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1-20 OF 67 RESULTS FOR
rhodesite
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Journal Article
Natromelansonite, Na 3 Zr[Si 7 AlO 19 ]⋅4–5H 2 O, a new member of the rhodesite mero-plesiotype series from Mont Saint-Hilaire, Quebec, Canada
Journal: Mineralogical Magazine
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...
Journal Article
Melansonite, (Na,□)□ 2 KZrSi 8 O 19 ·5H 2 O, a New Member of the Rhodesite Group, from Mont Saint-Hilaire, Québec, Canada: Characterization, Crystal-Structure Determination, and Origin
Publisher: Mineralogical Association of Canada
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...
Journal Article
Two new members of the rhodesite mero-plesiotype series close to delhayelite and hydrodelhayelite: synthesis and crystal structure
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
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...
Journal Article
Polysomatic Aspects of Microporous Minerals – Heterophyllosilicates, Palysepioles and Rhodesite-Related Structures
Publisher: Mineralogical Society of America
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...
Journal Article
THE CRYSTAL STRUCTURE OF SEIDITE-(Ce), Na 4 (Ce,Sr) 2 {Ti(OH) 2 (Si 8 O 18 )}(O,OH,F) 4 ·5H 2 O, A MODULAR MICROPOROUS TITANOSILICATE OF THE RHODESITE GROUP
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
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...
Journal Article
Rhodesite from Trinity County, California
Journal: American Mineralogist
Publisher: Mineralogical Society of America
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...
in Two new members of the rhodesite mero-plesiotype series close to delhayelite and hydrodelhayelite: synthesis and crystal structure
> European Journal of Mineralogy
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 rhodesite series (Table 1 )....
in Two new members of the rhodesite mero-plesiotype series close to delhayelite and hydrodelhayelite: synthesis and crystal structure
> European Journal of Mineralogy
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
Image
COMPARATIVE DATA FOR MELANSONITE AND RHODESITE-RELATED MINERALS
in Melansonite, (Na,□)□ 2 KZrSi 8 O 19 ·5H 2 O, a New Member of the Rhodesite Group, from Mont Saint-Hilaire, Québec, Canada: Characterization, Crystal-Structure Determination, and Origin
> The Canadian Journal of Mineralogy and Petrology
Published: 07 July 2023
TABLE 8. COMPARATIVE DATA FOR MELANSONITE AND RHODESITE-RELATED MINERALS
Journal Article
Experimental study on the formation of zeolites from obsidian by interaction with NaOH and KOH solutions at 150 and 200 degrees C
Journal: Clays and Clay Minerals
Publisher: Clay Minerals Society
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 rhodesite showing an ordered a...
in IUPAC Nomenclature for Ordered Microporous and Mesoporous Materials and its Application to Non-zeolite Microporous Mineral Phases
> Reviews in Mineralogy and Geochemistry
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.
Image
(a) Projection of the host structure of rhodesite showing the silicate doub...
in IUPAC Nomenclature for Ordered Microporous and Mesoporous Materials and its Application to Non-zeolite Microporous Mineral Phases
> Reviews in Mineralogy and Geochemistry
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.
Image
Crystal structure of rhodesite seen along [010] (a) and [001] (b). Cations ...
in Polysomatic Aspects of Microporous Minerals – Heterophyllosilicates, Palysepioles and Rhodesite-Related Structures
> Reviews in Mineralogy and Geochemistry
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
Image
Tetrahedral sheets in apophyllite (a), rhodesite (b) and seidite-(Ce) (c).
in Polysomatic Aspects of Microporous Minerals – Heterophyllosilicates, Palysepioles and Rhodesite-Related Structures
> Reviews in Mineralogy and Geochemistry
Published: 01 January 2005
Figure 17. Tetrahedral sheets in apophyllite (a), rhodesite (b) and seidite-(Ce) (c).
Image
“Octahedral” sheets in rhodesite (a), monteregianite-(Y) (b), delhayelaite ...
in Polysomatic Aspects of Microporous Minerals – Heterophyllosilicates, Palysepioles and Rhodesite-Related Structures
> Reviews in Mineralogy and Geochemistry
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.
Image
Silicate layer formed by 4- and 8-membered rings in the structure of shlyko...
in Crystal structures of shlykovite and cryptophyllite: comparative crystal chemistry of phyllosilicate minerals of the mountainite family
> European Journal of Mineralogy
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).
Image
Double silicate layer showing channels delimited by eight-membered rings al...
in Two new members of the rhodesite mero-plesiotype series close to delhayelite and hydrodelhayelite: synthesis and crystal structure
> European Journal of Mineralogy
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
Crystal structures of shlykovite and cryptophyllite: comparative crystal chemistry of phyllosilicate minerals of the mountainite family
Natalia V. Zubkova, Yaroslav E. Filinchuk, Igor V. Pekov, Dmitry Yu. Pushcharovsky, Elena R. Gobechiya
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
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). ...
Journal Article
Microporous titanosilicates – Synthesis and structural characterization of a new orthorhombic-type labuntsovite
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
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...
Image
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
1