According to geologic mapping and strain analysis, the regional S-N tectonics only developed in Pre-Ordovician areas, and the northeast of Tesibahan Faults formed before Hercynian orogeny.

• 通过地质填图综合调查和应变分析研究，区域性的南-北向构造仅发育于前奥陶系分布区，特斯巴汗断裂北东，是海西运动前的产物。