Abstract:
The inverse gravity and magnetic problems on reconstruction of interface surfaces are solved for threelayers model of medium using real gravitational and magnetic data derived for an region of Middle Ural. First, on the base of a specific technique the anomalous effect for every boundary is extracted and the nonlinear gravity problem is solved by regular iterative methods. Then using obtained solution an averaged value of the vertical component of the magnetization vector is determined and the nonlinear magnetometry problem is solved. Comparative analyses of obtained results are given.