Gold vein in Xigou area of Qixia city is controlled by fault structure with the trend of NNE, country rocks of mineralization are mainly composed of medium size monzonitic granite in Fushan unit of Wendeng superunit in Indo-China period. Geophysical abnormality and gold mineralization are very evident, which is a typical alteration type gold deposit. This area locates in west part of Douya—Taiqian fault belt with the trend of NE, secondary fault structure with the trend of NE, NNE developed well, and minera...