At the course of subduction, collision and collage among the Siberia, Khazakstan and Junggar blocks, the geotectonic environment underwent a few evolutional stages, they provided good congenital, parturient and postnatal conditions for the deposit.

• 在西伯利亚、哈萨克斯坦－准噶尔板块多阶段的俯冲、碰撞、拼合过程中，矿床所处的大地构造环境经历了多个开合演化阶段，为该矿床提供了良好的先天、临产及后天条件。