Dolomite is a carbonate rock containing calcium and magnesium. It is mainly composed of dolomite, with a small amount of calcite, clay minerals, chert, magnesite, and sometimes gypsum, celestite, barite, pyrite and organic matter. Dolomite is generally off-white in color and similar in appearance to limestone. Some transitional types of ores can be divided between limestone and dolomite according to the different proportions of calcite and dolomite. Generally called dolomite refers to relatively pure dolomite with a calcite content of less than 5%.
China is rich in dolomite resources.Most of the deposits have been developed and utilized, and their production areas are spread across all provinces. At present, dolomite is widely used in metallurgy, chemical industry, construction and other industries. Dolomite is a non-metallic mineral resource with great economic value and can be developed and utilized in many ways. It is of great significance to adhere to the fine processing and efficient and rational utilization of dolomite.
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