RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 21, ES3002, doi:10.2205/2021ES000766, 2021
Figure 4. The results of approximation of $\Delta T$ anomalies (sources – rods and the depth of their edges are shown) (a) and reduction to the magnetic pole (b). $Z$ map is colored, and $\Delta T$ contours are shown with dashed lines.
Citation: Martyshko P. S., N. V. Fedorova, A. L. Rublev (2021), Numerical algorithms for structural magnetometry inverse problem solving, Russ. J. Earth Sci., 21, ES3002, doi:10.2205/2021ES000766.
Copyright 2021 by the Geophysical Center RAS.
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