geology

The Apsheron field area presents the most promising prospect within the Shallow Water Transition Zone of the Apsheron archipelago across all potential reservoir levels. This assessment aims to identify the exploration potential of the area and the associated new business opportunities. The region encompasses water depths ranging from 10 to 20 meters. Methodologically, we utilized available new seismic data, evaluated reference well data, and considered other geological factors within the Petrel program.

The purpose of the work is to present widely to the scientific community and analyze in detail the structure and oil and gas bearing of the Bukovyna lithosphere (the eastern part of the Carpathian region of Ukraine) based on the unique data on the regional RWМ-CDP profile RP-5 and on the neighboring regional profiles with the involvement of other geological and geophysical data.

Purpose. Statistical information for the period from 2016 to 2021 was used to analyze seismic activity. Objective. The aim of the study is to identify the relationship between changes in water level and local seismic activity in the region. Using HPP and Psing filtering, the hypocenters of earthquakes within a radius of 30 km from the seismic station with the NDNU index were selected, and using geographic information technology tools, the hypocenters of earthquakes were compared with the geological structure of the region. Methodology.

Based on the analysis of archival sources, Julian Medvedski’s studies at the Przemysl German Gymnasium were studied. Despite successful training, the future Ukrainian professor took an active part in Ukrainian student life. The creation of the “Hromada” in Przemysl was the beginning of the dissemination of the ideas of the modern Ukrainian nation. The symbol of this is the cult of Taras Shevchenko.

The model of the geologic evolution of the Carpathians both in terms of the terrane analysis and in the light of the new data of the geologic mapping are represented.

Most of the ore deposits are located in the ore-magmatic systems, which are spatially and genetically connected with the ring structures. Studying of the geology and all available map materials allows to detect the type and background of different signs of deposit mineralization and to develop the criteria for exploration of mineral deposits.