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从走滑构造及派生的伸展构造和升降史入手，研究了胶莱盆地的运动学特征．该盆地是一个白垩纪走滑拉分盆地，其升降活动、断块掀斜活动和伸展活动在时间上和强度上密切相关，控制上述活动的是主控断裂的走滑运动。盆地的发育经历了北东向拉分、北西─南东向扩展、南北向拉分和盆地萎缩四个阶段。盆地的拉分过程控制着内部油气藏的形成条件。
Starting from the structure of the strike slip and the derived extensional structure and the history of the rise and fall, the kinematic characteristics of the Jiaolai Basin are studied. The basin is a Cretaceous strike-slip basin. The up-and-down activities, the fault-lift activities and the extension activities are closely related in time and intensity. The main activities of the basin are the strike-slip movement of the main fault. The development of the basin experienced four stages: the north-east division, the northwest-south-east expansion, the north-south division and the basin shrinkage. The sub-division of the basin controls the formation conditions of the internal reservoirs.