The antimony deposit occurs on the south side of the major Muzitage sliding fault.The mineralization belt is controlled by secondary faults striking NEE and EW.

• 锑矿产于木孜塔格大型走滑断裂南侧，矿化带受NEE向及EW向次级断裂控制，矿体形态相对复杂，多为似层状、脉状、网脉状、囊状等。