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Bobshannonite, Na2KBa(Mn,Na)8(Nb,Ti)4(Si2O7)4O4(OH)4(O,F)2, a new TS-block mineral from Mont Saint-Hilaire, Québec, Canada: Description and crystal structure

Published online by Cambridge University Press:  02 January 2018

E. Sokolova*
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada
F. Cámara
Affiliation:
Dipartimento di Scienze della Terra, Università di Torino, I-10125, Torino, Italy CrisDi – Interdepartmental Center for Crystallography, via Giuria 7, 10126, Torino, Italy
Y.A. Abdu
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada
F.C. Hawthorne
Affiliation:
Department of Geological Sciences, University of Manitoba, Winnipeg, MB, R3T 2N2, Canada
L. Horváth
Affiliation:
594 Main Road, Hudson Heights, Québec J0P 1J0, Canada
E. Pfenninger-Horváth
Affiliation:
594 Main Road, Hudson Heights, Québec J0P 1J0, Canada
*

Abstract

Bobshannonite, Na2KBa(Mn,Na)8(Nb,Ti)4(Si2O7)4O4(OH)4(O,F)2, is a new TS-block mineral from Mont Saint-Hilaire, Québec, Canada. It occurs as blocky crystals 0.5–1 mm across,perched on sérandite and albite. Other associated minerals are epididymite, catapleiite, aegirine, kupletskite, rhodochrosite and rhabdophane-(Ce). Bobshannonite occurs as vitreous to frosty, transparent to translucent very pale brown to orange brown crystals, has a very pale brown streak, hackly fracture and does not fluoresce under cathode or ultraviolet light. Cleavage is {001} very good, no parting was observed, Mohs hardness is ∼4, it is brittle and Dcalc. = 3.787 g/cm3. Crystals are twinned extensively and do not extinguish in cross-polarized light. Bobshannonite is triclinic, C1, a = 10.839(6), b = 13.912(8), c = 20.98(1) Å, α = 89.99(1), β = 95.05(2), γ = 89.998(9)°, V = 3152(5) Å3. The six strongest reflections in the powder X-ray diffraction data [d (Å),I, (hkl)] are: 2.873, 100, (241, 241, 044, 044, 241, 241); 3.477, 60, (006); 3.193, 59, (224, 224); 2.648, 40, (402, 243, 243); 2.608, 35, (008, 226, 226); 1.776, 30, (249). Chemical analysis by electron microprobe gave Ta2O5 0.52, Nb2O5 19.69,TiO2 5.50, SiO2 26.31, Al2O3 0.06, BaO 7.92, ZnO 1.02, FeO 0.89, MnO 26.34, MgO 0.06, Rb2O 0.42, K2O 2.38, Na2O 4.05, F 0.70, H2Ocalc. 1.96, O = –0.29, total 97.53 wt.%, where the H2O content was calculated from the crystal-structure analysis. The empirical formula on the basis of 38 anions is Na1.89(K0.93Rb0.08)Σ1.01Ba0.95(Mn6.85Na0.52Zn0.23Fe0.232+Mg0.03Al0.02)Σ7.88(Nb2.73Ti1.27Ta0.04)Σ4.04(Si8.07O28)O9.32H4.01F0.68,Z = 4. The crystal structure was refined to R1 = 2.55% on the basis of 7277 unique reflections [F > 4σ(F)] and can be described as a combination of a TS (Titanium Silicate) block and an I (Intermediate) block. The TS block consists ofHOH sheets (H – heteropolyhedral, O – octahedral). The topology of the TS block is as in Group II of the Ti disilicates: Ti + Nb = 2 a.p.f.u. per (Si2O7)2 [as defined by Sokolova (2006)]. In the O sheet, ten[6]MO sitesare occupied mainly by Mn, less Na and minor Zn, Fe2+, Mg and Al, with <MO–ϕ> = 2.223 Å. In the H sheet, four [6]MH sites are occupied by Nb and Ti (Nb > Ti), with <MH–ϕ> = 1.975 Å,and eight [4]Si sites are occupied by Si, with <Si–O> = 1.625 Å. The MH octahedra and Si2O7 groups constitute the H sheet. The TS blocks link via common vertices of MH octahedra. In the I block, Ba and Kare ordered at the AP(1) and AP(2) sites with Ba:K = 1:1 and the two BP sites are occupied by Na. The ideal composition of the I block is Na2KBa a.p.f.u. Bobshannonite, perraultite, surkhobite and jinshajiangite are topologically identical Group-II TS-block minerals. Bobshannonite is the Nb-analogue of perraultite. The mineral is named bobshannonite after Dr. Robert (Bob) D. Shannon (b. 1935), in recognition of his major contributions to the field of crystal chemistry in particular and mineralogy in general through his development of accurate and comprehensive ionic radii and his work on dielectric properties of minerals.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2015

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References

Aksenov, S.M., Rastsvetaeva, R.K. and Chukanov, N.V. (2014) The crystal structure of emmerichite Ba2Na3Fe3+ Ti2(Si2O7)2O2F2, a new lamprophyllite-group mineral. Zeitschriftfür Kristallographie, 229(1), 1-7.Google Scholar
Brown, I.D. (1981) The bond valence method: an empirical approach to chemical structure and bonding. Pp. 1-30 in: Structure and Bonding in Crystals II (M. O'Keeffe and A. Navrotsky, editors). Academic Press, New York.Google Scholar
Cámara, F., Sokolova, E. andNieto, F (2009) Cámaraite,2 +II. The crystal structure and crystal chemistry of a new group-II Ti-disilicate mineral. Mineralogical Magazine, 73, 855870.CrossRefGoogle Scholar
Cámara, F., Sokolova, E., Abdu, Y and Hawthorne, F.C. (2010) The crystal structures of niobophyllite, kupletskite-(Cs) and Sn-rich astrophyllite; revisions to the crystal chemistry of the astrophyllite-group minerals. The Canadian Mineralogist, 48, 116.CrossRefGoogle Scholar
Cámara, F., Sokolova, E., Abdu, Y.A., Hawthorne, F.C. and Khomyakov, A.P. (2013) Kolskyite, (Cap) Na2Ti4(Si2O7)2O4(H2O)7, a Group-IV Ti-disilicate mineral from the Khibiny alkaline massif, Kola Peninsula, Russia: description and crystal structure. The Canadian Mineralogist, 51, 921936.CrossRefGoogle Scholar
Cámara, F., Sokolova, E., Abdu, Y.A. and Hawthorne, F.C. (2014) Saamite, BanTiNbNa3Ti(Si2O7)2O2(OH)2 (H2O)2, a Group-III Ti-disilicate mineral from the Khibiny alkaline massif, Kola Peninsula, Russia: Description and crystal structure. The Canadian Mineralogist, 52, 745761.CrossRefGoogle Scholar
Chao, G.Y (1991) Perraultite, a new hydrous Na-K-Ba-Mn-Ti-Nb silicate species from Mont Saint-Hilaire, Québec. The Canadian Mineralogist, 29, 355358.Google Scholar
Guan, Ya-Syan, Simonov, V.I. and Belov, N.V. (1963) Crystal structure of bafertisite, BaFe2TiO[Si2O7](OH)2. Doklady Akademii Nauk SSSR, 149, 14161419 [in Russian].Google Scholar
Hong, W. and Fu, P. (1982) Jinshajiangite, anew Ba-Mn-Fe-Ti-bearing silicate mineral. Geochemistry (China), 1, 458464.Google Scholar
Pekov, I.V., Belovitskaya, Yu.V., Kartashov, P.M., Chukanov, N.V., Yamnova, N.A. and Egorov-Tismenko, Yu.K. (1999) The new data on perraultite (the Azov Sea region). Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva, 128, 112120 [in Russian].Google Scholar
Pouchou, J.L. and Pichoir, F. (1985) “PAP” (jρΖ) procedure for improved quantitative microanalysis. Pp. 104-106 in: Microbeam Analysis (J.T. Armstrong, editor). San Francisco Press, San Francisco, California, USA.Google Scholar
Rastvetaeva, R.K., Eskova, E.M., Dusmatov, V.D., Chukanov, N.V and Schneider, F. (2008) Surkhobite: revalidation and redefinition with the new formula, (Ba,K)2CaNa(Mn,Fe2 + ,Fe3+)8Ti4(Si2O7)4O4(F,OH,O)6 . European Journal of Mineralogy, 20, 289295.CrossRefGoogle Scholar
Shannon, R.D. (1976) Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides. Acta Crystallographica, A32, 751767.CrossRefGoogle Scholar
Sheldrick, G.M. (2008) A short history of SHELX. Acta Crystallographica, A64, 112122.CrossRefGoogle Scholar
Sokolova, E. (2006) From structure topology to chemical composition. I. Structural hierarchy and stereochemistry in titanium disilicate minerals. The Canadian Mineralogist, 44, 12731330.CrossRefGoogle Scholar
Sokolova, E. and Cámara, F. (2013) From structure topology to chemical composition. XVI. New developments in the crystal chemistry and prediction of new structure topologies for titanium disilicate minerals with the TS block. The Canadian Mineralogist, 51, 861891.CrossRefGoogle Scholar
Sokolova, E., Cámara, F., Hawthorne, F.C. and Abdu, Y. (2009a) From structure topology to chemical composition. VII. Titanium silicates: the crystal structure and crystal chemistry of jinshajiangite. European Journal of Mineralogy, 21, 871883.CrossRefGoogle Scholar
Sokolova, E., Abdu, Y., Hawthorne, F.C., Stepanov, A.V., Bekenova, G.K. and Kotel'nikov, P.E. (2009b) Cámaraite, Ba3NaTi4(Fe2+,Mn)8(Si2O7)4O4(OH,F)7. I. A new titanium-silicate mineral from the Verkhnee Espe deposit, Akjailyautas Mountains, Kazakhstan. Mineralogical Magazine, 73, 847854.CrossRefGoogle Scholar
Sokolova, E., Abdu, Y.A., Hawthorne, F.C., Genovese, A., Cámara, F and Khomyakov, A.P. (2015) From structure topology to chemical composition. XVIII. Titanium silicates: revision of the crystal structure and chemical formula of betalomonosovite, a Group-IV TS-block mineral from the Lovozero alkaline massif, Kola Peninsula, Russia. The Canadian Mineralogist, 53, 401428.CrossRefGoogle Scholar
VanNoorden, R., Maher, B. andNuzzo, R. (2014) The top 100 papers. Nature, 514, 550561.CrossRefGoogle Scholar
Wilson, A.J.C. (editor) (1992) International Tables for Crystallography. Volume C: Mathematical, physical and chemical tables. Kluwer Academic Publishers, Dordrecht, The Netherlands.Google Scholar
Yamnova, N.A., Egorov-Tismenko, Yu.K and Pekov, I.V. (1998) Crystal structure of perraultite from the coastal region ofthe Seaof Azov. Crystallography Reports, 43, 401–110.Google Scholar
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