FIELD: geophysics.
SUBSTANCE: method comprises selecting the seismic-generating lineaments, observing forerunners of earthquakes in this region, finding the step-like anomalies of shear deformations, mapping the lines of constant amplitudes of the deformations, extracting statistically valuable components in the lines, determining the epicenter of the expected earthquake, and determining the depth of the source zone from the amplitudes of the anomalies at the epicenter.
EFFECT: enhanced reliability.
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