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Volume 39 Issue 1
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Article Navigation >  Haiyang Xuebao  > 2017  >  39(1): 52-63
Bi Dongjie, Zhang Daojun, Zhai Shikui, Liu Xinyu, Xiu Chun, Zhang Aibin, Cao Jiaqi. The coupling relationships among the Qinghai-Tibet Plateau uplifting, the Qiongdongnan Basin subsiding and the Xisha Islands' Reefs developing[J]. Haiyang Xuebao, 2017, 39(1): 52-63. doi: 10.3969/j.issn.0253-4193.2017.01.006
Citation: Bi Dongjie, Zhang Daojun, Zhai Shikui, Liu Xinyu, Xiu Chun, Zhang Aibin, Cao Jiaqi. The coupling relationships among the Qinghai-Tibet Plateau uplifting, the Qiongdongnan Basin subsiding and the Xisha Islands' Reefs developing[J]. Haiyang Xuebao, 2017, 39(1): 52-63. doi: 10.3969/j.issn.0253-4193.2017.01.006
shu

The coupling relationships among the Qinghai-Tibet Plateau uplifting, the Qiongdongnan Basin subsiding and the Xisha Islands' Reefs developing

doi: 10.3969/j.issn.0253-4193.2017.01.006
  • 1.

    The Key Lab of Sub Marine Geosciences and Prospecting Techniques, Ministry of Education, Ocean University of China, Qingdao 266100, China;School of Marine Geosciences, Ocean University of China, Qingdao 266100, China

  • 2.

    Zhanjiang Branch Institute of China National Offshore Oil Corporation(CNOOC) Limited, Zhanjiang 524057, China

  • Received Date: 2016-03-02
  • Rev Recd Date: 2016-05-17
    Abstract
  • Based on the drilling data of the 15 wells in the Qiongdongnan Basin and "Xike-1" well in the Shi Island of Xisha Islands, combining with the seismic section through those wells, this passage systematically analyzed the subsiding (sediments filling) rates of Qiongdongnan Basin, the developing rates of the Xisha Islands' reefs and their variation features. Additionally, the coupling relationships among the Qinghai-Tibet Plateau uplifting, the Qiongdongnan Basin subsiding and the Xisha Islands' reefs developing were also discussed. The former three exhibit a high degree of consistency in development time and process. The ancient seawater Sr isotopic composition of the South China Sea composition provides an important evidence for this consistency. The changes of the sediment accumulation rates in the shallow water can better reflect the changes of the basin subsiding rates in comparison to the deep water. The processes of Qiongdongnan Basin subsiding (sediments accumulation) and Xisha Islands' reefs developing can both be divided into three stages, corresponding to the three phases of the Qinghai-Tibet Plateau uplifting, they are:23-16 Ma BP, 16-5.5 Ma BP, 5.5 Ma BP-today respectively in chronological order. In comparison, the coupling relationship between the reefs developing process and Qinghai-Tibet Plateau uplifting is more closely. In the rapid uplifting stage of the Qinghai-Tibet Plateau, the basin sedimentary filling (sediments accumulation) rates and the reefs growth rates accelerated correspondingly, and 87Sr/86Sr ratios of the South China Sea increased. It indicates that the Qinghai-Tibet Plateau uplifting is the main factor that impacted the basin subsidence (sedimentary fill), reefs development and ancient seawater Sr isotopic composition in the Qiongdongnan Basin even the entire South China Sea.
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