FIELD: seismology. SUBSTANCE: method is based on determining phases of the creep. Moments are measured of activation of acoustic and high-frequency seismic noises and micro-earthquakes in the zone of an active fracture of crust, and the final phase of the creep movement is determined. The acoustic and high-frequency seismic radiation are registered at different depths of the crust. EFFECT: higher accuracy. 2 dwg
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