mafic oor Fins
mafic
en
(geology) Describing rocks, such as silicate minerals, magmas, and volcanic and intrusive igneous rocks, which contain relatively high concentrations of heavier elements.
Vertalings in die woordeboek Engels - Fins
Mafinen
en
silicate mineral or rock that is rich in magnesium and iron
mafinen
fi
1|magnesiumia, alumiinia ja rautaa sisältävä
Geskatte vertalings
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Generally speaking, more mafic magmas, such as those that form basalt, are hotter and less viscous than more silica-rich magmas, such as those that form rhyolite.
Henkilökohtaisista syistäWikiMatrix WikiMatrix
One example concerns crystallization of melts that form mafic and ultramafic rocks.
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Mineral deposits related to mafic and ultramafic plutonism and resulting from magmatic processes such as fractional crystallisation.
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Often the species of mafic minerals is included in the name, for instance, hornblende-bearing granite, pyroxene tonalite or augite megacrystic monzonite, because the term "granite" already assumes content with feldspar and quartz.
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ultramafic / mafic
PähkinänkuoressaEurLex-2 EurLex-2
Typically, primitive melts of this composition form lamprophyre, lamproite, kimberlite and sometimes nepheline-bearing mafic rocks such as alkali basalts and essexite gabbros or even carbonatite.
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Of the mafic minerals present, augite is the most common.
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In the experiments we emplaced gold-palladium capsules (with a diameter of 2.3 to 3.0 mm and length of 6-10mm) containing black schist powder to the furnace, which was then melted in the desired run conditions that ranged from 700 to 1100°C and from 1 to 2 kbar (roughly corresponding to depth of 4 to 8 km in Earth’s crust in contact with hot mafic magma).
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The lower crust consists of tonalitic gneiss, mafic garnet granulite, hornblendite, pyroxenite and minor mafic eclogite.
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Common mafic rocks include basalt, dolerite and gabbro.
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In some cases, felsic volcanic rocks may contain phenocrysts of mafic minerals, usually hornblende, pyroxene or a feldspar mineral, and may need to be named after their phenocryst mineral, such as 'hornblende-bearing felsite'.
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The monzodioritic rocks are presumed to represent the last liquids of the mafic magmas of the complex, and the hornblende granite and the granitic veins are presumed to represent the first felsic melts of the granitic intrusion stage.
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Among the rock types in the anorthosite inclusions, leucogabbronorite has the highest potential to be utilized, because it is the most common mafic rock type in the inclusions and contains the most spectrolite.
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Water and other volatiles can more easily and gradually escape from mafic lava, so eruptions of volcanoes made of mafic lavas are less explosively violent than felsic-lava eruptions.
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These accumulations typically occur on the floor of the magma chamber, although they are possible on the roofs if anorthite plagioclase is able to float free of a denser mafic melt.
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The anorthosite inclusions of Mättö, Pahaoja and Ylijärvi are composed of mafic rock types, but Jokimies and Niemistenpitkä (E and W) anorthosites contain mafic rock types only in the centre.
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