A5029560444- Geological Formations and Processes Exploration
- Mining and Gasification Technologies
- Geotechnical and Geomechanical Engineering
- Geological and Geochemical Analysis
- Geological Studies and Exploration
- earthquake and tectonic studies
- Pelvic and Acetabular Injuries
- Sarcoidosis and Beryllium Toxicity Research
- Advanced Data Processing Techniques
- Economic Issues in Ukraine
- Scientific Research and Studies
- Superconducting Materials and Applications
- Geochemistry and Geologic Mapping
- Labor Market and Education
- Advanced Power Generation Technologies
- Spinal Fractures and Fixation Techniques
- Diverse Scientific Research in Ukraine
- High-pressure geophysics and materials
National Academy of Sciences of Ukraine
2017-2025
GFZ Helmholtz Centre for Geosciences
2023-2024
Seismological monitoring is vital for both fundamental research and applied geophysics. Even in regions with moderate seismicity, a robust seismic network crucial hazard assessment geoscientific advancements. In Ukraine, this need has intensified due to the ongoing recovery modernization following war. Ukraine’s historically faced significant challenges, including outdated equipment minimal upgrades since independence. The war exacerbated these issues, resulting funding cuts,...
To better understand the geological and tectonic conditions of Ukraine, it is necessary to improve regional earthquake monitoring by upgrading existing seismic stations installing new ones. Ukraine's western, southwestern, southern regions are located within a seismically active belt formed collision Eurasian African plates. This spans from Azores through Mediterranean, Black Sea, Caucasus regions, extending Hindu Kush. It includes key areas such as Carpathian Arc, which experiences...
The oil and gas fields of Forecarpathian region are compared with the structure earth’s crust regional faults. Most condensate localized in Borislav-Pokutia nappe over Precarpathian Fault zone. majority located under thrusting zone Sambir fault, which is a gently dipping detachment connected fault other faults autochthonous basement. gravity low Carpathian Foredeep also limited from northeast by southwest Uzhok fault. tends to central part low. Transverse Tyachev-Nadvorna displaces delimits...
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 studies include the materials of field tectonophysical observations 2013―2018 and reinterpreted data 1990―1995. In order to determine stress tensor structural-paragenetic kinematic methods were used. Application optimizing procedure, implemented Vin Tensor program, allowed taking into account sliding fissures without determined types not involved previous processing. Determining part in formation development Ukrainian Carpathians was played by tectonic forces southwestern 220° direction....
Tectonophysical interpretation of 80 mechanisms earthquake sources (80—172 km deep) during 1940—2011 has been performed for seismogenic zone Vranchea. Functioning nodal planes have identified as the uplifts and uplift-shifts that were formed under conditions sub-horizontal pressure. Structural scheme deep Vranchea plotted where functioning united into thrust-fault, uplift-shift zones extending in northeastern, northwestern, north-northwestern sub-latitudinal directions. It shown orientation...
The tectonic structure of Dobrogea and Fore-Dobrogea trough are considered on the basis geological geophysical data. key areas for understanding Central Europe geodynamics, because they located within southeastern part Trans-European Suture Zone (TESZ), which is available here direct field research. current position these units in foreland Carpathians north-eastern coast Black Sea makes them a link that connects Pannonian-Carpathian region Crimean-Black region. deep study area described by...
The article concerns results of studying two significant seismic events — an explosion (23.09.2020 09:00) and earthquake (30.09.2020 20:00), which occurred in the area city Kryvyi Rih. There were developed algorithms to process records by Rih station. was done a comprehensive interpretation seismologic geological-geophysical data. events’ coordinates determined, quality seismological data processing evaluated based on expert method, level trustworthiness resulting parameters estimated....
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 seismic hazard department and of the Carpathian region seismicity Subbotin Institute Geophysics National Academy Science Ukraine, with support collaboration U.S. Department Energy, Lawrence Livermore Laboratory, Michigan State University, EarthScope Consortium had done first steps to expand Ukrainian Seismic Network (UT) through installation permanent broadband stations in territory Ukraine.The main goal Expansion Modernization Ukraine is improve regional network coverage by making...
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...
Seismic activity in Ukraine varies across regions with notable active zones the Carpathians and Crimean-Black Sea segments. Southwest is affected by Vrancea seismic zone (Romania) demands attention, alongside rare but potentially powerful events stable Ukrainian shield. Mining industrial activities also induce ground vibrations (Mw 2.5–4) otherwise areas. Although major destructive earthquakes are infrequent, cumulative impact of smaller can shape geological geophysical landscape...
Editorial| March 18, 2024 Early Publication Ukrainian Seismic Network: Current Status and Challenges Tetiana Amashukeli; Amashukeli * 1Helmholtz Centre Potsdam ‐ GFZ German Research for Geosciences, Potsdam, Germany2Subbotin Institute of Geophysics National Academy Sciences Ukraine, Kyiv, Ukraine *Corresponding author: amashuke@gfz-potsdam.de https://orcid.org/0000-0002-8932-8656 Search other works by this author on: GSW Google Scholar Liudmyla Farfuliak; Farfuliak 2Subbotin...
As of 2022, the National System Seismic Observations Ukraine had a network observation points run by S.I. Subbotin Institute Geophysics Academy Sciences and Main Center for Special Control State Space Agency Ukraine. These institutions established unified Data Center, where data is collected, processed, analyzed. Information provided both in real time later, after an in-depth analysis, form seismological bulletins earthquake catalogs. According to observations, 160 earthquakes occurred on...
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...
The National System of seismic observations Ukraine has accumulated a network observation seismicpoints the joint management S.I. Subbotin Institute Geophysics Academy Sciences and Main Special Monitoring Center State Space Agency Ukraine. two institutions together established database in which are collected, processed analyzed. Alongside live updates, data systematized as seismological bulletins an earthquake catalogs. According to data, nearby countries there happened 2021 over one hundred...
Summary The Carpathian-Pannonian region is traditionally interpreted as accretionary prism - back-arc basin system, although alternative models exist. This study presents balanced geological cross-section, crust tectonic model on base of seismic images obtained by migration method combined the depth asthenosphere along PANCAKE profile to understand geodynamics region. cross-section shows thrust tectonics with significant horizontal NE displacements. A basal detachment Carpathian allochthon...
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 monitoring hazardous natural processes in order to assess risks the public and industrial facilities ensure safety has become starting point for creation of appropriate systems. development a modern hardware base entailed need develop methods processing continuous stream information real-time. main trend field seismological is introduction technology automation collection accumulation processes.The largest most extensive currently existing systems world IRIS GSN, network that actively...
The Institute of Geophysics the NASU organizes and carries out continuous regional local seismic observations on territory Ukraine. article presents a universal modern model activity monitoring process, which is used in most international seismological agencies (USGS, EMSC, NEIC) describes typical stationary point National Seismological Network NAS network complex systems consisting points registration waves, distributed system transfer collecting information, also center operative...
Carried out in 2021, the wide-angle reflection and refraction (WARR) SHIELD’21 profile crosses, from SW to NE, main tectonic structures of Ukraine. It 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 Dnipro-Donetsk Basin. The ~650 km long is an extension previously realized...
In February 2022, the Ukrainian seismic network already faced multiple critical issues and its modernization was needed. The war exacerbated all existing accelerated need for a fundamental reorganization modernization. this presentation we will report on network’s status draft reconstruction plans. As of January 5th 2023, has been damaged by as follows:partial or complete destruction facilities infrastructure caused power internet outages; inability to serve stations; Zmiinyi...
Summary The seismic hazard department and of activity Carpathian area the Subbotin Institute Geophysics National Academy Science Ukraine, with support collaboration U.S. Department Energy (DOE), Lawrence Livermore Laboratory (LLNL), Michigan State University (MSU), EarthScope Consortium (EarthScope) plan to expand national network through installation permanent broadband stations in territory Ukraine. This is due fact that western, south-western southern parts Ukraine are located within...