| Reference Type | Journal (article/letter/editorial) |
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| Title | Crystal structure of the high-pressure monoclinic phase-II of cristobalite, SiO2 |
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| Journal | Mineralogical Magazine |
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| Authors | Dove, M. T. | Author |
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| 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 |
| Year | 2000 (June) | Volume | 64 |
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| Issue | 3 |
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| Publisher | Mineralogical Society |
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| DOI | doi:10.1180/002646100549436Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 243176 | Long-form Identifier | mindat:1:5:243176:9 |
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| GUID | 0 |
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| Full Reference | 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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| Plain Text | 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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| Abstract/Notes | AbstractThe 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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