摘要
泌阳凹陷的两条边界同生大断裂控制了该凹陷的形成、发育、以及凹陷的沉降沉积中心和生油中心,并派生出了一些同生局部构造。凹陷内部构造和断裂构造类型、形成机制多种多样,它们对油气的形成和聚集起着重要的控制作用。
The origination,developing of Miyang depression and its sedimentary centre of subsi- dence,origining centre of hydrocarbon was controlled by two syngenetic boundary faults which in- duced some local syngenetie structures.There are various for inner structures,types and genetic mechanism of faults in Miyang depression.Which played an important role for origining and stack- ing of hydrocarbon.
出处
《矿物岩石》
CAS
CSCD
1996年第4期54-59,共6页
Mineralogy and Petrology
关键词
同生构造
派生构造
油气聚集
泌阳凹陷
油气藏
syngenetic structure
induced structure
stacking of hydrocarbon
Miyang depression
