The structural analysis based on the explanation of seismic profiles indicates that a lot of thrust faults and strike-slip faults of Late Cenozoic occur in western Hexi Corridor and nearby regions.

• 基于地震剖面解释的构造分析表明,河西走廊西段及邻区发育有许多晚第三纪第四纪的逆断层与走滑断层。