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titanosilicates

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Series: European Mineralogical Union Notes in Mineralogy
Published: 01 January 2011
DOI: 10.1180/EMU-notes.11.3
EISBN: 9780903056458
...Abstract Abstract Layered materials have much potential for applications as ion exchangers, gas sorbents and catalysts. Layered titanosilicates are of particular interest because on the one hand they possess large amounts of titanium and, on the other, they exhibit a wide variety of crystal...
FIGURES | View All (14)
Journal Article
Published: 01 October 2009
American Mineralogist (2009) 94 (10): 1450–1458.
... O, ivanyukite-K, K 2 [Ti 4 (OH) 2 O 2 (SiO 4 ) 3 ]·9H 2 O, and ivanyukite-Cu, Cu[Ti 4 (OH) 2 O 2 (SiO 4 ) 3 ]·7H 2 O, are new microporous titanosilicates found in a natrolitized microcline-aegirine-sodalite lens in the orthoclase-bearing urtite at the Koashva Mountain (Khibiny Massif, Kola Peninsula...
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Journal Article
Published: 01 March 2007
European Journal of Mineralogy (2007) 19 (2): 217–222.
... microporous titanosilicates hydrothermal synthesis The labuntsovite group ( Chukanov et al. , 2002 ; 2003 ) includes hydrous titanium and niobium alkali silicates represented by the general formula A 4 B 4 [ C 4−2 x (H 2 O,OH) 2 x ] D x [ M 8 (Si 4 O 12 ) 4 (OH,O) 8 ] · n H 2 O...
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Journal Article
Published: 01 April 1996
European Journal of Mineralogy (1996) 8 (2): 241–249.
Journal Article
Published: 01 December 2001
The Canadian Mineralogist (2001) 39 (6): 1665–1673.
...Giovanni Ferraris; Elena Belluso; Angela Gula; Svetlana V. Soboleva; Olga A. Ageeva; Boris E. Borutskii Abstract Bornemanite is a rare alkali titanosilicate occurring in the natrolite zone of the Yubileynaya hyperagpaitic pegmatite, on Karnasurt Mountain, in the Lovozero massif, Kola Peninsula...
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<span class="search-highlight">TITANOSILICATES</span> OCCURING IN THE LOVOZERO MASSIF FOR WHICH THE STRUCTURE IS ...
Published: 01 December 2001
TABLE 3. TITANOSILICATES OCCURING IN THE LOVOZERO MASSIF FOR WHICH THE STRUCTURE IS KNOWN AND BASED ON A BAFERTISITE-LIKE HETEROPHYLIOSILICATE HOH LAYER
Journal Article
Published: 01 August 2004
The Canadian Mineralogist (2004) 42 (4): 1027–1035.
... structural information. The quadrupolar interaction (QI) can be described by the quadrupolar coupling constant (C q ) and asymmetry parameters (η), which are determined from the EFG at the nuclear site ( Slichter 1992 ): © 2004 Mineralogical Association of Canada 2004 penkvilksite titanosilicate...
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Distribution of apical bond-lengths in the  D ϕ 6  octahedron and cation po...
Published: 01 February 2003
F ig . 14. Distribution of apical bond-lengths in the D ϕ 6 octahedron and cation position in astrophyllite-group minerals and other titanosilicates. A. Positional displacement of [6] Ti in this group and in other titanosilicates. B. Lengthening of D –O(2) and shortening of D –ϕ(16) due
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Crystal structure of Ti-bearing litidionite: (a) general view; (b) titanosi...
Published: 16 February 2022
Fig. 6. Crystal structure of Ti-bearing litidionite: (a) general view; (b) titanosilicate heteropolyhedral layer; and (c) silicate tubes.
Journal Article
Published: 01 June 2004
The Canadian Mineralogist (2004) 42 (3): 769–780.
... to R = 5.41%, wR 2 = 18.50%. It consists of eight-membered (8MR) rings of SiO 4 tetrahedra, linked to adjacent rings to form vierer double chains along [001], which are cross-linked by TiO 6 octahedra to produce a mixed tetrahedron–octahedron titanosilicate framework similar to that found in zorite...
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( a ) Projection of the crystal structure of kihlmanite-(Ce), ( b ) Structu...
Published: 01 June 2014
F ig . 7. ( a ) Projection of the crystal structure of kihlmanite-(Ce), ( b ) Structure of titanosilicate and ( c ) Ce–CO 3 layers.
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COMPARISON OF (Ti,Nb)–ϕ APICAL BOND-LENGTHS IN ASTROPHYLLITE-GROUP MINERALS...
Published: 01 February 2003
TABLE 7. COMPARISON OF (Ti,Nb)–ϕ APICAL BOND-LENGTHS IN ASTROPHYLLITE-GROUP MINERALS AND OTHER TITANOSILICATES AND NIOBOSILICATES
Journal Article
Published: 01 February 2010
The Canadian Mineralogist (2010) 48 (1): 41–50.
...Victor N. Yakovenchuk; Gregory Yu. Ivanyuk; Yakov A. Pakhomovsky; Ekaterina A. Selivanova; Yurii P. Men’Shikov; Julia A. Korchak; Sergey V. Krivovichev; Dar’ya V. Spiridonova; Oleg A. Zalkind Abstract Punkaruaivite, ideally LiTi 2 [Si 4 O 11 (OH)](OH) 2 ·H 2 O, is a new species of Li titanosilicate...
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Journal Article
Published: 01 October 2004
American Mineralogist (2004) 89 (10): 1561–1565.
... Facility (ESRF, Grenoble, France). The structure was refined to R 1 = 0.101 on the basis of 2359 unique observed reflections with | F o | ≥ 4σ F . The structure of yuksporite is based upon titanosilicate nanorods elongated along a and with an elliptical cross-section of ca. 16 × 19 Å = 1.6 × 1.9 nm...
FIGURES
Journal Article
Published: 01 October 2003
The Canadian Mineralogist (2003) 41 (5): 1183–1192.
...Giovanni Ferraris; Elena Belluso; Angela Gula; Svetlana V. Soboleva; Alexander P. Khomyakov Abstract Seidite-(Ce), Na 4 (Ce,Sr) 2 {Ti(OH) 2 (Si 8 O 18 )}(O,OH,F) 4 ·5H 2 O, is a titanosilicate recently discovered in the Yubileynaya pegmatite at Mount Karnasurt, Lovozero alkaline massif, Kola...
FIGURES
Journal Article
Published: 01 October 2001
The Canadian Mineralogist (2001) 39 (5): 1307–1316.
...Giovanni Ferraris; Gabriella Ivaldi; Dmitry Yu. Pushcharovsky; Natalia V. Zubkova; Igor V. Pekov Abstract By using a crystal from a new locality, the structure of delindeite has been refined to R = 0.054 for 703 unique reflections with I > 2σ ( I ). This titanosilicate [ideally Ba 2 {(Na,K,□) 3...
FIGURES
Journal Article
Published: 01 August 2001
The Canadian Mineralogist (2001) 39 (4): 1095–1104.
... to an R value of 4.6% using 1074 unique observed (| F o | > 4σ F ) reflections collected with a single-crystal diffractometer fitted with a CCD detector and Mo K α X-radiation. Polyakovite-(Ce) is a sorosilicate of Cr 3+ , Ti 4+ , Fe 2+ and REE 3+ , and the first titanosilicate where Cr 3+ is a species...
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Loparite crystals experimentally obtained at 450 °C and 1 kbar in complex s...
Published: 01 April 2013
Fig. 7. Loparite crystals experimentally obtained at 450 °C and 1 kbar in complex silicate–salt systems. a , Sample 5641; b , sample 5639. Lop, loparite; SS, sodium sulfate; STS, sodium titanosilicate; Ccn, cancrinite. Back-scattered electron photos.
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Crystal structure of chivruaiite ( a ) (some H 2 O molecules are omitted fo...
Published: 01 May 2006
F igure 2. Crystal structure of chivruaiite ( a ) (some H 2 O molecules are omitted for clarity) and nodal representation of its titanosilicate framework (Ti and Si centers are symbolized by black and white vertices respectively) ( b ). In b , positions of K + and Ca 2+ cations are indicated.
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<span class="search-highlight">Titanosilicate</span> ETS-10 projections: (a) down [110] direction for polymorph B...
Published: 01 January 2005
Figure 1. Titanosilicate ETS-10 projections: (a) down [110] direction for polymorph B (space group C 2/ c ); (b) down [100] direction for polymorph A (space group P 4 1 ). Dark TiO 6 octahedra, light grey SiO 4 tetrahedra.