RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 21, ES3002, doi:10.2205/2021ES000766, 2021


Figure 3. Magnetic anomalies of the Western Ural region (a) and separated magnetic anomalies from upper layer of the Earth's crust 0–5 km (b), granite layer 5–20 km (c) and basalt layer (d). The designations are shown in Figure 1.


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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.


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