feldspar oor Indonesies
feldspar
en
(mineralogy) Any of a large group of rock-forming minerals that, together, make up about 60% of the earth's outer crust. The feldspars are all aluminum silicates of the alkali metals sodium, potassium, calcium and barium. Feldspars are the principal constituents of igneous and plutonic rocks.
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Feldspar
en
mineral group
A kind of stone, usually dark red, purple, or sometimes green, containing feldspar crystals.
Sejenis batu, biasanya berwarna merah tua, ungu, atau adakalanya hijau, yang mengandung kristal-kristal feldspar.
feldspar
A kind of stone, usually dark red, purple, or sometimes green, containing feldspar crystals.
Sejenis batu, biasanya berwarna merah tua, ungu, atau adakalanya hijau, yang mengandung kristal-kristal feldspar.
felspar
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Other minerals, such as olivines, pyroxenes, amphiboles, micas, feldspars, and quartz, may be found in metamorphic rocks, but are not necessarily the result of the process of metamorphism.
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The mineral assembly is usually abundant feldspathoids (nepheline or leucite), plagioclase, and augite, together with olivine and lesser iron-titanium oxides such as ilmenite and magnetite-ulvospinel; minor alkali feldspar may be present, as illustrated by the position of the field for basanite in the QAPF diagram.
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Feldspars are also found in many types of sedimentary rocks.
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The relative proportions of feldspars and quartz in dacite, and in many other volcanic rocks, are illustrated in the QAPF diagram.
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With this there is practically always a smaller amount of plagioclase, usually oligoclase; but the potassium feldspar (sanidine) often contains a considerable proportion of the sodium feldspar (albite), and has rather the characteristics of anorthoclase or cryptoperthite than of pure sanidine.
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Dacite consists mostly of plagioclase feldspar with biotite, hornblende, and pyroxene (augite and/or enstatite).
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Feldspars are a common example: anorthoclase is an alkali aluminum silicate, where the alkali metal is interchangeably either sodium or potassium.
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They often cover the surfaces of the larger feldspars or line the steam cavities of the rock, where they may be mingled with amorphous opal or fibrous chalcedony.
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Flake mica comes from several sources: the metamorphic rock called schist as a byproduct of processing feldspar and kaolin resources, from placer deposits, and from pegmatites.
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Feldspar.
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According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% to 90% of the feldspar is plagioclase.
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Orthoclase (potassium feldspar) is a common rock-forming mineral.
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In this series, quartz is the most stable, followed by feldspar, micas, and finally other less stable minerals that are only present when little weathering has occurred.
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Amphibolite is a grouping of rocks composed mainly of amphibole and plagioclase feldspar, with little or no quartz.
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Its mineral assemblage is usually alkali feldspar and plagioclase in approximately equal amounts.
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The term 'aplite' or 'aplitic' is often used as a textural term to describe veins of quartz and feldspar with a fine to medium-grain "sugary" texture.
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Less quartz content would lead to "quartz alkali feldspar syenite".
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Feldspars (KAlSi3O8 – NaAlSi3O8 – CaAl2Si2O8) are a group of rock-forming tectosilicate minerals that make up about 41% of the Earth's continental crust by weight.
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The texture can be similar to micrographic texture and to the coarser graphic intergrowths of quartz and alkali feldspar common in pegmatite.
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The calcium rich plagioclase feldspar (labradorite-bytownite) and pyroxene content vary between 10–90% in gabbro.
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This bone contains particulates of quartz and feldspar.
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A kind of stone, usually dark red, purple, or sometimes green, containing feldspar crystals.
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Some minerals, like quartz, mica or feldspar are common, while others have been found in only a few locations worldwide.
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The minerals best suited for dating include biotite, muscovite, metamorphic hornblende, and volcanic feldspar; whole rock samples from volcanic flows and shallow instrusives can also be dated if they are unaltered.
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The arkose sandstone which makes up the formation is composed of grains that show little sorting based on grain size, exhibit very little rounding and the feldspars in the rock are relatively fresh in appearance.
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50 sinne gevind in 9 ms. Hulle kom uit baie bronne en word nie nagegaan nie.