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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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Reference TypeJournal (article/letter/editorial)
TitleHematophanite, a derivative of the perovskite structure
JournalMineralogical Magazine
AuthorsRouse, R. C.Author
Year1973 (March)Volume39
Issue301
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_39/39-301-49.pdf+
DOIdoi:10.1180/minmag.1973.039.301.06Search in ResearchGate
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Mindat Ref. ID6635Long-form Identifiermindat:1:5:6635:2
GUID0
Full ReferenceRouse, R. C. (1973) Hematophanite, a derivative of the perovskite structure. Mineralogical Magazine, 39 (301) 49-53 doi:10.1180/minmag.1973.039.301.06
Plain TextRouse, R. C. (1973) Hematophanite, a derivative of the perovskite structure. Mineralogical Magazine, 39 (301) 49-53 doi:10.1180/minmag.1973.039.301.06
In(1973, March) Mineralogical Magazine Vol. 39 (301) Mineralogical Society
Abstract/NotesSummaryHematophanite, 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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