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Dove, M. T., Craig, M. S., Keen, D. A., Marshall, W. G., Redfern, S. A. T., Trachenko, K. O., Tucker, M. G. (2000) Crystal structure of the high-pressure monoclinic phase-II of cristobalite, SiO2. Mineralogical Magazine, 64 (3) 569-576 doi:10.1180/002646100549436

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Reference TypeJournal (article/letter/editorial)
TitleCrystal structure of the high-pressure monoclinic phase-II of cristobalite, SiO2
JournalMineralogical Magazine
AuthorsDove, M. T.Author
Craig, M. S.Author
Keen, D. A.Author
Marshall, W. G.Author
Redfern, S. A. T.Author
Trachenko, K. O.Author
Tucker, M. G.Author
Year2000 (June)Volume64
Issue3
PublisherMineralogical Society
DOIdoi:10.1180/002646100549436Search in ResearchGate
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Mindat Ref. ID243176Long-form Identifiermindat:1:5:243176:9
GUID0
Full ReferenceDove, M. T., Craig, M. S., Keen, D. A., Marshall, W. G., Redfern, S. A. T., Trachenko, K. O., Tucker, M. G. (2000) Crystal structure of the high-pressure monoclinic phase-II of cristobalite, SiO2. Mineralogical Magazine, 64 (3) 569-576 doi:10.1180/002646100549436
Plain TextDove, M. T., Craig, M. S., Keen, D. A., Marshall, W. G., Redfern, S. A. T., Trachenko, K. O., Tucker, M. G. (2000) Crystal structure of the high-pressure monoclinic phase-II of cristobalite, SiO2. Mineralogical Magazine, 64 (3) 569-576 doi:10.1180/002646100549436
Abstract/NotesAbstractThe crystal structure of the high-pressure phase-II of cristobalite has been solved by neutron diffraction (space group P21/c, a = 8.3780(11) Å, b = 4.6018(6) Å, c = 9.0568(13) Å, β = 124.949(7)°, at P = 3.5 GPa). This phase corresponds to a distortion of the high-temperature cubic β-phase, rather than of the ambient temperature and pressure tetragonal α-phase.

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