摘要
二连盆地的形成与演化经历了早、中侏罗世,晚侏罗-早白垩世的裂陷作用和中侏罗世末,早白垩世末和晚白垩世末的反转作用,可以识别出压性,压扭性等反转构造,盆地的裂陷期是生油岩主要发育期,而反转作用期形成的各种叠加构造圈闭则是油气聚集的重要场所。
The formation and evolution of Erlian Basin withstood rifting at early-middle Jurassic and late
Jurassic-early Cretaceaous and inversion at the end of middle Jurassic and early Cretaceaous and
late Cretaceous:which may help us identify compressive and compressive-shear inversion. The rift
ing phase of basin is the development stage of source rocks,but various superimposition of struc
tural traps formed during inversion phase are important place where the oil and gas accumulated.
出处
《中国海上油气(地质)》
1997年第2期106-110,共5页
China Offshore Oil and Gas(Geology)