olivine oor Kroaties
olivine
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(mineralogy) any of a group of olive green magnesium-iron silicate minerals that crystallize in the orthorhombic system
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olivin
Olivin
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Translucent olivine is sometimes used as a gemstone called peridot (péridot, the French word for olivine).
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Olivine, nickel green [9]
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Olivine for building
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Unwrought or semi-wrought precious stones and semi-precious stones, in particular agates, Chalcedony, jet, Imitation jet, Jades, Jet, Cubic zirconia, Marcassites, Olivine, Opal, Ruby, Emeralds, Spinels, Topaz, Sardonyx, Peridot, Sapphires
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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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olivine, nickel green; [9]
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Olivine [gems]
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Olivine is named for its typically olive-green color (thought to be a result of traces of nickel), though it may alter to a reddish color from the oxidation of iron.
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Compositions of olivine are commonly expressed as molar percentages of forsterite (Fo) and fayalite (Fa) (e.g., Fo70Fa30).
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Another large olivine-rich outcrop is in Ganges Chasma, an eastern side chasm of Valles Marineris (pictured).
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Olivine [silicate mineral]
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Some of the finest gem-quality olivine has been obtained from a body of mantle rocks on Zabargad Island in the Red Sea.
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Olivine, nickel green; [9]
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The metamorphism of impure dolomite or other sedimentary rocks with high magnesium and low silica content also produces Mg-rich olivine, or forsterite.
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Olivine occurs in both mafic and ultramafic igneous rocks and as a primary mineral in certain metamorphic rocks.
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It also forms as a retrograde product rimming relict orthopyroxenes and olivine, and as an accessory mineral in cordierite-bearing gneisses and schists.
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Below depths of about 410 km (250 mi) olivine undergoes an exothermic phase transition to the sorosilicate, wadsleyite and, at about 520 km (320 mi) depth, wadsleyite transforms exothermically into ringwoodite, which has the spinel structure.
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The spectral signature of olivine has been seen in the dust disks around young stars.
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The tails of comets (which formed from the dust disk around the young Sun) often have the spectral signature of olivine, and the presence of olivine was verified in samples of a comet from the Stardust spacecraft in 2006.
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Olivine [gems], peridot
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It contains a higher ratio of olivine to carbonate than most sand on island.
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For instance in mafic and ultramafic melts, the MgO and SiO2 contents determine whether forsterite olivine is precipitated or whether enstatite pyroxene is precipitated.
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