A5021828451- Geological Formations and Processes Exploration
- Geological Studies and Exploration
- Geological and Geochemical Analysis
- Mining and Gasification Technologies
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Seismic Imaging and Inversion Techniques
- Pelvic and Acetabular Injuries
- Geotechnical and Geomechanical Engineering
- Geochemistry and Geologic Mapping
- Hydrocarbon exploration and reservoir analysis
- Methane Hydrates and Related Phenomena
- Seismology and Earthquake Studies
- Marine and environmental studies
- Reservoir Engineering and Simulation Methods
- Spinal Fractures and Fixation Techniques
- Hydraulic Fracturing and Reservoir Analysis
National Academy of Sciences of Ukraine
2014-2024
Palladin Institute of Biochemistry
2003
The Scythian Platform (ScP) with a heterogeneous basement of Baikalian–Variscan–Cimmerian age is located between the East European Craton (EEC) on north and Crimean–Caucasus orogenic belt Black Sea (BS) Basin south. In order to get new constrains basin architecture crustal structure ScP better understanding tectonic processes evolution southern margin EEC during Mesozoic Cenozoic time, 630-km-long seismic wide-angle refraction reflection (WARR) profile DOBRE-5 was acquired in 2011 October....
Between 1960 and 1990, extensive deep seismic studies were conducted in Ukraine, significantly enhancing the understanding of Earth’s crust mantle, particularly within Ukrainian Shield. This paper introduces a methodology for digitizing analog records preserved on photographic paper, representing crucial step safeguarding historical data. Test digitization section Geotraverse IV demonstrated feasibility creating vectorized images, enabling modern interpretation The results confirmed...
In order to study the lithospheric structure in southern Ukraine, a seismic wide-angle reflection/refraction project DOBRE-4 was conducted. The 500-km-long profile starts SW from Alpine/Variscan North Dobrudja Fold-Thrust Belt, being part of Trans-European Suture Zone. It runs NE, mostly along NW Black Sea coastal plain, towards centre Precambrian Ukrainian Shield. field acquisition October 2009 included 13 chemical shot points with charge sizes 600–1000 kg every 35–50 km and 230 recording...
The GEORIFT 2013 (GR'13) WARR (wide-angle reflection and refraction) experiment was carried out in the territory of Belarus Ukraine with broad international co-operation. aim work is to study basin architecture deep structure Pripyat–Dnieper–Donets Basin (PDDB), which deepest best studied Palaeozoic rift Europe. PDDB located southern part East European Craton (EEC) crosses Sarmatia—one three segments EEC. formed by Late Devonian rifting associated domal basement uplift magmatism. GR'13...
Abstract The DOBRE-2 wide-angle reflection and refraction profile was acquired in June 2007 as a direct, southwestwards prolongation of the 1999 DOBREfraction'99 that crossed Donbas Foldbelt eastern Ukraine. It crosses Azov Massif East European Craton, Sea, Kerch Peninsula (the easternmost part Crimea) northern Black Sea Basin, thus traversing entire Crimea–Caucasus compressional zone centred on Peninsula. recorded mix onshore explosive sources well airguns at sea. A variety single-component...
The TTZ-South seismic profile follows the Teisseyre-Tornquist zone (TTZ) at SW margin of East European craton (EEC). Investigation results reveal upper lithospheric structure as representing NW-vergent, NE-SW striking overthrust-type, Paleoproterozoic (~1.84–1.8 Ga) Fennoscandia-Sarmatia suture. Sarmatian segment EEC comprises two crustal-scale tectonic thrust slices: Moldavo-Podolian and Lublino-Volhynian basement units, overriding northerly located Lysogoro-Radomian unit Fennoscandian...
The work has been completed on the studies of Earth crust and upper mantle structure along DSS profile N26 using methods tomographic inversion seismic waves density modeling. conducted revealed complicated block-like region with riftogenesis processes playing active part in its formation. It shown that Kiliysko-Zmiyine uplift Karkinitsky sag have got different lithosphere structure. Typical rift Odessa fault confirmed eastward incline revealed. results modeling give evidence presence two...
The wide-angle reflection and refraction (WARR) TTZ-South transect carried out in 2018 crosses the SW region of Ukraine SE Poland. profile targeted structure Earth's crust upper mantle Trans-European Suture Zone, as well southwestern segment East European Craton (slope Ukrainian Shield). ~550 km long (~230 Poland ~320 western Ukraine) is an extension previously realized projects Poland, TTZ (1993) CEL03 (2000). deep seismic sounding study along using TEXAN DATA-CUBE stations (320 units) made...
The interpretation of seismic refraction and wide angle reflection data usually involves the creation a velocity model based on an inverse or forward modelling travel times crustal mantle phases using ray theory approach. codes differ in terms parameterization, used for modelling, regularization result, etc. It is helpful to know capabilities, advantages limitations code compared others. This work compares some popular 2D dataset collected along wide-angle profile DOBRE-4, where quite...
Carried out in 2021, the wide-angle reflection-refraction (WARR) SHIELD’21 profile crosses, from SW to NE, main tectonic structures of Ukraine. It has targeted crustal and uppermost mantle structure underlying Archaean Paleoproterozoic crystalline complexes Ukrainian Shield adjacent platformal areas. To Shield, basement is overlain by Vendian through Paleozoic strata Volhyno-Podolian Homocline, plunging at its end below Carpathian belt Neogene foredeep. cratonic covered Devonian...
The paper consists of two parts. first part, which is presented here, briefly reviews the history geological and geophysical study platform part territory Ukraine, located within southwestern margin East European craton occupies a significant area Sarmatian lithospheric mini-plate. main attention focused on studies XXI century, made decisive contribution to revision some issues related geodynamic processes clarification tectonics deep structure studied region. method seismic sounding Earth's...
У другій частині статті продовжується розгляд, за комплексом геофізичних методів, глибинної будови земної кори регіонів України, зокрема Волино-Подільської плити (ВПП), а також поверхні Мохо і мантії до глибини 850 км. Наведено геотермічну, густинну, геомагнітну та геоелектричну моделі кори. За сейсмічними даними показано, що осадовий чохол ВПП на межі з Транс’європейською шовною зоною (ТТЗ) занурюється глибину біля 4 км проти 8—10 км, як вважалося раніше, тому решту частини Підкарпатського...
Summary The paper proposes reinterpretation of digitized seismic hodographs geotraverse VI (on the distance 440–520), and further calculation velocity model using tomographic inversion in order to clarify deep structure Pobuzkyi mining-ore district (PMOD) Ukrainian shield (USh), which is characterized by various mineral complexes crystalline Precambrian rocks.
The velocities’ distribution was obtained by interpretation of DSS data along profiles Dikanka - Druzhkovka and Reshetilovka Sinevka using seismic tomographic inversion first arrivals. That has allowed to allocate the fault zones. Research revealed that oil gas deposits crossing profile Sinevka, are associated with area minimum velocities in sedimentary cover. Sagaydakskoe is salt-dome structure, but Semirenkovskoe Tymofeevskoe deep faults. In section all local depressions characterized...
The wide-angle reflection and refraction (WARR) SHIELD’21 profile carried out in 2021 crosses from SW to NE the main tectonic of Ukraine. targeted structure Earth’s crust upper mantle southwestern margin East European Craton with overlying Neogene Carpathian Foredeep Vendian-Paleozoic Volyn-Podolian Monocline, Archaean Paleoproterozoic segments Ukrainian Shield Late Paleozoic Dnieper-Donets Basin. ~650 km long is an extension realized 2014 RomUkrSeis line Romania Ukraine Apuseni Mountains...
Summary The reinterpretation of the “old” seismic data along line 900 km long geotraverse profile is represented by a tomographic model. bitmap images original were converted into vector diagrams DIGITIZER computer program. This made it possible to represent hodographs as numerical sets and construct model line. velocity obtained inversion method first arrivals waves. deep tectonic structures are clearly outlined on In particular, Ukrainian Shield characterized Volyn, Podolsk, Bug Megablocks...
The wide-angle reflection and refraction (WARR) TTZ-South transect carried out in 2018 crosses the SW region of Ukraine SE Poland. profile targeted structure Earth’s crust upper mantle Trans-European Suture Zone, as well southwestern segment East European Craton (slope Ukrainian Shield). ~550 km long (~230 Poland ~320 western Ukraine) is an extension previously realized projects Poland, TTZ (1993) CEL03 (2000). deep seismic sounding study along using TEXAN DATA-CUBE stations (320 units) made...