Abstract
With the continuing growth in influence of near surface geophysics, the research of the surface geophysics is of great significance. Researchers want to understand the complex subsurface with gravity and magnetic data and inversion is a powerful tool. In this paper, researchers introduced how to formulate the 3D inversion of potential field data. Meanwhile, some other constrains such as depth-weighting are also employed to get more enhanced results. The method is applied to synthetic data for typical models of gravity anomalies.
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