由此表明，基底收缩作用和挤压作用的不对称性促使反冲断层的发育。
These facts show that substrate contraction and asymmetric compression can facilitate the development of rearward-ver-gent thrusts.
从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在，指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
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