The given paper describes the original algorithm of obtaining the seismic images of geological environment based on the diffraction transformation of wave fields of common offset gather. Also there is adduced the operator of such a transformation in the time domain. The examples of testing the transformation on the synthetic seismograms are shown. And there are demonstrated the results of testing the transforming algorithm on the experimental data. The shown time sections are obtained with help of the new technology represent the new original images of the geological environment. The analysis of these images can be particularly useful for studying the complicated structure of geological environments. The new technology of the diffraction transformation of seismic wave fields gives a whole range of different images of environment, including those on which either mirror or scattering components of the wave fields are emphasized.


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