Abstract: Panshanlou gold deposit is located in Fuxin,western Liaoning,and is one of the largest mylonite-type gold deposits in China that is currently known to be controlled by ductile shear zones.The mineralization in the Panshanlou gold deposit is found within the ancient Yujianping Group metamorphic mylonite fracture zone.The ore is heavily altered,but has a relatively low grade.Currently,the mine has been in a state of crisis due to years of mining,making it imperative to conduct exploration for replacement resources in order to increase ore reserves and extend the mines service life.Panshanlou gold deposit has been studied using deep penetration geochemical exploration methods for mineralization prediction.The main methods employed include analysis of hydrocarbon gases,adsorbed phased mercury,and radon gas in different geological settings.2 profiles were established,and a total of 73 soil geochemical samples were collected.Each sample was analyzed for adsorbed phased mercury and 7 organic hydrocarbon gas components.Additionally,radon gas measurements were conducted along 36 exploration lines.The research results indicate that methane,ethane,propylene,n-butane,and adsorbed mercury anomalies in the profiles show a good spatial correlation with the ore bodies.Methane and ethane exhibit single-peak anomalies above the ore bodies,while propylene,n-butane,and adsorbed phased mercury show multi-peak anomalies.Lastly,through comprehensive analysis and comparison of the hydrocarbon and mercury anomaly characteristics,4 prospective mineralization target areas were delineated.