Abstract
The paper describes application of an approach according to which the endogenous-nature electromagnetic field (EM) is included in the impedance relationships in an additive way, which allows distinguishing the EM field recoded on ground surface by the positions of sources. The case-studies of the endogenous EM field identification in the magnetotelluric sounding records obtained in the Tien Shan region are presented. The characteristics of the identified endogenous EM field are compared with the lunar-solar tides parameters and anisotropic properties of electrical resistivity. The found interconnections point at new options to study irreversible lithospheric deformations in the Tien Shan using magnetotelluric sounding data.
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