滑陷构造又称滑塌构造，是指已沉积的沉积层在重力作用下发生运动和位移所产生的各种同生变形构造的总称。
本文通过对方正地区所发现的负花状构造及其有关构造运动形迹分析的基础上，进一步提出方正断陷是走滑—拉分形成的断陷盆地。
Based on the negative flower shaped structure and its relative structural movement track in Fangzheng area, this paper suggests that Fangzheng rift is a rifted basin formed by strike slip pull apart.
在济阳坳陷拉张构造模式的基础上，着重研究了桩海地区的走滑和挤压构造特征。
The characters of strike - slip and extrusion structure in the Zhuanghai region were emphatically studied on the tensile structure model in the Jiyang Depression.
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