Reference Type | Journal (article/letter/editorial) |
---|
Title | Morimotoite, Ca3TiFe2+Si3O12, a new titanian garnet from Fuka, Okayama Prefecture, Japan |
---|
Journal | Mineralogical Magazine | ISSN | 0026-461X |
---|
Authors | Henmi, Chiyoko | Author |
---|
Kusachi, Isao | Author |
Henmi, Kitinosuke | Author |
Year | 1995 (March) | Volume | 59 |
---|
Issue | 394 |
---|
Publisher | Mineralogical Society |
---|
Download URL | https://rruff.info/doclib/MinMag/Volume_59/59-394-115.pdf |
---|
DOI | doi:10.1180/minmag.1995.59.394.11Search in ResearchGate |
---|
| Generate Citation Formats |
Mindat Ref. ID | 2617 | Long-form Identifier | mindat:1:5:2617:2 |
---|
|
GUID | 0 |
---|
Full Reference | 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 |
---|
Plain Text | 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 |
---|
In | (1995, March) Mineralogical Magazine Vol. 59 (394) Mineralogical Society |
---|
Abstract/Notes | AbstractMorimotoite, 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. |
---|
These are possibly similar items as determined by title/reference text matching only.