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Miyake, Akira (1985) Zn-rich staurolite from the Uvete area, central Kenya. Mineralogical Magazine, 49 (353) 573-578 doi:10.1180/minmag.1985.049.353.11

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Reference TypeJournal (article/letter/editorial)
TitleZn-rich staurolite from the Uvete area, central Kenya
JournalMineralogical MagazineISSN0026-461X
AuthorsMiyake, AkiraAuthor
Year1985 (September)Volume49
Issue353
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_49/49-353-573.pdf+
DOIdoi:10.1180/minmag.1985.049.353.11Search in ResearchGate
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Mindat Ref. ID3765Long-form Identifiermindat:1:5:3765:9
GUID0
Full ReferenceMiyake, Akira (1985) Zn-rich staurolite from the Uvete area, central Kenya. Mineralogical Magazine, 49 (353) 573-578 doi:10.1180/minmag.1985.049.353.11
Plain TextMiyake, Akira (1985) Zn-rich staurolite from the Uvete area, central Kenya. Mineralogical Magazine, 49 (353) 573-578 doi:10.1180/minmag.1985.049.353.11
In(1985, September) Mineralogical Magazine Vol. 49 (353). Mineralogical Society
Abstract/NotesAbstractZn-rich staurolite occurs in a pelitic gneiss from the Uvete area, central Kenya. The rock was metamorphosed to staurolite-kyanite grade during the Mozambique metamorphism. Microprobe analyses of the staurolite gave the following values (in wt. %): SiO2 26.2–27.3, Al2O3 52.4–53.5, FeO 8.3–9.2, MgO 2.2–2.6, and ZnO 6.0–7.5. Cell dimensions are a = 7.874(± 0.003), b = 16.620(±0.006), c = 5.656(±0.002) Å and β = 90.00 (± 0.002)°. Optical properties are 2Vz = 82–85°, α = 1.742 (±0.002), β = 1.747(±0.002) and γ = 1.753(±0.002). The optical dispersion is moderate and r > v. Density is 3.83(±0.01) g/cm3. Infra-red absorption spectra were also recorded. The cation correlation suggests that the principal substitutions in the staurolite are Zn ⇆ Fe in the tetrahedral sites in the hydroxide sheet and Al ⇆ Mg in the octahedral sites.


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