gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2026-17-2-0880MXEZWDgtcrust-2239Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSРОЛЬ ГЕОДИНАМИЧЕСКИХ ПРОЦЕССОВ В ОБРАЗОВАНИИ МЕСТОРОЖДЕНИЙ АНГАРО-КОВЫКТИНСКОЙ ЗОНЫ НЕФТЕГАЗОНАКОПЛЕНИЯ (ВОСТОЧНАЯ СИБИРЬ)THE ROLE OF GEODYNAMIC PROCESSES IN THE FORMATION OF DEPOSITS IN THE ANGARA-KOVYKTA OIL AND GAS ACCUMULATION ZONE (EASTERN SIBERIA)https://orcid.org/0000-0001-7227-8253ГладкочубД. П.GladkochubD. P.

664033, Иркутск, ул. Лермонтова, 128 

128 Lermontov St, Irkutsk 664033 

dima@crust.irk.ruhttps://orcid.org/0000-0003-1141-0518ДонскаяТ. В.DonskayaT. V.

664033, Иркутск, ул. Лермонтова, 128 

128 Lermontov St, Irkutsk 664033 

Институт земной коры СО РАНРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of SciencesRussian Federation202617042026172880880Copyright © Гладкочуб Д.П., Донская Т.В., 20262026Гладкочуб Д.П., Донская Т.В.Gladkochub D.P., Donskaya T.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/2239

Проведен анализ современных данных о геодинамической эволюции южного фланга Сибирской платформы в неопротерозое – раннем палеозое с целью выявления возможного времени и места формирования углеводородов в осадочных бассейнах и их дальнейшей миграции из очагов нефтегазообразования в зоны их накопления, а именно в осадочные отложения чорской свиты мотской серии венда (парфеновский продуктивный горизонт). Условия для накопления углеводородов могли возникнуть в осадочных бассейнах пассивной окраины Сибирского кратона, сформированных в неопротерозое (710–650 млн лет назад) после распада суперконтинента Родиния, отделения Сибири от этого суперконтинента и раскрытия Палеоазиатского океана, а также в периферическом форландовом бассейне, образованном после трансформации этой пассивной окраины на временном рубеже около 610 млн лет. В прибайкальской части Сибирской платформы накопление углеводородсодержащих отложений могло иметь место в породах улунтуйской и качергатской свит байкальской серии, сформированных в бассейне пассивной континентальной окраины и форландовом бассейне соответственно. В результате крупномасштабных позднекембрийских ‒ ордовикских аккреционно-коллизионных событий, фиксирующих становление Центрально-Азиатского складчатого пояса, углеводороды мигрировали в западном направлении из вендских отложений улунтуйской и качергатской свит в отложения чорской свиты мотской серии, сформировав месторождения Ангаро-Ковыктинской зоны нефтегазонакопления (Ангаро-Ленская нефтегазоносная область). Принимая во внимание тот факт, что к отложениям пассивных окраин и форландовых бассейнов приурочено свыше 90 % мировых запасов углеводородов, вполне допустимо, что предлагаемая гипотеза может объяснить природу происхождения углеводородов, их миграции и накопления в месторождениях Ангаро-Ленской нефтегазоностной области. Последующие процессы, существенно повлиявшие на перераспределение углеводородов уже в пределах этой нефтегазоносной области, были обусловлены неотектонической активизацией, способствовавшей формированию месторождений Ангаро-Ковыктинской зоны нефтегазонакопления.

The analysis has been made on the modern data about the Neoproterozoic – Early Paleozoic geodynamic evolution of the southern flank of the Siberian Platform in order to identify the probable time and place of formation of hydrocarbons in sedimentary basins and their further migration from the foci of oil and gas formation to the zones of their accumulation, namely to the sedimentary deposits of the Chora formation of the Vendian Moty group (productive Parfenovo horizon). The conditions for the accumulation of hydrocarbons could arise in sedimentary basins of the passive margin of the Siberian craton, formed in the Neoproterozoic (710–650 Ma) after the breakup of the supercontinent Rodinia, separation of the Siberian craton therefrom and opening of the Paleoasian Ocean, as well as in the peripheral foreland basin, formed after the transformation of this passive margin at about 610 Ma ago. In the Baikal part of the Siberian Platform, the accumulation of hydrocarbon-containing sediments could occur in the rocks of the Uluntuy and Kachergat formations of the Baikal group, formed in the basin of the passive continental margin and the foreland basin, respectively. As a result of the large-scale Late Cambrian-Ordovician accretion-collision events that mark the formation of the Central Asian Orogenic Belt, hydrocarbons migrated westward from the Vendian deposits of the Uluntuy and Kachergat formations to the sedimentary sequences of the Chora formation of the Moty group, having formed the deposits of the Angara-Kovykta oil and gas accumulation zone (Angara-Lena oil and gas bearing region). Since over 90 % of the world hydrocarbon reserves are confined to sedimentary sequences of passive margins and foreland basins, it can be assumed that the proposed hypothesis may explain the nature of the origin of hydrocarbons, their migration, and accumulation in the deposits of the Angara-Lena oil and gas region. Subsequent processes, which significantly affected the redistribution of hydrocarbons specifically within this oil and gas region, were caused by neotectonic activation, which contributed to the formation of deposits in the Angara-Kovykta oil and gas accumulation zone.

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The authors declare that there are no conflicts of interest present.