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《Earth Science(Journal of China University of Geosciences)》 2012-04
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Crustal Structure of the Northwest Sub-Basin of the South China Sea and Its Tectonic Implication

AO Wei 1 ,ZHAO Ming-hui 1*,QIU Xue-lin1,RUAN Ai-guo2,LI Jia-biao2 1.KeyL aboratory of Marginal Sea Geology,SouthC hina Sea Institute of Oceanology,ChineseA cademy of Sciences,Guangzhou 510301,China 2.Second Institute of Oceanography,State Oceanic Administration,Hangzhou 310012,China  
Deep crustal structure in the northwest sub-basin contains the key information of the rifting process of the northern continental margin of the South China Sea(SCS).A 386km-long seismic profile(OBS2006-2)with wide-angle reflective and refractive ocean bottom seismometer(OBS)data was acquired across Xisha block and the Northwest sub-basin(NW sub-basin) of the SCS in NEE direction,which is the only profile hitherto parallel to the expanding ridge of the NW sub-basin.The crustal structure along OBS2006-2has been obtained by using ray-tracing simulation method(RAYINVR),which yields information on the velocities,tectonics,and geophysical properties.Our velocity structure indicates that sediment thickness increases from Xisha block(about 1-2km)to NW sub-basin(about 2-3km).Moho interface changes from typical continent margin of South China(~27km)to oceanic crust(~12km).The velocity at the top of upper mantle varies from 7.8to 8.0km/s.No high velocity layer and low velocity layer have been identified.Voluminous magmatism in transition zone between Xisha block and NW sub-basin,is possibly related to the initial extending of the NW sub-basin.The part of model in the domain of 220-370km would be of oceanic crust while the western part in the domain of 0-220km may be of thinned continental crust.Residual magma may exist under the speading ridge of the NW sub-basin deduced by the anomaly of Pn seismic phase.
【Fund】: 国家自然科学基金(Nos.41074066 41076029);; 国家基金重大研究计划(No.91028002)
【CateGory Index】: P736.1
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