Abstract:The paper studies magnetic fabric characteristic of faults developed in the typical ductility and weak deformation areas. The results show that the magnetic fabric can be used to determine the movement orientation of faults,structural deformation feature and deformation history. The magnetic fabric also reflects the correlation between fault deformation and metallogeny: gold mineralization and deformation intensity is positive correlation in ductile fault zone and negative correlation in Congshuban Pb-Zn area with weak deformation.