GEODYNAMICS AND RECONSTRUCTION OF THE EARTH’S INTERIORSTRUCTURE BY THE GEOID DATA IN DIFFERENTREGION OF THE WORLD OCEAN

摘要

Research with the ERS altimetric data stimulated arnsolving of an important geotectonic problem:rnreconstruction of the Earth's interior through the geoidrncharacteristics. It is known that elevations andrndepressions on the ocean surface by altimeterrnmeasurements correlate with location of disturbingrnearth masses. Therefore an inverse problem is anrnattractive for realization. We propose our approachrnwhich we named as a gravimetric tomography method.rnOwing to this the geoid data provides now not onlyrngeodesic and hydrodynamical research but a geologicalrninformation also.