Journal of Marine Sciences ›› 2013, Vol. 31 ›› Issue (1): 1-15.

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Post-rift subsidence anomaly and its mechanism in the Baiyun Sag, Pearl River Mouth Basin

FU Jie1,2,3, LI Ming-bi1, TANG Yong1,2, QIU Wen-xian1,4, WANG Hui5   

  1. 1. Second Institute of Oceanography, SOA, Hangzhou 310012, China;
    2. Laboratory of Submarine Geosciences, SOA, Hangzhou 310012, China;
    3. Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China;
    4. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China;
    5. China Petroleum Logging Co., Ltd, Xi'an 710201, China
  • Received:2011-06-29 Revised:2012-07-03 Online:2013-03-15 Published:2022-11-29

Abstract: Post-rift subsiding anomalies have been discovered in many basins in the northern continental margin of South China Sea, of which Baiyun Sag is a typical one. We used software Temis Suite 2007 to build the backstripping model of three NNW—SEE-oriented seismic profiles crossing the Baiyun Sag, and analyzed the post-rift subsidence. The results show that the Baiyun Sag experienced anomalous post-rift subsidence. Compared with the Mckenzie's classic port-rift subsidence model, the Main Baiyun Sag subsided over 2.6 km deeper and the Southern Baiyun Sag subsided nearly 2 km. An accelerated subsidence stage could be conducted during 16.5~10.5 Ma, which might relate to the end of sea-floor spreading in the South China Sea. The ductile extension and extreme quick and thick deposition in the Baiyun Sag indicate that the lower-crustal flow might have been the mechanism for the anomaly subsidence.

Key words: Baiyun Sag, anomaly post-rift subsidence, backstripping modeling, subsidence analysis, South China Sea

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