The distribution of Au, Sb deposit is controlled by the NS right-handed torsion structure system. The Devonian Sb anomaly is in large scale, high intensity, with the clear concentration center, whereas the scattered Au anomaly is distributed in Triassic, Cambrian, in small scale. There are a series of prospecting trace, such as, Au, As, Sb assemblage anomaly; Sb in shallow, Au in deep of SE Sanjiacun Member; Au related to silicic rock in shallow of Xiyanghe Member; Au(Sb) in 2nd bed of Cuifengshan Formation.