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Mantle flow beneath the Asian continent and its force to the crust 被引量:3

Mantle flow beneath the Asian continent and its force to the crust
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摘要 The mantle unsteady flows, which are in an incompressible and isoviscous spherical shell, are investigated by using algorithms of the parallel Lagrange multiplier dissonant decomposition method (LMDDM) and the parallel Lagrange multiplier discontinuous deformation analyses (LMDDA) in this paper. Some physical fields about mantle flows such as velocity, pressure, temperature, stress and the force to the crust of the Asian continent are calculated on a parallel computer. The mantle unsteady flows, which are in an incompressible and isoviscous spherical shell, are investigated by using algorithms of the parallel Lagrange multiplier dissonant decomposition method (LMDDM) and the parallel Lagrange multiplier discontinuous deformation analyses (LMDDA) in this paper. Some physical fields about mantle flows such as velocity, pressure, temperature, stress and the force to the crust of the Asian continent are calculated on a parallel computer.
出处 《Acta Seismologica Sinica(English Edition)》 CSCD 2002年第3期241-246,共6页
基金 State Climbing Project (95-S-05-02) and State Natural Science Foundation of China (49724232).
关键词 parallel Lagrange multiplier dissonant decomposition method parallel Lagrange multiplier discontinuous deformation analyses Asian continent mantle unsteady flow coupling finite element method parallel Lagrange multiplier dissonant decomposition method parallel Lagrange multiplier discontinuous deformation analyses Asian continent mantle unsteady flow coupling finite element method
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