by use of coordinate transformation, the multilayered anisotropic medium is changed into a homogeneous isotropic medium and a theoretical t-d equation of seismic reflection wave is derived.
利用坐标变换方法,将多层的各向异性介质转换成均匀各向同性介质,从而推导出地震反射波理论时-深方程。通过模型的测定,介绍了各向异性系数的求取及地质剖面的构制方法。