From Structure Topology to Chemical Composition. XXX. Refinement of the Crystal Structure and Chemical Formula of Shkatulkalite, Na2Nb2Na3Ti(Si2O7)2O2(FO)(H2O)4(H2O)3, a Lamprophyllite-Group (Seidozerite Supergroup) TS-Block Mineral from the Lovozero Massif, Kola Peninsula, Russia

E. Sokolova, Maxwell C. Day, F. Hawthorne, F. Cámara
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引用次数: 2

Abstract

Shkatulkalite, ideally Na5TiNb2(Si2O7)2O3F(H2O)7, is a lamprophyllite-group (seidozerite supergroup) TS-block mineral from the Lovozero massif, Kola Peninsula, Russia. The crystal structure of shkatulkalite was refined as triclinic, space group P, a 5.464(1), b 7.161(1), c 15.573(1) Å, α 90.00(3), β 95.75(3), γ 90.00(3)°, V 606.3(4) Å3, R1 = 7.26%. The previously given chemical analysis has been modified to better fit the crystal structure: Nb2O5 24.15, TiO2 11.35, SiO2 27.22, BaO 1.15, SrO 2.20, MnO 1.68, CaO 0.46, K2O 0.29, Na2O 14.78, H2O 15.27, F 1.61, O = F −0.68, sum 99.48 wt.%; H2O was determined from structure-refinement results. The empirical formula was calculated on 25.27 (O + F) apfu (in accord with the crystal structure): (Na1.40Sr0.19Ba0.07K0.05)Σ1.71(Na2.86Mn0.10Ca0.07)Σ3.03(Nb1.62Ti1.27Mn0.11)Σ3Si4.03O24.52H15.11F0.75, Z = 1. The ideal structural formula is as follows: Na2Nb2Na3Ti(Si2O7)2O2(FO)(H2O)4(H2O)3. The crystal structure of shkatulkalite [basic structure type B5(LG)] is a combination of a TS (titanium-silicate) block and an I (intermediate) block. The TS block consists of HOH sheets (H-heteropolyhedral, O-octahedral). The TS block exhibits linkage and stereochemistry typical for the lamprophyllite group where Ti (+ Nb + Fe3+ + Mg) = 3 apfu. The O sheet is composed of Ti-dominant MO(1) and Na-dominant MO(2,3) octahedra. In the H sheet in shkatulkalite, Si2O7 groups link to Nb-dominant MH octahedra. The AP site occurs in the plane of the H sheet and splits into AP(1) and AP(2) sites, occupied by Na at 70% and Sr (less Ba and K) at 11%. The I block consists of H2O groups. The I block of shkatulkalite is topologically identical to those in the derivative structures of kazanskyite and nechelyustovite. The structure of the lamprophyllite-group mineral shkatulkalite has a counterpart structure in the murmanite group (Ti = 4 apfu): kolskyite, ideally Na2CaTi4(Si2O7)2O4(H2O)7 [basic structure type B7(MG)]: the two structures have TS blocks of different topology and similar I blocks, mainly occupied by H2O groups.
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从结构拓扑到化学成分。XXX。俄罗斯科拉半岛Lovozero地块钠2nb2na3ti (Si2O7)2O2(FO)(H2O)4(H2O)3煌斑岩群(Seidozerite超群)ts块状矿物Shkatulkalite晶体结构和化学式的细化
Shkatulkalite,理想名称为Na5TiNb2(Si2O7)2O3F(H2O)7,是一种产于俄罗斯科拉半岛Lovozero地块的煌斑岩群(seidozerite超群)ts块状矿物。shkatulkalite晶体结构为三斜晶,空间群P, a 5.464(1), b 7.161(1), c 15.573(1) Å, α 90.00(3), β 95.75(3), γ 90.00(3)°,V 606.3(4) Å3, R1 = 7.26%。先前给出的化学分析已被修改以更好地适应晶体结构:Nb2O5 24.15, TiO2 11.35, SiO2 27.22, BaO 1.15, SrO 2.20, MnO 1.68, CaO 0.46, K2O 0.29, Na2O 14.78, H2O 15.27, F 1.61, O = F−0.68,sum 99.48 wt.%;H2O由结构细化结果确定。在25.27 (O + F) apfu(符合晶体结构)上计算出经验公式:(Na1.40Sr0.19Ba0.07K0.05)Σ1.71(Na2.86Mn0.10Ca0.07)Σ3.03(Nb1.62Ti1.27Mn0.11)Σ3Si4.03O24.52H15.11F0.75, Z = 1。理想的分子式为:Na2Nb2Na3Ti(Si2O7)2O2(FO)(H2O)4(H2O)3。shkatulkalite的晶体结构[基本结构类型B5(LG)]是TS(硅酸钛)块体和I(中间)块体的组合。TS块由HOH片(h -杂多面体,o -八面体)组成。TS块具有典型的钛(+ Nb + Fe3+ + Mg) = 3 apfu的煌斑岩基团的连锁和立体化学特征。O片由ti -显性MO(1)和na -显性MO(2,3)八面体组成。在shkatulkalite的H薄片中,Si2O7基团与以nb为主的MH八面体相连。AP位点位于H片平面上,分为AP(1)和AP(2)两个位点,Na占70%,Sr(较少Ba和K)占11%。I区由H2O基团组成。什卡图尔石的I块体在拓扑结构上与喀山绢云石和绢云石的衍生构造相同。煌斑岩组矿物shkatulkalite的结构与硅长石组(Ti = 4 apfu)的结构相对应:kolskyite,理想为Na2CaTi4(Si2O7)2O4(H2O)7[基本结构类型B7(MG)]:两种结构具有不同拓扑的TS块体和相似的I块体,主要由H2O基团占据。
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