Fayalite R100104

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Record 2083 of 4216  

Name: Fayalite
RRUFF ID: R100104
Ideal Chemistry: Fe2+2(SiO4)
Locality: Dannemora, Uppsala Province, Sweden
Source: American Museum of Natural History 75253 [view label]
Owner: RRUFF
Description: Dark brown fragment, variety knebelite
Status: The identification of this mineral is confirmed by single-crystal X-ray diffraction and chemical analysis.
Mineral Group: [ Olivine (61) ]
Quick search: [ All Fayalite samples (8) ]
CHEMISTRY 
RRUFF ID: R100104.2
Sample Description: Microprobe Fragment
Measured Chemistry: (Fe+21.020Mn+20.931Mg0.052Ca0.002Zn0.001)Σ=2.006Si0.997O4
Microprobe Data File: [ Download Excel File ]
RAMAN SPECTRUM 
RRUFF ID:
Sample Description: Unoriented Raman on the primary sample
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BROAD SCAN WITH SPECTRAL ARTIFACTS
RRUFF ID: R100104
Wavelength:
Sample Description: Unoriented Raman on the primary sample
Instrument settings: Thermo Almega XR 532nm @ 100% of 150mW
POWDER DIFFRACTION 
RRUFF ID: R100104.9
Sample Description: Single crystal, powder profile is calculated
Cell Refinement Output: a: 4.8524(8)Å    b: 10.607(2)Å    c: 6.158(1)Å
alpha: 90°    beta: 90°    gamma: 90°   Volume: 316.93(6)Å3    Crystal System: orthorhombic
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Calculated diffraction file.

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Output file from the Bruker D8 Advance instrument. Includes device headers and XY data.

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REFERENCES for Fayalite

American Mineralogist Crystal Structure Database Record: [view record]

Anthony J W, Bideaux R A, Bladh K W, and Nichols M C (1990) Handbook of Mineralogy, Mineral Data Publishing, Tucson Arizona, USA, by permission of the Mineralogical Society of America. [view file]

Gmelin C G (1840) Chemische Untersuchung des Fayalits, Annalen der Physik und Chemie, 51, 160-164   [view file]

Gmelin C G (1840) Chemische untersuchung des Fayalits, eines neuen Minerals von der Azorischen Insel Fayal (Chemical analysis of fayalite, a new mineral from the Azores island of Fayal), Neues Jahrbuch für Mineralogie, Geognosie, Geologie und Petrefakten-Kunde, 1840, 596-597   [view file]

Wheeler E P (1965) Fayalitic olivine in northern Newfoundland-Labrador, The Canadian Mineralogist, 8, 339-346   [view file]

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Mossman D J, Pawson D J (1976) X-ray and optical characterization of the forsterite-fayalite-tephroite series with comments on knebelite from Bluebell mine, British Columbia, The Canadian Mineralogist, 14, 479-486   [view file]

Bayliss P (1977) X-ray and optical characterization of the forsterite-fayalite-tephroite series with comments on knebelite from Bluebell Mine, Britich Columbia: discussion, The Canadian Mineralogist, 15, 267-267   [view file]

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Takéuchi Y, Yamanaka T, Haga N, Hirano M (1984) High-temperature crystallography of olivines and spinels, in Materials Science of the Earth's Interior Terra Scientific Pub. Co. Tokyo 191-231

Kudoh Y, Takeda H (1986) Single crystal X-ray diffraction study on the bond compressibility of fayalite, Fe2SiO4 and rutile, TiO2 under high pressure, Physica B, 139, 333-336

Ballet O, Fuess H, Fritzsche T (1987) Magnetic structure and cation distribution in (Fe,Mn)2SiO4 (olivine) by neutron diffraction, Physics and Chemistry of Minerals, 15, 54-58

Boström D (1987) Single-crystal X-ray diffraction studies of synthetic Ni-Mg olivine solid solutions, American Mineralogist, 72, 965-972   [view file]

McCormick T C, Smyth J R, Lofgren G E (1987) Site occupancies of minor elements in synthetic olivines as determined by channeling-enhanced X-ray emission, Physics and Chemistry of Minerals, 14, 368-372

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Chopelas A (1991) Single crystal Raman spectra of forsterite, fayalite, and monticellite, American Mineralogist, 76, 1101-1109   [view file]

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Zhang L (1998) Single crystal hydrostatic compression of (Mg,Mn,Fe,Co)2SiO4 olivines, Physics and Chemistry of Minerals, 25, 308-312

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