Abstract
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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Original Russian Text © P.S. Martyshko, I.V. Ladovskiy, D.D. Byzov, 2016, published in Doklady Akademii Nauk, 2016, Vol. 471, No. 6, pp. 725–728.
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Martyshko, P.S., Ladovskiy, I.V. & Byzov, D.D. Stable methods of interpretation of gravimetric data. Dokl. Earth Sc. 471, 1319–1322 (2016). https://doi.org/10.1134/S1028334X16120199
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DOI: https://doi.org/10.1134/S1028334X16120199