peridotite oor Indonesies
peridotite
en
(mineralogy) A rock consisting of small crystals of olivine, pyroxene and hornblende; the major constituent of the Earth's mantle.
Vertalings in die woordeboek Engels - Indonesies
Peridotit
en
igneous rock
That would be Icelandic peridotite.
Tapi itu akan peridotit Icelandic.
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Peridotite is the dominant rock of the upper part of the Earth's mantle.
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Spinel, (Mg,Fe)(Al,Cr)2O4, is common in peridotite in the uppermost Earth's mantle, between approximately 20 km to approximately 120 km, possibly to lower depths depending on the chromium content.
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Metasomatism is thought to be particularly important in changing the composition of mantle peridotite below island arcs as water is driven out of ocean lithosphere during subduction.
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The Halmahera lavas also record a temporal change in the chemistry of the mantle component that resulted from induced convection above the falling Molucca Sea Plate drawing compositionally distinct peridotite into the mantle wedge.
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Dunite and other peridotite rocks are considered the major constituents of the Earth's mantle above a depth of about 400 kilometers.
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Peridotite, including dunite, at and near the seafloor and in mountain belts is converted to serpentine, brucite, magnetite, and other minerals — some rare, such as awaruite (Ni3Fe), and even native iron.
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Peridotite is derived from the Earth's mantle, either as solid blocks and fragments, or as crystals accumulated from magmas that formed in the mantle.
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At significantly shallower depths, above the Moho, calcic plagioclase is the more stable aluminous mineral in peridotite while garnet is the stable phase deeper in the mantle below the spinel stability region.
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Icelandic peridotite, naturally.
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The compositions of peridotite nodules found in certain basalts and diamond pipes (kimberlites) are of special interest, because they provide samples of the Earth's mantle brought up from depths ranging from about 30 km to 200 km or more.
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Harzburgite typically forms by the extraction of partial melts from the more pyroxene-rich peridotite called lherzolite.
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Classic peridotite is bright green with some specks of black, although most hand samples tend to be darker green.
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Magnesium-rich olivine forms a large proportion of peridotite, and so magnesium content is high.
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Icelandic peridotite, naturally.
Dia telah membunuh ProfessorOpenSubtitles2018.v3 OpenSubtitles2018.v3
The word peridotite comes from the gemstone peridot, which consists of pale green olivine.
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If partial melting of the harzburgite continues, all of the pyroxene may be extracted from it to form magma, leaving behind the pyroxene-poor peridotite called dunite.
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But, Professor, that would be Icelandic peridotite.
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Metasomatism is more complicated in the Earth's mantle, because the composition of peridotite at high temperatures can be changed by infiltration of carbonate and silicate melts and by carbon dioxide-rich and water-rich fluids, as discussed by Luth (2003).
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That would be Icelandic peridotite.
Aku tidak akan pergi sendirianOpenSubtitles2018.v3 OpenSubtitles2018.v3
Ultramafic rocks such as peridotite and dunite can be residues left after extraction of magmas, and typically they are more enriched in olivine after extraction of partial melts.
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While green and yellow are the most common colors, peridotitic rocks may exhibit a wide range of colors such as blue, brown, and red.
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Lherzolite is known from the lower ultramafic part of ophiolite complexes (although harzburgite is more common in this setting), from alpine-type peridotite massifs, from fracture zones adjacent to mid-oceanic ridges, and as xenoliths in kimberlite pipes and alkali basalts.
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Proposed mechanisms of formation begin with partial melting of subducted material and of mantle peridotite (olivine and pyroxene) altered by water and melts derived from subducted material.
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In peridotite, plagioclase is stable at relatively low pressures (crustal depths), aluminous spinel at higher pressures (to depths of 60 km or so), and garnet at yet higher pressures.
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Tholeiitic basaltic magmas are initially generated as partial melts of peridotite (olivine and pyroxene) produced by decompression melting of the Earth's mantle.
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29 sinne gevind in 4 ms. Hulle kom uit baie bronne en word nie nagegaan nie.