| Reference Type | Journal (article/letter/editorial) |
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| Title | Hematophanite, a derivative of the perovskite structure |
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| Journal | Mineralogical Magazine |
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| Authors | Rouse, R. C. | Author |
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| Year | 1973 (March) | Volume | 39 |
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| Issue | 301 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_39/39-301-49.pdf+ |
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| DOI | doi:10.1180/minmag.1973.039.301.06Search in ResearchGate |
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| Generate Citation Formats |
| Mindat Ref. ID | 6635 | Long-form Identifier | mindat:1:5:6635:2 |
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| GUID | 0 |
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| Full Reference | Rouse, R. C. (1973) Hematophanite, a derivative of the perovskite structure. Mineralogical Magazine, 39 (301) 49-53 doi:10.1180/minmag.1973.039.301.06 |
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| Plain Text | Rouse, R. C. (1973) Hematophanite, a derivative of the perovskite structure. Mineralogical Magazine, 39 (301) 49-53 doi:10.1180/minmag.1973.039.301.06 |
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| In | (1973, March) Mineralogical Magazine Vol. 39 (301) Mineralogical Society |
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| Abstract/Notes | SummaryHematophanite, ideally Pb4Fe3O8Cl, is tetragonal, space group P4mm, with a = 3·92 and c = 15·31 Å. The crystal structure, which has been refined to an R-factor of 9·1 %, may be described as an interlayering of perovskite-like units with a cesium chloride or, alternatively, a nadoritelike unit. The nadorite-like part consists of a double layer of PbO4Cl4 distorted square antiprisms. Iron atoms are in 6-fold (tetragonal bipyramidal) and 5-fold (square pyramidal) coordination. |
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