RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 21, ES3002, doi:10.2205/2021ES000766, 2021
Figure 5. The results of modeling sources in upper 0–5 km layer of the Earth's crust (a), the granite layer (d) and the surface of the basalt layer (c). The designations are shown in Figure 1.
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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