摘要
由于郯庐断裂的羽状断裂带——泰洲走滑断裂带和真武—小纪走滑断裂带的活动,加上盆地深处壳下物质活动、地幔上隆、莫霍面抬升,导致地块沿印支剥蚀面滑移,从而形成了溱潼、高邮两拉分盆地。沿走滑断裂带两侧形成的一系列局部构造,是油气聚集的良好场所。
Because of the action of the feather fault belts of Tanlu fault-Tai-zhou strike-slip faults and Zhenwu-Xiaoji strike-slip faults,together with the action of deep subcrustal materials in the basin, the uplift of the mantle and the rising of Mho-plane, the block is caused to slip along Yinzhi erosion surface so as to form both Qintong and Gaoyou pull-apart basins. Along both sides of the strike-slip faults are formed a series of structures, which are good places of oil and gas accumulation.
出处
《西南石油学院学报》
CAS
CSCD
1989年第2期17-24,共8页
Journal of Southwest Petroleum Institute
