The studied area is located in the middle section of the north margin of North China craton, which is one of the most important gold and nonferrous metal metallogenic belts. According to the diagram of coexistence surface, the ore-forming pres- sure can be calculated and it is in the range of 16~28 MPa, the ore-forming depth is in the range of 1.6~2.8 km. In contrast to other orogenic gold deposits worldwide, Xiaotazigou gold deposit is defined as epizonal orogenic gold deposit and the intracontinent collision was its metallogenic dynamic background.