The tectonic differences between the east and the west in the deep-water area of the northern South China Sea

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• 作者：Zhongyu Xia ; Zhifeng Wan ; Xianqing Wang ; Qiuhua Shi ; Song Cai…
• 关键词：structural feature ; tectonic evolution ; tectonic difference ; deep ; water basins ; northern South China Sea
• 刊名：Acta Oceanologica Sinica
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：35
• 期：1
• 页码：86-95
• 全文大小：2,489 KB
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• 作者单位：Zhongyu Xia (1)
  Zhifeng Wan (1) (2) (3)
  Xianqing Wang (1)
  Qiuhua Shi (4)
  Song Cai (5)
  Bin Xia (1)
  
  1. School of Marine Sciences, Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering/Key Laboratory of Offshore Oil Exploration and Development of Guangdong Higher Education Institutes, Sun Yat-sen University, Guangzhou, 510006, China
  2. The State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Southwest Petroleum University), Chengdou, 610500, China
  3. The Key Laboratory of Gas HydrateMinistry of Land and Resources, Qingdao, 266071, China
  4. Center for Assessment and Development of Real Estate, Shenzhen, 518034, China
  5. Shenzhen Branch of CNOOC Ltd., Guangzhou, 510240, China
  
• 刊物主题：Oceanography; Climatology; Ecology; Engineering Fluid Dynamics; Marine & Freshwater Sciences; Environmental Chemistry;
• 出版者：Springer Berlin Heidelberg
• ISSN：1869-1099

文摘

The deep-water area of the northern South China Sea, which has active and complicated tectonics, is rich in natural gas and gas hydrate. While the tectonic characteristics is different obviously between the east and the west because of the special tectonic position and tectonic evolution process. In terms of submarine geomorphology, the eastern shelf-slope structure in Pearl River Mouth Basin is characterized by having wide sub-basins and narrow intervening highs, whereas the western (Qiongdongnan Basin) structure is characterized by narrow subbasins and wide uplift. As to the structural features, the deep-water sags in the east are all structurally halfgrabens, controlled by a series of south-dipping normal faults. While the west sags are mainly characterised by graben structures with faulting in both the south and north. With regards to the tectonic evolution, the east began neotectonic activity when the post-rifting stage had completed at the end of the Middle Miocene. In the Baiyun Sag, tectonic activity became strong and was characterised by rapid subsidence and obvious faulting. Whereas in the west, neotectonic activity began at the end of the Late Miocene with rapid deposition and weak fault activity. Key words structural feature tectonic evolution tectonic difference deep-water basins northern South China Sea