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Popugaevaite, Ca3[B5O6(OH)6]FCl2·8H2O, a new phylloborate mineral

Published online by Cambridge University Press:  08 November 2024

Igor V. Pekov*
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
Natalia V. Zubkova
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
Ilya I. Chaikovskiy
Affiliation:
Mining Institute, Ural Branch of the Russian Academy of Sciences, Sibirskaya str., 78a, 614007 Perm, Russia
Nikita V. Chukanov
Affiliation:
Federal Research Center of Problems of Chemical Physics and Medicinal Chemistry of the Russian Academy of Sciences, 142432 Chernogolovka, Moscow, Russia
Dmitry I. Belakovskiy
Affiliation:
Fersman Mineralogical Museum of the Russian Academy of Sciences, Leninsky Prospekt 18-2, 119071 Moscow, Russia;
Vasiliy O. Yapaskurt
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
Yana V. Bychkova
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
Dmitry A. Ksenofontov
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
Elena P. Chirkova
Affiliation:
Mining Institute, Ural Branch of the Russian Academy of Sciences, Sibirskaya str., 78a, 614007 Perm, Russia
Sergey N. Britvin
Affiliation:
St Petersburg State University, Universitetskaya Nab. 7/9, 199034 St Petersburg, Russia
Dmitry Yu. Pushcharovsky
Affiliation:
Faculty of Geology, Moscow State University, Vorobievy Gory, 119991 Moscow, Russia
*
Corresponding author: Igor Pekov; Email: [email protected]

Abstract

The new mineral popugaevaite Ca3[B5O6(OH)6]FCl2·8H2O was found at the Internatsional’nyi diamond mine, Internatsional’naya kimberlite pipe, Sakha (Yakutia) Republic, Russia. It belongs to the low-temperature hydrothermal mineral assemblage formed in the contact zone between kimberlite and a boron-bearing halite rock. Popugaevaite occurs as veinlets in massive aggregates of ekaterinite and crusts (up to 0.7 mm thick and up to 1 cm × 4 cm in area) on ekaterinite nodules embedded in halite. Other associated minerals are Fe-rich szaibélyite, serpentine, dolomite, pyrrhotite and chalcopyrite. Crude prismatic crystals of popugaevaite are up to 0.3 × 1 mm. The mineral is transparent, colourless, with vitreous lustre and perfect {010} cleavage. It is optically biaxial (–), α 1.502(2), β 1.523(2), γ 1.530(2) and 2Vmeas = 50(10)°. The chemical composition (wt.%, electron-microprobe, boron by ICP-MS, H2O calculated by stoichiometry) is: CaO 28.54, B2O3 28.62, F 3.19, Cl 11.50, H2O 32.83, O = (F,Cl) –3.94, total 100.74. The empirical formula, calculated based on 23 O+F+Cl and 22 H atoms per formula unit, is Ca3.07B4.96O6.03(OH)6F1.01Cl1.96·8H2O. Popugaevaite is monoclinic, space group Pn, a = 8.7055(11), b = 8.1025(11), c = 14.812(2) Å, β = 91.367(7)°, V = 1044.5(2) Å3 and Z = 2. The strongest reflections of the powder X-ray diffraction pattern [d,Å(I,%)(hkl)] are: 8.12(100)(010), 4.058(27)(020), 3.577(15)($\bar 1$21), 2.936(10)(123), 2.834(16)(301, $\bar 1$05) and 2.283(10)(133). The crystal structure was solved based on single-crystal XRD data and refined on powder data by the Rietveld method, Rwp = 0.0058, Rp = 0.0043 and Robs = 0.0241. Popugaevaite is an isostructural analogue of brianroulstonite Ca3[B5O6(OH)6](OH)Cl2·8H2O with F instead of the OH group non-bound with boron. The structure is based upon the layers of twelve-membered rings of alternating BO3 triangles and BO2(OH)2 tetrahedra. The mineral is named in honour of the Russian geologist Larisa Anatol’evna Popugaeva (1923–1977), one of the principal discoverers of diamondiferous kimberlite pipes in Yakutia.

Type
Article
Copyright
© The Author(s), 2024. Published by Cambridge University Press on behalf of The Mineralogical Society of the United Kingdom and Ireland.

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Footnotes

Associate Editor: David Hibbs

Deceased 16 June 2020

References

Agashev, A.M., Nakai, S.I., Serov, I.V., Tolstov, A.V., Garanin, K.V. and Kovalchuk, O.E. (2018) Geochemistry and origin of the Mirny field kimberlites, Siberia. Mineralogy and Petrology, 112, 597608.Google Scholar
Agilent Technologies (2014) CrysAlisPro Software system, version 1.171.37.34. Agilent Technologies UK Ltd, Oxford, UK.Google Scholar
Brese, N.E. and O‘Keeffe, M. (1991) Bond-valence parameters for solids. Acta Crystallographica, B47, 192197.Google Scholar
Britvin, S.N., Dolivo-Dobrovolsky, D.V. and Krzhizhanovskaya, M.G. (2017) Software for processing the X-ray powder diffraction data obtained from the curved image plate detector of Rigaku RAXIS Rapid II diffractometer. Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 146, 104107 [in Russian].Google Scholar
Burns, P.C., Grice, J.D. and Hawthorne, F.C. (1995) Borate minerals. I. Polyhedral clusters and fundamental building blocks. The Canadian Mineralogist, 33, 11311151.Google Scholar
Chukanov, N.V. (2014) Infrared Spectra of Mineral Species: Extended Library. Springer-Verlag, Dordrecht, Netherlands, pp.Google Scholar
Chukanov, N.V. and Chervonnyi, A.D. (2016) Infrared Spectroscopy of Minerals and Related Compounds. Springer-Verlag, Cham, Switzerland, pp.Google Scholar
Crystal Impact (2014) Diamond – Crystal and Molecular Structure Visualization. Dr. H. Putz & Dr. K. Brandenburg GbR, Kreuzherrenstr. 102, 53227 Bonn, Germany, https://www.crystalimpact.de/diamond.Google Scholar
Gagné, O.C. and F.C, Hawthorne. (2015) Comprehensive derivation of bond-valence parameters for ion pairs involving oxygen. Acta Crystallographica, B71, 562578.Google Scholar
Grice, J.D., Burns, P.C. and Hawthorne, F.C. (1994) Determination of the megastructures of the borate polymorphs pringleite and ruitenbergite. The Canadian Mineralogist, 32, 114.Google Scholar
Grice, J.D., Gault, R.A. and Van Velthuizen, J. (1996) Penobsquisite: a new borate mineral with a complex framework structure. The Canadian Mineralogist, 34, 657665.Google Scholar
Grice, J.D., Gault, R.A. and van Velthuizen, J. (1997) Brianroulstonite: a new borate mineral with a sheet structure. The Canadian Mineralogist, 35, 751758.Google Scholar
Grice, J.D., Burns, P.C. and Hawthorne, F.C. (1999) Borate minerals. II. A hierarchy of structures based upon the borate fundamental building block. The Canadian Mineralogist, 37, 731762.Google Scholar
Grice, J.D., Gault, R.A. and Van Velthuizen, J. (2005) Borate minerals of the Penobsquis and Millstream deposits, Southern New Brunswick, Canada. The Canadian Mineralogist, 43, 14691487.Google Scholar
Kopylova, M.G., Kostrovitsky, S.I. and Egorov, K.N. (2013) Salts in southern Yakutian kimberlites and the problem of primary alkali kimberlite melts. Earth-Science Reviews, 119, 116.Google Scholar
Mandarino, J.A. (1981) The Gladstone-Dale relationship. Part IV. The compatibility concept and its application. The Canadian Mineralogist, 14, 498502.Google Scholar
Nikulin, I.I. and Eremeev, R.V. (2011) New finds of ekaterinite in kimberlites of Western Yakutia. Voronezh State University Geology Bulletin, 1, 95102 [in Russian].Google Scholar
Pekov, I.V., Zubkova, N.V., Ksenofontov, D.A., Chukanov, N.V., Yapaskurt, V.O., Korotchenkova, O.V., Chaikovskiy, I.I., Bocharov, V.M., Britvin, S.N. and Pushcharovsky, D.Yu. (2018) Redefinition of satimolite. Mineralogical Magazine, 82, 10331047.Google Scholar
Pekov, I.V., Zubkova, N.V., Chaikovskiy, I.I., Chukanov, N.V., Belakovskiy, D.I., Yapaskurt, V.O., Bychkova, Y.V., Ksenofontov, D.A., Chirkova, E.P., Britvin, S.N., and Pushcharovsky, D.Y. (2020) Popugaevaite, IMA 2019-115. CNMNC Newsletter No. 54. Mineralogical Magazine, 84, 359365, 10.1180/mgm.2020.21.Google Scholar
Petříček, V., Dušek, M. and Palatinus, L. (2006) Jana2006. Structure Determination Software Programs. Institute of Physics, Praha, Czech Republic.Google Scholar
Rezvukhin, D.I., Rashchenko, S.V., Sharygin, I.S., Malkovets, V.G., Alifirova, T.A., Pautov, L.A., Nigmatulina, E.N. and Seryotkin, Y.V. (2023) Botuobinskite and mirnyite, two new minerals of the crichtonite group included in Cr-pyrope xenocrysts from the Internatsionalnaya kimberlite. Mineralogical Magazine, 87, 433442.Google Scholar
Sheldrick, G.M. (2015) Crystal structure refinement with SHELXL. Acta Crystallographica, С71, 38.Google Scholar
Yakubovich, O.V., Massa, W. and Chukanov, N.V. (2008) Crystal structure of britvinite [Pb7(OH)3F(BO3)2(CO3)][Mg4.5(OH)3 (Si5O14)]: A new layered silicate with an original type of silicon–oxygen networks. Crystallography Reports, 53, 206215.Google Scholar
Zubkova, N.V., Pekov, I.V., Chukanov, N.V., Chaikovskiy, I.I., Yapaskurt, V.O. and Pushcharovsky, D.Yu. (2020) A new iron-rich variety of szaibélyite and its crystal chemical features. Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 149, 7279 [in Russian].Google Scholar
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