Furthermore, this paper illustrated the reason of transition of basin evolution style, i.e. from rifting and extension to uplifting and whole subsidence during Dongying movement of Bohai Bay Basin.

• 岩石圈快速拉伸、上地幔上涌和温度升高以及壳下岩石圈的弹性回返可以很好地解释东营运动的形成过程以及渤海湾盆地演化阶段的转折。