Using the joint time-frequency (TF) analysis method, we interpret transient electromagnetic (TEM) data so as to fully employ information contained in TEM signals. We choose joint TF distribution (or representation) of Wigner-Will distribution and Gabor expansion to transform the one-dimensional time-domain signal to the two-dimensional TF plane, which not only distinguishes responses of different geo-electric sections from each other successfully, but also provides clear physical meaning between exhibited signal feature and electrical structure of the stratum. This describes the transient eddy field excitation and underground attenuation process in time and frequency respects. The fitting difference is reduced and the precision of quantitative interpretation is improved by means of joint TF inversion with time and frequency window data.
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