Anisotropy magnetic and density tomography subsoil and Earth crust

Considered: invention anisotropic magnetic - density geotomography of subsoil and earth crust (AMDGS) and the possibility of new computer technology that allows reliable, objective and cost-effectively images geological structures of the ore fields and units for the purpose of reproduction of reserves at already developed areas and deep geological investigation on the regional traverse. The advanced technology and the anisotropic magnetic- density geotomography subsoil created by improving the early and modern algorithms and programs of statistical-spectral correlation analysis of data in information media "COSKAD 3D». At the heart of AMDGS established an author of the anisotropic magnetic characteristics of the Archean and Paleoproterozoic rocks - magnetic susceptibility and density, which released, on the data modern magnetic and gravity survey. Anisotropic magnetic and density markers position, in the form of diverse tomographic images, unambiguous and reproducible manner reflects deep geological structure of the earth crust and their upper parts. AMDGS helpful for formalized geological mapping at all stages of the exploration process and dealing with different applications.