摘要
运用平衡剖面和去压实校正原理,从几何学、运动学的角度,对济阳坳陷沾化凹陷的渤南地区新生代构造特征及演化进行了研究。结果表明:①渤南地区新生代以发育盆倾的盖层滑脱正断层为主要构造特点,由于基岩和边界断层的影响,东部和西部的构造有明显差异。②新生代构造演化可以分为古近纪断陷阶段和新近纪、第四纪坳陷阶段,孔店组至沙三段沉积时期是主要的断陷期。③构造运动控制了圈闭的分布和类型,第三系油气圈闭主要分布在陈家庄凸起北斜坡向北凸出的部位,且自南而北分别由以地层圈闭为主过渡到以构造圈闭、构造-岩性圈闭为主。在圈闭的空间分布上,坡折带以南的斜坡上部以地层圈闭为主;坡折带附近及深洼区以构造圈闭和构造-岩性圈闭为主。
Based on the balanced section and the decompaction correction principle, the tectonic evolution of Cenozoic in the Bonan Region is analyzed from tectonic geometry and movement. The marginal slip normal faults are the main feature of the structure. Influenced by basement rocks and border faults, the structures in the west and in the east are obviously different. The Cenozoic tectonic evolution is divided into Paleogene faulting episode, Neogene depressing episode and Quaternary Depressing episode. The period between Ek and Es3 is the primary faulting phase. The tectonic movement controls the distribution and type of traps. The Tertiary traps mainly occur in the northward bulge in the northern slope of the Chenjiazhuang uplift, with the stratigraphic trap in the south and the structural and structural lithologic traps in the north. The stratigraphic trap is the main type in the upper position of the slope south of the slope break, while the structural trap and the structural-lithologic trap dominate in the deep water area and the in the vicinity of the slope break.
出处
《石油勘探与开发》
SCIE
EI
CAS
CSCD
北大核心
2006年第5期572-575,共4页
Petroleum Exploration and Development
基金
国家"十五"科技攻关项目(2001BA605A09)
关键词
渤南地区
新生代
构造演化
圈闭
油气成藏
Bonan Region
Cenozoic
tectonic evolution
trap
hydrocarbon accumulation
作者简介
马宝军（1975-），男，河北易县人，博士，石家庄经济学院教师，主要从事油区构造解析、沉积盆地分析方向的研究。地址：河北省石家庄市槐安东路136号，石家庄经济学院资源学院，邮政编码：050031。E-mail：bjma_009@163．com
