摘要
渤海湾盆地是一个主要受壳-幔活动控制而发展起来的新生代含油气盆地。按壳-幔拱张活动的强弱可将第三系凹陷和凸起划分为壳-幔强烈拱张型的一级凹陷和凸起、中等拱张型的二级凹陷和凸起及弱量拱张型的三级凹陷和凸起。盆地深部的壳-幔结构控制了大地热流场、凹陷的类型和含油气丰度。以及油气的分布和富集规律。
Bohaiwan basin is a Cenozoic petroleum bearing basin whose development was mainly controlled by the crust-mantle activities. According to the uplifting strength of the crustmantle, the Tertiary sags and uplifts can be classified into 3 types, i.e. (1) strongly uplifting sags and uplifts; (2) moderatly uplifting sags and uplifts; (3) weakly uplifting sags and uplifts. The deep crust-mantle structure of the basin controlled the heat flow, the types of sags, the abundance of petroleum, and the distribution and accumulation of oil and gas.
出处
《石油勘探与开发》
SCIE
EI
CAS
CSCD
北大核心
1993年第6期1-7,14,共8页
Petroleum Exploration and Development
