The relation between seismic anisotropy in crust and in upper mantle can show the geodynamic specialties of shallow and deep structure, and can hint information about geodynamic mechanism;
上地幔介质各向异性与地壳介质各向异性的关系能够反应区域浅部与深部介质动力学特征，并暗含区域动力机制信息；
The relation between seismic anisotropy in crust and in upper mantle can show the geodynamic specialties of shallow and deep structure, and can hint information about geodynamic mechanism;
上地幔介质各向异性与地壳介质各向异性的关系能够反应区域浅部与深部介质动力学特征，并暗含区域动力机制信息；
应用推荐