| Reference Type | Journal (article/letter/editorial) |
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| Title | The crystal structure of phlogopite by neutron diffraction |
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| Journal | Mineralogical Magazine |
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| Authors | Rayner, J. H. | Author |
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| Year | 1974 (December) | Volume | 39 |
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| Issue | 308 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_39/39-308-850.pdf+ |
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| DOI | doi:10.1180/minmag.1974.039.308.04Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 6806 | Long-form Identifier | mindat:1:5:6806:6 |
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| GUID | 0 |
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| Full Reference | Rayner, J. H. (1974) The crystal structure of phlogopite by neutron diffraction. Mineralogical Magazine, 39 (308) 850-856 doi:10.1180/minmag.1974.039.308.04 |
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| Plain Text | Rayner, J. H. (1974) The crystal structure of phlogopite by neutron diffraction. Mineralogical Magazine, 39 (308) 850-856 doi:10.1180/minmag.1974.039.308.04 |
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| In | (1974, December) Mineralogical Magazine Vol. 39 (308) Mineralogical Society |
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| Abstract/Notes | SummaryThe positions of all the atoms including hydrogen have been found by a partial three-dimensional single-crystal neutron-diffraction study in which about one-third of the reflections in the reciprocal sphere to 1·5 Å were measured. The hydroxyl group is perpendicular to the plane of the silicate sheets. The fluorine content of this phlogopite is enough to occupy 25 % of the (OH, F) sites. Site occupancy refinement suggests that there is a small deficiency of hydrogen at the remaining sites and that the two crystallographically different octahedral sites are fully occupied by the same proportions of Mg, Ti, Fe, and Ca. |
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