The Biliutai Lead-Zinc Deposit, a newly discovered deposit in the southern section of the Greater Khingan Mountains, is located in the eastern part of the Huanggang-Ganjur Temple-Ulanhot metallogenic belt. It is hosted in the shallow metamorphic rock series of the Permian Linxi Formation and primarily controlled by NE-trending structures. By analyzing 1:10 000 soil geochemical survey data through parameter statistics, single-element anomaly analysis, cluster analysis, factor analysis, and factor anomaly analysis, the F1 factor anomaly zone (Ag-Pb-Zn-Mn assembly) was identified as a critical prospecting indicator for silver-lead-zinc mineralization. High-precision magnetic survey data were processed using reduction-to-pole, continuation, horizontal first derivative, and vertical second derivative methods to extract structural planes/inear structures and geological bodies/ring-shaped structures. Building on geological exploration, combined with soil geochemical anomalies and high-precision magnetic survey interpretations, this study integrates geological. geochemical, and geophysical prospecting indicators to provide a basis for determining further prospecting directions and engineering layouts.