内地壳和上地幔S波速度结构与强震的关系和强震活动的深部背景进行了探讨。
Study to the relation between strong earthquakes and S-wave velocity structures in the crust and upper mantle in the studied area.
结果表明两大构造单元基底的岩石波速差异较大,从而认为两者物质组成迥异,地壳结构完全不同。
As a result, the wave velocity of the two structural units are different obviously, so we think there is great difference in the constituted materials, and the crust structures are entirely different.
理论数值实验显示:在反演地壳S波速度结构时,SV分量接收函数比径向接收函数具有更好的收敛性。
The synthetic tests show that the convergence of SV-component receiver function inversion is faster than that of the radial receiver function inversion.
应用推荐