地球本征模在地球内部物理结构和动力学机制研究中一直是一个重要的课题，与地球物理学、地震学联系紧密。
The study of the Earth's eigen mode is an important way to study physical properties and dynamics in the Earth's interior, and is closely related with geophysics and seismology closely.
地壳与上地幔各向异性研究在地球动力学领域有广泛的应用和重要的科学意义，其研究有助于许多地质和地球物理基本问题的解释。
Studies of seismic anisotropy in the crust and mantle are of wide application and scientific implication in geodynamics, which could interpret much geological and geophysical problem.
地壳与上地幔各向异性研究在地球动力学领域有广泛的应用和重要的科学意义，其研究有助于许多地质和地球物理基本问题的解释。
Studies of seismic anisotropy in the crust and mantle are of wide application and scientific implication in geodynamics, which could interpret much geological and geophysical problem.
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