Detailed analyses of satellite images and field investigation have revealed that the active Kaidu River fault zone on the southern margin of the basin is a strike-slip fault zone.

详细的卫星图像分析和野外调查表明活动断层(开都河断层带)主要分布在盆地的南缘，具典型的走滑断层特征。

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The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.

伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。

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Jiaolai basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian -jimo-muping Fault.

胶莱盆地是中生代走滑拉分盆地，其形成与发育受到沂沭断裂和五莲-即墨-牟平断裂的控制。

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