The degree of activity of marginal structural belt of Junggar basin assumes obvious decline since Hercynian, weak adjustment in Mesozoic and reascending in Cenozoic with less level than in Hercynian.

• 准噶尔盆地的6边形边缘带划分为6个边缘构造带分段构造组合：准噶尔盆地南缘西段、南缘东段、准东隆起西缘段、乌伦古边缘构造段、加依尔山边缘段和准噶尔盆地西部边缘段。