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A method for interpretation of potential geophysical fields, based on a stable inversion algorithm, is proposed. The stability of the algorithm is provided by an original choice of the zero approximation model and stepwise solution of the inverse problem by a correctness set. The three-dimensional density distribution of local structures as grid functions is reconstructed by layer-wise anomalies of a spilt field. Examples of interpretation of the practical gravimetric data illustrating the efficiency of the method are given.
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Ladovskiy I. V. Martyshko P. S. Byzov D. D. Tsidaev A. G. 《Doklady Earth Sciences》2019,488(1):1072-1075
Doklady Earth Sciences - An analytical solution for the stationary problem of thermal conjugation is obtained for the model of inhomogeneous layered media. The heat flux components for the crust... 相似文献
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