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However, the inversion test suggests that in the lower lithosphere, for this class of anisotropy, the 1D profile would well represent the background conductivity, with the most conductive direction not sensed.
The first maintains the background model as the most conductive direction and forms a more resistive model (by a factor of α) for the orthogonal direction (type 1).
On the other hand, there is the possibility that cracks and faults formed at the mid-ocean ridge induce an electrical anisotropy with the most conductive direction parallel to the ridge.
Even if lithospheric anisotropy exists, the most conductive direction in the anisotropic lithospheric structure should be sufficiently conductive (likely < 1000 Ω m) to resolve a difference between it and an isotropic lithosphere using isotropic inversion.
For the anisotropic lithosphere, the red line shows a most conductive direction that is supposed to be parallel to the fossil spreading direction (y-direction), and the black line shows a least conducive direction that is supposed to be perpendicular to a fossil spreading direction (x-direction).
If we switch the most conductive direction and the least conductive direction in the models (i.e., x-direction is the most conductive and y-direction is the least conductive), however, the sense of splitting is switched not only in apparent resistivity but also in phase, as expected.
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