【摘要】 地震各向异性是地球内部介质的一种重要属性 .地震各向异性研究不仅有助于准确认识地球内部精细结构 ,还有助于研究地球内部活动过程 .本文从海洋岩石圈与大陆岩石圈各向异性结构两个方面较详细地论述了地震各向异性与地球深层动力过程的相互关系 ,论证了地震各向异性是指示地球深层动力过程的地球物理“化石”更多还原

【Abstract】 Seismic anisotropy is an important character of the interior medium of the earth. It is helpful to understand precisely the fine structure and the inner dynamic process of the globe to research it. Basing on the anisotropic structure of the rock lithosphere of the ocean and the continent, this article discussed the relation between the seismic anisotropy and the deep dynamical process of the earth in greater detail, and proved that seismic anisotropy is the geophysical "fossil", which can indicate the deep dynamical course of the earth.更多还原