| Li Sanzhong,Xu Shumei,Shan Yehua,Li Xishuang,Zhou Lihong,Hao Yinquan,Fan Zheqing,Liang Huilan.Basin assemblages and tectonic evolution in the Bohai Gulf and its neighbors[J].Acta Oceanologica Sinica,2000,(4):91-105 |
| Basin assemblages and tectonic evolution in the Bohai Gulf and its neighbors |
| Basin assemblages and tectonic evolution in the Bohai Gulf and its neighbors |
| 投稿时间：2000-06-15 修订日期：2000-06-21 |
| DOI： |
| 中文关键词: Bohai Basin tectonic evolution basin assemblage Precambrian Cenozoic |
| 英文关键词:Bohai Basin tectonic evolution basin assemblage Precambrian Cenozoic |
| 基金项目: |
| 作者 | 单位 | | Li Sanzhong | Ocean University of Qingdao, Qingdao 266003, China | | Xu Shumei | Ocean University of Qingdao, Qingdao 266003, China | | Shan Yehua | Ocean University of Qingdao, Qingdao 266003, China | | Li Xishuang | Ocean University of Qingdao, Qingdao 266003, China | | Zhou Lihong | Dagang Oilfield Group Company Ltd., Tianjin 300280, China | | Hao Yinquan | Dagang Oilfield Group Company Ltd., Tianjin 300280, China | | Fan Zheqing | Dagang Oilfield Group Company Ltd., Tianjin 300280, China | | Liang Huilan | Dagang Oilfield Group Company Ltd., Tianjin 300280, China |
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| 中文摘要: |
| According to multi-disciplinary research advances in recent years, three blocks which named Jiaoliao-Bohai block, central North China block and Ordos block are divided.The differences of the tectonic association, types, styles and features in the space, and ewlution fmm Archaean to Cenozoic in the time, between the former two blocks are discussed.Tectonic features and evolution in the four tectonic stages of Precambrian, Indo-China, Yanshanian and Cenozoic are emphasized especially here.All of them described above have inherit and neogenic property.The temporal-spatial change and interaction among basin assemblages in the above four stagers are analyzed.Escape tectonic model is employed to interpret coeval compressive and extensional basins in the study area. |
| 英文摘要: |
| According to multi-disciplinary research advances in recent years, three blocks which named Jiaoliao-Bohai block, central North China block and Ordos block are divided.The differences of the tectonic association, types, styles and features in the space, and ewlution fmm Archaean to Cenozoic in the time, between the former two blocks are discussed.Tectonic features and evolution in the four tectonic stages of Precambrian, Indo-China, Yanshanian and Cenozoic are emphasized especially here.All of them described above have inherit and neogenic property.The temporal-spatial change and interaction among basin assemblages in the above four stagers are analyzed.Escape tectonic model is employed to interpret coeval compressive and extensional basins in the study area. |
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