提出了地幔底辟和深断裂带右旋走滑位移两种动力机制联合作用主导了东濮凹陷的新生代应力场演化的构造动力学模式。
It indicates that two dynamical mechanisms of mantle diaper and right-lateral strike slip in deep faulted zone lead tectonic dynamics model evolved in Cenozoic stress field of Dongpu depression.
进入新生代喜马拉雅期，本区的构造格局发生了重大变革，即由原来的NW—SE向挤压构造应力场变为ne—sw挤压构造应力场。
In the Cenozoic Himalayan period, great changes took place in the tectonic framework in the study area, i. e. the original NW-SE compressional stress field changed into a NE-SW one.
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