ASGP (2012), vol. 82: 65-80
ASSESSMENT OF HYDROCARBON POTENTIAL OF THE LOWER PALAEOZOIC STRATA IN THE TARNOGRÓD–STRYI AREA (SE POLAND AND WESTERN UKRAINE)
Dariusz WIĘCŁAW(1), Paweł KOSAKOWSKI(1), Maciej J. KOTARBA(1), Yuriy V. KOLTUN(2) & Adam KOWALSKI(1)
1) AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, Al. Mickiewicza 30, 30-059 Kraków, Poland, e-mail: wieclaw at agh.edu.pl
2) National Academy of Sciences of Ukraine, Institute of Geology and Geochemistry of Combustible Minerals, 3a Naukova Street, 79053 Lviv, Ukraine
Więcław, D., Kosakowski, P., Kotarba, M. J., Koltun, Y. V. & Kowalski, A., 2012. Assessment of hydrocarbon potential of the Lower Palaeozoic strata in the Tarnogród–Stryi area (SE Poland and western Ukraine). Annales Societatis Geologorum Poloniae, 82: 65–80.
Abstract: Quantity, genetic type and maturity of organic matter dispersed in the Lower Palaeozoic sequence from the Lower Cambrian to Silurian strata of the Polish and Ukrainian parts of the Carpathian Foredeep basement in the Tarnogród–Stryi area were evaluated based on the results of geochemical analyses of 475 rock samples collected from 45 wells. The best source rocks were found in the Silurian strata where the present total organic carbon (TOC) content is up to 2.6 wt%. They occur in the vicinity of Wola Obszańska, where the median of the present and the initial total organic carbon (TOC) contents in the individual wells amount to 0.98 and 1.6 wt%, respectively. The Cambrian and Ordovician strata have a poorer hydrocarbon potential and their present TOC content never exceeds 1 wt%. In all of the investigated Lower Palaeozoic strata, organic matter is represented by the oil-prone Type-II kerogen deposited in anoxic or sub-oxic conditions. The maturity of source rocks ranges from early mature (the initial phase of the low-temperature thermogenic processes) in selected zones of the Silurian strata in the vicinity of Wola Obszańska, through the middle and the final phase of “oil window” in the Ordovician and Cambrian strata in the Polish part of the study area, to the overmature stage in the Ordovician strata in the south-eastern part of the study area (Ukraine).
