Fayalite R100104

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Record 1307 of 4043  

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
  File Type Information Close
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]

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

Fisher G W (1967) Fe-Mg olivine solid solutions, Carnegie Institution of Washington Year book, 66, 209-217

Birle J D, Gibbs G V, Moore P B, Smith J V (1968) Crystal structures of natural olivines, American Mineralogist, 53, 807-824   [view file]

Louisnathan S J, Smith J V (1968) Cell dimensions of olivine, Mineralogical Magazine, 36, 1123-1134   [view file]

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Fisher G W, Medaris L G (1969) Cell dimensions and X-ray determinative curve for synthetic Mg-Fe olivines, American Mineralogist, 54, 741-753   [view file]

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Smyth J R (1975) High temperature crystal chemistry of fayalite, American Mineralogist, 60, 1092-1097   [view file]

Mokeeva V I, Simonov M A, Belokoneva E L, Makarov E S, Ivanov V I, Rannev N V (1976) X-ray study of details of structure and distribution of magnesium and iron atoms in lunar and terrestrial olivines, Akademii Nauk SSSR, Eksperimental’no-Metodicheskie Issledovaniya Rudnykh Mineralov, Moscow, 13, 84-92

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]

Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine, American Mineralogist, 62, 286-295   [view file]

Schwab R G, Küstner D (1977) Präzisionsgitterkonstantenbestimmung zur Festlegung röntgenographischer Bestimmungskurven für synthetische Olivine der Mischkristallreihe Forsterit-Fayalit, Neues Jahrbuch für Mineralogie, Monatshefte, 5, 205-215

Riekel C, Weiss A (1978) Cation-ordering in synthetic Mg2-xFexSiO4-olivines, Zeitschrift für Naturforschung B Anorganische Chemie, Organische Chemie, 33b, 731-736

Takei H (1978) Growth of fayalite (Fe2SiO4) single crystals by the floating-zone method, Journal of Crystal Growth, 43, 463-468

Fujino K, Sasaki S, Takéuchi Y, Sadanaga R (1981) X-ray determination of electron distributions in forsterite, fayalite and tephroite, Acta Crystallographica, B37, 513-518

Suzuki I, Seya K, Takei H, Sumino Y (1981) Thermal expansion of fayalite Fe2SiO4, Physics and Chemistry of Minerals, 7, 60-63

Annersten H, Ericsson T, Filippidis A (1982) Cation ordering in Ni-Fe olivines, American Mineralogist, 67, 1212-1217   [view file]

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Annersten H, Filippidis A (1984) Cation ordering in Ni-Fe olivines: reply, American Mineralogist, 69, 164-164   [view file]

Ike E C, Bowden P, Martin R F (1984) Fayalite and clinopyroxene in the porphyries of the Tibchi anorogenic ring-complex, Nigeria: postmagmatic initiation of a peralkaline trend, The Canadian Mineralogist, 22, 401-409   [view file]

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

Motoyama T, Matsumoto T (1989) The crystal structures and the cation distributions of Mg and Fe of natural olivines, Mineralogical Journal, 14, 338-350

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

Akamatsu T, Kumazawa M, Aikawa N, Takei H (1993) Pressure effect on the divalent cation distribution in nonideal solid solution of forsterite and fayalite, Physics and Chemistry of Minerals, 19, 431-444

Kolesov B A, Tanskaya J V (1996) Raman spectra and cation distribution in the lattice of olivines, Materials Research Bulletin, 31, 1035-1044   [link]

Müller-Sommer M, Hock R, Kirfel A (1997) Rietveld refinement study of the cation distribution in (Co, Mg)-olivine solid solution, Physics and Chemistry of Minerals, 24, 17-23

Pani E, Rizzo R, Raudsepp M (1997) Manganoan-fayalite-bearing granitic pegmatite from Quirra, Sardinia: relation to host plutonic rocks and tectonic affiliation, The Canadian Mineralogist, 35, 119-133   [view file]

Rasmussen M G, Evans B W, Kuehner S M (1998) Low–temperature fayalite, greenalite, and minnesotaite from the Overlook gold deposit, Washington: phase relations in the system FeO–SiO2–H2O, The Canadian Mineralogist, 36, 147-162   [view file]

Redfern S A T, Knight K S, Henderson C M B, Wood B J (1998) Fe-Mn cation ordering in fayalite-tephroite (FexMn1-X)2SiO4 olivines: a neutron diffraction study, Mineralogical Magazine, 62, 607-615   [view file]

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

Ovchinnikov N O, Nikitina L P (1999) The real structure and thermodynamic properties of olivine solid solutions (FexMn1-x)2SiO4, Doklady Akademii Nauk, 368, 535-539

Merli M, Oberti R, Caucia F, Ungaretti L (2001) Determination of site population in olivine: Warnings on X-ray data treatment refinement, American Mineralogist, 86, 55-65   [view file]

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Kroll H, Kirfel A, Heinemann R (2014) Axial thermal expansion and related thermophysical parameters in the Mg,Fe olivine solid-solution series, European Journal of Mineralogy, 26, 607-621

Xu H, Shen Z, Konishi H, Fu P, Szlufarska I (2014) Crystal structures of laihunite and intermediate phases between laihunite-1M and fayalite: Z-contrast imaging and ab initio study, American Mineralogist, 99, 881-889

Burnley P C (2015) Elastic plastic self-consistent (EPSC) modeling of plastic deformation in fayalite olivine, American Mineralogist, 100, 1424-1433

Martin A M, Médard E, Devouard B, Keller L P, Righter K, Devidal J L, Rahman Z (2015) Fayalite oxidation processes in Obsidian Cliffs rhyolite flow, Oregon, American Mineralogist, 100, 1153-1164

Glassley W E, Korstgård J A, Sørensen K (2016) Further observations related to a possible occurrence of terrestrial ahrensite, American Mineralogist, 101, 2347-2350

Zhang J S, Hu Y, Shelton H, Kung J, Dera P (2017) Single-crystal X-ray diffraction study of Fe2SiO4 fayalite up to 31 GPa, Physics and Chemistry of Minerals, 44, 171-179

Breitenfeld L B, Dyar M D, Carey C J, Tague T J, Wang P, Mullen T, Parente M (2018) Predicting olivine composition using Raman spectroscopy through band shift and multivariate analyses, American Mineralogist, 103, 1827-1836

Morrison S M, Downs R T, Blake D F, Prabhu A, Eleish A, Vaniman D T, Ming D W, Rampe E B, Hazen R M, Achilles C N, Treiman A H, Yen A S, Morris R V, Bristow T F, Chipera S J, Sarrazin P C, Fendrich K V, Morookian J M, Farmer J D, Des Marais D J, Craig P I (2018) Relationships between unit-cell parameters and composition for rock-forming minerals on Earth, Mars, and other extraterrestrial bodies, American Mineralogist, 103, 848-856

Morrison S M, Downs R T, Blake D F, Vaniman D T, Ming D W, Hazen R M, Treiman A H, Achilles C N, Yen A S, Morris R V, Rampe E B, Bristow T F, Chipera S J, Sarrazin P C, Gellert R, Fendrich K V, Morookian J M, Farmer J D, Des Marais D J, Craig P I (2018) Crystal chemistry of martian minerals from Bradbury Landing through Naukluft Plateau, Gale crater, Mars, American Mineralogist, 103, 857-871