Solution of the Gravimetric Inverse Problem Using Multidimensional Grids

摘要

New computer technologies for two- and three-dimensional density modeling are required for solution of detailed density modeling problems, which are applicable for processing numerical datasets of high dimension. Construction of density models based on gravity field anomalies is reduced to solution of the direct and inverse gravimetric problems. High-efficiency algorithms of "fast" solution of the direct gravimetric problems over multidimensional grids are required for successful realization of functional and iteration solution schemes to solve inverse problems.