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Bell, A. M. T., Henderson, C. M. B. (2012) High-temperature synchrotron X-ray powder diffraction study of Cs2XSi5O12(X = Cd, Cu, Zn) leucites. Mineralogical Magazine, 76 (5) 1257-1280 doi:10.1180/minmag.2012.076.5.12

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Reference TypeJournal (article/letter/editorial)
TitleHigh-temperature synchrotron X-ray powder diffraction study of Cs2XSi5O12(X = Cd, Cu, Zn) leucites
JournalMineralogical Magazine
AuthorsBell, A. M. T.Author
Henderson, C. M. B.Author
Year2012 (October)Volume76
Issue5
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2012.076.5.12Search in ResearchGate
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Mindat Ref. ID244283Long-form Identifiermindat:1:5:244283:3
GUID0
Full ReferenceBell, A. M. T., Henderson, C. M. B. (2012) High-temperature synchrotron X-ray powder diffraction study of Cs2XSi5O12(X = Cd, Cu, Zn) leucites. Mineralogical Magazine, 76 (5) 1257-1280 doi:10.1180/minmag.2012.076.5.12
Plain TextBell, A. M. T., Henderson, C. M. B. (2012) High-temperature synchrotron X-ray powder diffraction study of Cs2XSi5O12(X = Cd, Cu, Zn) leucites. Mineralogical Magazine, 76 (5) 1257-1280 doi:10.1180/minmag.2012.076.5.12
Abstract/NotesAbstractSynchrotron X-ray powder diffraction data have been collected on three synthetic leucite analogues with the general formula Cs2XSi5O12(X = Cd, Cu, Zn) between 295 and 1173 K. All three samples have the orthorhombic Pbca leucite structure at room temperature with ordered framework T-site cations. The sample with X = Cd retains the Pbca structure over the whole of the investigated temperature range. The sample with X = Cu also retains the Pbca structure, but there is a transition to a less distorted structure with a larger unit-cell volume at ∼333 K. The sample with X = Zn shows evidence for a transition to a previously unknown Pa cubic structure, with some T-site cation disorder, at 566 K, on heating. This transition is reversible on cooling to 633 K.


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