Barite is the most common mineral of barium, and its composition is barium sulfate. It occurs in low-temperature hydrothermal veins, such as quartz-barite veins, fluorite-barite veins and so on, and is often associated with galena, sphalerite, chalcopyrite, cinnabar, etc. Most barite deposits in Hunan, Guangxi, Qinghai and Jiangxi are huge hydrothermal single mineral veins. Barite can also occur in sedimentary rocks, appearing as nodules, mainly in sedimentary manganese deposits and shallow-sea argillaceous and sandy sedimentary rocks. In the residual clay clays of weathered residual deposits, they often form nodules and lumps. Barite crystals are large tubular, aggregated crystals sometimes form rose-shaped or bifurcated blocks, which are called crown barite. Pure barite is colorless and transparent, generally white, light yellow, with glass luster.
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