В. Г. Бахмутов

ORCID: 0000-0003-3804-9953
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About
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Research Areas
  • Geomagnetism and Paleomagnetism Studies
  • Geological and Geochemical Analysis
  • Geology and Paleoclimatology Research
  • Marine and environmental studies
  • Geological Formations and Processes Exploration
  • Geochemistry and Geologic Mapping
  • Geological Studies and Exploration
  • Earthquake Detection and Analysis
  • Ancient and Medieval Archaeology Studies
  • Atmospheric Ozone and Climate
  • Solar and Space Plasma Dynamics
  • Methane Hydrates and Related Phenomena
  • Paleontology and Stratigraphy of Fossils
  • Pleistocene-Era Hominins and Archaeology
  • earthquake and tectonic studies
  • Mining and Gasification Technologies
  • Soil and Environmental Studies
  • Medical and Biological Sciences
  • Hydrocarbon exploration and reservoir analysis
  • High-pressure geophysics and materials
  • Geophysics and Gravity Measurements
  • Geological and Geophysical Studies
  • Atmospheric chemistry and aerosols
  • Atmospheric and Environmental Gas Dynamics
  • Polar Research and Ecology

National Academy of Sciences of Ukraine
2015-2025

Polish Academy of Sciences
2022-2025

Institute of Geophysics
2016-2025

Comenius University Bratislava
2022

Ministry of Education and Science
2018-2021

State Institution National Antarctic Scientific Center
2018-2021

Taras Shevchenko National University of Kyiv
2020

Czech Academy of Sciences, Institute of Geophysics
2018-2020

National Institute of Geophysics, Geodesy and Geography
2013

Institute of Geophysics
1990

SUMMARY The time-averaged geomagnetic field is generally purported to be uniformitarian across Earth history—close a geocentric axial dipole, with average strength within one order of magnitude that at present. Nevertheless, recent studies have reported the was approximately ten times weaker than present in mid-Palaeozoic (∼410–360 Ma) and late Ediacaran (∼565 Ma). Here we first whole-rock palaeointensity determinations age outside Laurentia. These were obtained by Thellier-Coe, Wilson...

10.1093/gji/ggz566 article EN Geophysical Journal International 2019-12-12

SUMMARY Changes in the geomagnetic field over geologic timescales can be used to study evolution and processes of its sources Earth's deep interior. As a stark contrast behaviour recent past, late Neoproterozoic is defined by ambiguous polar wander paths, ultralow strengths period extreme reversal hyperactivity. Palaeointensity data from this time are still scarce conclusions made these suffer large uncertainties brought low sampling density. In study, we present new palaeomagnetic...

10.1093/gji/ggac186 article EN cc-by Geophysical Journal International 2022-05-17

The Antarctic Peninsula (AP) is a composite magmatic arc terrane formed at the Pacific margin of Gondwana. Through late Mesozoic and Cenozoic subduction has stopped progressively from southwest to northeast as result series ridge trench collisions. Subduction may be active today in northern part AP adjacent South Shetland Islands. system confined by Shackleton Hero fracture zones. continental marked high-amplitude gravity magnetic anomaly belts reaching highest amplitudes region Islands...

10.1111/j.1365-246x.2010.04867.x article EN Geophysical Journal International 2010-11-30

10.1016/s1464-1895(99)00113-1 article EN Physics and Chemistry of the Earth Part A Solid Earth and Geodesy 1999-01-01

Summary The soil magnetism is the indicator of physical and chemical processes occurring in pedosphere. current war Ukraine arise new challenge related to studying magnetic properties at areas military activities, different drones missiles attacks, unexploded ordnance (UXO), other weapon pieces particulate matter which are constant sources organic inorganic pollution. study area Ozera-15 located Forest zone Ukraine. predominant Umbric Albeluvisols Abruptic according WRB-FAO. measurements...

10.3997/2214-4609.202410637 article EN 2024-01-01

A collection of 306 oriented samples from 43 Permian and Triassic intrusions the Ukrainian Shield, southwest portion East European Craton, has yielded valuable palaeomagnetic directions with new ages obtained using 40Ar/39Ar method. Andesitic have Late (six dating samples) 204.2 ± 1.6 Ma to 215.7 2.0 dual-polarity Dec/Inc = 60.1°/+64.4°, k 96, α95= 4.5°, derived N 12 sites. Trachyte dykes an early Artinskian (mid-Early Permian) age (one sample) 282.6 2.6 Ma, 204.3°/−23.8°, 27.7, 6.5°, 19 The...

10.1111/j.1365-246x.2010.04889.x article EN Geophysical Journal International 2010-12-22

A combined palaeodirectional and palaeointensity study of a representative collection plutonic rocks from the Antarctic Peninsula batholith western part Peninsula, near Ukrainian base 'Academik Vernadsky' were carried out. Petrographically, includes gabbros, diorites quartz diorites, tonalities, granodiorites granites. The ages igneous complex emplacement vary 50 to 117 Ma with most belonging Cretaceous Normal Superchron. characteristic remanent magnetizations isolated by stepwise thermal...

10.1111/j.1365-246x.2012.05357.x article EN Geophysical Journal International 2012-02-15

We provide a revised magnetostratigraphy and magnetic susceptibility stratigraphy of the most complete thickest (to nearly 60 m) loess-palaeosol sequences in Ukraine spanning past 1 My: Roksolany (Black Sea Lowland) Vyazivok (Dnieper sections. The Matuyama–Brunhes boundary has been detected both stratigraphically different palaeosol units according to current regional chronostratigraphic schemes. Hypotheses large lock-in depth at lithostratigraphic incompleteness do not resolve this...

10.7306/gq.1544 article EN Geological Quarterly 2020-09-01

New paleomagnetic and geochronological results on late Cretaceous-Paleogene intrusive effusive complexes of the western part Antarctic Peninsula have been obtained. isotopic dating "fills" regularly temporal gap from 96 to 61 Ma demonstrating uninterrupted character development considered active margin phase its origination collapse. For most analyzed rocks early associations Andian complex (96- 88 Ma) subductively-enriched lithospheric source can be definitely detected. younger Cenozoic...

10.24028/gzh.0203-3100.v35i3.2013.116387 article EN cc-by Geofizicheskiy Zhurnal 2013-04-01

We present evidence for the uppermost Jurassic–lowest Cretaceous interval in Crimea, coastal southern Ukraine. Three facies zones are distinguished upper Dvuyakornaya and Mayak formations of eastern Crimean Peninsula: basinal, slope toe-of-slope zones. In this we identify lowest Berriasian Jacobi Grandis subzones authors, expanded form, exceeding 160 metres thickness. new magnetostratigraphic interpretations, two normal reversed polarity intervals, assigned to M19n, M18r, M18n M17r, with...

10.7306/gq.1404 article EN Geological Quarterly 2018-04-10

The results of investigations in 2006–2010 for hydrocarbon and gas hydrates on the Antarctic Peninsula continental margin are given. In 2004 2006, marine geoelectric researches by methods forming a short-pulsed electromagnetic field (FSPEF) vertical electric-resonance sounding (VERS) had been conducted this region. “deposit” type anomaly was mapped FSPEF survey, anomalous polarized layers “hydrocarbon deposit” were chosen VERS within region UAS “Academician Vernadsky.” Anomalous zones “gas...

10.1155/2011/514082 article EN Journal of Geological Research 2011-11-14

Over the past decade, development of unmanned aerial technologies has allowed them to be considered a tool for conducting remote Earth sensing research. The use such systems is primarily associated with solving geological and archaeological tasks. However, armed aggression by Russian Federation contaminated Ukrainian territory at an unprecedented scale, including unexploded ordnance (UXO). It necessary check vehicles (UAVs) can used address this issue. An efficient solution significantly...

10.24028/gj.v45i5.289117 article EN cc-by-nc-sa Geofizicheskiy Zhurnal 2023-10-31

Variations of rock magnetic parameters in loess-palaeosol sequences, related to climatic and environmental conditions during their formation, are a powerful tool for palaeoclimate reconstruction. Combined enviromagnetic study loess deposits Ukraine its assessment the palaeoreconstruction purposes carried out framework National Research Foundation project 2020.02/0406 ‘Magnetic proxies palaeoclimatic changes sequences Ukraine’. Environmental/climatic reconstructions past fulfilled using...

10.24028/gzh.v43i3.236378 article EN cc-by-nc-sa Geofizicheskiy Zhurnal 2021-07-28

Background. One of the dangerous effects on environment caused by military actions in Ukraine is destruction soil. This includes its pollution, redistribution genetic horizons, compaction, change physical and chemical agronomic indicators, etc. Accumulated experience shows that most these processes are reflected magnetic properties soils. Methods. The applied method a full range field laboratory studies. More detailed mineralogical methods measurements described in. Results. On basis diagram...

10.17721/1728-2713.106.01 article EN Visnyk of Taras Shevchenko National University of Kyiv Geology 2024-01-01

Combined rock magnetic and palaeomagnetic studies of loess-soil sections — Lower Paleolithic sites in the valley Southern Bug (Medzhybizh, Holovchintsi) have been performed for first time order to determine suitability these objects study establishment magnetostratigraphic markers. Investigated by characteristics are closest Volynian Upland, refer intermediate «Chinese» type formation properties, with an admixture «Alaskan» mechanism. These characterized a low concentration ferrimagnetic...

10.24028/gzh.0203-3100.v43i1.2021.225539 article EN cc-by-nc-sa Geofizicheskiy Zhurnal 2021-03-13

Main principles of magnetostratigraphy, paleomagnetic method measurement and its applying in Quaternary stratigraphy have been set forth. Results Matuyama-Brunhes (M/B) boundary detection loess-soil sediments Ukraine other territories given the previous studies are presented. Attention has paid to contradictions determination M/B position episodes inverse polarity within Brunhes chron according data different authors. The situation is notably shown on Roxolany section West Black Sea region...

10.24028/gzh.0203-3100.v38i4.2016.107801 article EN cc-by Geofizicheskiy Zhurnal 2017-07-28
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