gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2026-17-4-0906KGSDRJgtcrust-2353Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSРЕКОНСТРУКЦИЯ ИСТОЧНИКОВ СНОСА ЮРСКИХ ОТЛОЖЕНИЙ ПРЕДЪЕНИСЕЙСКОЙ ПЕРСПЕКТИВНОЙ НЕФТЕГАЗОНОСНОЙ ОБЛАСТИ ЗАПАДНО-СИБИРСКОЙ НЕФТЕГАЗОНОСНОЙ ПРОВИНЦИИRECONSTRUCTION OF PROVENANCE OF JURASSIC DEPOSITS IN THE PRE-YENISEY OIL AND GAS PROMISING AREA OF THE WEST SIBERIAN PETROLEUM PROVINCEШариповФ. А.SharipovE. A.

105118, Москва, ш. Энтузиастов, 36

36 Rte Entuziastov, Moscow 105118

sharipov@vnigni.ruСоловьевА. В.SolovievA. V.

105118, Москва, ш. Энтузиастов, 36; 119017, Москва, Пыжевский пер., 7, стр. 1

36 Rte Entuziastov, Moscow 105118; 7-1 Pyzhevsky Ln, Moscow 119017

КотлерП. Д.KotlerP. D.

420008, Казань, ул. Кремлевская, 18;  630090, Новосибирск, пр-т Академика Коптюга, 3

18 Kremlyovskaya St, Kazan 420008; 3 Academician Koptyug Ave, Novosibirsk 630090

КуликоваА. В.KulikovaA. V.

420008, Казань, ул. Кремлевская, 18;  630090, Новосибирск, пр-т Академика Коптюга, 3

18 Kremlyovskaya St, Kazan 420008; 3 Academician Koptyug Ave, Novosibirsk 630090

УхловаГ. Д.UkhlovaG. D.

105118, Москва, ш. Энтузиастов, 36

36 Rte Entuziastov, Moscow 105118

КирсановА. М.KirsanovA. M.

105118, Москва, ш. Энтузиастов, 36

36 Rte Entuziastov, Moscow 105118

МиннебаевК. Р.MinnebaevK. R.

420008, Казань, ул. Кремлевская, 18

18 Kremlyovskaya St, Kazan 420008

СаетгалееваЯ. Я.SaetgaleevaYa. Ya.

420008, Казань, ул. Кремлевская, 18

18 Kremlyovskaya St, Kazan 420008

Всероссийский научно-исследовательский геологический нефтяной институтРоссияAll-Russian Scientific Research Geological Oil InstituteRussian FederationВсероссийский научно-исследовательский геологический нефтяной институт; Геологический институт РАНРоссияAll-Russian Scientific Research Geological Oil Institute; Geological Institute, Russian Academy of SciencesRussian FederationКазанский (Приволжский) федеральный университет; Институт геологии и минералогии им. В.С. Соболева СО РАНРоссияKazan Federal University; Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesRussian FederationКазанский (Приволжский) федеральный университетРоссияKazan Federal UniversityRussian Federation202619082026174906906Copyright © Шарипов Ф.А., Соловьев А.В., Котлер П.Д., Куликова А.В., Ухлова Г.Д., Кирсанов А.М., Миннебаев К.Р., Саетгалеева Я.Я., 20262026Шарипов Ф.А., Соловьев А.В., Котлер П.Д., Куликова А.В., Ухлова Г.Д., Кирсанов А.М., Миннебаев К.Р., Саетгалеева Я.Я.Sharipov E.A., Soloviev A.V., Kotler P.D., Kulikova A.V., Ukhlova G.D., Kirsanov A.M., Minnebaev K.R., Saetgaleeva Y.Y.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/2353

В статье представлены результаты комплексного изучения терригенных пород урманской, пешковской, тюменской и максимоярской свит юрского возраста скважины Северо-Кетская 1 с целью палеогеографической реконструкции юго-восточной части Западно-Сибирской нефтегазоносной провинции. Петрографический анализ выявил две ассоциации песчаников: кварцевые граувакки и аркозовые песчаники раннесреднеюрского возраста и мезомиктовые породы позднеюрского возраста. Также по классификационной диаграмме «кварц – полевые шпаты – обломки пород» по мере омоложения рассматриваемых пород фиксируется уменьшение доли обломочного материала, образованного за счет разрушения эффузивных пород кислого состава, в сторону сноса материала, формирование которого связано с разрушением осадочных толщ кварцевого состава. Анализ минерального состава песчаников на диаграмме Дикинсона показывает эволюцию областей сноса терригенного материала с вулканических дуг в раннесреднеюрское время к рециклированным орогенам в позднеюрское время, обусловленную позднеюрско-раннемеловым орогенезом Колывань-Томской и Обь-Зайсанской складчатых систем. U-Pb датирование детритовых цирконов демонстрирует смену питающих провинций: от доминирующей роли местных раннепалеозойских источников в раннеюрское время к преобладанию удаленных верхнепалеозойских и юрских источников сноса в средне- и позднеюрское время. Эта эволюция связана с мезозойским внутриконтинентальным орогенезом юго-восточного обрамления Западно-Сибирского бассейна и южного обрамления Сибирской платформы, вызванным закрытием Палеотетиса и Монголо-Охотского океана. Установлено, что увеличение доли мезозойских и палеопротерозойских цирконов от ранней юры к поздней юре связано с усилением тектонических процессов в пределах южного обрамления Сибирской платформы, а транспортировка терригенного материала осуществлялась Пра-Ангарой. Комплексная интерпретация данных позволила реконструировать возможные источники сноса терригенного материала и уточнить палеогеографические схемы.

 

The paper presents the results for Jurassic terrigenous rocks of the Urman, Peshkov, Tyumen and Maksimoyar formations, encountered in Severo-Ketskaya 1 parametric well, that have been studied thoroughly to re­construct the paleogeographic evolution of the southeastern part of the West Siberian petroleum province. Petrographic analysis reveals two sandstone associations: quartz graywackes and arkosic sandstones of the Early – Middle Jurassic age and mesomictic sandstones of the Late Jurassic age. Plotting the samples on the Q–F–L (quartz – feldspar – lithic fragments) ternary diagram shows the upsection decrease in proportion of acidic volcanic clasts with increasing detritus removal from the eroded quartz-rich sediment. Detrital modes on the QFL Dickinson diagram indicate an evolution of teggigenous source areas from volcanic arc settings in the Early – Middle Jurassic to recycled orogens in the Late Jurassic, driven by the Late Jurassic – Early Cretaceous orogenic uplift within the Kolyvan-Tomsk and Ob-Zaisan fold belts. U-Pb dating of detrital zircons documents a provenance shift from predominantly local Early Paleozoic sources in the Early Jurassic to primarily distant Upper Paleozoic and Jurassic source areas in the Middle – Late Jurassic. This evolution re­flects the Mesozoic intracontinental orogeny along the southeastern margin of the West Siberian basin and the southern margin of the Siberian Platform, associated with the closure of the Paleo-Tethys and Mongol-Okhotsk oceans. The upsec­tion increase in Mesozoic and Paleoproterozoic zircon populations from Early to Late Jurassic is interpreted as a response to intensification of tectonic activity along the southern margin of the Siberian Platform, whereas the terrigenous material was transported in the Pra-Angara river system. The integrated dataset constrains the likely sediment source areas and improves paleogeographic reconstructions.

терригенные отложения юрыюго-восточная часть Западно-Сибирской нефтегазоносной провинцииПредъенисейская ПНГОреконструкции источников сносаU-Pb датирование цирконовмезозойский внутриконтинентальный орогенезюго-восточное обрамление Западно-Сибирского бассейнаюжное обрамление Сибирской платформыПра-Ангарапараметрическая скважина Северо-Кетская 1Jurassic clastic depositssoutheastern part of the West Siberian petroleum provincePre-Yenisey promisimg oil and gas areareconstruction of sediment provenanceU-Pb zircon datingMesozoic intracontinental orogenysoutheastern margin of the West Siberian basinsouthern margin of the Siberian PlatformPra-Angara river systemSevero-Ketskaya 1 parametric wellИсследование проведено в рамках работ по объекту ВНИГНИ («Параметрическое бу­рение на Северо-Кетской площади Предъенисейской провинции с целью выявления новых крупных зон нефте­газонакопления. Второй этап. Бурение до глубины 5200 м», 2022–2024 гг.), финансировавшихся Федеральным агентством по недропользованию и за счет средств Программы стратегического академического лидерства КФУ (ПРИОРИТЕТ-2030).The study was carried out as part of the project of the VNIGNI ("Parametric drilling in the Severo-Ketskaya area of the Pre-Yenisey province aimed at identifying new large oil and gas accumulation zones. Stage 2. Drilling to a depth of 5200 m", 2022–2024), and funded both by the Federal Agency for Mineral Resources and by the Priority 2030 Strategic Academic Leadership Program of the Kazan Federal University.ReferencesArzhannikova A.V., Demonterova E.I., Jolivet M., Arzhannikov S.G., Mikheeva E.M., Ivanov A.V., Khubanov V.B., Pavlova L.A., 2020. Late Mesozoic Topographic Evolution of Western Transbaikalia: Evidence for Rapid Geodynamic Changes from the Mongol-Okhotsk Collision to Widespread Rifting. 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The authors declare that there are no conflicts of interest present.