Localization of Geological Inhomogeneities on the Arctic Shelf by Analysis of the Seismoacoustic Wave Field Mode Structure

The results of analysis of wave modes in the ambient noise induced in the layered structure “lithosphere–hydrosphere–ice sheet” are presented. It is shown that instrumental monitoring over background noises in an ice-covered shallow sea allows us to apply methods of seismic tomography in order to determine the structural parameters of a layered geophysical media.