Stable methods of interpretation of gravimetric data
- Авторы: Martyshko P.S.1, Ladovskiy I.V.1, Byzov D.D.1
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Учреждения:
- Bulashevich Institute of Geophysics, Ural Branch
- Выпуск: Том 471, № 2 (2016)
- Страницы: 1319-1322
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/189238
- DOI: https://doi.org/10.1134/S1028334X16120199
- ID: 189238
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Аннотация
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.
Об авторах
P. Martyshko
Bulashevich Institute of Geophysics, Ural Branch
Автор, ответственный за переписку.
Email: pmart3@mail.ru
Россия, Yekaterinburg, 620016
I. Ladovskiy
Bulashevich Institute of Geophysics, Ural Branch
Email: pmart3@mail.ru
Россия, Yekaterinburg, 620016
D. Byzov
Bulashevich Institute of Geophysics, Ural Branch
Email: pmart3@mail.ru
Россия, Yekaterinburg, 620016
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