Electrical anisotropy, manifested as varying resistivities of a medium with the direction of current flow, exists widely in nature. The electrical anisotropy can be divided into microanisotropy and macroanisotropy. The microanisotropy belongs to the attribute characteristics of media that shows anisotropic characteristics in very small scale. The anisotropy studied in geophysics is generally macroanisotropy, which is caused by the tiny isotropic structures that have same orientations, such as layering. Due to the limited resolution of electromagnetic (EM) methods, these tiny structures are generally treated as a whole and replaced by the parameter of anisotropy. These are typical macroanisotropy in EM geophysics. In the past decades, more and more long-period magnetotelluric (MT) signal shows that the electrical anisotropy exists widely in the deep crust and mantle (