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The purpose of the work is to determine the position of the carbonate zone and the location of the source rocks in the upper Paleozoic section at the transit zone between offshore and onshore parts of the Timan-Pechora oil and gas province. This research is based on the modeling of processes of formation of the domanik-tournaisian carbonate complex. The work was done for the purpose of clarification and verification of paleogeographic models and forecast of oil and gas potential of the study area. Regarding to the previous paleo-reconstruction study and results of seismic interpretation the reef system may have submeridional and sublatitudinal orientations. According to results of the modeling the most reasonable system of domanik-syracusecoe barrier reef is sublatitudinal. Which turned out to be the most consistent on most parameters. The resulting sediment zonation allowed us to localize the zone of distribution of the reefs. In frontreef area within synclines were determined several positive structures with different relief. The arches of these structures might represent different types of single reefs. The result of this study shows different deposition type in the Pomorskiy val area. The deposits are representing the single reef in backreef zone, but according to the earlier study it was determined as continuation of the barrier reef. As a result, the paleo-facies map for the frasnian age was corrected and detailed.

proceedings

Generation Potential and the Coverage Area of Domanik Formation in the Northern Part of the Timan-Pechora Province Based on Geochemical Studies and Depositional Modelling