摘要
北方黄海盆是中生代和新生代盆。把外形基于盆边缘，沉积变瘦，盆和 vitrinite 反射的尺寸和形状，诺思黄海盆不是剩余盆。盆的开发的分析三结构的层，独立石油系统，边界差错活动， MesozoicCenozoic 沉积中心的移植，在不同时期期间形成的不同的盆结构，和二阶段的扩大的盆和一个阶段消沉盆的重叠，北方黄海盆作为附加的盆被认出。
The North Yellow Sea Basin is a Mesozoic and Cenozoic basin. Based on basin-margin facies, sedimentary thinning, size and shape of the basin and vitrinite reflectance, North Yellow Sea Basin is not a residual basin. Analysis of the development of the basin＇s three structural layers, self-contained petroleum systems, boundary fault activity, migration of the Mesozoic--Cenozoic sedimentation centers, different basin structures formed during different periods, and superposition of a two-stage extended basin and one-stage depression basin, the North Yellow Sea Basin is recognized as a superimposed basin.
基金
supported by the National Important Special Project of Science and Technology of China(No.GZH200200301)
关键词
北黄海盆地
残留盆地
叠加
新生代盆地
沉积中心
盆地边缘
石油系统
断层活动
Superimposed basin
Residual basin
Identification method
Basinal structures
Basin superposition
North Yellow Sea Basin
