Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Enricofrancoite, KNaCaSi4O10, a new Ca-K-Na silicate from Somma-Vesuvius volcano, southern Italy. / Balassone, G.; 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.; Mondillo, N.; Moliterni, A.; Altomare, A.; Izzo, F.
в: Mineralogical Magazine, Том 88, № 3, 26.06.2024, стр. 277-287.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Enricofrancoite, KNaCaSi4O10, a new Ca-K-Na silicate from Somma-Vesuvius volcano, southern Italy
AU - Balassone, G.
AU - Panikorovskii, T.L.
AU - Pellino, A.
AU - Bazai, A.V.
AU - Bocharov, V.N.
AU - Goychuk, O.F.
AU - Avdontseva, E.Y.
AU - Yakovenchuk, V.N.
AU - Krivovichev, S.V.
AU - Petti, C.
AU - Cappelletti, P.
AU - Mondillo, N.
AU - Moliterni, A.
AU - Altomare, A.
AU - Izzo, F.
N1 - Export Date: 11 March 2024 Адрес для корреспонденции: Panikorovskii, T.L.; Kola Science Centre, 14 Fersman Street, Russian Federation; эл. почта: t.panikorovskii@ksc.ru Пристатейные ссылки: (2014) CrysAlis CCD and CrysAlis RED, , Agilent Technologies Oxford Diffraction Ltd, Yarnton, Oxfordshire; Aksenov, S.M., Rastsvetaeva, R.K., Chukanov, N.V., Kolitsch, U., Structure of calcinaksite KNa[Ca(H2O)][Si4Ol0], the first hydrous member of the litidionite group of silicates with [Si8O20]8− tubes (2014) Acta Crystallographica Section B Structural Science, Crystal Engineering and Materials, 70, pp. 768-775; Armbruster, T., Gnos, E., Dixon, R., Gutzmer, J., Hejny, C., Döbelin, N., Medenbach, O., Manganvesuvianite and tweddillite, two new Mn3+-silicate minerals from the Kalahari manganese fields, South Africa (2002) Mineralogical Magazine, 66, pp. 121-135; Balassone, G., Talla, D., Beran, A., Mormone, A., Altomare, A., Moliterni, A., Mondillo, N., Petti, C., Vesuvianite from Somma-Vesuvius volcano (southern Italy): Chemical, X-ray diffraction and single-crystal polarized FTIR investigations (2011) Periodico di Mineralogia, 80, pp. 369-384; Balassone, G., Petti, C., Mondillo, N., Panikorovskii, T.L., de Gennaro, R., Cappelletti, P., Altomare, A., D’Orazio, L., Copper Minerals at Vesuvius Volcano (Southern Italy): A Mineralogical Review (2019) Minerals, 9, p. 730; Balassone, G., Panikorovskii, T.L., Pellino, A., Bazai, A.V., Bocharov, V.N., Krivovichev, S.V., Petti, C., Mondillo, N., The complex mechanism of Ti4+ incorporation into litidionite from the Somma–Vesuvius volcano, Italy (2022) Mineralogical Magazine, 86, pp. 222-233; Balassone, P., Panikorovskii, T.L., Pellino, A., Bazai, A.V., Bocharov, V.N., Goychuk, O.F., Avdontseva, E.Y., Altomare, A., Enricofrancoite, IMA 2023-002. CNMNC Newsletter 74 (2023) Eur. J. Mineral, 35, pp. 659-664; Baur, W.H., The geometry of polyhedral distortions. Predictive relationships for the phosphate group (1974) Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry, 30, pp. 1195-1215; Brandão, P., Rocha, J., Reis, M.S., dos Santos, A.M., Jin, R., Magnetic properties of compounds (2009) Journal of Solid State Chemistry, 182, pp. 253-258; Brese, N.E., O’Keefe, M., Bond-valence parameters for solids (1991) Acta Crystallographica, B47, pp. 192-197; Chukanov, N.V., Aksenov, S.M., Rastsvetaeva, R.K., Blass, G., Varlamov, D.A., Pekov, I.V., Belakovskiy, D.I., Gurzhiy, V.V., Calcinaksite, KNaCa(Si4O10) H2O, a new mineral from the Eifel volcanic area, Germany (2015) Mineralogy and Petrology, 109, pp. 397-404; Day, M.C., Hawthorne, F.C., A structure hierarchy for silicate minerals: chain, ribbon, and tube silicates (2020) Mineralogical Magazine, 84, pp. 165-244; Dolivo-Dobrovolsky, D.D., (2016) MINAL, free software, , http://www.dimadd.ru, Saint-Petersburg. < >; Dolomanov, O.V., Bourhis, L.J., Gildea, R.J., Howard, J.A.K., Puschmann, H., OLEX2: a complete structure solution, refinement and analysis program (2009) Journal of Applied Crystallography, 42, pp. 339-341; Durand, G., Vilminot, S., Richard-Plouet, M., Derory, A., Lambour, J.P., Drillon, M., Magnetic Behavior of Na2MSi4O10 (M=Co, Ni) Compounds (1997) Journal of Solid State Chemistry, 131, pp. 335-340; Franco, E., de Gennaro, M., Panunzite; a new mineral from Mt. Somma-Vesuvio, Italy (1988) American Mineralogist, 73, pp. 420-421; Galuskin, E.V., Lazic, B., Armbruster, T., Galuskina, I.O., Pertsev, N.N., Gazeev, V.M., Wlodyka, R., Dubrovinsky, L.S., 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 (2012) American Mineralogist, 97, pp. 1998-2006; de Gennaro, M., Franco, E., La K-Cabasite di alcuni «tufi del Vesuvio (1974) Atti della Accademia Nazionale dei Lincei, 60, pp. 490-497; Golovachev, V.P., Drozdov, Y.N., Kuz’min, E.A., Belov, N.V., The crystal structure of fenaksite, NaKFeSi4O10 (1970) Doklady Akademii Nauk SSSR, 194, pp. 818-820. , Russian; Groat, L.A., Hawthorne, F.C., Ercit, T.S., The chemistry of Vesuvianite (1992) The Canadian Mineralogist, 30, pp. 19-48; Hawthorne, F.C., Ferguson, R.B., Refinement of the crystal structure of kröhnkite (1975) Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry, 31, pp. 1753-1755; Holland, T.J.B., Redfern, S.A.T., Unit cell refinement from powder diffraction data: the use of regression diagnostics (1997) Mineralogical Magazine, 61, pp. 65-77; Karimova, O., Burns, P.C., Silicate Tubes in the Crystal Structure of Manaksite (2008) Minerals as Advanced Materials I, pp. 153-156. , Springer Berlin Heidelberg, Berlin, Heidelberg; Katz, A.K., Glusker, J.P., Beebe, S.A., Bock, C.W., Calcium Ion Coordination: A Comparison with That of Beryllium, Magnesium, and Zinc (1996) Journal of the American Chemical Society, 118, pp. 5752-5763; Khomyakov, A.P., Kurova, T.A., Nechelyustov, G.N., Manaksite NaKMnSi4O10: a new mineral (1992) Zapiski RMO, 121, pp. 112-114; Kornev, A.N., Maksimov, B.A., Lider, V.V., Ilyukhin, V.V., Belov, N.V., Crystal structure of Na2CuSi4O10 (1972) Soviet Physics Doklady, 17, pp. 735-737; Lafuente, B., Downs, R.T., Yang, H., Stone, N., The power of databases: the RRUFF project (2015) Highlights in Mineralogical Crystallography, pp. 1-30; Liebau, F., (1985) Structural Chemistry of Silicates, , Springer Berlin Heidelberg, Berlin, Heidelberg; McCusker, L.B., Liebau, F., Engelhardt, G., Nomenclature of structural and compositional characteristics of ordered microporous and mesoporous materials with inorganic hosts (2003) Microporous and Mesoporous Materials, 58, pp. 3-13; Merlino, S., Franco, E., Mattia, C.A., Pasero, M., De Gennaro, M., The crystal structure of panunzite (natural tetrakalsilite) (1985) Neues Jahrbuch Fur Mineralogie Monatshefte, 7, pp. 322-328; Momma, K., Izumi, F., VESTA 3 for three-dimensional visualization of crystal, volumetric and morphology data (2011) Journal of Applied Crystallography, 44, pp. 1272-1276; Ohkawa, M., Yoshiasa, A., Takeno, S., Crystal chemistry of vesuvianite: site preferences of square- pyramidal coordinated sites (1992) American Mineralogist, 77, pp. 945-953; Pakhomovsky, Y.A., Panikorovskii, T.L., Yakovenchuk, V.N., Ivanyuk, G.Yu., Mikhailova, J.A., Krivovichev, S.V., Bocharov, V.N., Kalashnikov, A.O., 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) (2018) European Journal of Mineralogy, 30, pp. 525-535; Panikorovskii, T.L., Chukanov, N.V., Aksenov, S.M., Mazur, A.S., Avdontseva, E.Yu., Shilovskikh, V.V., Krivovichev, S.V., Alumovesuvianite, Ca19Al(Al,Mg)12Si18O69(OH)9, a new vesuvianite-group member from the Jeffrey mine, asbestos, Estrie region, Québec, Canada (2017) Mineralogy and Petrology, 111, pp. 833-842. , Mineralogy and Petrology; Panikorovskii, T.L., Shilovskikh, V.V., Avdontseva, E.Yu., Zolotarev, A.A., Pekov, I.V., Britvin, S.N., Hålenius, U., Krivovichev, S.V., Cyprine, Ca19Cu2+(Al,Mg,Mn)12Si18O69(OH)9, a new vesuvianite-group mineral from the Wessels mine, South Africa (2017) European Journal of Mineralogy, 29, pp. 295-306; Panikorovskii, T.L., Shilovskikh, V.V., Avdontseva, E.Yu., Zolotarev, A.A., Karpenko, V.Yu., Mazur, A.S., Yakovenchuk, V.N., Pekov, I.V., Magnesiovesuvianite, Ca19Mg(Al,Mg)12Si18O69(OH)9, a new vesuvianite-group mineral (2017) Journal of Geosciences (Czech Republic), 62, pp. 25-36; Panikorovskii, T.L., Chukanov, N.V., Rusakov, V.S., Shilovskikh, V.V., Mazur, A.S., Balassone, G., Ivanyuk, G.Yu., Krivovichev, S.V., Vesuvianite from the Somma-Vesuvius Complex: New Data and Revised Formula (2017) Minerals, 7, p. 248; Pekov, I.V., Zubkova, N.V., Belakovskiy, D.I., Lykova, I.S., Yapaskurt, V.O., Vigasina, M.F., Sidorov, E.G., Pushcharovsky, D.Yu., Sanguite, KCuCl3, A New Mineral From the Tolbachik Volcano, Kamchatka, Russia (2015) The Canadian Mineralogist, 53, pp. 633-641; Pozas, J.M., Rossi, G., Tazzoli, V., Re-examination and Crystal Structure Analysis of Litidionite (1975) American Mineralogist, 60, pp. 471-474; Rainho, J.P., Carlos, L.D., Rocha, J., New phosphors based on Eu3+-doped microporous titanosilicates (2000) Journal of Luminescence, 87-89, pp. 1083-1086; Rozhdestvenskaya, I.V., Bannova, I.I., Nikishova, L.V., Soboleva, T.V., The crystal structure of fenaksite K2Na2Fe2Si8O20 (2004) Dokladyof the Russian Academy of Sciences, 398, pp. 1029-1033; Scacchi, E., Lapilli azzurri del Vesuvio (1880) Rendiconto dell’Accademia delle Scienze Fisiche e Matematiche, 19, pp. 175-179; Sheldrick, G.M., Crystal structure refinement with SHELXL (2015) Acta Crystallographica Section C Structural Chemistry, 71, pp. 3-8; Siidra, O.I., Lukina, E.A., Nazarchuk, E.V., Depmeier, W., Bubnova, R.S., Agakhanov, A.A., Avdontseva, E.Yu., Kovrugin, V.M., 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 (2018) Mineralogical Magazine, 82, pp. 257-274; Yakovenchuk, V., Pakhomovsky, Y., Panikorovskii, T., Zolotarev, A., Mikhailova, J., Bocharov, V., Krivovichev, S., Ivanyuk, G., 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) (2019) Minerals, 9, p. 219
PY - 2024/6/26
Y1 - 2024/6/26
N2 - Enricofrancoite (IMA 2023-002), 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 colorless Si-glass. Single crystals of enricofrancoite are transparent colorless 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)Σ=0.97Si4.02O10. The Raman spectrum contains bands at 133, 248, 265, 290, 335, 400, 438, 510, 600, 690, 1120 cm-1 and the wavenumbers of the IR absorption bands are: 424, 470, 492, 530, 600, 630, 690, 750, 788, 970, 1040, 1160 cm-1. The eight strongest lines of the powder X-ray diffraction pattern are (I-d(A)-hkl): 42-6.75-01-1, 20-3.65-11-2, 100-3.370-02-2, 52-3.210-102, 18-3.051-111, 25-3.033-2-1-2, 22-2.834-02-3, 72-2.411-03-2. Enricofrancoite is triclinic, space group P-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),° 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. © 2024 Cambridge University Press. All rights reserved.
AB - Enricofrancoite (IMA 2023-002), 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 colorless Si-glass. Single crystals of enricofrancoite are transparent colorless 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)Σ=0.97Si4.02O10. The Raman spectrum contains bands at 133, 248, 265, 290, 335, 400, 438, 510, 600, 690, 1120 cm-1 and the wavenumbers of the IR absorption bands are: 424, 470, 492, 530, 600, 630, 690, 750, 788, 970, 1040, 1160 cm-1. The eight strongest lines of the powder X-ray diffraction pattern are (I-d(A)-hkl): 42-6.75-01-1, 20-3.65-11-2, 100-3.370-02-2, 52-3.210-102, 18-3.051-111, 25-3.033-2-1-2, 22-2.834-02-3, 72-2.411-03-2. Enricofrancoite is triclinic, space group P-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),° 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. © 2024 Cambridge University Press. All rights reserved.
KW - crystal structure
KW - enricofrancoite
KW - Italy
KW - litidionite group
KW - new mineral
KW - Somma-Vesuvius
KW - Absorption spectroscopy
KW - Alumina
KW - Aluminum oxide
KW - Copper oxides
KW - Feldspar
KW - Magnesia
KW - Magnetite
KW - Perovskite
KW - Potassium compounds
KW - Silica
KW - Silicon
KW - Single crystals
KW - Sodium compounds
KW - Ternary alloys
KW - Titanium dioxide
KW - Volcanoes
KW - Crystals structures
KW - Cu bearings
KW - Enricofrancoite
KW - Group members
KW - Highest temperature
KW - Litidionite group
KW - New mineral
KW - Southern Italy
KW - Crystal structure
UR - https://www.mendeley.com/catalogue/67452c80-55fb-31bc-acc7-0abdd0ef02f8/
U2 - 10.1180/mgm.2024.9
DO - 10.1180/mgm.2024.9
M3 - статья
VL - 88
SP - 277
EP - 287
JO - Mineralogical Magazine
JF - Mineralogical Magazine
SN - 0026-461X
IS - 3
ER -
ID: 117487485