Abstract
A fundamentally new approach to solving inverse problems in geophysics based on the linear integral representation method and the theories of discrete gravity and the magnetic potential is proposed. This approach makes it possible to reconstruct the continuously distributed masses with a relatively high accuracy from the heterogeneous data at some grid points.
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This work was carried out under a State Assignment of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences.
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Translated by E. Maslennikova
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Stepanova, I.E., Kolotov, I.I. Solution of the Interpretation Tomography Problem in Geophysics under the Linear Integral Representation Method and Theories of Discrete Gravity and the Magnetic Potential. Dokl. Earth Sc. (2024). https://doi.org/10.1134/S1028334X24600907
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DOI: https://doi.org/10.1134/S1028334X24600907