Tectonic inversion of the Dnipro-Donets basin. Part 3. Tectonic style of deformations

Keywords: structural pictures, kinematic models, downthrow riftogenic framework, inverted shear-thrust framework, alpine-type deformations, Cenozoic hinged-jointed highlands, West-Donets orocline deformations


The purpose. The peculiarities of the spatial distribution and tectonic style of collisional deformations of the riftogenic structure of the Dnipro-Donets Basin were investigated.

Method. Kinematic and paragenetic analyses were used, structural drawings were studied, kinematic models of alpine-type deformations in the folded floors of the southeastern segment of the Basin were compiled.

The results. It was found that the riftogenic structure along the strike different style and intensity of inversion complications was been undergone. The structural border between the weakly and significantly located territory along the meridian of the city of Balaklia was determined. To the west of the border the rift downthrows acquired arc-shaped contours and a pendulum structure due to horizontal movements. Zones of Hercynian folding are divided into separate branches by echelon systems of landslides located diagonally to their axes. To the east of the border, at first the regional board faults bend to the west, and then to the east of the city of Donetsk, the northern ones bend to the east, and the southern ones - to the southeast. The zones of nearboard and axial regional faults are destroyed, and because of this, the lines of the Kochubiyivsko-Volvenkivskyi and Sosnivsko-Stepkivskyi axial salt dome shafts are interrupted. The relic is the Axial fault with the Druzhkiv-Komyshuva shaft adapted to it. Instead of a reset rift, a shear-thrust inversion frame of orocline form was formed. Alpinotype dislocations on most of the territory of the Basin are weakly pronounced (scattered, low-amplitude faults and uplifts), but the southeastern segment significant fault-folding and cover-thrust deformations has undergone. The analysis of the structure of the Oligocene-Miocene sediments shows that neotectonic structures in the sole of the Cenozoic cover and the daytime relief are reflected. On the northern board of the Basin, a number of arc-like elongated uplands that located in the hanging wings of the Hercynian thrusts were formed. A sign of uplands` formation in the geodynamic environment of transpression is oscillating articulation and diagonal placement relative to shear-thrust zones.

Scientific novelty. By the analysis of structural pictures of Elements of tectonics characteristic of transpression zones was identified. For the first time the nature of alpine-type deformations on kinematic models was identified. The Cenozoic movements along the re-mobilized zones of the Hercynian thrusts formed dynamically coupled ensembles of neotectonic structures was established. The hinged-jointed structural parageneses were formed by the mechanism of longitudinal elongation of the geological space due to the horizontal movements of right kinematics over the zones of dynamic influence of shear-thrusts of the foundation. It was found the tectonic style of the latest deformation ensembles is inherent in the platform fold-thrust geostructures of the tectonic breakaway. For the first time the newest platform structure - the West-Donetsk tectonic orocline of cover-folding deformations was identified.

Practical significance. Data on the distribution of alpine-type complications of the West-Donets Graben for paleogeodynamic reconstructions and improvement of the regional scheme of tectonic zoning of the Dnipro-Donetsk Basin can be used.


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Author Biographies

Oleksii Bartaschuk Bartaschuk , Ukrainian Scientific Research Institute for Natural Gases

DSc (Geology), Leading Researcher

Vasyl Suyarko, V. N. Karazin Kharkiv National University

DSc (Geology and Mineralogy), Professor

Oleksandr Chuienko, V. N. Karazin Kharkiv National University

Head of laboratory for the study of rocks, minerals and fossil organisms


Shatsky N. (1964). Basins of the Donetsk type. Favorites work, 2. M., Nauka, 544-553. [in Russian]

Sedimentary basins: study methodology, structure and evolution (2004). Edited by Yu. Leonov, Yu. Volozh. Works of GYNRAN, 543. M., Nauchny mir, 526. [in Russian]

Leonov M., Morozov Yu., Stefanov Yu., Bakeev R. (2018). Zones of concentrated deformation (flower structures): natural observations and modeling data. Geodynamics and tectonophysics, 9, 3, 693–720. https://doi.org/10.5800/GT-2018-9-3-0368 [in Russian]

Chebanenko I. I. (1977). Theoretical aspects of tectonic divisibility of the earth's crust. Kyiv, Nauk. dumka, 84. [in Russian]

Gintov O. (2005). Field tectonophysics and its application in the study of deformations of the earth's crust of Ukraine. Kyiv, Phoenix, 572. [in Russian]

Bartaschuk O. V. (2019). Evolution of the stressed-deformed state of the earth's crust of the Dnipro-Donetsk paleo-rift in the Phanerozoic. Reports of the National Academy of Sciences of Ukraine, 3, 62-65. [in Ukrainian]

Goryainov S. V. (2013). Cenozoic tectonic movements of Eastern Europe. Geology and minerals of the World Ocean, 3, 55-65. [in Russian]

Goryainov S. V. (2004). On the Laramie complication of the geological structure in various regions of Ukraine. Re-ports of the National Academy of Sciences, 3, 92-95. [in Russian]

Kopp M. L., Korchemagin V. A. (2010). Cenozoic stress/deformation fields of the Donbass and their probable sources. Geodynamics, 1(9), 37-49. https://doi.org/10.23939/jgd2010.01.037. [in Russian]

Meijers, M. J., Hamers, M. F., van Hinsbergen, D. J., van der Meer, D. G., Kitchka, A., Langereis, C. G., & Stephen-son, R. A. (2010). New late Paleozoic paleopoles from the Donbas Foldbelt (Ukraine): Implications for the Pangea A vs. B controversy. Earth and Planetary Science Letters, 297(1-2), 18-33. https://doi.org/10.1016/j.epsl.2010.05.028

Stampfli, G. M., & Borel, G. D. (2002). A plate tectonic model for the Paleozoic and Mezozoic constrained by dynamic plate boundares and restored synthetic ocean izochrons. Earth and Planetary ScienceLetters, 196(1-2), 17-33. https://doi.org/10.1016/S0012-821X(01)00588-X

Natal’in, B. A. & Sengor, A. M. C. (2005). Late Paleozoic to Triassic evolution of the Turan and Scythian platforms: the prehistory Paleo-Thethian closure. Tectonophisics, 404 (3-4), 175-202. https://doi.org/10.1016/j.tecto.2005.04.011

Goryainov S. V., Aksenov S. V., Altukhov A. S., Vorobyev S. V., Isaeva E. P., Korenev V. V. (2009). Metamorphic and metasomatic complexes of the Azov region and Southern Donbass. Kharkiv, Ekograf, 304. [in Russian]

Khain V. E. (1977). Regional geotectonics. Non-Alpine Europe and Western Asia. M., Nedra, 185-205. [in Rus-sian]

Korchemagin V. A., Ryaboshtan Yu. S. (1987). Tectonics and tension fields of Donbas. Stress fields and defor-mations in the earth's crust. M., Nauka, 167-170. [in Russian]

Goryainov S. V. (2015). Hercynian tectonic movements of Eastern Ukraine. Latest problems of geology. Materials of the scientific and practical conference for the 100th an. of the birth of V.P. Makridin (Kharkiv, May 21-23, 2015). Ed. I. S. Ivanchenko, 162–165. [in Russian]

Gonchar V. V. (2019). Tectonic inversion of the Dnieper-Donetsk Basin and Donbass (models and reconstructions). Geophys. journal, 41, 5, 47-86. https://doi.org/10.24028/gzh.0203-3100.v41i5.2019.184444 [in Russian]

Forecast of the localization and gas content of lithological traps of the southeast of the DDZ within the license areas of Shebelinkagavydobuvannya GPU. Part 1. Creation of a structural and geological basis: report on the NDR (final): No. 100 SHGV 2017-2017 (topic No. 34.521/2017-2017) Resp. exclamation S. Horyainov, Yu. Sklyarenko (2017). Kharkiv, UKRNDIGAZ, 203. [in Ukrainian]

Bartaschuk O. V. (2021). Geodynamic conditions of oil and gas bearing capacity of the Dnipro-Donetsk paleorift: autoref. diss... Dr. geol. of science. Kyiv, Institute of Geological Sciences of the National Academy of Sciences of Ukraine, 33. [in Ukrainian]

Bartaschuk O. V. (2020). Tectonic inversion of the Dnieper-Donetsk depression. Part 1. Collision tectonics of the Western Donetsk Graben. Visnyk of V. N. Karazin Kharkiv National University, series "Geology. Geography. Ecol-ogy", (52), 10-23. https://doi.org/https://doi.org/10.26565/2410-7360-2020-52-01 [in Ukrainian]

Bartaschuk O.V. (2020). Tectonic inversion of the Dnieper-Donetsk depression. Part 2. Geodynamic conditions and kinematic mechanism of deformations of the riftogenic structure. Visnyk of V. N. Karazin Kharkiv National University, series "Geology. Geography. Ecology", (53), 10-23. https://doi.org/10.26565/2410-7360-2020-53-01 [in Ukrainian]

Goryainov S. V., Korenev V. V. (2007). Cross-thrust structure of the Donbas junction zone with the Azov block of the Ukrainian shield. Geology and issues of geological mapping and study of Precambrian formations of the Ukrainian Shield. Materials of the 4th scientific and industrial meeting of geologists-surveyors of Ukraine (Octo-ber 8-12, 2007, Kryvyi Rih). Dnipropetrovsk, 102-104. [in Russian]

Bartashchuk, O., & Suyarko, V. (2020). Geodynamics of formation of the transition zone between the Dnieper-Donets basin and the donbas foldbelt. Tectonic style of inversion deformations. Geodynamics, 2(29), 51-65. https://doi.org/10.23939/jgd2020.02.051

Bartashchuk, O., & Suyarko, V. (2021). Geodynamics of formation of the transition zone between the Dnieper-Donets basin and the Donbas foldbelt. Tectonic regimes and kinematic mechanisms of inversion. Geodynamics, 1(30), 25-35. https://doi.org/10.23939/jgd2021.01.025

Bartashchuk, O., & Suyarko, V. (2021). Geodynamics of formation of the transition zone between the Dnieper-Donets basin and the Donbas foldbelt. Tectonic inversion of rift-like structure. Geodynamics, 2(31), 53-65. https://doi.org/10.23939/jgd2021.02.053

Timurziev A. I. (2009). Newest strike-slip tectonics of sedimentary basins: tectonophysical and fluid dynamic as-pects: autoref. diss... Dr. Geol.-Miner. Sc. MSU, 40. [in Russian]

Atmaoui N., Kukowski N., Stockhert B., Konig D. (2006). Initiation and development of pull-apart basins with Riedel shear mechanism: insights from scaled clay experiments. Int. J. Earth Sci. (Geol Rundsch.), 95, 225–238. https://doi.org/10.1007/s00531-005-0030-1

Goryainov S. V. (2022). Alpine tectonic movements and salt tectonics of eastern Ukraine. Visnyk of V. N. Karazin Kharkiv National University, series "Geology. Geography. Ecology", (56), 67-75. https://doi.org/10.26565/2410-7360-2022-56-04 [in Ukrainian]

Deep geological sections of the Dnieper-Donets basin (due to prospects for oil and gas). Explanatory note to geo-logical maps of VAT on sections -5000 and -6000 m scale 1:500000. Glushko V. (editor) (1978). Kyiv, UKRNIIGAZ, UKRNIGRY, 88, 2 maps. [in Russian]

Regional seismic research in the zone of articulation of Central Donbas and DDZ. Pobedash M. (editor) (2014). Kyiv, DGP "Ukrgeofizika" Technological Center, TP 113/06, 20 sheets. [in Ukrainian]

Lowell J. D. (1985). Structural Styles in Petroleum Exploration. OGCI Publications. Oil & Gas Consultants Int. Tulsa, 470.

How to Cite
Bartaschuk , O. B., Suyarko, V., & Chuienko, O. (2023). Tectonic inversion of the Dnipro-Donets basin. Part 3. Tectonic style of deformations. Visnyk of V. N. Karazin Kharkiv National University, Series "Geology. Geography. Ecology", (58), 12-28. https://doi.org/10.26565/2410-7360-2023-58-01