Superimposed versus residual basin:The North Yellow Sea Basin

作     者：Wenyong Li Wenfen Lu Yanxu Liu Jianchun Xu 

作者机构：China Aero Geophysical Survey and Remote Sensing Center for Land and ResourcesBeijing 100083China 

出 版 物：《Geoscience Frontiers》 (地学前缘（英文版）)

年 卷 期：2012年第3卷第1期

页      面：33-39页

核心收录：

学科分类：081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 

基　　金：supported by the National Important Special Project of Science and Technology of China(No.GZH200200301) 

主　　题：Superimposed basin Residual basin Identification method Basinal structures Basin superposition North Yellow Sea Basin 

摘      要：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.