ZHAO Huan-ting, WANG Li-rong, YUAN Jia-yi. ORIGIN AND TIME OF QIONGZHOU STRAIT[J]. Marine Geology & Quaternary Geology, 2007, 27(2): 33-40.
Citation: ZHAO Huan-ting, WANG Li-rong, YUAN Jia-yi. ORIGIN AND TIME OF QIONGZHOU STRAIT[J]. Marine Geology & Quaternary Geology, 2007, 27(2): 33-40.
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ORIGIN AND TIME OF QIONGZHOU STRAIT

  • 1 CAS Key Laboratory of Marginal Sea Geology, Guangzhou 510301, China;

  • 2 South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;

  • 3 Department of Geosciences, Zhongshan University, Guangzhou 510275, China

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  • Received Date: November 09, 2006
  • Revised Date: January 07, 2007
    Graphical Abstract
    • Abstract
  • The origin of Qiongzhou Strait has 3 causes:coast erosion, tectonic rifing and marine transgression. And the time for Hainan Island and Leizhou Peninsula to separate from each other also has some explanations:Pliocene, the beginning of Quaternary, before middle Pleistocene, after middle Pleistocene and Holocene. The latest data about the geology, oceanography and regional palaeo-biogeography of Qiongzhou Strait are analyzed in the paper, and it is thought that Qiongzhou Strait is not a rift. It grew out of a normal low land, and was formed in the middle Holocene, about (10 570±560)~(7 125±96) aBP, when marine transgressed the original normal low land. It is inferred that the average speed of central trough valley undercutting is 0.7 cm·a-1, and the average speed of tidal current delta accumulation outside the west mouth is 0.17~0.31 cm·a-1 after the Qiongzhou Strait formed.
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    • References (39)
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