Экстремальные итерационные методы решения обратной задачи магнитометрии при исследованиях на кристаллическом фундаменте

Abstract

Iterative methods of the solution of the inverse linear and nonlinear problems of magnetometry are developed. Extreme algorithms of the calculation of depths down to the horizontal division borders of blocks with the maximal difference of magnetic properties are used. By practical examples, the opportunities to determine the intensity of the magnetization of rocks are shown. The depths down to the top sides of approximating parallelepipeds of the physical model of a geological environment are calculated.