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Volume 20 Issue 1
Feb 2009
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Article Contents
Di Zhou, Zhen Sun, Jie Liao, Zhongxian Zhao, Min He, Xiangjie Wu, Xiong Pang. Filling History and Post-Breakup Acceleration of Sedimentation in Baiyun Sag, Deepwater Northern South China Sea. Journal of Earth Science, 2009, 20(1): 160-171. doi: 10.1007/s12583-009-0015-2
Citation: Di Zhou, Zhen Sun, Jie Liao, Zhongxian Zhao, Min He, Xiangjie Wu, Xiong Pang. Filling History and Post-Breakup Acceleration of Sedimentation in Baiyun Sag, Deepwater Northern South China Sea. Journal of Earth Science, 2009, 20(1): 160-171. doi: 10.1007/s12583-009-0015-2

Filling History and Post-Breakup Acceleration of Sedimentation in Baiyun Sag, Deepwater Northern South China Sea

doi: 10.1007/s12583-009-0015-2
Funds:

the National Natural Science Foundation of China 40576027

the National Natural Science Foundation of China 40238060

the High-Tech R&D Program of China 2008AA09Z306

More Information
  • Corresponding author: Zhou Di, zhoudiscs@scsio.ac.cn
  • Received Date: 28 Oct 2008
  • Accepted Date: 01 Dec 2008
  • The Baiyun (白云) sag in the southern Pearl River Mouth basin is the largest and deepest sag in deepwater northern South China Sea. Researches and exploration in this sag have revealed many distinct features of the sag. This article reports its filling history through backstripping of depth data of interpreted sequence boundaries. Maps of sediment rates of 10 sequences from 49 Ma to the present were constructed, showing the spatio-temporal variation of the sediment rate. Three stages of sediment infilling, 49–17.5 Ma, 17.5–10.5 Ma, and 10.5–0 Ma, were divided by abrupt changes of sedimentary patterns. If the breakup of the South China Sea took place at ~30 Ma, significant post-breakup acceleration of sedimentation was observed at 17.5–15.5 Ma and 13.8–12.5 Ma, indicating acceleration of subsidence at these times. We propose that the onset of strong post-breakup subsidence at ~17.5 Ma was an important tectonic event that changed the pattern of sedimentation from discrete and medium-rate deposition centers in both main and south subsags to restricted but high-rate deposition in the main subsag. The cause and implications of this newly recognized event need to be investigated.

     

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