Monitoring of tectonomagnetic observations was carried out at the Antarctic polygon in the area of the Akademik Vernadsky station for the period from 1998 to 2020. Time series of changes in the local magnetic field were constructed for each observation point of the network and maps of tectonomagnetic anomalies were constructed for different periods of research. It has been established that three anomalous zones are observed in the spatial structure of the tectonomagnetic field of the Wilhelm archipelago, which are confined to the geological inhomogeneities of the earth's crust. The spatio-temporal relationship of tectonomagnetic anomalies with the seismic activity of the region was studied.
Yu. Maksymchuk, I. O.Chobotok, T. A.Klymkovych, R. S. Kuderavets, E. F. Nakalov, Y. S.Otruba [2018]. Complex magnetovariational and tectonomagnetic monitoring of recent geodynamics in the western slope of the Antarctic peninsula // Ukrainian Antarctic Journal, 17, 3-19 https://doi.org/10.33275/1727-7485.1(17).2018.27 (in Ukrainian).
Murovskaya, A. V., Bakhmutov, V. G. [2015]. Preliminary results of field tectonophysical study in the West Coast of the Antarctic Peninsula. Ukrainian Antarctic Journal, 14, 66–73. https://doi.org/10.33275/1727-7485.14.2015.173
Mytrokhyn, O., Bakhmutov, V. [2021]. Geological mapping of the Ukrainian Antarctic Station area (Wilhelm Archipelago and Kyiv Peninsula, Graham Coast). In European Association of Geoscientists & Engineers Source: Conference Proceedings, XIV International Scientific Conference “Monitoring of Geological Processes and Ecological Condition of the Environment”, Vol. 2021. (pp. 1–5). https://doi.org/10.3997/2214-4609.20215K2082
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