Carbonatite is an igneous rock consisting primarily of carbonate minerals crystallized from a carbonate magma. There are three main hypotheses for the origin of carbonatite melts: 1) immiscible separation of parental carbonated silicate magmas, 2) crystal fractionation of carbonated silicate magmas, and 3) low-degree partial melting of carbonated mantle peridotite. Carbonatites can be classified based on their main carbonate mineral component, such as dolomite-carbonatite or ferroan-carbonatite. They commonly occur as shallow intrusive bodies like volcanic necks, dykes, and cone-sheets associated with alkali-rich silicate ig