Abstract: The Baguamiao superlarge deposit is hosted in the Devonian of Qinling, Shaanxi. The processes of the regional tectonics evolution in Qingling orogenic belt play an important role in metallization. The mineralization intensity and mineralized field is controlled by brittle-ductile shear zone and the converging junctures of brittle-ductile shear zone and fault. Based on the comprehensive analysis of orefield geology, characteristics of orebody and metallotect, the author summarizes the metallogenic regularities, and points out the direction for prospecting.