摘要
舍女寺地区位于渤海湾盆地黄骅坳陷的南部，新生代主要发育了上、下两个相对独立而又互相关联的断层系统。下部断层系统的走向优势方位为北东３０°～４０°，按倾向分为同向正断层和反向正断层两组；上部断层系统的走向优势方位为北东７０°～８０°。断层的分布和组合规律控制着以地堑（半地堑）与地垒（半地垒）为主的多种构造组合样式，从而控制了以断块油气藏为主、不同类型油气藏上下叠合的舍女寺复式油气聚集带的形成。
Shenusi area. situated at the south part of Huanghua Depression of Bohai Bay Basin, develops two independent but interrelated fault systems which had different distribution and various fault assemblages in both lower and upper sequences. The dominant strik direction of fault system in the lower sequence is NE 30°￣40°,and the upper one is NE 70°￣80°.The relationship between deformation and hydrocarbon accumulation and distribution shows that the structural styles and the oil and gas traps are directely controlled by the fault systems.
出处
《石油大学学报（自然科学版）》
CSCD
1996年第A00期6-10,共5页
Journal of the University of Petroleum,China(Edition of Natural Science)
关键词
新生代
断层
类型
构造组合
油气藏
发育
Cenozoic, Fault type,Structural assemblages. Oil and gas reservoir.Huanghua depression
