The gold deposits in Dongping area, northern Hebei Province are firstly found among the alkaline complex in China. These gold deposits are often recognized as alkaline rock-related gold deposits because of surrounding rocks. Alterations and mineralization of the Dongping gold deposit can be divided into four stages. They are 1) feldspar-quartz veins stage, 2) pyrite-white quartz stage, 3) sulphides-smoky gray quartz vein stage, and 4) late carbonate stage. It is more reasonable to consider the gold deposit in the Dongping area as intrusion-related gold deposits, based on geological setting, hydrothermal alteration, ore mineral assemblage, and characteristics of fluid inclusions.