Answers are grounded in this paper and cite their sources.
The pole-pole 3-D DC-resistivity inverse problem is solved by converting the inverse problem into an objective-function optimization problem, using the adjoint equation to compute the gradient of the objective function, and using a conjugate-graient minimization. Two examples of the application of the resulting inversion algorithm are given. First, a large synthetic data set is inverted, and second, the inversion algorithm is used to invert E-SCAN field data of relevance to mineral exploration.
No takes yet. Share an insight, caveat, or question.
Еllis et al. (1994) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: