Crystalline Basement as a Possible Source of Hydrocarbons in the Republic of Tatarstan

Ulyana S. Guzaeva, Rinat R. Afiyatunov, Venera G. Bazarevskaya, Albert P. Safarov, Olga G. Gibadullina

Author details

Ulyana S. Guzaeva
TatNIPIneft R&D Institute of the PJSC TATNEFT named after V.D. Shashin, Almetyevsk, Russian Federation
Rinat R. Afiyatunov
PJSC TATNEFT named after V.D. Shashin, Almetyevsk, Russian Federation
Venera G. Bazarevskaya
TatNIPIneft R&D Institute of the PJSC TATNEFT named after V.D. Shashin, Almetyevsk, Russian Federation
Albert P. Safarov
TatNIPIneft R&D Institute of the PJSC TATNEFT named after V.D. Shashin, Almetyevsk, Russian Federation
Olga G. Gibadullina
TatNIPIneft R&D Institute of the PJSC TATNEFT named after V.D. Shashin, Almetyevsk, Russian Federation

https://doi.org/10.15593/2712-8008/2025.4.3

As is well known, the crystalline basement is the lower level (of both ancient and young platforms), composed of dislocated sedimentary, volcanic, metamorphic, and intrusive rocks. In this study, the basement and its weathering crust are examined from the perspective of natural reservoirs capable of accumulating and retaining hydrocarbons. It is noted that subduction-obduction and rifting geodynamic regimes provide the best geological conditions for the formation of zones of decompressed fractured rocks (granites, granite gneisses, schists, phyllites, etc.) and oil and gas accumulations. Based on data published in the scientific literature (both foreign and domestic) on the petroleum potential of crystalline basement rocks in foreign countries, the total oil and gas reserves contained in basement rocks and their weathering crust at developed international fields were calculated. A conceptual framework for the formation of hydrocarbon deposits in basement rocks was developed, with the aim of predicting promising zones within crystalline basement rocks in the Republic of Tatarstan. It was found that, in terms of the geological and tectonic structure of the basement, the Archean-Lower Proterozoic basement of the Northern Structural-Tectonic Zone of the Pripyat Trough and the northern edge of the Dnieper-Donets Aulagen can serve as an analogue for the republic's territory. Oil, gas, and condensate deposits have been identified within these territories. Based on the analyzed material on the study of crystalline basement rocks, promising directions for searching for possible hydrocarbon accumulations both in the basement body itself and in its weathering crust, as well as possible migration routes for hydrocarbons within the territory of the Republic of Tatarstan, have been identified.

Keywords

crystalline basementprotrusiongeodynamic regimemigrationfielddepositreservoirhydrocarbonsoil and gas potentialRepublic of Tatarstanforeign experiencegranitesdecompression zonetectonic faultfracturing

Кристаллический фундамент как возможный источник углеводородов в Республике Татарстан

Как известно, кристаллический фундамент является нижним этажом (как древних, так и молодых платформ), сложенным дислоцированными осадочными, вулканогенными, а также метаморфическими и интрузивными горными породами. В данном исследовании фундамент и его кора выветривания рассматриваются с позиции природных резервуаров, способных накапливать и удерживать углеводороды. Отмечается, что наилучшими геологическими условиями для формирования зон развития разуплотненных трещиноватых пород (гранитов, гранитогнейсов, сланцев, филлитов и др.) и нефтегазовых скоплений характеризуются субдукционно-обдукционный и рифтогенный геодинамические режимы. На основе данных, опубликованных в научной литературе (как зарубежной, так и отечественной) по нефтегазоносности пород кристаллического фундамента зарубежных стран, подсчитаны суммарные запасы нефти и газа, содержащиеся в породах фундамента и его коре выветривания на разрабатываемых зарубежных месторождениях, а также сформировано некое представление о формировании залежей углеводородов в породах фундамента с целью прогнозирования перспективных зон в породах кристаллического основания на территории Республики Татарстан. Выявлено, что по геологическому и тектоническому строению фундамента для территории Республики аналогом может служить архейско-инженнеторозсийский фундамент Северной структурно-тектонической зоны Припятского прогиба и северного борта Днепровско-Донецкого авалокагена. В пределах данных территорий выявлены залежи нефти, газа и конденсата. На основании проанализированного материала по изучению пород кристаллического фундамента определены перспективные направления для поиска возможных скоплений углеводородов как в самом теле фундамента, так и в его коре выветривания, а также возможные пути миграции углеводородов в пределах территории Республики Татарстан.

Ключевые слова

кристаллический фундаментвыступгеодинамический режиммиграцияместорождениезалежьколлекторуглеводородынефтегазоносностьРеспублика Татарстанзарубежный опытгранитызона разуплотнениятектонический разломтрещиноватость

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Article information

Published: 21 November 2025
Issue date: 21 November 2025
Issue: Vol. 25, No. 4 (2025)