GEODYNAMICS AND RECONSTRUCTION OF THE EARTH'S INTERIOR STRUCTURE BY THE GEOID DATA IN DIFFERENT REGION OF THE WORLD OCEAN

摘要

Research with the ERS altimetric data stimulated a solving of an important geotectonic problem: reconstruction of the Earth's interior through the geoid characteristics. It is known that elevations and depressions on the ocean surface by altimeter measurements correlate with location of disturbing earth masses. Therefore an inverse problem is an attractive for realization. We propose our approach which we named as a gravimetric tomography method. Owing to this the geoid data provides now not only geodesic and hydrodynamical research but a geological information also.