Mineral resources are the products of the crust in its long-term formation, development and evolution, and are formed by the accumulation of natural minerals under certain geological conditions and through certain geological processes. Different geological processes can form different types of minerals. According to the different geological processes, energy and material sources that form mineral resources, the geological processes that form mineral resources, namely mineralization, are generally divided into endogenetic mineralization, exogenetic mineralization, metamorphic mineralization and superimposed mineralization. Endogenetic mineralization refers to various geological processes that lead to the formation of ore deposits due to the influence of the earth's internal thermal energy. Exogenic mineralization refers to various geological processes that form deposits on the surface of the crust under the direct action of solar energy and in the interaction process of the upper lithosphere, hydrosphere, biosphere and aerosphere caused by the earth's external stress. Metamorphic mineralization refers to the geological process that changes the mineral assemblage, chemical composition, physical properties and structure of the ore deposits or ore bearing rocks formed by internal and external mineralization due to the change of the geological environment, especially through deep burial or other thermal dynamic events, to form another type of deposit with different properties and quality. Superimposed mineralization is a kind of composite mineralization, which refers to a geological process of forming ore deposits due to the composite superposition of multiple mineralization. These four different mineralization processes form four different types of deposits, namely endogenetic deposits, exogenetic deposits and superimposed deposits. Whether, how much and whether the minerals can be formed in a region are directly related to the quality of the metallogenic geological conditions in the region.