Wu-Xia fault belt is located in the eastern part of thrust zone in northwestern margin of Junggar basin, which was tectonically the most active area here.

 
  • 準噶爾盆地西北緣沖斷帶東段的烏夏斷裂帶是西北緣構造活動(dòng)最為強烈的地區。由于多期的構造活動(dòng),斷裂的平面和剖面形態(tài)呈現出復雜化和多樣性。
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