A5074720127- Hydrocarbon exploration and reservoir analysis
- Geological Formations and Processes Exploration
- Geological Studies and Exploration
- Geology and Environmental Impact Studies
- Paleontology and Stratigraphy of Fossils
- Methane Hydrates and Related Phenomena
- Geochemistry and Geologic Mapping
- Petroleum Processing and Analysis
- Geology and Paleoclimatology Research
- Marine and environmental studies
- Reservoir Engineering and Simulation Methods
- Fossil Insects in Amber
- Mining and Industrial Processes
- Integrated Water Resources Management
- Geological and Geochemical Analysis
- Renewable energy and sustainable power systems
- Coleoptera Taxonomy and Distribution
- Coal Properties and Utilization
- Enhanced Oil Recovery Techniques
- Hydraulic Fracturing and Reservoir Analysis
- Coal and Coke Industries Research
- Plant Diversity and Evolution
- Polish Legal and Social Issues
- Biological Activity of Diterpenoids and Biflavonoids
- dental development and anomalies
AGH University of Krakow
2014-2024
University of Science and Technology
2023
Polish Geological Institute
2021
The distributions and concentrations of polycyclic aromatic hydrocarbons (PAHs) plant-derived biomarkers were analysed in Middle Jurassic strata from central Poland. These compounds abundant all samples indicating the occurrence specific palaeoflora families intensity palaeo-wildfires. Moreover, calculated fusinite reflectance values revealed that temperature wildfires may have exceeded 950 °C, consistent with high oxygen atmosphere during this period. content charred organic matter has an...
Palaeo-wildfires were a common phenomenon in the Earth history. Their products can influence on some biomarker indicators characterising palaeo-environment conditions. Selected plant-derived aromatic biomarkers and polycyclic hydrocarbons (PAHs) analysed Jurassic strata from Polish Basin, Mesozoic basement of Carpathian Foredeep Neogene Foredeep. Marked compounds recorded varied input palaeoflora families variable intensity palaeo-wildfires. Retene (Ret), cadalene (Cad),...
Organic-rich claystones and mudstones can be very good source rocks for hydrocarbons. Middle Jurassic organic-rich siliciclastic horizons are known from the Polish Basin area, however, there no hydrocarbon accumulations associated with these horizons. The main scientific goal of this paper is to propose why did not produce significant hydrocarbons quantities. To deal it, we characterised organic matter origin, maturity level, potential strata. Palaeoenvironmental conditions were also...
Fossil resins are the one of several fossil tree products, together with leaves, wood, seeds, or pollen. As an emanation organic matter, made compounds, predominantly terpenes. Terpenes broadly identified from various living organisms such as higher plants, fungi, bacteria. In resins, these compounds occur in forms – usually mono-, sesqui-, di-, and tri-terpenes. Some terpenes present provide information about their ancestors paleoenvironmental conditions during resin expulsion. These known...
Major hydrocarbon accumulations are located in western Ukraine within the Mesozoic‐Cenozoic flysch sequence frontal parts of External Carpathians, and adjacent autochthonous foreland. The occur three different structural settings: Carpathian belt; pre‐Neogene foreland autochthon; Miocene foredeep molasse. petroleum potential organic‐rich rocks belonging to a number sedimentary cycles tectonic units was studied by Rock‐Eval pyrolysis. Two significant units, both with basin‐scale distribution,...
Assessment of hydrocarbon potential Jurassic and Cretaceous source rocks in the Tarnogród-Stryi area (SE Poland W Ukraine) The Jurassic/Cretaceous stratigraphic complex forming a part sedimentary cover both eastern Małopolska Block adjacent Łysogóry-Radom Polish as well Rava Rus'ka Kokhanivka Zones Ukrainian basement Carpathian Foredeep were studied with geochemical methods order to evaluate possibility generation. In study area, Mesozoic strata characterized on basis analytical results 121...
The Lower Palaeozoic succession in SE Poland and West Ukraine has source rock potential, particularly the Ordovician Silurian which contain oil‐prone Type II kerogen. thermal maturity of these units ranges from early to late‐phase oil window (locally up gas window). Within Mesozoic succession, potential is highest Middle Jurassic TOC 26 wt% a genetic 39 mg/g rock, with organic matter dominated by gas‐prone III In Poland, this unit generally immature, whereas maturities are sufficient for...
The Ediacaran (Upper Neoproterozoic) succession in west and SW Ukraine Moldova rests on a Cryogenian or basement. is exposed at the surface along southern margin of Ukrainian Shield dips to towards Carpathian Overthrust; where burial depths are sufficient, it mature for oil gas generation. made up terrigenous siliciclastics ranging from conglomerates sandstones siltstones mudstones, includes shale interval (the Kalus Beds) which may have source rock potential. Organic matter shales...