Subsidence History of the Bohaiwan Basin and Implication for Cenozoic Dynamic Processes in Eastern China
The Bohalwan basin belongs to a family of extensional basins in East China. The Cenozoic subsidence of the basin is controlled by a combination of lithospheric thinning and polycyclic strike-slip movements. Three episodic riftings have been identified, the Paleocence-Early Eocene, Middle-Late Eocene and Oligocene rifting. Similar to a general extension basin, the basin underwent rifting and post-rifting stages. However, superimposed dextral movement of strike-slip fault resulted in intensified subsidence or local inversion during the Oligocene and Late Miocene-Quaternary in the Bozhong depression. The results indicate that there is a close relationship between formation and evolution of the Bohaiwan basin and lithospheric thinning.
tectonic subsidence dextral movement dynamic topography Bohaiwan basin.
Xie Xinong Li Sitian Ren Jianye Gong Zaisheng Dong Weiliang
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China China National Offshore Oil Corporation, Beijing 100087, China
国际会议
The IPACES 6th Annual Meeting(“现代地球科学,交流与合作国际学术研讨会暨第六届IPACES学术年会)
武汉
英文
207-208
2007-04-25(万方平台首次上网日期,不代表论文的发表时间)