摘要
Qingchengzi ore concentration area consists of Qingchengzi Pb-Zn ore field and its peripheral Au-Ag deposits.Their geological characteristics,geochemical features and mineralizing process had been discussed separately in the past.The author believes that both the ore field and its peripheral deposits share the same deposit genesis,and both of them are sedimentation-exhalation origin and were formed in Paleoproterozoic Era.They established consistent mineralization model,and experienced reconstruction that produced by different geologic processes.The magmatic-tectonic action in Indo-Chinese epoch of Mesozoic Era has the most influence on reconstruction of the Au-Ag deposits.