摘要
Qiaohuote copper deposit, located at suture zone of Nalati Plate, is a medium-sized ore related to plate subduction. The ore body is lenticular, vein and cystic with surface of group-distribution. The ore is controlled by several factors including stratum, volcanic rock, intrusive rock and fracture. It belongs to medium-low temperature hydrothermal deposit with magmatic process controlled by fracture structure.