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岩石圈板块或壳层理论用来解释与板块边界有关的构造现象是成功的。但是,某些地震活动和地壳变形发生在板块内部,与板块边界上发生的这些活动没有明显的关系。根据地球重力位的调和函数,能够很近似地算出地幔对
The lithospheric plate or shell theory used to explain the tectonic phenomena associated with plate boundaries is a success. However, some seismic activity and crustal deformation occur inside the plate and have no obvious relationship with these activities occurring on the plate boundary. Based on the harmonic function of the Earth’s gravitation, the mantle pair can be calculated very closely