fayalite oor Spaans
fayalite
en
(mineralogy) Yellow, olive green, brown or black mineral with orthorhombic crystals of the olivine group, Fe <sub>2</sub> SiO <sub>4</sub> .
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Fayalita
en
olivine, nesosilicate mineral
fayalita
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Characteristic is the fayalite content (Fa) in olivine of 21 to 25 mol%.
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Characteristic is the fayalite (Fa) content of the olivine of 16 to 20 mol%.
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In the absence of atmospheric oxygen (O 2), in deep geological conditions prevailing far away from Earth atmosphere, hydrogen (H 2) is produced during the process of serpentinization by the anaerobic oxidation by water protons (H+) of the ferrous (Fe2+) silicate present in the crystal lattice of fayalite (Fe 2SiO 4, the olivine iron-endmember).
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Such is the case, for example, with the olivine (forsterite-fayalite) system.
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In the olivine structure, the main olivine series of (Mg, Fe)2SiO4 consist of magnesium-rich forsterite and iron-rich fayalite.
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For example, the olivine group is described by the variable formula (Mg, Fe)2SiO4, which is a solid solution of two end-member species, magnesium-rich forsterite and iron-rich fayalite, which are described by a fixed chemical formula.
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It is accompanied by fayalite-forsterite and labradorite.
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Cristobalite with Tridymite and Fayalite on Obsidian
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It belongs to the forsterite-fayalite mineral series. Peridot is an idiochromatic gem, meaning its color comes from the basic chemical composition of the mineral itself and not from minor traces of impurities.
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MINERALOGY: It is a mineral belonging to an isomorphic series at one end the fosferita (Mg2 [SiO4]) and the other fayalite (Fe2 [SiO4]), has primary origin in deep rocks composed of ultrabasic magmas.
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Or even in Pirdov, Aurubis seat, whose copper concentrates processing plant employs 820 people to produce copper anodes and cathodes and copper byproducts such as sulfuric acid and fayalite.
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Minerals & Meteorites - Fayalite-olivine-group
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An evaluation of the volume of liquid infiltration and the time needed to reach the maximum level were compared for three types of industrial refractories and three types of molten phases: fayalitic slag, matte and copper.
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It belongs to the forsterite-fayalite mineral series. Peridot is an idiochromatic gem, meaning its color comes from the basic chemical composition of the mineral itself and not from minor traces of impurities.
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