Abstract

The Timan–Pechora oil and gas province (TPP), despite the good geological and geophysical knowledge of its central and southern regions, remains poorly studied in the extreme northwestern part within the north of the Izhma–Pechora depression and the Malozemelsk–Kolguev monocline, and in the extreme northeast within the Predpaikhoisky depression. Assessing the oil and gas potential of the Lower Paleozoic part of the section is urgently required in the northwestern part of the TPP, the productivity of which has been proven at the border and in the more eastern regions of the province (Pechora–Kolva, Khoreyverskaya, Varandei–Adzva regions), that have been evaluated ambiguously. A comprehensive interpretation of the seismic exploration of regional works was carried out, with the wells significantly clarifying the structural basis and the boundaries of the distribution of the main seismic facies’ complexes. The capabilities of potentially oil- and gas-producing strata in the Silurian–Lower Devonian were studied. An analysis of migration routes in transit strata used for basin modeling in order to reconstruct the conditions of oil and gas formation that are common in the land and water areas of the Arctic zone of the TPP was carried out. Modeling allowed us to reach an understanding of the formation of large zones with possible accumulations of hydrocarbons, including the time at which the formation occurred and under what conditions, to establish space–time links with possible centers of generation to identify migration directions and, based on a comparison with periods of intensive generation of hydrocarbons both directly located within the work area and beyond (noting the possible migration), to identify zones of the paleoaccumulation of hydrocarbons. The body of existing literature on the subject made it possible to outline promising oil and gas accumulation zones, with the allocation of target objects for further exploration in the Lower Paleozoic part of the section.

Highlights

  • More than 5500 deep oil and gas wells with a drilling volume of 10 million meters have been drilled within the Timan–Pechora sedimentary basin (TP SB)

  • 54 wells have been drilled in the water area of the sedimentary basin, most of which have only exposed Mesozoic deposits

  • With regards to the water area, the southern parts of the Kara and Barents Seas have the greatest potential, which are where all the deposits identified on the Arctic shelf and, the oil, gas, and condensate reserves are located

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Summary

Introduction

More than 5500 deep oil and gas wells with a drilling volume of 10 million meters have been drilled within the Timan–Pechora sedimentary basin (TP SB). 2. In the been studied to a much extent—the drilling depth onlyis m/km water the eastern half of Kolguev Island (East Kolguev structural zone), the drilling density is area on the eastern half of Kolguev. A promising direction for further study in of the the Ordovician region is the study of the lying storage res- under the reservoir and flow behavior shale formation directly. Silurian oil source clayshale strata, which is a lying high-quality impermeable ervoir and flow behavior in and the gas Ordovician formation directly under thelayer. Studies capacity and flow behavior in the shale formation, have been carried out by the Journal of of the capacity of similar shale strata, from the point of view of the possibility of CO2. Storage capacity and flow behavior in the shale formation, have been carried out by the Journal of Petroleum Science and Technology 2022 [Error! A detailed geological study and the industrial development of Resources 2022, 11, 3

The Economic Significance of the Resource Development of the Hydrocarbon
Materials and Methods
Source Material
Prospects of Oil and In
Malozemelsko–Kolguevskaya and
Development of the Structural Frame
Cambrian-Lower-Middle Ordovician Terrigenous Complex
Middle Ordovician-Lower Devonian Terrigenous-Carbonate OGC
Seismogeological
Natural
Natural Reservoirs of the Silurian Carbonate Subcomplex
Natural Reservoirs of the Lower Devonian Carbonate-Terrigenous Subcomplex
Basin Modeling
Findings
Conclusions

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