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运用古地磁学方法研究了库车坳陷第三系同沉积褶皱，同褶皱检验发现上新统和渐新统原生剩磁主要是同沉积剩磁，说明该区上新世和渐新世表现出较强的构造活动性；因而，对推断控制库车坳陷油气分布的构造格架和相关的构造形迹有十分重要的地质意义。
Using palaeomagnetic method to study the syndepositional fold of the Tertiary in the Kuqa Depression. It is found from the same fold test that the primary residual magnetism of the Upper Pleistocene and Oligocene are mainly the same sedimentary remnant, indicating the Pliocene and Oligocene Therefore, it is of great geological significance to infer the tectonic framework and related tectonic features of the hydrocarbon distribution in the Kuche Depression.