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Henmi, Chiyoko, Kusachi, Isao, Henmi, Kitinosuke (1995) Morimotoite, Ca3TiFe2+Si3O12, a new titanian garnet from Fuka, Okayama Prefecture, Japan. Mineralogical Magazine, 59 (394) 115-120 doi:10.1180/minmag.1995.59.394.11

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Reference TypeJournal (article/letter/editorial)
TitleMorimotoite, Ca3TiFe2+Si3O12, a new titanian garnet from Fuka, Okayama Prefecture, Japan
JournalMineralogical MagazineISSN0026-461X
AuthorsHenmi, ChiyokoAuthor
Kusachi, IsaoAuthor
Henmi, KitinosukeAuthor
Year1995 (March)Volume59
Issue394
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_59/59-394-115.pdf
DOIdoi:10.1180/minmag.1995.59.394.11Search in ResearchGate
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Mindat Ref. ID2617Long-form Identifiermindat:1:5:2617:2
GUID0
Full ReferenceHenmi, Chiyoko, Kusachi, Isao, Henmi, Kitinosuke (1995) Morimotoite, Ca3TiFe2+Si3O12, a new titanian garnet from Fuka, Okayama Prefecture, Japan. Mineralogical Magazine, 59 (394) 115-120 doi:10.1180/minmag.1995.59.394.11
Plain TextHenmi, Chiyoko, Kusachi, Isao, Henmi, Kitinosuke (1995) Morimotoite, Ca3TiFe2+Si3O12, a new titanian garnet from Fuka, Okayama Prefecture, Japan. Mineralogical Magazine, 59 (394) 115-120 doi:10.1180/minmag.1995.59.394.11
In(1995, March) Mineralogical Magazine Vol. 59 (394) Mineralogical Society
Abstract/NotesAbstractMorimotoite, Ca3TiFe2+Si3O12, has been found in contaminated rocks which are considered to be a kind of endoskarn at Fuka, Bitchu-Cho, Okayama Prefecture, Japan. Morimotoite is derived from andradite, , by the substitution Ti + Fe2+ = 2Fe3+. It is associated with calcite, vesuvianite, grossular, wollastonite, hematite, prehnite, fluorapatite, perovskite, zircon, baddeleyite and calzirtite. It is cubic with space group Ia3d. The unit cell dimension a is 12.162(3) Å. Its refractive index n is 1.995(2) and the density 3.75(2) g cm−3 (meas.), 3.80 g cm−3 (calc.). The Mohs' hardness is 7.5. Calculation of the analytical data on the basis of twelve oxygen atoms and eight cations shows that this mineral has a simplified chemical formula Ca3(Ti,Fe2+Fe3+)2(Si,Fe3+)3O12 where Ti > Fe2+ > 0.5. Morimotoite was synthesized at low oxygen fugacities, 650 and 700°C and 1 kbar total pressure.

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Fuka mine, Fuka, Bitchū, Takahashi City, Okayama Prefecture, Japan

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Morimotoite

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LocalityMineral(s)
Fuka mine, Fuka, Bitchū, Takahashi City, Okayama Prefecture, Japan Morimotoite


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