除具陆相盆地的一般特征外，还具有十分突出的叠加褶皱变形特征，因而极为少见。
It has not only common characters of continental basins, but also remarkable superimposed fold deformation.
准噶尔盆地西北缘前陆冲断带构造样式复杂多样，除规模较大的逆断层外，还发育一系列北西向的走滑断层。
The foreland thrust belt has complex and various structural styles. Besides the large-scale reverse faults, there are a series of north-west strike-slip faults.
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