Hostname: page-component-848d4c4894-hfldf Total loading time: 0 Render date: 2024-06-08T08:24:20.940Z Has data issue: false hasContentIssue false

Enricofrancoite, KNaCaSi4O10, a new Ca–K–Na silicate from Somma–Vesuvius volcano, southern Italy

Published online by Cambridge University Press:  26 February 2024

Giuseppina Balassone
Affiliation:
Department of Earth Science, Environment and Resources (DiSTAR), University of Naples Federico II, Via Cintia, 26, Naples I-80126, Italy Center for Research on Archaeometry and Conservation Science (CRACS), University of Naples Federico II, Via Cintia, 26, Naples I-80126, University of Sannio, Via dei Mulini 73, Benevento I-82100, Italy National Institute of Geophysics and Volcanology (INGV), Vesuvius Observatory, Via Diocleziano I-80124 Naples, Italy
Taras L. Panikorovskii*
Affiliation:
Kola Science Centre, Russian Academy of Sciences, 14 Fersman Street, Apatity 184200, Russia Department of Crystallography, St. Petersburg State University, 7–9 Universitetskaya Naberezhnaya, St. Petersburg 199034, Russia
Annamaria Pellino
Affiliation:
Department of Earth Science, Environment and Resources (DiSTAR), University of Naples Federico II, Via Cintia, 26, Naples I-80126, Italy
Ayya V. Bazai
Affiliation:
Kola Science Centre, Russian Academy of Sciences, 14 Fersman Street, Apatity 184200, Russia
Vladimir N. Bocharov
Affiliation:
Geo Environmental Centre “Geomodel”, Saint-Petersburg State University, 1 Ul'yanovskay Str., St. Petersburg 198504, Russia
Olga F. Goychuk
Affiliation:
Kola Science Centre, Russian Academy of Sciences, 14 Fersman Street, Apatity 184200, Russia
Evgenia Yu. Avdontseva
Affiliation:
Department of Crystallography, St. Petersburg State University, 7–9 Universitetskaya Naberezhnaya, St. Petersburg 199034, Russia
Victor N. Yakovenchuk
Affiliation:
Department of Crystallography, St. Petersburg State University, 7–9 Universitetskaya Naberezhnaya, St. Petersburg 199034, Russia
Sergey V. Krivovichev
Affiliation:
Department of Crystallography, St. Petersburg State University, 7–9 Universitetskaya Naberezhnaya, St. Petersburg 199034, Russia
Carmela Petti
Affiliation:
Centro Museale “Centro Musei delle Scienze Naturali e Fisiche”, University of Naples Federico II, Via Mezzocannone 8, 80134 Napoli, Italy
Piergiulio Cappelletti
Affiliation:
Department of Earth Science, Environment and Resources (DiSTAR), University of Naples Federico II, Via Cintia, 26, Naples I-80126, Italy Center for Research on Archaeometry and Conservation Science (CRACS), University of Naples Federico II, Via Cintia, 26, Naples I-80126, University of Sannio, Via dei Mulini 73, Benevento I-82100, Italy Centro Museale “Centro Musei delle Scienze Naturali e Fisiche”, University of Naples Federico II, Via Mezzocannone 8, 80134 Napoli, Italy
Nicola Mondillo
Affiliation:
Department of Earth Science, Environment and Resources (DiSTAR), University of Naples Federico II, Via Cintia, 26, Naples I-80126, Italy
Anna Moliterni
Affiliation:
Istituto di Cristallografia, CNR, Via Amendola 122/O, 70126 Bari, Italy
Angela Altomare
Affiliation:
Istituto di Cristallografia, CNR, Via Amendola 122/O, 70126 Bari, Italy
Francesco Izzo
Affiliation:
Department of Earth Science, Environment and Resources (DiSTAR), University of Naples Federico II, Via Cintia, 26, Naples I-80126, Italy Center for Research on Archaeometry and Conservation Science (CRACS), University of Naples Federico II, Via Cintia, 26, Naples I-80126, University of Sannio, Via dei Mulini 73, Benevento I-82100, Italy
*
Corresponding author: Taras L. Panikorovskii; Email: t.panikorovskii@ksc.ru

Abstract

Enricofrancoite (IMA2023–002), ideally KNaCaSi4O10, is a new litidionite-group member found as the product of high-temperature alteration of hosting silicates with the enrichment by Cu-bearing fluids at the rock–fumaroles interface related to the 1872 eruption of Somma–Vesuvius volcano, southern Italy. It occurs as euhedral and platy crystals or crusts together with litidionite, tridymite, wollastonite and Al- and Fe-bearing diopside, kamenevite, perovskite, rutile, Ti-rich magnetite and colourless Si-glass. Single crystals of enricofrancoite are transparent colourless or light blue with a vitreous lustre. Mohs hardness is 5.5. Dmeas is 2.63(3) g/cm3 and Dcalc is 2.63 g/cm3. The mineral is optically biaxial (−), α = 1.542(5), β = 1.567(5),γ = 1.575(5); 2V(meas) = 60(2)° and 2Vcalc = 58°. The mean chemical composition (wt.%, electron-microprobe data) is: SiO2 64.81, Al2O3 0.03, TiO2 0.08, FeO 0.07, MgO 1.71, CaO 10.64, CuO 2.22, Na2O 8.56, K2O 11.41, total 99.94. The empirical formula based on 10 O apfu is: K0.90Na1.03(Ca0.71Mg0.16Cu0.10)Σ0.97Si4.02O10. The Raman spectrum contains bands at 133, 248, 265, 290, 335, 400, 438, 510, 600, 690 and 1120 cm–1 and the wavenumbers of the IR absorption bands are: 424, 470, 492, 530, 600, 630, 690, 750, 788, 970, 1040 and 1160 cm–1. The eight strongest lines of the powder X-ray diffraction pattern are [d, Å (I, %) hkl]: 6.75 (42) 01$\bar{1}$, 3.65 (20) 11$\bar{2}$, 3.370 (100) 02$\bar{2}$, 3.210 (52) 102, 3.051 (18) 111, 3.033 (25) 2$\bar{1}\bar{2}$, 2.834 (22) 02$\bar{3}$ and 2.411 (72) 03$\bar{2}$. Enricofrancoite is triclinic, space group P$\bar{1}$, unit-cell parameters refined from the single-crystal data are a = 7.0155(4) Å, b = 8.0721(4) Å, c = 10.0275(4) Å, α = 104.420(4)°, β = 99.764(4)°, γ = 115.126(5)° and V = 472.74(5) Å3. The crystal structure has been refined from single-crystal X-ray diffraction data to R1 = 0.035 on the basis of 2078 independent reflections with Fo > 4σ(Fo). Enricofrancoite is an H2O-free analogue of calcinaksite with 5-coordinated Ca2+ at the M site.

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

References

Agilent Technologies (2014) CrysAlis CCD and CrysAlis RED. Oxford Diffraction Ltd, Yarnton, Oxfordshire.Google Scholar
Aksenov, S.M., Rastsvetaeva, R.K., Chukanov, N. V. and Kolitsch, U. (2014) Structure of calcinaksite KNa[Ca(H2O)][Si4Ol0], the first hydrous member of the litidionite group of silicates with [Si8O20]8− tubes. Acta Crystallographica, B70, 768775.Google Scholar
Armbruster, T., Gnos, E., Dixon, R., Gutzmer, J., Hejny, C., Döbelin, N. and Medenbach, O. (2002) Manganvesuvianite and tweddillite, two new Mn3+-silicate minerals from the Kalahari manganese fields, South Africa. Mineralogical Magazine, 66, 121135.CrossRefGoogle Scholar
Balassone, G., Talla, D., Beran, A., Mormone, A., Altomare, A., Moliterni, A., Mondillo, N., Saviano, M. and Petti, C. (2011) Vesuvianite from Somma-Vesuvius volcano (southern Italy): Chemical, X-ray diffraction and single-crystal polarized FTIR investigations. Periodico di Mineralogia, 80, 369384.Google Scholar
Balassone, G., Petti, C., Mondillo, N., Panikorovskii, T.L., de Gennaro, R., Cappelletti, P., Altomare, A., Corriero, N., Cangiano, M. and D'Orazio, L. (2019) Copper Minerals at Vesuvius Volcano (Southern Italy): A Mineralogical Review. Minerals, 9, 730.CrossRefGoogle Scholar
Balassone, G., Panikorovskii, T.L., Pellino, A., Bazai, A.V., Bocharov, V.N., Krivovichev, S.V., Petti, C., Cappelletti, P. and Mondillo, N. (2022) The complex mechanism of Ti4+ incorporation into litidionite from the Somma–Vesuvius volcano, Italy. Mineralogical Magazine, 86, 222233.CrossRefGoogle Scholar
Balassone, P., Panikorovskii, T.L., Pellino, A., Bazai, A.V., Bocharov, V.N., Goychuk, O.F., Avdontseva, E.Y., Yakovenchuk, V.N., Krivovichev, S.V., Petti, C., Cappelletti, P.A., Mondillo, N., Moliterni, A. and Altomare, A. (2023) Enricofrancoite, IMA 2023-002. CNMNC Newsletter 74. Mineralogical Magazine, 87, 783787. https://doi.org/10.1180/mgm.2023.54.Google Scholar
Baur, W.H. (1974) The geometry of polyhedral distortions. Predictive relationships for the phosphate group. Acta Crystallographica, B30, 11951215.CrossRefGoogle Scholar
Brandão, P., Rocha, J., Reis, M.S., dos Santos, A.M. and Jin, R. (2009) Magnetic properties of compounds. Journal of Solid State Chemistry, 182, 253258.CrossRefGoogle Scholar
Brese, N.E. and O'Keefe, M. (1991) Bond-valence parameters for solids. Acta Crystallographica, B47, 192197.CrossRefGoogle Scholar
Chukanov, N.V., Aksenov, S.M., Rastsvetaeva, R.K., Blass, G., Varlamov, D.A., Pekov, I.V., Belakovskiy, D.I. and Gurzhiy, V.V. (2015) Calcinaksite, KNaCa(Si4O10) H2O, a new mineral from the Eifel volcanic area, Germany. Mineralogy and Petrology, 109, 397404.CrossRefGoogle Scholar
Day, M.C. and Hawthorne, F.C. (2020) A structure hierarchy for silicate minerals: chain, ribbon, and tube silicates. Mineralogical Magazine, 84, 165244.CrossRefGoogle Scholar
de Gennaro, M. and Franco, E. (1974) La K-Cabasite di alcuni «tufi del Vesuvio». Atti della Accademia Nazionale dei Lincei, 60, 490497.Google Scholar
Dolivo-Dobrovolsky, D.D. (2016) MINAL, free software. Saint-Petersburg, Russia. <http://www.dimadd.ru>.Google Scholar
Dolomanov, O. V., Bourhis, L.J., Gildea, R.J., Howard, J.A.K. and Puschmann, H. (2009) OLEX2 : a complete structure solution, refinement and analysis program. Journal of Applied Crystallography, 42, 339341.CrossRefGoogle Scholar
Durand, G., Vilminot, S., Richard-Plouet, M., Derory, A., Lambour, J.P. and Drillon, M. (1997) Magnetic behavior of Na2MSi4O10 (M=Co, Ni) compounds. Journal of Solid State Chemistry, 131, 335340.CrossRefGoogle Scholar
Franco, E. and de Gennaro, M. (1988) Panunzite; a new mineral from Mt. Somma-Vesuvio, Italy. American Mineralogist, 73, 420421.Google Scholar
Galuskin, E. V., Lazic, B., Armbruster, T., Galuskina, I.O., Pertsev, N.N., Gazeev, V.M., Wlodyka, R., Dulski, M., Dzierzanowski, P., Zadov, A.E. and Dubrovinsky, L.S. (2012) Edgrewite Ca9(SiO4)4F2-hydroxyledgrewite Ca9(SiO4)4(OH)2, a new series of calcium humite-group minerals from altered xenoliths in the ignimbrite of Upper Chegem caldera, Northern Caucasus, Kabardino-Balkaria, Russia. American Mineralogist, 97, 19982006.CrossRefGoogle Scholar
Golovachev, V.P., Drozdov, Y.N., Kuz'min, E.A. and Belov, N.V. (1970) The crystal structure of fenaksite, NaKFeSi4O10. Doklady Akademii Nauk SSSR, 194, 818820 [in Russian].Google Scholar
Groat, L.A., Hawthorne, F.C. and Ercit, T.S. (1992) The chemistry of Vesuvianite. The Canadian Mineralogist, 30, 1948.Google Scholar
Hawthorne, F.C. and Ferguson, R.B. (1975) Refinement of the crystal structure of kröhnkite. Acta Crystallographica, B31, 17531755.CrossRefGoogle Scholar
Holland, T.J.B. and Redfern, S.A.T. (1997) Unit cell refinement from powder diffraction data: the use of regression diagnostics. Mineralogical Magazine, 61, 6577.CrossRefGoogle Scholar
Karimova, O. and Burns, P.C. (2008) Silicate tubes in the crystal structure of manaksite. Pp. 153156 in: Minerals as Advanced Materials I. Springer Berlin Heidelberg, Berlin, Heidelberg.CrossRefGoogle Scholar
Katz, A.K., Glusker, J.P., Beebe, S.A. and Bock, C.W. (1996) Calcium ion coordination: a comparison with that of beryllium, magnesium, and zinc. Journal of the American Chemical Society, 118, 57525763.CrossRefGoogle Scholar
Khomyakov, A.P., Kurova, T.A. and Nechelyustov, G.N. (1992) Manaksite NaKMnSi4O10: a new mineral. Zapiski RMO, 121, 112114.Google Scholar
Kornev, A.N., Maksimov, B.A., Lider, V.V., Ilyukhin, V.V. and Belov, N.V. (1972) Crystal structure of Na2CuSi4O10. Soviet Physics Doklady, 17, 735737.Google Scholar
Lafuente, B., Downs, R.T., Yang, H. and Stone, N. (2015) The power of databases: the RRUFF project. Pp. 130 in: Highlights in Mineralogical Crystallography (Armbruster, T. and Danisi, R.M., editors). W. De Gruyter, Berlin, Germany.Google Scholar
Liebau, F. (1985) Structural Chemistry of Silicates. Springer, Berlin, Heidelberg.CrossRefGoogle Scholar
Mandarino, J.A. (2007) The Gladstone-Dale compatibility of minerals and its use in selecting mineral species for further study. The Canadian Mineralogist, 45, 13071324.CrossRefGoogle Scholar
McCusker, L.B., Liebau, F. and Engelhardt, G. (2003) Nomenclature of structural and compositional characteristics of ordered microporous and mesoporous materials with inorganic hosts. Microporous and Mesoporous Materials, 58, 313.CrossRefGoogle Scholar
Merlino, S., Franco, E., Mattia, C.A., Pasero, M. and De Gennaro, M. (1985) The crystal structure of panunzite (natural tetrakalsilite). Neues Jahrbuch Fur Mineralogie Monatshefte, 7, 322328.Google Scholar
Momma, K. and Izumi, F. (2011) VESTA 3 for three-dimensional visualization of crystal, volumetric and morphology data. Journal of Applied Crystallography, 44, 12721276.CrossRefGoogle Scholar
Ohkawa, M., Yoshiasa, A. and Takeno, S. (1992) Crystal chemistry of vesuvianite: site preferences of square- pyramidal coordinated sites. American Mineralogist, 77, 945953.Google Scholar
Pakhomovsky, Y.A., Panikorovskii, T.L., Yakovenchuk, V.N., Ivanyuk, G.Yu., Mikhailova, J.A., Krivovichev, S.V., Bocharov, V.N. and Kalashnikov, A.O. (2018) Selivanovaite, NaTi3(Ti,Na,Fe,Mn)4[(Si2O7)2O4(OH,H2O)4]⋅nH2O, a new rock-forming mineral from the eudialyte-rich malignite of the Lovozero alkaline massif (Kola Peninsula, Russia). European Journal of Mineralogy, 30, 525535.CrossRefGoogle Scholar
Panikorovskii, T.L., Chukanov, N.V., Aksenov, S.M., Mazur, A.S., Avdontseva, E.Yu., Shilovskikh, V.V. and Krivovichev, S.V. (2017a) Alumovesuvianite, Ca19Al(Al,Mg)12Si18O69(OH)9, a new vesuvianite-group member from the Jeffrey mine, asbestos, Estrie region, Québec, Canada. Mineralogy and Petrology, 111, 833842.CrossRefGoogle Scholar
Panikorovskii, T.L., Chukanov, N.V., Rusakov, V.S., Shilovskikh, V.V., Mazur, A.S., Balassone, G., Ivanyuk, G.Yu. and Krivovichev, S.V. (2017b) Vesuvianite from the Somma-Vesuvius Complex: New Data and Revised Formula. Minerals, 7, 248.CrossRefGoogle Scholar
Panikorovskii, T.L., Shilovskikh, V.V., Avdontseva, E.Yu., Zolotarev, A.A., Karpenko, V.Yu., Mazur, A.S., Yakovenchuk, V.N., Bazai, A.V., Krivovichev, S.V. and Pekov, I.V. (2017c) Magnesiovesuvianite, Ca19Mg(Al,Mg)12Si18O69(OH)9, a new vesuvianite-group mineral. Journal of Geosciences (Czech Republic), 62, 2536.CrossRefGoogle Scholar
Panikorovskii, T.L., Shilovskikh, V.V., Avdontseva, E.Yu., Zolotarev, A.A., Pekov, I.V., Britvin, S.N., Hålenius, U. and Krivovichev, S.V. (2017d) Cyprine, Ca19Cu2+(Al,Mg,Mn)12Si18O69(OH)9, a new vesuvianite-group mineral from the Wessels mine, South Africa. European Journal of Mineralogy, 29, 295306.CrossRefGoogle Scholar
Pekov, I.V., Zubkova, N.V., Belakovskiy, D.I., Lykova, I.S., Yapaskurt, V.O., Vigasina, M.F., Sidorov, E.G. and Pushcharovsky, D.Yu. (2015) Sanguite, KCuCl3, A new mineral from the Tolbachik Volcano, Kamchatka, Russia. The Canadian Mineralogist, 53, 633641.CrossRefGoogle Scholar
Pozas, J.M., Rossi, G. and Tazzoli, V. (1975) Re-examination and crystal structure analysis of litidionite. American Mineralogist, 60, 471474.Google Scholar
Rainho, J.P., Carlos, L.D. and Rocha, J. (2000) New phosphors based on Eu3+-doped microporous titanosilicates. Journal of Luminescence, 87–89, 10831086.CrossRefGoogle Scholar
Rozhdestvenskaya, I.V., Bannova, I.I., Nikishova, L.V. and Soboleva, T.V. (2004) The crystal structure of fenaksite K2Na2Fe2Si8O20. Doklady of the Russian Academy of Sciences, 398, 10291033.Google Scholar
Scacchi, E. (1880) Lapilli azzurri del Vesuvio. Rendiconto dell'Accademia delle Scienze Fisiche e Matematiche, 19, 175179.Google Scholar
Sheldrick, G.M. (2015) Crystal structure refinement with SHELXL. Acta Crystallographica, C71, 38.Google Scholar
Siidra, O.I., Lukina, E.A., Nazarchuk, E.V., Depmeier, W., Bubnova, R.S., Agakhanov, A.A., Avdontseva, E.Yu., Filatov, S.K. and Kovrugin, V.M. (2018) Saranchinaite, Na2Cu(SO4)2, a new exhalative mineral from Tolbachik volcano, Kamchatka, Russia, and a product of the reversible dehydration of kröhnkite, Na2Cu(SO4)2(H2O)2. Mineralogical Magazine, 82, 257274.CrossRefGoogle Scholar
Yakovenchuk, V., Pakhomovsky, Y., Panikorovskii, T., Zolotarev, A., Mikhailova, J., Bocharov, V., Krivovichev, S. and Ivanyuk, G. (2019) Chirvinskyite, (Na,Ca)13(Fe,Mn,□)2(Ti,Nb)2(Zr,Ti)3–(Si2O7)4(OH,O,F)12, a new mineral with a modular wallpaper structure, from the Khibiny Alkaline Massif (Kola Peninsula, Russia). Minerals, 9, 219.CrossRefGoogle Scholar
Supplementary material: File

Balassone et al. supplementary material

Balassone et al. supplementary material
Download Balassone et al. supplementary material(File)
File 179.5 KB