In the east of Hongshui River, there was an intense magmatic activity and it develops into a series of quartzdiorite porphyrite and tonaliteporphyrite. The alteration characteristics of porphyry mineralized, such as chloritization, epidotization, carbonatization, potash feldspathization, kaolinization, dicanization, sericitization and skarnization, are commonly developed in the intrusion, wallrock and their contact zone. In this area, there are broad Cu, Mo, W geochemical composite anomalies, which are the typical elements assemblage of porphyry copper deposits. So, eastern of Hongshui River has the ore-forming geological conditions of Porphyry Cu-Mo deposit and there is a big potential for porphyry copper-molybdenum.