Abstract
Robust noise technology for analysis of seismic acoustic signal is offered, which allows using the noise in the signal as a carrier of information in the beginning of anomalous seismic processes preceding earthquakes. A station has been built based on this technology, which receives seismic acoustic noises from the deep strata of the earth by means of steel bores of 3-6 kilometers deep suspended oil wells, performing monitoring of the beginning of the latent period of earthquake formation. Experiments, which have been carried out on such stations at Qum Island in the Caspian Sea since 01.05.2010 and in the town of Shirvan in the south of Azerbaijan since 20.11.2011, proved the reliability and adequacy of results of monitoring and identification of earthquakes within a radius of 300-500 kilometers 10-15 hours before earthquakes are detected by standard seismic stations.
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