Definition, Betydelse & Anagram | Engelska ordet CHLORITE

Definition av CHLORITE

1. klorit

Exempel på hur man kan använda CHLORITE i en mening

• It is a common alteration product of periclase in marble; a low-temperature hydrothermal vein mineral in metamorphosed limestones and chlorite schists; and formed during serpentinization of dunites.
• It has as a geological limit the La Victoria Fault, where the rocks of the Gran Caracas group outcrop, on the igneous-metamorphic basement of the Sebastopol Complex of the lower Paleozoic, which is constituted by gneissic granite and chlorite schist.
• The name comes from the green hue imparted by the colour of the metamorphic minerals within the mafic rocks: The typical green minerals are chlorite, actinolite, and other green amphiboles.
• The minute crystals of graphite, sericite, or chlorite, or the translucent fine-grained white mica, impart a silky, sometimes golden sheen to the surfaces of cleavage, called "phyllitic luster".
• Blueschist often has a lepidoblastic, nematoblastic or schistose rock microstructure defined primarily by chlorite, phengitic white mica, glaucophane, and other minerals with an elongate or platy shape.
• Other minerals in the ore, but which had no economic importance include quartz, calcite, epidote, pumpellyite, chlorite and feldspar.
• Accessory minerals include chlorite, apatite, zircon and magnetite, with rare biotite, hornblende or pyroxene.
• It occurs in skarns developed in contact metamorphosed impure limestones or calcic igneous rocks; in chlorite schists and serpentinites and in alkalic igneous rocks (typically titaniferous).
• Mixing sodium chlorite solution with a weak food-grade acid solution (commonly citric acid), both stable, produces short-lived acidified sodium chlorite (ASC) which has potent decontaminating properties.
• The company produces magnesia clinker, slightly burnt magnesia, chlorite, firebricks and fireproofing materials.
• In uralitization, secondary hornblende replaces augite; chloritization is the alteration of augite (biotite or hornblende) to chlorite, and is seen in many diabases, diorites and greenstones.
• He observed that as a pelitic rock undergoes higher pressures and temperatures, its mineral assemblage changes from predominantly chlorite to biotite to garnet to staurolite to kyanite to sillimanite.
• During the transition from blueschist to greenschist facies, paragonite and glaucophane are transformed into chlorite and albite.
• occurs naturally as the mineral eskolaite, which is found in chromium-rich tremolite skarns, metaquartzites, and chlorite veins.
• Among these ores and minerals are: apatite, biotite, calcite, chlorite group, chondrodite, corundum, danburite, elbaite, fluor-cannilloite, graphite, humite, lepidolite, varieties of microcline such as amazonite, muscovite, olivine, orthoclase, paragonite, pargasite, phlogopite, pyrite, quartz and smoky quartz, rossmanite, rutile, schorl, spinel, titanite and tourmaline; gemstones such as rubies, spinel, and tourmaline.
• Thuringite is a variety of the chlorite mineral chamosite, a hydrous iron and aluminium silicate mineral.
• In the presence of water it weathers into minerals such as goethite, chlorite, smectite, maghemite, and hematite.
• Delessite is a mineral variety, a magnesium-rich form of chamosite which is a member of the chlorite group.
• Quartz crystals make up 25%, plagioclase 5%, alkali feldspar 10%, biotite 5–10% which is altered to chlorite, epidote and leucoxene.
• In argillaceous sedimentary rocks the assemblage is quartz, illite, albite, and stilpnomelane chlorite.

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