A method of geophysical surveying polymictic ore bodies provides for excitation in the rock massiv to be explored elastic waves leading to electrostatic polarization in the ore bodies after which, within the time period of existence of the electrostatic polarization charge, elastic waves are subsequently excited and a pulse electromagnetic radiation generated by the ore bodies under the influence of those elastic waves is registered depending on the number of pulse bursts of which the number of the ore bodies is determined.
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