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Name: Fayalite RRUFF ID: X050077 Ideal Chemistry: Fe2+2SiO4 Locality: synthetic Source: G.R. Rossman 618 Owner: Caltech Description: Status: The identification of this mineral has been determined only by Raman spectroscopy |
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| Quick search: [ All Fayalite samples (8) ] | ||
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| REFERENCES for Fayalite | |
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American Mineralogist Crystal Structure Database Record: [view record] |
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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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Gmelin C G (1840) Chemische untersuchung des fayalits, Annalen der Physik und Chemie, 51, 160-164 [view file] |
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Wheeler E P (1965) Fayalitic olivine in northern Newfoundland-Labrador, The Canadian Mineralogist, 8, 339-346 [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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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] |
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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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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] |
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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 |
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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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Kolesov B A, Tanskaya J V (1996) Raman spectra and cation distribution in the lattice of olivines, Materials Research Bulletin, 31, 1035-1044 [link] |
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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] |
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Rasmussen M G, Evans B W, Kuehner S M (1998) Lowtemperature fayalite, greenalite, and minnesotaite from the Overlook gold deposit, Washington: phase relations in the system FeOSiO2H2O, The Canadian Mineralogist, 36, 147-162 [view file] |
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Kolesov B A, Geiger C A (2004) A Raman spectroscopic study of Fe-Mg olivines, Physics and Chemistry of Minerals, 31, 142-154 [link] |
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Mouri T, Enami M (2008) Raman spectroscopic study of olivine-group minerals, Journal of Mineralogical and Petrological Sciences, 103, 100-104 [view file] |
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Dyar M D, Sklute E C, Menzies O N, Bland P A, Lindsley D, Glotch T, Lane M D, Schaefer M W, Wopenka B, Klima R, Bishop J L, Hiroi T, Pieters C, Sunshine J (2009) Spectroscopic characteristics of synthetic olivine: An integrated multi-wavelength and multi-technique approach, American Mineralogist, 94, 883-898 [view file] |
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