Geodynamical interpretation of the geological and geophysical heterogeneity of the Dniepr-Donets basin lithosphere

Authors

  • V.I. Starostenko S.I. Subbotin Institute of Geophysics of the NAS of Ukraine, Kiev
  • I.K. Pashkevich S.I. Subbotin Institute of Geophysics of the NAS of Ukraine, Kiev
  • I.B. Makarenko S.I. Subbotin Institute of Geophysics of the NAS of Ukraine, Kiev
  • P.Ya. Kuprienko S.I. Subbotin Institute of Geophysics of the NAS of Ukraine, Kiev
  • O.S. Savchenko S.I. Subbotin Institute of Geophysics of the NAS of Ukraine, Kiev

DOI:

https://doi.org/10.15407/dopovidi2017.09.084

Keywords:

deep structure, Dnieper-Donets basin, geodynamics, heterogeneity of the lithosphere

Abstract

For the first time on the base of 3D gravity and magnetic modeling results with the use of the data of DSS, seis mic tomography, geological structure of the Precambrian basement, and sedimentary cover, the geologo-geophysical heterogeneities of the lithosphere are considered as indicators of different stages of the rift formation — the initial passive and subsequent active ones. The roles of shear deformations and rotational movements in the formation and development of the rift are shown.

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References

Stovba, C. N. (2008) Geodynamic evolution of the Dnieper-Donets Basin and Donbas (Unpublished Doctoral thesis). Research Institute of Oil and Gas Industry (SA Naukanaftogaz), NAK Naftogaz Ukraine, Kyiv, Ukraine (in Russian).

Stephenson, R. & Stovba, S. (2012). The Dniepr-Donets Basin. In Roberts D.G., Bally A.W. (Eds.). Regional Geology and Tectonics: Phanerozoic Rift System and Sedimentary Basins (pp. 420-441.), Amsterdam: Elsevier. https://doi.org/10.1016/B978-0-444-56356-9.00015-8

Map of Precambrian structural zoning of south-western part of the East European platform. Scale 1:1 000 000 (1992). Galeckij, L.S. (Ed.). In Complete set of the maps Geology and Metallogeny of the south-western part of the East European Platform. Scale 1:1 000 000. Zarickij, A.I. (Ed.). (6 sheets), Kiev: Goskomgeologia, Geoprognoz,Centergeology, PA “Belarus”, All-Russian Geological Institute, Voroneg State University (in Russian).

Starostenko, V. I., Rusakov, O. M., Pashkevich, I. K., Kutas, R. I., Gladun, V. V., Orlyuk, M. I., Kuprienko, P. Ya., Makarenko, I. B., Maksimchuk, P. J., Kozlenko, Yu. V., Kozlenko, M. V., Legostaeva, O. V., Lebed', T. V. & Savchenko, A. S. (2015). Tectonics and hydrocarbon potential of the crystalline basement of the Dnieper-Donets Basin. Kiev: Galaktika (in Russian).

Kuprienko, P. Ya., Makarenko, I. B., Starostenko, V. I., Legostaeva, O. V. & Savchenko, A. S. (2010). Threedimensional density model of the crust and upper mantle of the Dnieper-Donets Basin and Donbas. Geofiz. zhurn., 32, No. 6, pp.175-214 (in Russian).

Pashkevich, I. K., Orljuk, M. I. & Lebed', T. V. (2014). Magnetic heterogeneity, fault tectonics of the crys talline crust and petroleum potential of the Dnieper-Donets aulacogene. Geofiz. zhurn., 36, No. 1, pp. 64-80 (in Russian).

Stovba, S. N., Starostenko, V. I., Ljashkevich, Z. N. & Sjejntot, A. (2006). The study of the dynamics and geological processes of the Dnieper-Donets paleorift. In The structure and dynamics of the lithosphere of Eastern Europe (pp. 307-314), Moscow: Geokart-GEOS (in Russian).

Cvetkova, T. A. & Bugaenko, I. V. (2012). Seismotomography of the mantle beneath the East-European platform. Geophysical journal, 34, No. 5, pp.161-172 (in Russian).

Ziegler, P.A. & Cloetingh, S. (2004). Dynamic processes controlling evolution of rifted basins. Earth-Science Review, 64, pp. 1-50. https://doi.org/10.1016/S0012-8252(03)00041-2

Goncharov. M. A. (2007). Convective mechanism for the transition from passive to active rifting. Proceedings of the KhI tectonic meeting Fundamental problems of geotectonics, Vol. 1 (pp.195-198), Moscow: GEOS (in Russian).

Chekunov, A. V. (1994). To the geodynamics of the Dnieper-Donets rift-syncline. Geofiz. zhurn., 16, No. 3, pp. 3-13 (in Russian).

Chekunov, A. V. & Pashkevich, I. K. (1989). Tectonic nature of magnetic heterogeneities in the lithosphere of Ukraine. Dokl. AN USSR. Ser. B, No. 5, pp. 22-26.

Starostenko, V. I., Danilenko, V. A., Vengrovich, D. B., Kutas, R. I., Stifenson, R. A. & Stovba, S. N. (2001). Modeling of the sedimentary basins evolution with tacing into account the natural environment structure and processes of self-organization. Fizika Zemli, No. 12, pp. 40-50 (in Russian).

Kutas, R. I. & Tsvyashchenko, V. A. (1993). Thermal processes in the geological history of the Donbas. Geofiz. zhurn., 15, No. 2, pp. 42-53 (in Russian).

Chekunov, A. V., Gavrish, V. K., Kutas, R. I. & Ryabchun, L. I. (1992). Dnieper-Donets palaeorift. Tectonophysics, 208, pp. 257-272. https://doi.org/10.1016/0040-1951(92)90348-A

Published

17.09.2024

How to Cite

Starostenko, V., Pashkevich, I., Makarenko, I., Kuprienko, P., & Savchenko, O. (2024). Geodynamical interpretation of the geological and geophysical heterogeneity of the Dniepr-Donets basin lithosphere . Reports of the National Academy of Sciences of Ukraine, (9), 84–94. https://doi.org/10.15407/dopovidi2017.09.084