The Jiaolai strike-slip pull-apart basin is characterized by: 1 shallow-water sequences along the strike-slip faults and deep-water sequences far from the strike-slip faults;

胶莱走滑拉分盆地层序特征表现为：（1）靠近走滑断层的区域发育浅水型层序，而远离走滑断层的区域发育深水型层序；

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According to the analysis of Mesozoic and Cenozoic tectonic evolution, Bohai Bay basin is a strike slip pull apart basin formed in the Cenozoic Eocene epoch.

从渤海湾盆地的中、新生代构造演化分析，渤海湾盆地是一个新生代早第三纪始新世形成的走滑拉分盆地。

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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.

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。

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