Several copper-molybdenum-gold polymetallic deposits have been found in the Tethys metallogenic province, western Yunnan Province and this type of deposit is related to the intrusion and evolution of alkaline porphyry rocks. By studying an ore-host structural system of the deposit, it shows that the intrusive contact structures control the ore-forming process. A contact structural system due to magmatic intrusion is the main rock-and ore-control structures.