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.

中文翻译：

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线性积分表示法和离散重力和磁势理论解决地球物理解释层析成像问题

摘要

提出了一种基于线性积分表示法和离散重力和磁势理论解决地球物理反问题的全新方法。这种方法使得可以从某些网格点的异构数据以相对较高的精度重建连续分布的质量。