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胶莱盆地的运动学特征
引用本文:戴俊生,陆克政,宋全友,陈书平.胶莱盆地的运动学特征[J].中国石油大学学报(自然科学版),1995(2).
作者姓名:戴俊生  陆克政  宋全友  陈书平
作者单位:石油大学勘探系
摘    要: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。

关 键 词:构造  拉张  运动学  胶莱盆地

KINEMATIC CHARACTERISTICS OF JIAOLAI BASIN
Dai Jultsheng, Lu Kezheng, Song Quanyou,Chen Shuping.KINEMATIC CHARACTERISTICS OF JIAOLAI BASIN[J].Journal of China University of Petroleum,1995(2).
Authors:Dai Jultsheng  Lu Kezheng  Song Quanyou  Chen Shuping
Abstract:Based on studies about the strike-slip tectonics and the natures of uplifting, subsidence and extension of the Jiaolai basin, this paper researches the kinematic characteristics of the basin. It was a Cretaceous strike-slip pull-apart basin and its uplifting,subsidence and the fault block tilting were closely correlated with the extension both on time and on intensity. These were all controlled by the strike-slip of the master fractures.The development of the basin experienced successively northeast pull-aparting northwest-southeast extension,north-south pull-aparting and withering.The pull-aparting controlled the formation of oil and gas pool in the basin.
Keywords:tructure: Pull-apart basin:Kinematics:Jiaolai basin  
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