Wuxu Ore Field is located in the southeast end of Danchi metallogenic belt in northwest Guangxi,where there are many polymetallic deposits distributed.Wuxu ore field has been studied for many years by predecessors and a lot of achievements have been made.In this paper,the genesis of the deposit,the study of ore-forming fluid inclusions,isotope and rare earth elements analysis,and the metallogenic regularity and prediction are discussed in detail,and the achievements of predecessors on the Wuxu Ore Field in recent years are summarized.Based on the recent outdoor geological survey,the analysis of trace elements in sphalerite and rare earth elements,the study believes that strong folding,faulting and magmatic intrusion took place in Wuxu Ore Field during Indosinian-Yanshanian,and the metallogenic pattern was mainly filling.The ore-forming fluid is characterized by medium-low temperature,rich CO₂ and low salinity.The ore-forming fluid mainly derived from magmatic hydrothermal fluid,with addition of a small amount of surrounding rock material.There are good prospecting prospects in the deep part of Wuxu Ore Field,and the prospecting work should start from the center and deep part of Jianzhupo Deposit.