International cooperation of S. I. Subbotin Institute Geophysics, NAS of Ukraine for 2010—2020

Authors

  • V. I. Starostenko Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Ukraine
  • O. M. Rusakov Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Ukraine
  • A. I. Yakimchik Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine, Ukraine

DOI:

https://doi.org/10.24028/gzh.v43i3.236390

Keywords:

Institute of Geophysics, NAS of Ukraine, international projects and target teams, the Antarctic Peninsula, Southeast Asia, impact factors of journals

Abstract

The geological structure of the lithosphere of the main tectonic structures has been refined for the territory of Ukraine and adjacent regions of Slovakia, Poland, Romania, Russia, as well as Bulgaria, the Antarctic Peninsula (West Antarctica) and Southeast Asia, and new data have been obtained on geophysical impacts that can affect the environment. A geodynamic scenario has been developed for the formation of large-scale folding of the Fore- Dobrudzja Trough, the South Ukrainian monocline and the Ingul block of the Ukrainian Shield, caused by tectonic events associated with the closing of the Paleotethys and Neotethys oceans in the Mesozoic. In the Pripyat-Dnieper-Donets Basin, the structure of the earth’s crust and upper mantle can reflect different intensities of rifting, from its passive stage in the Dnieper Graben to active rifting in the Pripyat Trough. An analysis of the geoelectric structure of the Earth’s crust in the Ukrainian Eastern Carpathians indicates that seismic events occur mainly in resistive solid rock domainswhich surrounded by aseismic high conductive zones consisting of at least partially melted material. The present-day mutual position of the Ukrainian shield and Fennoscandia stabilized 1720—1660 Ma. The age, distribution, orientation and composition have been studied for the LatePalaeoproterozoicdykes in the Volyn, Ingul and Azov blocks of the Ukrainian Shield. Eastern Crimea and the Sorokin Trough are fragments of a tectonic wedge formed after the Paleocene. The geothermal conditions of the Intra-Carpathian region are due to subduction during the closure of the Pannonian sea basin and the collisional interaction of the Eurasian plate with the microplates system of this region. In Bulgaria, most earthquakes occur outside high-resistive domains. The tectonic stages are reconstructed for the formation of the northern part of the Antarctic Peninsula in the Mesozoic-Cenozoic. The relationship has been established between the geomagnetic field and climate change, with it being different for the Northern and Southern Hemispheres. The results have been obtained within the framework of 25 international projects and 6 temporary international target teams of S. I. Subbotin Institute of Geophysics, NAS of Ukraine consisting of researchers from 23 countries. The results are presented in 53 publications, 38 of which are indexed in the Web of Scienct database, and 32 papers are published in 20 international journals and special publications of 10 countries with different impact factors (from 0,101 to 4,214), whose average impact factor is 3,341, and the total one is 66,815.

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Starostenko, V., Janik, T., Kolomiyets, K., Czuba, W., Środa, P., Grad, M., Kovács, I., Stephenson, R., Lysynchuk, D., Thybo, H., Artemieva, I. M., Omelchenko, V., Gintov, O., Kutas, R., Gryn, D., Guterch, A., Hegedus, E., Komminaho, K., Legostaeva, O., Tiira, T., & Tolkunov, A. (2013a). Seismic velocity model of the crust and upper mantle along profile PANCAKE across the Carpathians between the Pannonian Basin and the East European Craton. Tectonophysics, 608, 1049—1072. https://doi.org/10.1016/j.tecto.2013.07.008.

Starostenko, V., Janik, T., Lysynchuk, D., Sroda, P., Czuba, W., Kolomiyets, K., Aleksandrowski, P., Gintov, O., Omelchenko, V., Komminaho, K., Guterch, A., Tiira, T., Gryn, D., Legostaeva, O., Thybo, H., & Tolkunov, A. (2013b). Mesozoic (?) lithosphere-scale buckling of the East European Craton in southern Ukraine: DOBRE-4 deep seismic profile. Geophysical Journal International, 195(2), 740—766. https://doi.org/10.1093/gji/ggt292.

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Starostenko, V.I., Dolmaz, M.N., Kutas, R.I., Rusakov, O.M., Oksum, E., Hisarli, Z.M., Okyar, M., Kalyoncuoglu, U.Y., Tutunsatar, H.E., & Legostaeva, O.V. (2014). Thermal structure of the crust in the Black Sea: comparative analysis of magnetic and heat flow data. Marine Geophysical Research, 35(4), 345—359. https://doi.org/10.1007/s11001-014-9224-x.

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Udintsev, G.B., Kurentsova, N.A., Beresnev, A.F., Kol'tsova, A.V., Domoratskaya, L.G., Schenke, G.V., Bakhmutov, V.G., & Solov'ev, V.D. (2012a). Tectonics of the Drake Passage-Scotia Sea Zone in the Southern Ocean. Doklady Earth Sciences, 445(2), 1029—1035. https://doi.org/10.1134/s1028334x12080260.

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Wimbledon, W.A.P., Bakhmutov, V., Halasova, E., Svobodova, A., Rehakova, D., Frau, C., & Bulot, L.G. (2020). Comments on the geology of the Crimean Peninsula and a reply to a recent publication on the Theodosia area by Arkadiev et al. (2019): “The calcareous nannofossils and magnetostratigraphic results from the Upper Tithonian-Berriasian of Feodosiya region (Eastern Crimea)”. Geologica Carpathica, 71(6), 516—525. https://doi.org/10.31577/GeolCarp.71.6.3.

Yegorova, T., & Bakhmutov, V. (2013). Crustal structure of the Antarctic Peninsula sector of the Gondwana margin around Anvers Island from geophysical data. Tectonophysics, 585, 77—89. https://doi.org/10.1016/j.tecto.2012.09.029.

Yuan, K., Van der Voo, R., Bazhenov, M.L., Bakhmutov, V., Alekhin, V., &Hendriks, B.W.H. (2011). Permian and Triassic palaeolatitudes of the Ukrainian shield with implications for Pangea reconstructions. Geophysical Journal International, 184(2), 595—610. https://doi.org/10.1111/j.1365-246X.2010.04889.x.

Published

2021-10-05

How to Cite

Starostenko, V. I., Rusakov, O. M. ., & Yakimchik, A. I. . (2021). International cooperation of S. I. Subbotin Institute Geophysics, NAS of Ukraine for 2010—2020. Geofizičeskij žurnal, 43(3), 205–226. https://doi.org/10.24028/gzh.v43i3.236390

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International cooperation