The structural ore-controlling regularities in mid-segment of Yishu River fault zone was summarized according to the attitude of stratum,the lithology and the tectonic joint in the field survey,and the microscopically observation,the sample test analysis.The wield tectonic theory was used to research the mineralization background.The metallogeny of gold deposits there can be merotomized two stages which is inheritance relationship between the basement of ductile shear belt and the fault zone.The gold deposit is not occurrented in the ductile shear belt,and the ductile shear belt acts as the main ore-controlling structure and control the attitude of ore deposit.The secondary structure controls the spread and extends of the ore deposit.The ore deposit is located in the stress concentration belt,which is fierce and superposed tectonic activity area.The ductile shear belt ore-controlling regularity is that the gold controlled gradient-like in vertical direction.The ore-controlling structure which derivatives from the Yishu River fault zone shows ductility-transition-brittle evolution rules(geocyclic) from east to west,and the structure combination configuration shows like a fall "N".Associated structure shows associated geocyclic and constitute law level tectonic association.