| The Xiongcun district is located on the southern margin of the central segment of the Gangdese metallogenic belt. Extensive research and exploration have been conducted in this area. Through geophysical and geochemical exploration combined with engineering validation, the Xiongcun No. 1 and No. 2 porphyry Cu-Au deposits have beendiscovered. The total Cu metal content exceeds 2.5 million tons, with associated Au over 250 tons and Ag over 1000 tons, making it an exceptionally large-scale deposit. However, many soil and rock Cu-Au element anomalies still exist in the periphery of No.1 and No.2 deposits in Xiongcun district, requiring further evaluation to guide the deployment of exploration work. In this context, by summarising the geochemical anomalies of soil and rock in the Xiongcun district, this paper carries out an electro-excitation physical survey in the Puqinmu-Yada area. And circles the J1 anomalous area with high apparent polarisation and low apparent resistivity in Puqinmu, and the J2 anomalous area with medium-high apparent polarisation and medium-low apparent resistivity in Yada. The two anomalies were also verified by drilling and trenching engineering, which revealed copper-gold ore bodies at the depth of the J1 anomaly and the surface of the J2 anomaly. It also concluded that the two anomalies are mineralised. It proposed that the deep and marginal parts of the J1 anomaly and the deep parts of the J2 anomaly have significant potential for ore searching, and are the key areas for future ore searching in the Xiongcun district. |