Carbonate is a mineral that is composed of the carbonate ion (CO3) combined with a metal. The most common carbonate mineral is calcite, which is the main component of limestone and marble.
Carbonate minerals are formed through the precipitation of carbonates from water solutions. They are commonly found in sedimentary rocks such as limestone and dolomite. They can also occur in hydrothermal veins and metamorphic rocks.
Carbonate minerals have various industrial uses. For example, limestone is used in the production of cement, while dolomite is used as a source of magnesium and as a decorative stone in construction.