http://www.cnr.it/ontology/cnr/individuo/prodotto/ID29752
From structure topology to chemical composition. X. Titanium silicates: the crystal structure and crystal chemistry of nechelyustovite, a group III Ti-disilicate mineral (Articolo in rivista)
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- Label
- From structure topology to chemical composition. X. Titanium silicates: the crystal structure and crystal chemistry of nechelyustovite, a group III Ti-disilicate mineral (Articolo in rivista) (literal)
- Anno
- 2009-01-01T00:00:00+01:00 (literal)
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- Camara F.; Sokolova E. (literal)
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- In: Mineralogical Magazine, vol. 73 (5) pp. 753 - 775. Mineralogical Society, 2009. (literal)
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- CNR-IGG, Pavia, Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, Canada. Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry, Moscow, Russia (literal)
- Titolo
- From structure topology to chemical composition. X. Titanium silicates: the crystal structure and crystal chemistry of nechelyustovite, a group III Ti-disilicate mineral (literal)
- Abstract
- The crystal structure of nechelyustovite, ideally Na4Ba2Mn1.5{square}2.5Ti5Nb(Si2O7)4O4(OH)3F(H2O)6, a 5.447(1) Å, b 7.157(1) Å, c 47.259(9) Å, {alpha} 95.759(4)°, ² 92.136(4)°, {gamma} 89.978(4)°, V 1831.7(4) Å3, space group PFormula, Z = 2, Dcalc. 3.041 g cm-3, from Lovozero alkaline massif, Kola Peninsula, Russia, has been solved and refined to R1 = 13.9% on the basis of 1745 unique reflections (Fo > 15{sigma}F). Electron microprobe analysis yielded the empirical formula (Na4.21FormulaCa0.46{square}1.22){Sigma}7.00(Ba1.28Sr0.50K0.30{square}0.92){Sigma}3.00(Ti4.14Nb1.43FormulaFormulaAl0.04){Sigma}6.00(Si8.03O28)O3.99[(OH)2.94F1.06]{Sigma}4.00(H2O)6.01, Z = 2, calculated on the basis of 42 (O + F) a.p.f.u., H2O and OH are calculated from structure refinement (H2O = 6 p.f.u.; F + OH = 4 p.f.u.). The crystal structure of nechelyustovite 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 Group III (Ti = 3 a.p.f.u.) of Ti-disilicate minerals: two H sheets connect to the O sheet such that two (Si2O7) groups link to the trans edges of a Ti octahedron of the O sheet. There are two distinct TS blocks of the same topology, TS1 and TS2, that differ in the cations of the O sheet, [(Na1.5Mn1{square}0.5)Ti] and [(Na2Mn0.5{square}0.5)Ti] (4 a.p.f.u.) respectively. The TS1 and TS2 blocks have two different H sheets, H1,2 and H3,4, where (Si2O7) groups link to [5]- and [6]-coordinated (Ti,Nb) polyhedra respectively. There are three peripheral sites, AP(1-3), occupied mainly by Ba (less Sr and K) at 96, 86 and 26% and one peripheral site AP(4) occupied by Na at 50%. There are two I blocks: the I1 block is a layer of Ba atoms; the I2 block consists of H2O groups and AP(3) atoms. TS blocks alternate with I blocks or link through hydrogen bonds (as in epistolite). There is a sequence of four TS blocks and three I blocks per the c cell parameter: TS2 - I1 - TS1 - I2 - TS1 - I1 - TS2. (literal)
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