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Fanfani, L., Giuseppetti, G., Tadini, C., Zanazzi, P. F. (1980) The crystal structure of kogarkoite, Na3SO4F. Mineralogical Magazine, 43 (330) 753-759 doi:10.1180/minmag.1980.043.330.08

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Reference TypeJournal (article/letter/editorial)
TitleThe crystal structure of kogarkoite, Na3SO4F
JournalMineralogical MagazineISSN0026-461X
AuthorsFanfani, L.Author
Giuseppetti, G.Author
Tadini, C.Author
Zanazzi, P. F.Author
Year1980 (June)Volume43
Issue330
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_43/43-330-753.pdf+
DOIdoi:10.1180/minmag.1980.043.330.08Search in ResearchGate
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Mindat Ref. ID3130Long-form Identifiermindat:1:5:3130:5
GUID0
Full ReferenceFanfani, L., Giuseppetti, G., Tadini, C., Zanazzi, P. F. (1980) The crystal structure of kogarkoite, Na3SO4F. Mineralogical Magazine, 43 (330) 753-759 doi:10.1180/minmag.1980.043.330.08
Plain TextFanfani, L., Giuseppetti, G., Tadini, C., Zanazzi, P. F. (1980) The crystal structure of kogarkoite, Na3SO4F. Mineralogical Magazine, 43 (330) 753-759 doi:10.1180/minmag.1980.043.330.08
In(1980, June) Mineralogical Magazine Vol. 43 (330) Mineralogical Society
Abstract/NotesSummaryThe crystal structure of synthetic kogarkoite has been determined from X-ray data collected on an automatic diffractometer. The refinement was performed by a least-squares method employing anisotropic thermal parameters. The 3157 reflections with I > 3σ(I) converged to a conventional R value of 0.033. The cell content is 12 Na3SO4F, the space-group P21/m, a = 18.074, b = 6.958, c = 11.443 Å, β = 107.71°.Kogarkoite presents a marked trigonal subcell with c′ corresponding to [102] of the monoclinic cell. The tridimensional framework can be considered built up by nine differently stacked layers of Na atoms approximately perpendicular to the c′ axis (five sheets are present in galeite, six in sulphohalite, and seven in schairerite). The very close structural relationships between these minerals are discussed.

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Kogarkoite


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