a new mineral species from the Darai-Pioz alkaline massif and its implications as a new microporous filter for large ions. American Mineralogist, 100, 15021508.CrossRefGoogle Scholar
Anthony, J.W., Bideaux, R.A., Bladh, K.W. and Nichols, M.C. (1995) Handbook of Mineralogy. Vol. II: Silica, Silicates. Mineral Data Publishing, Tuscon, USA, 904 pp.Google Scholar
Birkett, T.C., Miller, R.R., Roberts, A.C. and Mariano, A.N. (1992) Zirconium-bearing minerals from the Strange Lake intrusive complex, Quebec-Labrador. The Canadian Mineralogist, 30, 191205.Google Scholar
Cametti, G., Armbruster, T. and Nagashima, M. (2016) Dehydration and thermal stability of elpidite: An in-situ single crystal X-ray diffraction study. Microporous Mesoporous Materials, 2016, 227, 8187.CrossRefGoogle Scholar
Cannillo, E., Rossi, G. and Ungaretti, L. (1973) The crystal structure of elpidite. American Mineralogist, 58, 106109.Google Scholar
Chukanov, N.V. and Chervonnyi, A.D. (2016) Infrared Spectroscopy of Minerals and Related Compounds. Springer, Cham, Switzerland, 1109 pp.CrossRefGoogle Scholar
Grigor'eva, A.A., Zubkova, N.V., Pekov, I.V., Kolitsch, U., Pushcharovsky, D.Yu., Vigasina, M.F., Giester, G., Ðorðevic, T., Tillmanns, E. and Chukanov, N.V. (2011) Crystal chemistry of elpidite from Khan Bogdo (Mongolia) and its K- and Rb-exchanged forms. Crystallography Reports, 56, 832841.CrossRefGoogle Scholar
Ilyushin, G.D., Dem'yanets, L.N., Ilyukhin, V.V., Belov, N.V. (1983) Formation of mineral analogs and synthetic phases in the hydrothermal system NaOH–ZrO2–SiO2–H2O. Doklady AN SSSR, 271, 11331136 [in Russian].Google Scholar
Ivanyuk, G.Yu., Pakhomovsky, Ya.A., Yakovenchuk, V.N., Men'shikov, Yu.P., Bogdanova, A.N. and Mikhailova, Yu.A. (2006) Rare-metal minerals of microcline-quartz veins in volcanogenic-sedimentary rocks of Kitknyun Mt. (Lovozero massif). Zapiski RMO (Proceedings of the Russian Mineralogical Society ), 135, 6681 [in Russian].Google Scholar
Kabalov, Y.K., Zubkova, N.V., Pushcharovsky, D.Y., Schneider, J. and Sapozhnikov, A.N. (2000) Powder Rietveld refinement of armstrongite, CaZr[Si6O15]⋅3H2O. Zeitschrift für Kristallographie, 215, 757761.Google Scholar
Kempe, U., Möckel, R., Graupner, T., Kynicky, J. and Dombon, E. (2015) The genesis of Zr–Nb–REE mineralisation at Khalzan Buregte (Western Mongolia) reconsidered. Ore Geology Reviews, 64, 602625.CrossRefGoogle Scholar
Kovalenko, V.I., Tsaryeva, G.M., Goreglyad, A.V., Yarmolyuk, V.V., Troitsky, V.A., Hervig, R.L. and Farmer, G. (1995) The peralkaline granite-related Khaldzan-Buregtey rare metal (Zr, Nb, REE) deposit, western Mongolia. Economic Geology, 90, 530547.CrossRefGoogle Scholar
Kynicky, J., Chakhmouradian, A.R., Xu, C., Krmicek, L. and Galilova, M. (2011) Distribution and evolution of zirconium mineralization in peralkaline granites and associated pegmatites of the Khan Bogd Complex, southern Mongolia. The Canadian Mineralogist, 49, 947965.CrossRefGoogle Scholar
Mesto, E., Kaneva, E., Schingaro, E., Vladykin, N., Lacalamita, M. and Scordari, F. (2014) Armstrongite from Khan Bogdo (Mongolia): Crystal structure determination and implications for zeolite-like cation exchange properties. American Mineralogist, 99, 24242432.CrossRefGoogle Scholar
Neronova, N.N. and Belov, N.V. (1964) Crystal structure of elpidite, Na2ZrSi6O15⋅(H2O)3. Soviet Physics, Crystallography, 9, 700705.Google Scholar
Pekov, I.V. (2000) Lovozero Massif: History, Pegmatites, Minerals. OP, Moscow, 480 pp.Google Scholar
Pekov, I.V., Chukanov, N.V., Kononkova, N.N. and Pushcharovsky, D.Yu. (2003) Rare-metal “zeolites” of the hilairite group. New Data on Minerals, 38, 2033.Google Scholar
Pekov, I.V., Turchkova, A.G., Lovskaya, E.V. and Chukanov, N.V. (2004) Zeolites of Alkaline Massifs. Ecost Association, Moscow, 168 pp. [in Russian].Google Scholar
Pekov, I.V., Grigorieva, A.A., Turchkova, A.G. and Lovskaya, E.V. (2008) Natural ion exchange in microporous minerals: different aspects and implications. Pp. 715 in: Minerals as Advanced Materials I. (Krivovichev, S.V., editor). Springer, Berlin–Heidelberg, Germany.CrossRefGoogle Scholar
Pushcharovsky, D.Yu., Pekov, I.V., Pasero, M., Gobechia, E.R., Merlino, S. and Zubkova, N.V. (2002) The crystal structure of cation-deficient calciohilairite and possible mechanisms of decationization in mixed-frameworks minerals. Crystallography Reports, 47, 748758.CrossRefGoogle Scholar
Rigaku Oxford Diffraction (2018) CrysAlisPro Software System, v. 1.171.39.46. Rigaku Corporation, Oxford, UK.Google Scholar
Roelofsen, J.N. and Veblen, D.R. (1999) Relationships among zirconosilicates: Examination by cathodoluminescence and transmission electron microscopy. Mineralogy and Petrology, 67, 7184.CrossRefGoogle Scholar
Salvi, S. and Williams-Jones, A.E. (2001) Zirconosilicate phase relations in the Strange Lake (Lac Brisson) Pluton, Quebec-Labrador, Canada. American Mineralogist, 13, 355363.Google Scholar
Sapozhnikov, A.N. and Kashaev, A.A. (1978) Features of the crystal structure of calcium-containing elpidite. Soviet Physics, Crystallography, 23, 2427.Google Scholar
Sheldrick, G.M. (2015) Crystal structure refinement with SHELXL. Acta Crystallographica, C71, 38.Google Scholar
Turchkova, A.G., Pekov, I.V. and Bryzgalov, I.A. (2006) Cation-exchange properties of natural zeolite-like sodium zirconosilicates: an experimental study in aqueous solutions at 80–90°C and 1 atm. Abstracts, 19th General Meeting of IMA. Kobe, Japan, p. 280.Google Scholar
Vladykin, N.V., Kovalenko, V.I. and Dorfman, M.D. (1981) Mineralogical and Geochemical Features of the Khan Bogdo Massif of Alkaline Granites. Nauka Publishing, Moscow, 136 pp. [in Russian].Google Scholar
Yakovenchuk, V.N., Ivanyuk, G.Yu., Pakhomovsky, Ya.A. and Men'shikov, Yu.P. (2005) Khibiny. Laplandia Minerals Ltd, Apatity, Russia, 467 pp.Google Scholar
Zubkova, N.V., Ksenofontov, D.A., Kabalov, Yu.K., Chukanov, N.V. and Nedel'ko, V.V. (2011) Dehydration-induced structural transformations of the microporous zirconosilicate elpidite. Inorganic Materials, 47, 506512.CrossRefGoogle Scholar
Zubkova, N.V., Nikolova, R.P., Chukanov, N.V., Kostov-Kytin, V.V., Pekov, I.V., Varlamov, D.A., Larikova, T.S., Kazheva, O.N., Chervonnaya, N.A., Shilov, G.V. and Pushcharovsky, D.Yu. (2019) Crystal chemistry and properties of elpidite and its Ag-exchanged forms. Minerals, 9, paper 420, 116.CrossRefGoogle Scholar
Supplementary material: File

Zubkova et al. supplementary material

Zubkova et al. supplementary material

Download Zubkova et al. supplementary material(File)
File 608 KB