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Dove, Martin T., Heine, Volker, Hammonds, Kenton D. (1995) Rigid unit modes in framework silicates. Mineralogical Magazine, 59 (397) 629-639 doi:10.1180/minmag.1995.059.397.07

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Reference TypeJournal (article/letter/editorial)
TitleRigid unit modes in framework silicates
JournalMineralogical MagazineISSN0026-461X
AuthorsDove, Martin T.Author
Heine, VolkerAuthor
Hammonds, Kenton D.Author
Year1995 (December)Volume59
Issue397
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_59/59-397-629.pdf+
DOIdoi:10.1180/minmag.1995.059.397.07Search in ResearchGate
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Mindat Ref. ID2694Long-form Identifiermindat:1:5:2694:3
GUID0
Full ReferenceDove, Martin T., Heine, Volker, Hammonds, Kenton D. (1995) Rigid unit modes in framework silicates. Mineralogical Magazine, 59 (397) 629-639 doi:10.1180/minmag.1995.059.397.07
Plain TextDove, Martin T., Heine, Volker, Hammonds, Kenton D. (1995) Rigid unit modes in framework silicates. Mineralogical Magazine, 59 (397) 629-639 doi:10.1180/minmag.1995.059.397.07
In(1995, December) Mineralogical Magazine Vol. 59 (397) Mineralogical Society
Abstract/NotesAbstractWe describe a model for framework silicates in which the SiO4 (and AlO4) tetrahedra are treated as perfectly rigid and freely jointed. From this model we are able to identify low-energy modes of distortion of the structure, which we call Rigid unit modes. These modes can act as soft modes to allow easy distortions at phase transition. We discuss three forces that will operate at a phase transition in conjunction with the candidate soft modes to determine which of the rigid unit modes will actually precipitate a phase transition, and illustrate these ideas by detailed discussions of the phase transitions in quartz, leucite and cristobalite. The model can also be used to estimate the transition temperature, and the theory highlights an important role for the stiffness of the tetrahedra.


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