Dissymmetrization in eudialyte-group minerals. IV. Features of the blocky isomorphism in the structure of the Nb-deficient oneillite analogue in the frame of P3-symmetry

The crystal structure of a potentially new member of the eudialyte group, the Nb-deficient analogue of oneillite from Mont Saint-Hilaire, Québec, Canada, with the idealized formula: Na13(Ca3Mn3)Zr3(Fe,Mn)3(,Nb)(Si,Nb,) [Si3O9]2[Si9O27]2(O,OH,Cl)3•2H2O, has been re-studied within the space group P3. The unit-cell parameters are: a = 14.134(3), c = 30.178(6) Å, V = 52201 Å3. The crystal structure of the mineral has been previously investigated using the space group R3 (typical for the members of oneillite family). In this work a structural model characterized by 155 crystallographic sites was solved in the frame of the low symmetry space group P3 and refined to R = 5.9 % using 4179 reflections with F > 2(F). The cation distribution between the key sites in low symmetry is more detailed.

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Publication Details

Journal
Vestnik of Geosciences
Published
2024-10-08
DOI
https://doi.org/10.19110/geov.2024.8.4
Citations
1
Primary Topic
Crystal Structures and Properties
Type
article
Field-Weighted Citation Impact
0.12
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article

Dissymmetrization in eudialyte-group minerals. IV. Features of the blocky isomorphism in the structure of the Nb-deficient oneillite analogue in the frame of P3-symmetry

Sergey M. Aksenov, Р. К. Расцветаева, V. M. Gridchina, Н. В. Чуканов
1 citations
Vestnik of Geosciences
Crystal Structures and Properties
0.12
article

Dissymmetrization in eudialyte-group minerals. IV. Features of the blocky isomorphism in the structure of the Nb-deficient oneillite analogue in the frame of P3-symmetry

Sergey M. Aksenov, Р. К. Расцветаева, V. M. Gridchina, Н. В. Чуканов
article en
1 citations

Abstract

The crystal structure of a potentially new member of the eudialyte group, the Nb-deficient analogue of oneillite from Mont Saint-Hilaire, Québec, Canada, with the idealized formula: Na13(Ca3Mn3)Zr3(Fe,Mn)3(,Nb)(Si,Nb,) [Si3O9]2[Si9O27]2(O,OH,Cl)3•2H2O, has been re-studied within the space group P3. The unit-cell parameters are: a = 14.134(3), c = 30.178(6) Å, V = 52201 Å3. The crystal structure of the mineral has been previously investigated using the space group R3 (typical for the members of oneillite family). In this work a structural model characterized by 155 crystallographic sites was solved in the frame of the low symmetry space group P3 and refined to R = 5.9 % using 4179 reflections with F > 2(F). The cation distribution between the key sites in low symmetry is more detailed.

Vestnik of GeosciencesVol. 0(8)
Russian Academy of Sciences (RU), Kurchatov Institute (RU), Institute of Problems of Chemical Physics (RU), Geological Institute (RU), A.V. Shubnikov Institute of Crystallography (RU), Material Sciences (United States) (US)
Life in Land
Openalex Percentile: Top 66%
Crystal Structures and Properties
0.12
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