Abstract
The experimental MT data and theoretical data calculated by the thin sheet technique for a low-frequency telluric field are analysed and compared for the Kamchatka Peninsula. The comparison shows a good agreement between the experimental and theoretical data and results in a conclusion that the DC-type distortions of the telluric field play the most important role in the structure of the MT field. The component of the telluric field which is parallel to the general direction of the Kamchatka Peninsula is less distorted and should be used for the estimation of deep geoelectric structures.
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