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Moore, Paul B., Ito, Jun (1978) Kidwellite, NaFe93+(OH)10(PO4)6·5H2O, a new species. Mineralogical Magazine, 42 (321) 137-140 doi:10.1180/minmag.1978.042.321.21

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Reference TypeJournal (article/letter/editorial)
TitleKidwellite, NaFe93+(OH)10(PO4)6·5H2O, a new species
JournalMineralogical MagazineISSN0026-461X
AuthorsMoore, Paul B.Author
Ito, JunAuthor
Year1978 (March)Volume42
Issue321
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_42/42-321-137.pdf+
DOIdoi:10.1180/minmag.1978.042.321.21Search in ResearchGate
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Full ReferenceMoore, Paul B., Ito, Jun (1978) Kidwellite, NaFe93+(OH)10(PO4)6·5H2O, a new species. Mineralogical Magazine, 42 (321) 137-140 doi:10.1180/minmag.1978.042.321.21
Plain TextMoore, Paul B., Ito, Jun (1978) Kidwellite, NaFe93+(OH)10(PO4)6·5H2O, a new species. Mineralogical Magazine, 42 (321) 137-140 doi:10.1180/minmag.1978.042.321.21
In(1978, March) Mineralogical Magazine Vol. 42 (321) Mineralogical Society
Abstract/NotesKidwellite, NaFe93+(OH)10(PO4)6·5H2O, monoclinic, Z = 2, a = 20·61(7) Å, b = 5·15(1) Å, c = 13·75(6) Å, β = 112·64(15)·, space group A2/m, Am, or A2, is a new species that occurs in moderate abundance as a late-stage mineral associated with rockbridgeite, dufrenite, beraunite, and strengite in novaculite deposits. Colour lively pale chartreuse-green, to greenish-yellow, greenish-white, and bright yellow. H = 3, lustre silky, streak yellow, cleavage {100} perfect, habit acicular elongated parallel to [010], flattened on {100}, biaxial (−), α = 1·787(5), β = 1·800(5), γ = 1·805(5), 2V large, β∥b, not discernibly pleochroic.The mineral is moderately widespread as a replacement of rockbridgeite and beraunite from the Ouachita Mountains, Arkansas; Indian Mountain, Alabama; Irish Creek, Virginia; Waldgirmes, West Germany. A related, but apparently distinct, species is also noted from the McMahon pegmatite, South Australia, and the Sapucaia pegmatite, Minas Gerais, Brazil.

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