TO A QUESTION OF LOCALIZATION OF LARGE HETEROGENEITIES IN GEOLOGICAL STRUCTURES ON LAND AND IN SEA
Technology of geo-acoustic monitoring on surface waves provides data of the local structure of geophysical section by depth using the information of the spectral composition and dynamic properties of natural microseismic noise. Our own long-term field expeditions have confirmed that at transformation of surface waves on deep irregularities attenuation of high frequency components is observed, while the long-wave oscillations reflect the structure of inhomogeneity.