LOW-TEMPERATURE STUDY OF NATURAL MELILITE (CA1.89SR0.01NA0.08K0.02) (MG0.92AL0.08)(SI1.97AL0.03)O7: TOWARDS A COMMENSURATE VALUE OF THE Q VECTOR

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dc.contributor.author Bindi L.
dc.contributor.author Bonazzi P.
dc.date.accessioned 2022-02-13T04:46:09Z
dc.date.available 2022-02-13T04:46:09Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=5108140
dc.identifier.citation Physics and Chemistry of Minerals, 2003, 30, 9, 523-526
dc.identifier.issn 0342-1791
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35278
dc.description.abstract As is usual for peculiar chemical compositions, melilite-type compounds exhibit a two-dimensional incommensurately modulated structure which can be described with two wave vectors: q1=α(a* + b*) and q2=α(-a* + b*), where a* and b* are the tetragonal reciprocal axes of the basic cell. The low-temperature dependence of the modulation wave vector of a natural melilite crystal with chemical composition (Ca1.89Sr0.01 Na0.08K0.02)(Mg0.92Al0.08)(Si1.97Al0.03)O7 has been studied by X-ray single-crystal diffraction methods in the temperature range 298-100 K. The value of the α coefficient shows a continuous linear increase, ranging from 0.281(1) at 298 K to 0.299(1) at 100 K. No plateau-like temperature dependence was observed throughout the temperature studied, thus indicating that no independent phase with a specific q stabilizes in this natural crystal. A comparison with the low-temperature behaviour of synthetic Ca2MgSi2O7 is given.
dc.subject AKERMANITE
dc.subject MELILITE
dc.subject INCOMMENSURATE STRUCTURES
dc.subject LOW TEMPERATURE
dc.subject Q VECTOR
dc.title LOW-TEMPERATURE STUDY OF NATURAL MELILITE (CA1.89SR0.01NA0.08K0.02) (MG0.92AL0.08)(SI1.97AL0.03)O7: TOWARDS A COMMENSURATE VALUE OF THE Q VECTOR
dc.type Статья


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