Abstract: The Shahedele lead-zinc deposit in Ejina Banner represents a recent discovery of a lead-zinc deposit in the Hazhu Yagan deep fault zone. The ore body is situated within the upper formation of the Queershan Group marble formation, with the nearly east-west secondary fault acting as the controlling structure in the area. The surrounding rock alteration is characterized by silicification, carbonation, epidotization, and kaolinization, and is indicative of a mesothermal deposit. The geophysical characteristics of the ore-bearing structural alteration zone exhibit high resistance and high polarization. The geochemical anomaly elements are primarily composed of Pb, Zn, W, Mo, and so forth, exhibiting discernible concentration centers for each element and a notable anomaly intensity. Based on the geophysical, geochemical, ore-bearing construction, ore body characteristics, and rock alteration data collected in the work area, it can be preliminarily inferred that the Shaldere lead-zinc mining area has good prospecting potential.