Solution of the Interpretation Tomography Problem in Geophysics under the Linear Integral Representation Method and Theories of Discrete Gravity and the Magnetic Potential

被引：4

作者：

Stepanova, I. E. ^{[1
]}

Kolotov, I. I. ^{[2
]}

机构：

[1] Russian Acad Sci, Schmidt Inst Phys Earth, Moscow 123995, Russia

[2] Moscow MV Lomonosov State Univ, Moscow 119991, Russia

来源：

DOKLADY EARTH SCIENCES | 2024年 / 516卷 / 01期

关键词：

inverse problems in geophysics; theories of discrete gravity and the magnetic potential; S-APPROXIMATION METHOD; ALGEBRAIC EQUATIONS; INVERSE PROBLEMS; GRAVIMETRY; MAGNETOMETRY; UNIQUENESS; SYSTEMS;

D O I：

10.1134/S1028334X24600907

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

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.

引用

页码：835 / 843

页数：9

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