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《Crustal Deformation and Earthquake》 1988-01
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STRESS STATE RESULTED FROM MANTLE CONVECTION IN THE LAYERED LITHOSPHERE

Wang Shiren (Institute of Seismology, State Seismological Bureau)  
In order to investigate the effect of mantle convection under Lithosphere on the crust teetonic movement, a layered lithosphere model is established and the mantle convective stresses under Lithosphere, which can be obtained from Runcorn's model, are considered as the bottom boundary force exerting on the lithosphere. From this model, the equations to compute the stress state within the lithosphere, using gravity disturbance potential coefficients, which is resulted from mantle convection are derived. Using these equations and GEmlOB gravity potential coefficients, the crust stress field caused by mantle convection in China and environs is computed. After comparing the results with the characteristics of tectonic movement in the crust, it is found that the mantle convection under lithosphere is the main factor responsible for the crust tectonic motion for most regions, but other interpretations are need for Taiwan area and the south part of NS seismic belt in China.
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【Co-citations】
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【Co-references】
Chinese Journal Full-text Database 5 Hits
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【Secondary References】
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