摘要
Zhuyangguan-Xiaguan fault zone, which is 400 km long and reaching to the upper mantle in depth, is accompanied by lots of Yanshanian granite intrusion and a series of Cu, Au, Ag, Pb, Zn et al. geochemical anomaly, is favorable for colored and noble metal mineralization. The geological research indicated that Gaozhuang deposit is a typical auriferous quartz vein-and alteration-type gold deposit which in formed by submarine volcano exhalative-magmatic hydrothermal-structural hydrothermal activity process. The geological evidences, such as abundance Radiolarian-bearing pyrite bed in ~400 km long Erlangping Formation, large area of Cu-Au-Ag-Pb-Zn geochemical anomaly and lots of pyritized-, silicification- and polymetal sulfide-type alteration along Zhuanyangguan-Xiaguan fault zone, all indicate the great prospecting potential for gold polymetallic ore deposits in this area.