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Davis, R. J., Hey, M. H., Kingsbury, A. W. G. (1965) Xanthiosite and aerugite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 72-83 doi:10.1180/minmag.1965.035.269.10

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Reference TypeJournal (article/letter/editorial)
TitleXanthiosite and aerugite
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsDavis, R. J.Author
Hey, M. H.Author
Kingsbury, A. W. G.Author
Year1965 (March)Volume35
Page(s)72-83Issue269
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_35/35-269-72.pdf+
DOIdoi:10.1180/minmag.1965.035.269.10Search in ResearchGate
Mindat Ref. ID5846Long-form Identifiermindat:1:5:5846:3
GUID304be27b-ed66-4378-8844-f7390683b669
Full ReferenceDavis, R. J., Hey, M. H., Kingsbury, A. W. G. (1965) Xanthiosite and aerugite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 72-83 doi:10.1180/minmag.1965.035.269.10
Plain TextDavis, R. J., Hey, M. H., Kingsbury, A. W. G. (1965) Xanthiosite and aerugite. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (269) 72-83 doi:10.1180/minmag.1965.035.269.10
In(1965) Mineralogical Magazine Vol. 35 (269) Mineralogical Society
Abstract/NotesSummaryTwo nickel arsenates from South Terras mine, St. Stephen-in-Brannell, Cornwall, have been shown to be identical with the minerals xanthiosite and aerugite, described by C. Bergemann in 1858, and with two synthetic products described by J. B. Taylor and R. D. Heyding (1958). Xanthiosite is pure golden-yellow, monoclinic, with a 10·174, b 9·548, c 5·766 Å, β 92° 58½′, space group P21/a; with D154=5·42±0·10, the unit cell contains 4[Ni3(AsO4)2] (Dcalc 5·388±0·003). Aerugite is deep blue-green, monoclinic, with a 10·29, b 5·95, c 9·79 Å, β 110° 19′, space-group C2, Cm, or C2/m; the ideal unit cell formula is 2[Ni9As3O16], with one-sixth of the arsenic trivalent; the natural mineral has a lower Ni:As ratio, around 2·6. Both xanthiosite and aerugite are minerals new to Britain.


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