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Gatehouse, B. M., Jones, G. C., Pring, A., Symes, R. F. (1986) The chemistry and structure of redledgeite. Mineralogical Magazine, 50 (358) 709-715 doi:10.1180/minmag.1986.050.358.18

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Reference TypeJournal (article/letter/editorial)
TitleThe chemistry and structure of redledgeite
JournalMineralogical MagazineISSN0026-461X
AuthorsGatehouse, B. M.Author
Jones, G. C.Author
Pring, A.Author
Symes, R. F.Author
Year1986 (December)Volume50
Issue358
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_50/50-358-709.pdf+
DOIdoi:10.1180/minmag.1986.050.358.18Search in ResearchGate
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Mindat Ref. ID3917Long-form Identifiermindat:1:5:3917:2
GUID0
Full ReferenceGatehouse, B. M., Jones, G. C., Pring, A., Symes, R. F. (1986) The chemistry and structure of redledgeite. Mineralogical Magazine, 50 (358) 709-715 doi:10.1180/minmag.1986.050.358.18
Plain TextGatehouse, B. M., Jones, G. C., Pring, A., Symes, R. F. (1986) The chemistry and structure of redledgeite. Mineralogical Magazine, 50 (358) 709-715 doi:10.1180/minmag.1986.050.358.18
In(1986, December) Mineralogical Magazine Vol. 50 (358) Mineralogical Society
Abstract/NotesAbstractTwo distinct habits of redledgeite are described: small black bipyramidal crystals and yellow-green fibres. The mineral is a Ba-Cr-Ti oxide rather than a Mg-Cr-Ti oxide as previously supposed. Electron microprobe analysis gave Ba1.10(Cr1.82Ti5.95 Fe0.10V0.08)Σ7.95O16 and Ba1.27(Cr2.48Ti5.49Fe0.02)Σ7.99 O16 for the black and yellow-green forms respectively. The mineral is a monoclinic hollandite-type phase, space group I2/m, with a = 10.129(2); b = 2.959(1); c = 10.135(2) Å; β = 90.05(11)° and Z = 1; calculated density for the black form is 4.413 g cm−3. The crystal structure was refined to R 6.3%, Rw 7.4% using 1017 reflections with F > 3σ(F) from a set of 1062 unique reflections. Electron diffraction studies revealed weak superlattice reflections, with a period of 2.24b due to tunnel cation ordering.


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