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Fayalite - Wikipedia, the free encyclopedia

https://en.wikipedia.org/wiki/Fayalite

Fayalite (Fe 2 SiO 4; commonly abbreviated to Fa), also called iron chrysolite, is the iron-rich end-member of the olivine solid-solution series. In common with all ...

Fayalite: Fayalite mineral information and data.

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O'Neill, H.S.C. (1987) The quartz-fayalite-magnetite equilibria and free energies of formation of fayalite (Fe2SiO4) and magnetite (Fe3O4). American Mineralogist: ...

Fayalite Mineral Data

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Fayalite Crystallography: Axial Ratios: a:b:c =0.4666:1:0.5862 : Cell Dimensions: a = 4.76, b = 10.2, c = 5.98, Z = 4; V = 290.34 Den(Calc)= 4.66

Fayalite Minerals,Fayalite Information,Fayalite Uses ...

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Read about fayalite minerals, fayalite mineral, fayalite uses, fayalite information, fayalite occurrences, fayalite properties, fayalite hardness, fayalite specific ...

fayalite | mineral | Britannica.com

www.britannica.com/science/fayalite

Fayalite, iron-rich silicate mineral that is a member of the forsteritefayalite series of olivines.

FAYALITE (Iron Magnesium Silicate) - Amethyst Galleries

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Fayalite is named for the Island of Fayal of the Azores. It is one of two minerals that are simply known as olivine. The other mineral is forsterite.

Fayalite | Article about Fayalite by The Free Dictionary

encyclopedia2.thefreedictionary.com/fayalite

fayalite[fə′yä‚līt] (mineralogy) Fe2SiO4 A brown to black mineral of the olivine group, consisting of iron silicate and found either massive or in crystals ...

Fayalite | Define Fayalite at Dictionary.com

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noun 1. a rare brown or black mineral of the olivine group, consisting of iron silicate. Formula: Fe2SiO4

Forsterite - Wikipedia, the free encyclopedia

https://en.wikipedia.org/wiki/Forsterite

Forsterite (Mg 2 SiO 4; commonly abbreviated as Fo) is the magnesium-rich end-member of the olivine solid solution series. It is isomorphous with the iron-rich end ...

Fayalite - definition of fayalite by The Free Dictionary

www.thefreedictionary.com/fayalite

Magnetite is abundant (up to 10%), much of it replacing what may have been fayalite crystals, by comparison with similar alteration in syenite in the West Barneys ...