Beiya Gold Polymetallic Deposit is a typical skarn-porphyry type gold polymetallic deposit related to the alkali-rich porphyry in the Jinshajiang-Ailaoshan alkali-rich porphyry metallogenic belt.The deposit scale has reached a super large scale.Wandongshan Ore Section is one of the important ore sections of Beiya Gold Polymetallic District.The KT44 ore body is one of the main ore bodies in this section,and its gold metal content has exceeded 20 t.Earlier,it was believed that the KT44 ore body was produced in moderately inclined ore body in the interlayer fragmentation zone.With the progress of stripping work,it is now believed that the ore body is produced in the F6 fracture zone,with a steep incline to the west and nearly upright,and is not controlled along the strike and tendency.By summarizing the characteristics of the KT44 ore body and the geological characteristics and ore-controlling factors of the ore section,it is believed that the KT44 ore body still has a great prospecting potential in the deep and along strike and tendency of F6 fault,where it is expected to achieve a prospecting breakthrough.