Email this article Stable methods of interpretation of gravimetric data
- Authors: Martyshko P.S.1, Ladovskiy I.V.1, Byzov D.D.1
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Affiliations:
- Bulashevich Institute of Geophysics, Ural Branch
- Issue: Vol 471, No 2 (2016)
- Pages: 1319-1322
- Section: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/189238
- DOI: https://doi.org/10.1134/S1028334X16120199
- ID: 189238
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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.
About the authors
P. S. Martyshko
Bulashevich Institute of Geophysics, Ural Branch
Author for correspondence.
Email: pmart3@mail.ru
Russian Federation, Yekaterinburg, 620016
I. V. Ladovskiy
Bulashevich Institute of Geophysics, Ural Branch
Email: pmart3@mail.ru
Russian Federation, Yekaterinburg, 620016
D. D. Byzov
Bulashevich Institute of Geophysics, Ural Branch
Email: pmart3@mail.ru
Russian Federation, Yekaterinburg, 620016
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