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《Acta Geologica Sinica》 2011-09
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Movement Features of Mantle Fluid Flows based on the S-wave Velocity Structure of Asia

YANG Wencai,YU Changqing National Laboratory on "Tectonics and Dynamics",Institute of Geology,CAGS,Beijing,100037  
Based on analysis and comparison of global manle convection model,this study summarized the research results of S-wave seismic tomography,and investigated the general features of mantle S-wave volicty pattern in Asia and the model of mantle fluid movement.It is generally considered that the S-wave velocity structure features of the Upper Mantle can be explained by the plate tectonics.Heat accumulation may occur in the mantle beneath the central Eurasia superplate.A strong negative velocity disturbance occurs in the mantle below the Hainan Island and South China Sea,reflecting a modern mantle-plume system.Movement of mantle heat-fluid flows shows two different geometrical patterns: upward migration and oblique migration,both of which can happen one after another or alone,and then are of equal importance.
【Fund】: 中国地质调查局资助项目(编号科[2011]02-32-01)资助的成果
【CateGory Index】: P542.5
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