Skip to main content
Log in

The Causes of Tectonic and Seismic Activity of the Liskin Fault Zone (the Southeastern Voronezh Uplift, the East European Platform)

  • Published:
Moscow University Geology Bulletin Aims and scope Submit manuscript

Abstract

The Liskin fault zone located in the southeastern part of the East European Platform at the boundary between two large neotectonic structures, that is, the Voronezh Uplift and the Oka–Don basin, is considered. Earthquake epicenters are concentrated in the fault zone and the adjacent territory. The neotectonic structures of the territory, topography, structure of the multi-depth and age horizons of the sedimentary cover, basement, crust, Moho surface are investigated, and the causes of neotectonic and seismic activity of the zone are determined. At present, the Liskin fault develops as a thrust fault with a dextral strike-slip component under the conditions of submeridional compression and the adjacent territory is under the influence of multidirectional tectonic compression stresses: from the north, from the Oka–Don basin and from the south, from the Caucasian segment of the Alpine collision belt. This is reflected in the morphology and structure of the neotectonic structures. The deformation of multi-depth horizons as well as the Earth’s surface and the activation of seismicity are associated with the submeridional compression. The deep material and structural inhomogeneities of the Earth’s crust are of great importance. The collision zone between two oncoming submeridional stresses that led to active seismicity has been identified in the neotectonic structure of the south-eastern part of the East European Platform for the first time.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1.
Fig. 2.
Fig. 3.
Fig. 4.
Fig. 5.
Fig. 6.

REFERENCES

  1. Bachmanov, D.M., Kozhurin, A.I., and Trifonov, V.G., The active faults of Eurasia database, Geodynam. Tectonophys., 2017, vol. 8, no. 4, pp. 711–736.

    Article  Google Scholar 

  2. Efremenko, M.A. and Rogozhin, E.A., Geophysical fields and earthquakes in the territory of the Voronezh crystalline massif, Geofiz. Issled., 2010, vol. 11, no. 3, pp. 57–72.

    Google Scholar 

  3. Ezhova, I.T., Efremenko, M.A., and Tregub, A.I., Seismic activity and neotectonics of the Voronezh Crystalline Massif, Vestn. Voronezh. Gos. Univ. Ser. Geol., 2010, vol. 1, pp. 229–232.

    Google Scholar 

  4. Geologicheskaya karta SSSR masshtaba 1 : 200 000. Seriya Bryansko-Voronezhskaya. List M-37-X. Ob’’yasnit. Zap. (The 1 : 200 000 Geological Map of the USSR. Ser. Bryansk–Voronezh. Sheet M-37-X. Explanatory Note), Moscow: Nedra, 196.

  5. Kopp, M.L., Mobilistic neotectonics of patforms in the southeastern Europe, in Tr. GIN RAS, Vyp. 552 (Trans. Geol. Inst. Russ. Acad. Sci. Vol. 552), Leonov, Yu. G., Ed., Moscow: Nauka, 2004.

  6. Kosmotektonicheskaya karta Vostochno-Evropeiskoi platformy i ee obramleniya (Cosmotectonic Map of the East European Platform and Its Frame), Khain, V.E. and Trofimov, D.M., Eds., Moscow: Vseross. Nauchno-Issled. Geol. Inst., 1989.

    Google Scholar 

  7. Lavrushin, Yu.A., Chistyakova, I.A., Kuralenko, N.P., et al., The Divnogorsk glaciotectonics structure: Its composition, deformations of the glacial sheet bed and prerequisites for further geomorphic development, Byull. Kom. po Izucheniyu Chetvertich. Perioda, 2012, no. 72, pp. 5–27.

  8. Litosfera Voronezhskogo kristallicheskogo massiva po petrofizicheskim i geofizicheskim dannym (The Lithosphere of the Voronezh Crystalline Massif Based on Petrophysical and Geophysical Data), Chernyshov, N. M, Ed., Voronezh: Nauchn. Kniga, 2012.

  9. Makarov, V.I., The geodynamic formation conditions of the Oka–Don trough and Oka–Tsna swell (Russian Plate), Izv. Vyssh. Uchebn. Zaved., Geol. Razved., 2001, no. 1, pp. 43–53.

  10. Makarova, N.V., Makarov, V.I., Korchuganova, N.I., et al., The Oka–Don basin is a neotectonic active zone of the East European Platform, Izv. Vyssh. Uchebn. Zaved., Geol. Razved., 2002, no. 2, pp. 3–13.

  11. Nadezhka, L.I., Pivovarov, S.P., Efremenko, M.A., and Semenov, A.E., About earthquakes in the Voronezh Crystalline Massif, Vestn. Voronezh. Gos. Univ. Ser. Geol., 2010, vol. 1, pp. 233–242.

    Google Scholar 

  12. Nadezhka, L.I., Efremenko, M.A., Rogozhin, E.A., and Semenov, A.E., The possible causes of local earthquakes in the territory of the Voronezh crystalline massif, in Struktura, svoistva, dinamika, i minerageniya litosfery Vostochno-Evropeiskoi platformy, Mater. XIV Vseros. Soveshch. (Proc. XIV All-Russ. Conf. “Structure, Properties, Dynamics and Minerageny of the Lithosphere in the East European Platform”), Voronezh: Nauchn. Kniga, 2010.

  13. Raskatov, G.I., Luk’yanov, V.F., Starukhin, A.A., et al., Tektonika vostochnoi chasti Voronezhskogo kristallicheskogo massiva i ego osadochnogo chekhla (Tectonics of the Eastern Part of the Voronezh Crystalline Massif and Its Sedimentary Cover), Voronezh, 1976.

  14. Semenov, A.E., Zolototrubova, E.I., Nadezhka, L.I., and Efremenko, M.A., Geological-geophysical characteristics of the Liski seismoactive zone, in Mater. XX Vseross. konf. “Glubinnoe stroenie, minerageniya, sovremennaya geodinamika i seismichnost’ Vostochno-Evropeiskoi platformy i sopredel’nykh regionov” (Proc. XX All-Russ. Conf. “Deep Structure, Minerageny, Modern Geodynamics and Seismicity of the East European Platform and Adjacent Regions”), Voronezh, 2016, pp. 349–353.

  15. Starukhin, A.A., Neotectonics of the eastern limb of the Middle Russian Anteclise and the adjacent part of the Oka–Don depression, Cand. (Geol.–Mineral.) Dissertation, Voronezh, 1973.

  16. Tregub, A.I., Neotektonika territorii Voronezhskogo kristallicheskogo massiva (Neotectonics of the Territory of the Voronezh Crystalline Massif), Voronezh: Voronezh. Gos. Univ., 2002.

Download references

Author information

Authors and Affiliations

Authors

Corresponding authors

Correspondence to T. V. Sukhanova, N. V. Makarova, A. N. Stafeev, L. I. Nadezhka, A. I. Tregub, I. T. Ezhova or A. E. Semenov.

Ethics declarations

The authors declare that they have no conflicts of interest.

Additional information

Translated by D. Voroschuk

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Sukhanova, T.V., Makarova, N.V., Stafeev, A.N. et al. The Causes of Tectonic and Seismic Activity of the Liskin Fault Zone (the Southeastern Voronezh Uplift, the East European Platform). Moscow Univ. Geol. Bull. 78, 451–461 (2023). https://doi.org/10.3103/S0145875223040129

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.3103/S0145875223040129

Keywords:

Navigation