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rhodesite

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Journal Article
Published: 15 January 2024
Mineralogical Magazine (2024) 88 (2): 195–202.
...). The crystal structure, solved and refined from single-crystal X-ray diffraction data ( R 1 = 0.042), is based on a double sheet of tetrahedra (T) and a sheet of octahedra (O) that alternate along the [010] direction forming a TOT structure typical for members of the rhodesite mero-plesiotype series...
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Journal Article
Published: 07 July 2023
The Canadian Journal of Mineralogy and Petrology (2023) 61 (2): 387–400.
...− , H 2 O) octahedra that form infinite sheets on (001). Alternating T and O layers give rise to a TOT topology reminiscent of that observed in micas and characteristic of minerals, including rhodesite, delhayelite, hydrodelhayelite, and monteregianite-(Y), with which melansonite shares a crystal...
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Journal Article
Published: 01 April 2009
European Journal of Mineralogy (2009) 21 (2): 485–493.
...Marcella Cadoni; Giovanni Ferraris Abstract Two new members of the mero-plesiotype rhodesite series (KCa 2 Na[Si 8 O 19 ]·5H 2 O, abbreviated as TR03; a 6.5850, b 23.776, c 7.0250 Å; Pn 2 1 m ; and KNa 3 Sr[Si 8 O 19 ] ·4.3H 2 O, TR04; a 6.5699, b 23.7225, c 7.0225 Å, β 91.81°; P 2 1 / m ) have...
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Journal Article
Published: 01 January 2005
Reviews in Mineralogy and Geochemistry (2005) 57 (1): 69–104.
... module is kept constant, a second (third, etc.) module is peculiar of each member. A series is said to be plesiotype when all members share modules that, however, may still slightly differ in chemistry and configuration: see the mero-plesiotype series of bafertisite and rhodesite described later...
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Journal Article
Published: 01 October 2003
The Canadian Mineralogist (2003) 41 (5): 1183–1192.
... compounds belonging to the rhodesite group. Abstract La seidite-(Ce), Na 4 (Ce,Sr) 2 {Ti(OH) 2 (Si 8 O 18 )}(O,OH,F) 4 ·5H 2 O, est un titanosilicate découvert récemment dans la pegmatite de Yubileynaya, au mont Karnasurt, complexe alcalin de Lovozero, péninsule de Kola, en Russie. Les grains sont des...
FIGURES
Journal Article
Published: 01 February 1969
American Mineralogist (1969) 54 (1-2): 251–255.
...Richard A. Sheppard; Arthur J. Gude, 3rd Abstract Rhodesite occurs as aggregates of radiating white, silky fibers associated with magadiite and trioctahedral montmorillonite in an altered silicic lava. Indices of refraction are α = 1.501±0.001 and γ=1.513 ± 0.001. A least-squares refinement of X...
Image
Tetrahedral sheet in apophyllite [(a); (001)], seidite-(Ce) [(b); (100)] an...
Published: 01 April 2009
Fig. 1. Tetrahedral sheet in apophyllite [(a); (001)], seidite-(Ce) [(b); (100)] and other members of the rhodesite series reported in Table 1 [(c); (100) in rhodesite].
Image
The  O  layers in the following members of the <span class="search-highlight">rhodesite</span> series (Table 1 )....
Published: 01 April 2009
Fig. 3. The O layers in the following members of the rhodesite series (Table 1 ). Seidite-(Ce) (a); rhodesite, macdonaldite, hydrodelhayelite (b); monteregianite-(Y) and AV-5 (c); delhayelite (d); AV-9 (e); TR03 (f); TR04 (g). The layer plane is (100) in (a), (b), (d) and (e); the same plane
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COMPARATIVE DATA FOR MELANSONITE AND <span class="search-highlight">RHODESITE</span>-RELATED MINERALS
Published: 07 July 2023
TABLE 8. COMPARATIVE DATA FOR MELANSONITE AND RHODESITE-RELATED MINERALS
Journal Article
Published: 01 June 1997
Clays and Clay Minerals (1997) 45 (3): 365–377.
... microscopy (TEM), and energy dispersive X-ray analysis (EDX). Changes in chemical composition and pH value of solutions during the reactions were also measured. As the pH of reacting solutions was increased, smectite, phillipsite and rhodesite crystallized progressively in NaOH solutions, while smectite...
Image
The 2-dimensional silicate host structure of <span class="search-highlight">rhodesite</span> showing an ordered a...
Published: 01 January 2005
Figure 2. The 2-dimensional silicate host structure of rhodesite showing an ordered arrangement of channels within the layers. The silicate double layers are linked via chains of Ca octahedra.
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(a) Projection of the host structure of <span class="search-highlight">rhodesite</span> showing the silicate doub...
Published: 01 January 2005
Figure 13. (a) Projection of the host structure of rhodesite showing the silicate double layers linked via Ca octahedra. (b) the silicate double layer alone showing the K + (dark spheres) and H 2 O (light spheres) guest species in the 2-dimensional 8-ring channel system.
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Crystal structure of <span class="search-highlight">rhodesite</span> seen along [010] (a) and [001] (b). Cations ...
Published: 01 January 2005
Figure 16. Crystal structure of rhodesite seen along [010] (a) and [001] (b). Cations and water molecules occurring in the channels are not shown; a axis vertical. that had been kept in aqueous solution of Tl + , K + , Rb + , Cs + and Ba 2+ at room temperature for periods of 6–8 weeks: Na
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Tetrahedral sheets in apophyllite (a), <span class="search-highlight">rhodesite</span> (b) and seidite-(Ce) (c).
Published: 01 January 2005
Figure 17. Tetrahedral sheets in apophyllite (a), rhodesite (b) and seidite-(Ce) (c).
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“Octahedral” sheets in <span class="search-highlight">rhodesite</span> (a), monteregianite-(Y) (b), delhayelaite ...
Published: 01 January 2005
Figure 18. “Octahedral” sheets in rhodesite (a), monteregianite-(Y) (b), delhayelaite (c) and AV-9 (d). The Na polyhedra (dark grey) joining parallel rows of edge-sharing octahedra (light grey) have coordination number 6, 8, and 9 in (b), (c) and (d), respectively.
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Silicate layer formed by 4- and 8-membered rings in the structure of shlyko...
Published: 01 August 2010
Fig. 2. Silicate layer formed by 4- and 8-membered rings in the structure of shlykovite (a), mountainite (b) and rhodesite (c).
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Double silicate layer showing channels delimited by eight-membered rings al...
Published: 01 April 2009
Fig. 2. Double silicate layer showing channels delimited by eight-membered rings along two perpendicular directions that in rhodesite correspond to [010] (a) and [001] (b).
Journal Article
Published: 01 August 2010
European Journal of Mineralogy (2010) 22 (4): 547–555.
...Fig. 2. Silicate layer formed by 4- and 8-membered rings in the structure of shlykovite (a), mountainite (b) and rhodesite (c). ...
FIGURES
Journal Article
Published: 01 March 2007
European Journal of Mineralogy (2007) 19 (2): 217–222.
...Marcella Cadoni; Giovanni Ferraris Abstract The crystal structure of a new orthorhombic-type labuntsovite with composition Na 5.36 Ti 4 (Si 4 O 12 ) 2 (O 0.34 OH 0.66 ) 4 · 10.31H 2 O, obtained as side product of hydrothermal runs devoted to the synthesis of rhodesite-type microporous silicates...
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Double-sheets of tetrahedra based on the 3-connected plane net 4.8 2  plus ...
Published: 01 February 2019
Fig. 38. Double-sheets of tetrahedra based on the 3-connected plane net 4.8 2 plus an oikodoméic operation: ( a ) the (u 3 d) 1 (u 4 du 2 d) 1 arrangement in macdonaldite, monteregianite-(Y) and rhodesite ; ( b ) the (u 3 d) 1 (u 4 du 2 d) 1 arrangement in delhayelite and fivegite , note