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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/7020
Title: New Occurrence of Rusinovite, Ca10(Si2O7)3Cl2: Composition, Structure and Raman Data of Rusinovite from Shadil-Khokh Volcano, South Ossetia and Bellerberg Volcano, Germany
Authors: Środek, Dorota
Juroszek, Rafał
Krüger, Hannes
Krüger, Biljana
Galuskina, Irina
Gazeev, Victor
Keywords: Rusinovite; Raman spectroscopy; pyrometamorphism; stacking faults; Shadil-Khokh volcano; Bellerberg volcano
Issue Date: 2018
Citation: Minerals, Vol. 8, iss. 9 (2018), Art. No. 399
Abstract: Rusinovite, Ca10(Si2O7)3Cl2, was found at two new localities, including Shadil-Khokh volcano, South Ossetia and Bellerberg volcano, Caspar quarry, Germany. At both of these localities, rusinovite occurs in altered carbonate-silicate xenoliths embedded in volcanic rocks. The occurrence of this mineral is connected to specific zones of the xenolith characterized by a defined Ca:Si < 2 ratio. Chemical compositions, as well as the Raman spectra of the investigated rusinovite samples, correspond to the data from the locality of rusinovite holotype—Upper Chegem Caldera, Northern Caucasus, Russia. The most intense bands of the Raman spectra are related to vibrations of (Si2O7) groups. Unit cell parameters of rusinovite from South Ossetia are: a = 3.76330(4) Å, b = 16.9423(3) Å, c = 17.3325(2) Å, V = 1105.10(4) Å3, Z = 2. The performed synchrotron radiation diffraction experiments did not confirm a doubling of c as reported for the synthetic phase, Ca10(Si2O7)3Cl2. However, one-dimensional diffuse scattering parallel to b* has been observed. This can be interpreted with an ordered arrangement of Si2O7 groups creating layers with a doubled a parameter. Consequently, the two different displacements of neighbouring layers allow random stacking faults to occur.
URI: http://hdl.handle.net/20.500.12128/7020
DOI: 10.3390/min8090399
ISSN: 2075-163X
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