Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion.

 
  • 由于受區域構造長(cháng)期作用的影響,在北天山山前地區逐步發(fā)育形成了多排褶皺背斜及活動(dòng)斷裂,且運動(dòng)方式具有獨特性。
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