Iron ore is the primary raw material for steel production, and steel is one of the core materials for modern industry and infrastructure development. Hematite has the chemical composition α-Fe2O3 and is an oxide mineral belonging to the hexagonal crystal system. It is polymorphic with magnetohematite (γ-Fe2O3), which crystallizes in the isometric system, and has a Mohs hardness of 5.5–6. 5. Hematite accounts for a significant proportion of China's iron ore resources, characterized by wide distribution, large reserves, and low grade. Compared with magnetite, hematite has finer mineral dissemination size and higher clay content, making mineral processing more difficult. Hematite deposits in China are widely distributed, mainly concentrated in provinces such as Liaoning, Hebei, Gansu, Anhui, Henan, Inner Mongolia, Shanxi, Guizhou, and Hubei.