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Introduction of Chlorite

Chlorite is a kind of layered silicate mineral structure. Of chlorite, used usually refer to the main for Mg and Fe of mineral kinds, namely inclined chlorite, oolite chlorite, etc. It is some metamorphic rock forming minerals. Igneous rocks such as magnesium iron ore from biotite, hornblende, pyroxene under low temperature hot water is easy to the formation of chlorite. The color with the iron content of many different shades of green. Vitreous luster to matt, cleavage plane is pearl luster. Mainly middle and low temperature hydrothermal process, shallow product of metamorphism and sedimentation.

Physical Characteristics of Chlorite

The morphology of chlorite is false six-party crystal crystal plate, usually with a scaly or roses aggregate output form; Color: dark gray, or from light green to dark green; Streaks: same color; Transparency: transparent; Gloss: vitreous luster, cleavage plane visible pearl luster; Hardness: 6.5; Cleavage and fracture: cleaves completely, jagged fracture; Weight: 3.6 g/cm3; Other properties: the chip can be bent, but easy to break, inelastic; Identifying features: with high hardness and brittleness difference chlorite, with mica sheet is the difference between the inelastic; Origin and occurrence, formed in the regional metamorphic rocks formed, such as schist and phyllite, also Yu Weijing rock formation, associated minerals have white mica, chlorite, garnet and staurolite and kyanite.

Identify Characteristics of Chlorite

Chlorite and mica is extremely similar, but the former has the characteristics of green, flexible without elasticity. Chlorite is some metamorphic rock forming minerals. Igneous rocks such as magnesium iron ore from biotite, hornblende, pyroxene under low temperature hot water is easy to the formation of chlorite. Chlorite, which is also called jasper, produced in Taiwan province dipper tam Hualien county. The stone colors are yellow, green, brown, green, or blue green. Stone muscle is concave and convex, torsion, irregular spherical. Stone shape change, mountains, islands, lakes, animals, etc. Rock hard and dense, feel beautiful.

Chlorite Deposit Studies

Chlorite is widely distributed in the hydrothermal type polymetallic deposit nearly dizzy ore mineral, in a large deposit in the near mineral tourmaline – well sericite quartz metasomatite, quartz sericite chlorite – water – metasomatic rock and carbonate mineral metasomatic rock, chlorite, through to the great well chlorite deposit composition determination, and with the domestic and foreign, comparing the same type deposits of chlorite ingredients found chlorite composition of iron available to signal of different metal combination. Big well deposit for Ag, Cu, Sn, Pb, zinc combination, chlorite for iron with high degrees of species, Russia, tile in zinc and tin deposit, deposit is mainly lead and zinc combination, the chlorite is relatively low degree of iron species. Big well chlorite deposit composition of iron and output highly positive correlation characteristics, its element and chlorite activity fe, mg and solution ph value in different ore deposits and variation on the same vertical section of ore deposits. In addition, the big well deposit unit cell parameters of chlorite b0 value highly also showed positive correlation with its output characteristics, which are found in shallow chlorite b0 value is big, from deep chlorite b0 value is small, it is the result of the high pressure conditions conducive to close packing structure.

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