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《Chinese Journal of Geophysics》 2011-12
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Numerical simulation of Eastern South China Sea basin expansion

XU He-Hua~1,MA Hui~1,SONG Hai-Bin~2,CHEN Ai-Hua~1 1 Key Laboratory of Marginal Sea Geology,South China Sea Institute of Oceanology.Chinese Academy of Sciences, Guangzhou 510301,China 2 Key Laboratory of Petroleum Geophysics,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China  
The formation and evolution of South China Sea has been one of the hot spot of attention at home and abroad.The expansion of the South China Sea happened in early Oligocene-early Miocene,and the expansion of South China Sea includes ridge transition once at least.This paper uses a model of rising divergent mantle flow and convection coupling to simulate the expansion of eastern sea basin of the South China Sea,the ridge jump,and the process of lithosphere hot structure evolution and melting of magma after expansion.Numerical simulation results indicate that the ridge jump is an important process of the South China Sea expansion. Ridge jump forms a magma chamber between the two ridges,and the existence of the magma chamber makes the submarine volcanoes relatively more and also the terrain relatively high between the ridges.At the same time,it also leads to the terrain of both sides of south side ridge and the distribution of submarine volcano asymmetric,which in turn can also demonstrate the reasonability of the ridge jump model.
【Fund】: 国家重点基础研究发展计划(2007CB411704);; 中国科学院知识创新工程重要方向项目群项目(KZCX2-YW-Q05-04);; 国家高技术研究发展计划“863”课题(2008AA09Z306)资助
【CateGory Index】: P736.1
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