摘要
Through interpretation of the remote sensing geological structure in the south part of Jiapigou gold mining area,pointed out that the gold deposit occurrence in the district where was joint controlled by the "broom" type compresso-shear rift structure and "fan" type tensional fault structure system in the Mesozoic era.The "fan" type tensional fault structure system developed in the east half part of Xing’antun-Yunfengcun annular structure and the structures formed by the Mesozoic era granite magma intrusion,and supplied with available occurrence space for gold and other mineralizing elements.According to the relationship between the structure magmatic activities and gold mineralization,this paper discussed the genesis of gold ore in the study area.The research conclusion has important significance for the surface and deep prospecting in the south part of Jiapigou gold mining area.