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Results of geological media exploration using scattered waves extracted from multichannel seismic data are presented. The researches are based on original prestack migration method – Wave CDP method, which possesses possibility to construct two independent time sections: conventional image of reflectors and new image of space distribution of acoustic inhomogeneities - diffractors. The last are join with fracture zones – strong sources of scattered waves. Method was testes in areas with carbonate, volcanic and clay rocks.