Coalfields in Qinghai Province are mainly distributed in the Datong River Basin of the central Qilian Mountains and along the northern margin of the Qaidam Basin. The region includes several important identified mining areas such as Yuka, Juhu'geng, Jiangcang, Reshui, Datong, and Damaigou. The coal-bearing formations span multiple geological periods, from lower to upper: Carboniferous, Permian, Late Triassic, and Early to Middle Jurassic, with the Early to Middle Jurassic being predominant. The province contains nearly all coal types, with coking coal as the primary type, accounting for about half of the total proven reserves, followed by long-flame coal, non-caking coal, lean coal, gas coal, and anthracite. Coal from the Carboniferous system is generally low-ash lean coal and anthracite, with minor occurrences of gassy fat coal and coking coal, and locally higher sulfur content. The raw coal quality is characterized by ash content of 5–28%, volatile matter of 18.16–38%, total sulfur of 0.25–0.5%, carbon content of 89.96%, and a net calorific value on as-received basis (Qnet,ar) of 4000–6800 kcal/kg.