Three-Dimensional Assembly Technologies for the Interpretation of Gravimetric Data

摘要

The assembly method of solving a three-dimensional ore-type inverse problem is considered. The method is based on the unity of a grid (finite-element) approximation of a dense medium and a special type of structuring the iteration process of selection which makes it possible to effectively observe all a priori restrictions on the model of field sources. The examples of interpretations of gravity anomalies are presented.