Abstract
The structure of the mineral parakeldyshite Na1.93ZrSi2O6.93(OH)0.07 is refined by X-ray diffraction analysis. The main crystallographic data are as follows: space group P \(\overline 1 \), a = 6.617(2) Å, b = 8.813(1) Å, c = 5.426(1) Å, α = 87.26(3)°, β = 85.68(3)°, γ = 71.45(3)°, and R F = 0.0153. The initial structural model of this mineral is confirmed. Within this model, the structure of parakeldyshite is based on the heteropolyhedral framework formed by [Si2O7] diorthogroups, which are linked together through isolated zirconium octahedra. The fundamental difference between the structure under investigation and the initial structural model is associated with the arrangement of the extraframework cations. A comparative crystal chemical analysis of the zirconium silicates with [Si2O7] diorthogroups is performed.
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Original Russian Text © I.V. Pekov, N.V. Zubkova, D.Yu. Pushcharovsky, U. Kolitsch, E. Tillmanns, 2007, published in Kristallografiya, 2007, Vol. 52, No. 6, pp. 1100–1105
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Pekov, I.V., Zubkova, N.V., Pushcharovsky, D.Y. et al. Refined crystal structure of parakeldyshite and the genetic crystal chemistry of zirconium minerals with [Si2O7] diorthogroups. Crystallogr. Rep. 52, 1066–1071 (2007). https://doi.org/10.1134/S1063774507060223
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DOI: https://doi.org/10.1134/S1063774507060223