Dolomite is a naturally occurring carbonate mineral composed of calcium magnesium carbonate (CaMg(CO₃)₂). It is classified as a double carbonate mineral due to its unique crystal structure, which differs from that of calcite. Because of its distinct structural arrangement, dolomite does not readily dissolve in dilute hydrochloric acid, making it more chemically stable compared to other carbonate minerals. These properties make dolomite suitable for a wide range of industrial and commercial applications.
