gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2025-16-1-0808fsaxaogtcrust-1984Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSОБЛОМОЧНЫЕ ЦИРКОНЫ В ДОКЕМБРИЙСКИХ ОТЛОЖЕНИЯХ ИГАРСКОГО ПОДНЯТИЯ (СЕВЕРО-ЗАПАД СИБИРСКОЙ ПЛАТФОРМЫ)DETRITAL ZIRCONS FROM THE PRECAMBRIAN OF THE IGARKA UPLIFT (NORTHWESTERN SIBERIAN PLATFORM)КочневБ. Б.KochnevB. B.

630090, Новосибирск, пр-т Академика Коптюга, 3; 119017, Москва, Пыжевский пер., 7, стр. 1, 

3 Academician Koptyug Ave, Novosibirsk 630090; 7-1 Pyzhevsky Ln, Moscow 119017

СеменоваД. В.SemenovaD. V.

630090, Новосибирск, пр-т Академика Коптюга, 3

3 Academician Koptyug Ave, Novosibirsk 630090

ХубановВ. Б.KhubanovV. B.

123242, Москва, ул. Большая Грузинская, 10, стр. 1

10-1 Bolshaya Gruzinskaya St, Moscow 123242

ДанукаловаМ. К.DanukalovaM. K.

119017, Москва, Пыжевский пер., 7, стр. 1

7-1 Pyzhevsky Ln, Moscow 119017

МарусинВ. В.MarusinV. V.

630090, Новосибирск, пр-т Академика Коптюга, 3: 630090, Новосибирск, ул. Пирогова, 1

3 Academician Koptyug Ave, Novosibirsk 630090; 1 Pirogov St, Novosibirsk 630090

ХудолейА. К.KhudoleyA. K.

199034, Санкт-Петербург, наб. Университетская, 7-9

7-9 Universitetskaya Emb, Saint Petersburg 

Институт нефтегазовой геологии и геофизики им. А.А. Трофимука СО РАН; Геологический институт РАНРоссияTrofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences; Geological Institute, Russian Academy of SciencesRussian FederationИнститут геологии и минералогии им. В.С. Соболева СО РАНРоссияSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesRussian FederationИнститут физики Земли им. О.Ю. Шмидта РАНРоссияSchmidt Institute of Physics of the Earth, Russian Academy of SciencesRussian FederationГеологический институт РАНРоссияGeological Institute, Russian Academy of SciencesRussian FederationИнститут нефтегазовой геологии и геофизики им. А.А. Трофимука СО РАН; Новосибирский государственный университетРоссияTrofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences; Novosibirsk State UniversityRussian FederationСанкт-Петербургский государственный университетRussian FederationSaint Petersburg UniversityRussian Federation202519022025161808808Copyright © Кочнев Б.Б., Семенова Д.В., Хубанов В.Б., Данукалова М.К., Марусин В.В., Худолей А.К., 20252025Кочнев Б.Б., Семенова Д.В., Хубанов В.Б., Данукалова М.К., Марусин В.В., Худолей А.К.Kochnev B.B., Semenova D.V., Khubanov V.B., Danukalova M.K., Marusin V.V., Khudoley A.K.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/1984

Для докембрийских обломочных пород Игарского поднятия (северо-запад Сибирской платформы) методом LA-ICP-MS геохронологически изучены зерна обломочного циркона c восьми стратиграфических уровней неопротерозоя (верхний рифей и венд). В возрастных спектрах присутствуют мезо- и неоархейские (3100–2600 млн лет), палеопротерозойские (2100–1700 млн лет) и неопротерозойские (1000–600 млн лет) датировки, однако их распределение коренным образом отличается от образца к образцу. Зерна циркона с неопротерозойскими датировками, связанные с источником сноса в гипотетическом орогене во внешнем обрамлении Сибирского кратона, преобладают в отложениях континентального и переходного генезиса, которые формировались при низком стоянии уровня моря (губинская свита, базальные слои чернореченской, излучинская свита). В то же время в отложениях различного возраста, сформированных в морских обстановках (безымянская, лудовская, корабликовская и сухарихинская свиты), доминируют зерна циркона, связанные с продуктами эрозии кристаллического фундамента Сибирского кратона. В телах базитов, согласно залегающих в губинской свите верхнего рифея (криогений), продатированы зерна циркона, образующие конкордантный кластер с возрастом 835±4 млн лет, что противоречит максимальному возрасту осадконакопления вмещающих песчаников 716±10 млн лет и, предположительно, связано с захватом цирконов из более древнего магматического источника неясной природы.

 

Herein we report the results of LA-ICP-MS dating of detrital zircons from eight stratigraphic levels of the Proterozoic section of the Igarka uplift (northwestern Siberian Platform). The age spectra include the Meso- and Neoarchean (3100–2600 Ma), Paleoproterozoic (2100–1700 Ma) and Neoproterozoic (1000–600 Ma) ages. However, the age distribution drastically varies among the samples. The Neoproterozoic zircons, associated with the hypothetic orogenic belt at the platform periphery, dominate in the lowstand system-tract continental and marginal marine strata (Gubinskaya, basal Chernaya Rechka, and Izluchina formations). In contrast, the zircons in the Riphean and Vendian marine strata (Bezymyanny, Ludy, Korablik, and Sukharikha formations) mostly originate from erosion of the crystalline basement of the Siberian Platform. The concordant mafic bodies in the Upper Riphean (Criogenian) Gubinskaya formation contain the concordant cluster of zircons of 835±4 Ma. It contradicts with the maximum deposition age of 716±10 Ma of the host strata, hence the zircons in the mafic bodies supposedly comprise xenocrysts.

 

вендэдиакарийрифейнеопротерозойLA-ICP-MS геохронология обломочного цирконаИгарское поднятиеСибирская платформаVendianEdiacaranRipheanNeoproterozoicLA-ICP-MS detrital zircon geochronologyIgarka upliftSiberian PlatformОбобщение данных, подготовка рукописи и геохронологические исследования зерен обломочного циркона из трех образцов проведены при поддержке РНФ, грант № 22-77-10096. Содержание работы соответствует тематике проекта НИР FWZZ-2022-0002.Conceptualization, manuscript preparation and geochronological study of three samples were supported by Russian Science Foundation, grant 22-77-10096. The content of the work corresponds to research project FWZZ-2022-0002.ReferencesCzamanske G.K., Wooden J.L., Walker R.J., Fedorenko V.A., Simonov O.N., Budahn J.R., Siems D.F., 2000. Geochemical, Isotopic, and SHRIMP Age Data for Precambrian Basement Rocks, Permian Volcanic Rocks, and Sedimentary Host Rocks to the Ore-Bearing Intrusions, Noril’sk-Talnakh District, Siberian Russia. International Geology Review 42 (10), 895–927. https://doi.org/10.1080/00206810009465117.Czamanske G.K., Wooden J.L., Walker R.J., Fedorenko V.A., Simonov O.N., Budahn J.R., Siems D.F., 2000. Geochemical, Isotopic, and SHRIMP Age Data for Precambrian Basement Rocks, Permian Volcanic Rocks, and Sedimentary Host Rocks to the Ore-Bearing Intrusions, Noril’sk-Talnakh District, Siberian Russia. International Geology Review 42 (10), 895–927. https://doi.org/10.1080/00206810009465117.Геологическая карта СССР. Серия Тунгусская. Масштаб 1:200000. Лист Q-45-III, IV: Объяснительная записка. М.: ВСЕГЕИ, 1984. 99 с.Geological Map of the USSR, 1984. Tunguska Series. Scale of 1:200000. Sheet Q-45-III, IV. Explanatory Note. VSEGEI, Moscow, 99 p. (in Russian).Gladkochub D.P., Donskaya T.V., Stanevich A.M., Pisarevsky S.A., Zhang S., Motova Z.L., Mazukabzov A.M., Li H., 2019. U-Pb Detrital Zircon Geochronology and Provenance of Neoproterozoic Sedimentary Rocks in Southern Siberia: New Insights Into Breakup of Rodinia and Opening of Paleo-Asian Ocean. Gondwana Research 65, 1–16. https://doi.org/10.1016/j.gr.2018.07.007.Gladkochub D.P., Donskaya T.V., Stanevich A.M., Pisarevsky S.A., Zhang S., Motova Z.L., Mazukabzov A.M., Li H., 2019. U-Pb Detrital Zircon Geochronology and Provenance of Neoproterozoic Sedimentary Rocks in Southern Siberia: New Insights Into Breakup of Rodinia and Opening of Paleo-Asian Ocean. Gondwana Research 65, 1–16. https://doi.org/10.1016/j.gr.2018.07.007.Gladkochub D.P., Mazukabzov A.M., Stanevich A.M., Donskaya T.V., Motova Z.L., Vanin V.A., 2014. Precambrian Sedimentation in the Urik-Iya Graben, Southern Siberian Craton: Main Stages and Tectonic Settings. Geotectonics 48, 359–370. https://doi.org/10.1134/S0016852114050033.Gladkochub D.P., Mazukabzov A.M., Stanevich A.M., Donskaya T.V., Motova Z.L., Vanin V.A., 2014. Precambrian Sedimentation in the Urik-Iya Graben, Southern Siberian Craton: Main Stages and Tectonic Settings. Geotectonics 48, 359–370. https://doi.org/10.1134/S0016852114050033.Gladkochub D.P., Motova Z.L., Donskaya T.V., Khubanov V.B., Sizov A.V., 2022. Cambrian/Ordovician Boundary as a Milestone in the Sedimentation History of the Southern Siberian Craton: Evidence from U-Pb Dating of Detrital Zircons. Journal of Asian Earth Sciences: X 8, 100107. https://doi.org/10.1016/j.jaesx.2022.100107.Gladkochub D.P., Motova Z.L., Donskaya T.V., Khubanov V.B., Sizov A.V., 2022. Cambrian/Ordovician Boundary as a Milestone in the Sedimentation History of the Southern Siberian Craton: Evidence from U-Pb Dating of Detrital Zircons. Journal of Asian Earth Sciences: X 8, 100107. https://doi.org/10.1016/j.jaesx.2022.100107.Gladkochub D.P., Stanevich A.M., Mazukabzov A.M., Donskaya T.V., Pisarevsky S.A., Nicoll G., Motova Z.L., Kornilova T.A., 2013. Early Evolution of the Paleoasian Ocean: LA-ISP-MS Dating of Detrital Zircons from Late Precambrian Sequences of the Southern Margin of the Siberian Craton. Russian Geology and Geophysics 54 (10), 1150–1163. https://doi.org/10.1016/j.rgg.2013.09.002.Gladkochub D.P., Stanevich A.M., Mazukabzov A.M., Donskaya T.V., Pisarevsky S.A., Nicoll G., Motova Z.L., Kornilova T.A., 2013. Early Evolution of the Paleoasian Ocean: LA-ISP-MS Dating of Detrital Zircons from Late Precambrian Sequences of the Southern Margin of the Siberian Craton. Russian Geology and Geophysics 54 (10), 1150–1163. https://doi.org/10.1016/j.rgg.2013.09.002.Griffin W.L., Powell W.J., Pearson N.J., O’Reilly S.Y., 2008. GLITTER: Data Reduction Software for Laser Ablation ICPMS. In: P.J. Sylvester (Ed.), Laser Ablation ICP-MS in the Earth Sciences: Current Practices and Outstanding Issues. Mineralogical Association of Canada Short Course Series. Vol. 40. Vancouver, Canada, p. 308–311.Griffin W.L., Powell W.J., Pearson N.J., O’Reilly S.Y., 2008. GLITTER: Data Reduction Software for Laser Ablation ICPMS. In: P.J. Sylvester (Ed.), Laser Ablation ICP-MS in the Earth Sciences: Current Practices and Outstanding Issues. Mineralogical Association of Canada Short Course Series. Vol. 40. Vancouver, Canada, p. 308–311.Khubanov V.B., Buyantuev M.D., Tsygankov A.A., 2016. U-Pb Dating of Zircons from PZ3–MZ Igneous Complexes of Transbaikalia by Sector-Field Mass Spectrometry with Laser Sampling: Technique and Comparison with SHRIMP. Russian Geology and Geophysics 57 (1), 190–205. https://doi.org/10.1016/j.rgg.2016.01.013.Khubanov V.B., Buyantuev M.D., Tsygankov A.A., 2016. U-Pb Dating of Zircons from PZ3–MZ Igneous Complexes of Transbaikalia by Sector-Field Mass Spectrometry with Laser Sampling: Technique and Comparison with SHRIMP. Russian Geology and Geophysics 57 (1), 190–205. https://doi.org/10.1016/j.rgg.2016.01.013.Khudoley A., Chamberlain K., Ershova V., Sears J., Prokopiev A., MacLean J., Kazakova G., Malyshev S. et al., 2015. Proterozoic Supercontinental Restorations: Constraints from Provenance Studies of Mesoproterozoic to Cambrian Clastic Rocks, Eastern Siberian Craton. Precambrian Research 259, 78–94. https://doi.org/10.1016/j.precamres.2014.10.003.Khudoley A., Chamberlain K., Ershova V., Sears J., Prokopiev A., MacLean J., Kazakova G., Malyshev S. et al., 2015. Proterozoic Supercontinental Restorations: Constraints from Provenance Studies of Mesoproterozoic to Cambrian Clastic Rocks, Eastern Siberian Craton. Precambrian Research 259, 78–94. https://doi.org/10.1016/j.precamres.2014.10.003.Kochnev B.B., Khudoley A.K., Priyatkina N.S., Dufrane S.A., Pokrovsky B.G., Kuznetsov A.B., Kaurova O.K., Marusin V.V., 2022. Neoproterozoic Evolution of the Northwestern Margin of the Siberian Platform. Precambrian Research 382, 106877. https://doi.org/10.1016/j.precamres.2022.106877.Kochnev B.B., Khudoley A.K., Priyatkina N.S., Dufrane S.A., Pokrovsky B.G., Kuznetsov A.B., Kaurova O.K., Marusin V.V., 2022. Neoproterozoic Evolution of the Northwestern Margin of the Siberian Platform. Precambrian Research 382, 106877. https://doi.org/10.1016/j.precamres.2022.106877.Kochnev B.B., Pokrovsky B.G., Kuznetsov A.B., Marusin V.V., Kaurova O.K., Bykova N.V., Ivanova N.A., 2023. Early Ediacaran Positive C-Isotope Anomaly in Limestones of the Chernaya Rechka Formation, Igarka Uplift (Northwestern Siberian Platform). Lithology and Mineral Resources 58, 235–257. https://doi.org/10.1134/S0024490223700086.Kochnev B.B., Pokrovsky B.G., Kuznetsov A.B., Marusin V.V., Kaurova O.K., Bykova N.V., Ivanova N.A., 2023. Early Ediacaran Positive C-Isotope Anomaly in Limestones of the Chernaya Rechka Formation, Igarka Uplift (Northwestern Siberian Platform). Lithology and Mineral Resources 58, 235–257. https://doi.org/10.1134/S0024490223700086.Kouchinsky A.V., Bengston S., Pavlov V., Runnegar B., Torssander P., Young E., Ziegler K., 2007. Carbon Isotope Stratigraphy of the Precambrian-Cambrian Sukharikha River Section, Northwestern Siberian Platform. Geological Magazine 144 (4), 609–618. https://doi.org/10.1017/S0016756807003354.Kouchinsky A.V., Bengston S., Pavlov V., Runnegar B., Torssander P., Young E., Ziegler K., 2007. Carbon Isotope Stratigraphy of the Precambrian-Cambrian Sukharikha River Section, Northwestern Siberian Platform. Geological Magazine 144 (4), 609–618. https://doi.org/10.1017/S0016756807003354.Козлов Г.В., Александров В.С., Аксенова Л.А., Малахов В.П., Чунихина Л.Е. Опорные разрезы верхнедокембрийских осадочных и вулканогенно-осадочных толщ северо-запада Сибирской платформы. Т. 1: Медвежьинская и чернореченская свиты. Новосибирск: СНИИГГиМС, 1992. 123 с.Kozlov G.V., Aleksandrov V.S., Aksenova L.A., Malakhov V.P., Chunikhina L.E., 1992a. Reference Sections of Upper Precambrian Sedimentary and Volcanogenic-Sedimentary Sequences in the Northwest of the Siberian Platform. Vol. 1: Medvezhniskaya and Chernorechenskaya Formations. SNIIGGiMS, Novosibirsk, 123 p. (in Russian).Козлов Г.В., Александров В.С., Аксенова Л.А., Малахов В.П., Чунихина Л.Е. Опорные разрезы верхнедокембрийских осадочных и вулканогенно-осадочных толщ северо-запада Сибирской платформы. Т. 2: Лудовская, малиновосланцевая, ключа Спилитового (Ржевского), медвежьеостровная толщи, рудноручейная и гравийская свиты. Новосибирск: СНИИГГиМС, 1992. 99 с.Kozlov G.V., Aleksandrov V.S., Aksenova L.A., Malakhov V.P., Chunikhina L.E., 1992b. Reference Sections of Upper Precambrian Sedimentary and Volcanogenic-Sedimentary Stages in the Northwest of the Siberian Platform. Vol. 2: Ludovskaya, Malinovoslantsevaya, Kluch Spilitovogo (Rzhevskogo), Medvezheostrovnaya Stages, Rudnorucheynaya and Graviyevskaya Formations. SNIIGGiMS, Novosibirsk, 99 p. (in Russian).Kuptsova A.V., Khudoley A.K., Davis W., Rainbird R.H., Molchanov A.V., 2015. Results of the U-Pb Age of the Detrital Zircons from the Upper Proterozoic Deposits of the Eastern Slope of the Anabar Uplift. Stratigraphy and Geological Correlation 23 (3), 246–261. https://doi.org/S0869593815030053.Kuptsova A.V., Khudoley A.K., Davis W., Rainbird R.H., Molchanov A.V., 2015. Results of the U-Pb Age of the Detrital Zircons from the Upper Proterozoic Deposits of the Eastern Slope of the Anabar Uplift. Stratigraphy and Geological Correlation 23 (3), 246–261. https://doi.org/S0869593815030053.Кузьмичев А.Б., Данукалова М.К. Центрально-Таймырский складчатый пояс в докембрии: пассивная окраина Сибирского палеоконтинента в мезопротерозое, активная окраина в неопротерозое // Проблемы тектоники и геодинамики земной коры и мантии: Материалы L Тектонического совещания (30 января – 3 февраля 2018 г.). М.: ГЕОС, 2018. Т. 1. С. 352–356.Kuzmichev A.B., Danukalova M.K., 2018. The Central Taimyr Fold Belt in the Precambrian: Passive Margin of the Siberian Paleocontinent in the Mesoproterozoic and Active Margin in the Neoproterozoic. In: Problems of Tectonics and Geodynamics of the Earth’s Crust and Mantle. Proceedings of L Tectonic Meeting (January 30 – February 3, 2018). Vol. 1. GEOS, Moscow, p. 352–356 (in Russian).Кузьмичев А.Б., Данукалова М.К. Референсный Гаревский гранитный плутон Енисейского кряжа (Западное обрамление Сибирского кратона): финальная попытка воспроизвести палеопротерозойские Pb/U изотопные датировки М.И. Волобуева // Геодинамика и тектонофизика. 2024. Т. 15. № 2. 0746. https://doi.org/10.5800/GT-2024-15-2-0746.Kuzmichev A.B., Danukalova M.K., 2024. The Reference Garevka Granite (Yenisei Ridge, Western Frame of the Siberian Craton): The Final Attempt to Verify Paleoproterozoic Pb/U Isotopic Age by M.I. Volobuev. Geodynamics & Tectonophysics 15 (2), 0746 (in Russian). https://doi.org/10.5800/GT-2024-15-2-0746.Кузьмичев А.Б., Данукалова М.К., Бабицкий Е.Ф., Брянский Н.В., Дубенский А.С., Хубанов В.Б. Тектоностратиграфия неопротерозоя северной части Киселихинского террейна (Енисейский кряж), фрагмента активной окраины Сибирского палеоконтинента // Стратиграфия. Геологическая корреляция. 2025 (в печати).Kuzmichev A.B., Danukalova M.K., Babitsky E.F., Bryansky N.V., Dubensky A.S., Khubanov V.B., 2025 (in press). Neoproterozoic Tectonostratigraphy of the Northern Part of the Kiselikhinsky Terrane (Yenisei Ridge), a Fragment of the Active Margin of the Siberian Paleocontinent. Stratigraphy and Geological Correlation (in Russian).Кузьмичев А.Б., Данукалова М.К., Бабицкий Е.Ф., Сомсикова А.В., Хубанов В.Б., Брянский Н.В., Дубенский А.С. Поиски террейна, столкнувшегося с Енисейской окраиной Сибирского палеоконтинента в конце неопротерозоя. 1. Состав, возраст и геодинамическая позиция «островодужного» Порожнинского гранитного комплекса на СЗ окраине Енисейского кряжа // Геодинамическая эволюция литосферы Центрально-Азиатского подвижного пояса (от океана к континенту): Материалы научной конференции (18–21 октября 2022 г.). Иркутск: ИЗК СО РАН, 2022. Вып. 20. С. 158–160.Kuzmichev A.B., Danukalova M.K., Babitsky E.F., Somsikova A.V., Khubanov V.B., Bryansky N.V., Dubensky A.S., 2022. Search for a Terrane That Collided with the Yenisei Margin of the Siberian Paleocontinent at the End of the Neoproterozoic. 1. Composition, Age, and Geodynamic Position of the "Island-Arc" Porozhninsky Granite Complex on the NW Margin of the Yenisei Ridge. In: Geodynamic Evolution of the Lithosphere of the Central Asian Mobile Belt (from Ocean to Continent). Proceedings of Scientific Conference (October 18–21, 2022). Iss. 20. IEC SB RAS, Irkutsk, p. 158–160 (in Russian).Kuzmichev A.B., Sklyarov E.V., 2016. The Precambrian of Transangaria, Yenisei Ridge (Siberia): Neoproterozoic Microcontinent, Grenville-Age Orogen, or Reworked Margin of the Siberian Craton? Journal of Asian Earth Sciences 115, 419–441. https://doi.org/10.1016/j.jseaes.2015.10.017.Kuzmichev A.B., Sklyarov E.V., 2016. The Precambrian of Transangaria, Yenisei Ridge (Siberia): Neoproterozoic Microcontinent, Grenville-Age Orogen, or Reworked Margin of the Siberian Craton? Journal of Asian Earth Sciences 115, 419–441. https://doi.org/10.1016/j.jseaes.2015.10.017.Kuzmichev A.B., Storozhenko A.A., Danukalova M.K., Khubanov V.B., Dubensky A.S., 2023. The First Detrital Zircon Data on the Northwestern Precambrian Yenisei Ridge: Identification of the Continental-Arc Kiselikha Terrane. Stratigraphy and Geological Correlation 31, 507–521. https://doi.org/10.1134/S0869593823060060.Kuzmichev A.B., Storozhenko A.A., Danukalova M.K., Khubanov V.B., Dubensky A.S., 2023. The First Detrital Zircon Data on the Northwestern Precambrian Yenisei Ridge: Identification of the Continental-Arc Kiselikha Terrane. Stratigraphy and Geological Correlation 31, 507–521. https://doi.org/10.1134/S0869593823060060.Letnikova E.F., Kuznetsov A.B., Vishnevskaya I.A., Veshcheva S.V., Proshenkin A.I., Geng H., 2013. The Vendian Passive Continental Margin in the Southern Siberian Craton: Geochemical and Isotopic (Sr, Sm-Nd) Evidence and U-Pb Dating of Detrital Zircons by the LA-ICP-MS Method. Russian Geology and Geophysics 54 (10), 1177–1194. https://doi.org/10.1016/j.rgg.2013.09.004.Letnikova E.F., Kuznetsov A.B., Vishnevskaya I.A., Veshcheva S.V., Proshenkin A.I., Geng H., 2013. The Vendian Passive Continental Margin in the Southern Siberian Craton: Geochemical and Isotopic (Sr, Sm-Nd) Evidence and U-Pb Dating of Detrital Zircons by the LA-ICP-MS Method. Russian Geology and Geophysics 54 (10), 1177–1194. https://doi.org/10.1016/j.rgg.2013.09.004.Малышев С.В., Пасенко А.М., Худолей А.К., Иванов А.В., Прияткина Н.С., Пазухина А.А., Марфин А.Е., Дюфрейн Э.С., Шарыгин И.С., Гладкочуб Е.А. Каков возраст Уджинского палеорифта?: U-Pb возраст обломочных цирконов терригенных пород Уджинского бассейна, север Сибири // Вестник СПбГУ. Науки о Земле. 2022. Т. 67. № 4. С. 548–567. https://doi.org/10.21638/spbu07.2022.401.Malyshev S.V., Pasenko A.M., Khudoley A.K., Ivanov A.V., Priyatkina N.S., Pazukhina A.A., Marfin A.E., DuFrane S.A., Sharygin I.S., Gladkochub E.A., 2022. What Is the Age of the Udzha Paleorift?: U-Pb Age of Detrital Zircons from Udzha Basin Terrigenous Succession, Northern Siberia. Vestnik of Saint Petersburg University. Earth Sciences 67 (4), 548–567 (in Russian). https://doi.org/10.21638/spbu07.2022.401.Marusin V.V., Kochnev B.B., Izokh O.P., 2022. Thalassinoides and Olenichnus in the Terreneuvian Carbonates of the Igarka Uplift, NW Siberian Platform. Lethaia 55 (2), 1–17. https://doi.org/10.18261/let.55.2.6.Marusin V.V., Kochnev B.B., Izokh O.P., 2022. Thalassinoides and Olenichnus in the Terreneuvian Carbonates of the Igarka Uplift, NW Siberian Platform. Lethaia 55 (2), 1–17. https://doi.org/10.18261/let.55.2.6.Marusin V.V., Kochnev B.B., Karlova G.A., Izokh O.P., Sarsembaev Zh.A., Ivanova N.A., 2023. Precambrian-Cambrian Transition at the Igarka Uplift (Northwestern Siberian Platform). Russian Geology and Geophysics 64 (6), 682–697. https://doi.org/10.2113/RGG20224523.Marusin V.V., Kochnev B.B., Karlova G.A., Izokh O.P., Sarsembaev Zh.A., Ivanova N.A., 2023. Precambrian-Cambrian Transition at the Igarka Uplift (Northwestern Siberian Platform). Russian Geology and Geophysics 64 (6), 682–697. https://doi.org/10.2113/RGG20224523.Marusin V.V., Kolesnikova A.A., Kochnev B.B., Kuznetsov N.B., Pokrovsky B.G., Romanyuk T.V., Karlova G.A., Rud’ko S.V. et al., 2021. Detrital Zircon Age and Biostratigraphic and Chemostratigraphic Constraints on the Ediacaran-Cambrian Transitional Interval in the Irkutsk Cis-Sayan Uplift, Southwestern Siberian Platform. Geological Magazine 158, 1156–1172. https://doi.org/10.1017/S0016756820001132.Marusin V.V., Kolesnikova A.A., Kochnev B.B., Kuznetsov N.B., Pokrovsky B.G., Romanyuk T.V., Karlova G.A., Rud’ko S.V. et al., 2021. Detrital Zircon Age and Biostratigraphic and Chemostratigraphic Constraints on the Ediacaran-Cambrian Transitional Interval in the Irkutsk Cis-Sayan Uplift, Southwestern Siberian Platform. Geological Magazine 158, 1156–1172. https://doi.org/10.1017/S0016756820001132.Мельников Н.В., Якшин М.С., Шишкин Б.Б., Ефимов А.О., Карлова Г.А., Килина Л.И., Константинова Л.Н., Кочнев Б.Б. и др. Стратиграфия нефтегазоносных бассейнов Сибири. Рифей и венд Сибирской платформы и ее складчатого обрамления. Новосибирск: Гео, 2005. 428 с.Mel’nikov N.V., Yakshin M.S., Shishkin B.B., Efimov A.O., Karlova G.A., Kilina L.I., Konstantinova L.N., Kochnev B.B. et al., 2005. Stratigraphy of Oil and Gas Basins of Siberia. Riphean and Vendian of the Siberian Platform and Its Folded Frame. GEO, Novosibirsk, 428 p. (in Russian).Петров П.Ю. Условия накопления нижних свит рифея северной части Туруханского поднятия // Стратиграфия. Геологическая корреляция. 1993. Т. 1. № 2. С. 55–66.Petrov P.Yu., 1993. Depositional Environments of Lower Formations of the Riphean Sequence, Turukhansk Uplift. Stratigraphy and Geological Correlation 1 (2), 55–66 (in Russian).Powerman V., Shatsillo A., Chumakov N., Kapitonov I., Hourigane J., 2015. Interaction Between the Central Asian Orogenic Belt (CAOB) and the Siberian Craton as Recorded by Detrital Zircon Suites from Transbaikalia. Precambrian Research 267, 39–71. https://doi.org/10.1016/j.precamres.2015.05.015.Powerman V., Shatsillo A., Chumakov N., Kapitonov I., Hourigane J., 2015. Interaction Between the Central Asian Orogenic Belt (CAOB) and the Siberian Craton as Recorded by Detrital Zircon Suites from Transbaikalia. Precambrian Research 267, 39–71. https://doi.org/10.1016/j.precamres.2015.05.015.Priyatkina N., Collins W.J., Khudoley A., Zastrozhnov D., Ershova V., Chamberlain K., Shatsillo A., Proskurnin V., 2017. The Proterozoic Evolution of Northern Siberian Craton Margin: A Comparison of U-Pb-Hf Signatures from Sedimentary Units of the Taimyr Orogenic Belt and the Siberian Platform. International Geology Review 59 (13), 1289341. https://doi.org/10.1080/00206814.2017.1289341.Priyatkina N., Collins W.J., Khudoley A., Zastrozhnov D., Ershova V., Chamberlain K., Shatsillo A., Proskurnin V., 2017. The Proterozoic Evolution of Northern Siberian Craton Margin: A Comparison of U-Pb-Hf Signatures from Sedimentary Units of the Taimyr Orogenic Belt and the Siberian Platform. International Geology Review 59 (13), 1289341. https://doi.org/10.1080/00206814.2017.1289341.Priyatkina N., Collins W.J., Khudoley A.K., Letnikova E.F., Huang H.-Q., 2018. The Neoproterozoic Evolution of the Western Siberian Craton Margin: U-Pb-Hf Isotopic Records of Detrital Zircons from the Yenisey Ridge and the Prisayan Uplift. Precambrian Research 305, 197–217. https://doi.org/10.1016/j.precamres.2017.12.014.Priyatkina N., Collins W.J., Khudoley A.K., Letnikova E.F., Huang H.-Q., 2018. The Neoproterozoic Evolution of the Western Siberian Craton Margin: U-Pb-Hf Isotopic Records of Detrital Zircons from the Yenisey Ridge and the Prisayan Uplift. Precambrian Research 305, 197–217. https://doi.org/10.1016/j.precamres.2017.12.014.Priyatkina N., Khudoley A.K., Collins W.J., Kuznetsov N.B., Huang H.-Q., 2016. Detrital Zircon Record of Meso- and Neoproterozoic Sedimentary Basins in Northern Part of the Siberian Craton: Characterizing Buried Crust of the Basement. Precambrian Research 285, 21–38. https://doi.org/10.1016/j.precamres.2016.09.003.Priyatkina N., Khudoley A.K., Collins W.J., Kuznetsov N.B., Huang H.-Q., 2016. Detrital Zircon Record of Meso- and Neoproterozoic Sedimentary Basins in Northern Part of the Siberian Craton: Characterizing Buried Crust of the Basement. Precambrian Research 285, 21–38. https://doi.org/10.1016/j.precamres.2016.09.003.Priyatkina N.S., Kuznetsov N.B., Rud’ko S.V., Shatsillo A.V., Khudoley A.K., Romanyuk T.V., Maslov A.V., 2019. The Proterozoic Pogor’uy Formation of Yenisey Ridge: Age and Provenance Sources According to U/Pb Dating of Detrital Zircons. Doklady Earth Science 484, 28–31. https://doi.org/10.1134/S1028334X19010136.Priyatkina N.S., Kuznetsov N.B., Rud’ko S.V., Shatsillo A.V., Khudoley A.K., Romanyuk T.V., Maslov A.V., 2019. The Proterozoic Pogor’uy Formation of Yenisey Ridge: Age and Provenance Sources According to U/Pb Dating of Detrital Zircons. Doklady Earth Science 484, 28–31. https://doi.org/10.1134/S1028334X19010136.Romanov M., Sovetov J.K., Vernikovsky V.A., Rosenbaum G., Vernikovskaya A.E., Matushkin N.Yu., Kadilnikov P.I., Wilde S.A., 2020. Late Neoproterozoic Evolution of the Southwestern Margin of the Siberian Craton: Evidence from Sedimentology, Geochronology and Detrital Zircon Analysis. International Geology Review 63 (13), 1658–1681. https://doi.org/10.1080/00206814.2020.1790044.Romanov M., Sovetov J.K., Vernikovsky V.A., Rosenbaum G., Vernikovskaya A.E., Matushkin N.Yu., Kadilnikov P.I., Wilde S.A., 2020. Late Neoproterozoic Evolution of the Southwestern Margin of the Siberian Craton: Evidence from Sedimentology, Geochronology and Detrital Zircon Analysis. International Geology Review 63 (13), 1658–1681. https://doi.org/10.1080/00206814.2020.1790044.Розен О.М., Манаков А.В., Зинчук Н.Н. Сибирский кратон: формирование, алмазоносность. М.: Научный мир, 2006. 210 с.Rosen O.M., Manakov A.V., Zinchuk N.N., 2006. Siberian Craton: Formation, and Diamond Potential. Nauchny Mir, Moscow, 210 p. (in Russian).Rowland S.M., Luchinina V.A., Korovnikov I.V., Sipin D.P., Tarletskov A.I., Fedoseev A.V., 1998. Biostratigraphy of the Vendian-Cambrian Sukharikha River Section, Northwestern Siberian Platform. Canadian Journal of the Earth Sciences 35 (4), 339–352. DOI:10.1139/e98-002.Rowland S.M., Luchinina V.A., Korovnikov I.V., Sipin D.P., Tarletskov A.I., Fedoseev A.V., 1998. Biostratigraphy of the Vendian-Cambrian Sukharikha River Section, Northwestern Siberian Platform. Canadian Journal of the Earth Sciences 35 (4), 339–352. DOI:10.1139/e98-002.Rud’ko S., Kuznetsov N., Shatsillo A., Rud’ko D., Malyshev S., Dubensky A., Sheshukov V., Kanygina N., Romanyuk T., 2020. Sturtian Glaciation in Siberia: Evidence of Glacial Origin and U-Pb Dating of the Diamictites of the Chivida Formation in the North Yenisei Ridge. Precambrian Research 345, 105778. https://doi.org/10.1016/j.precamres.2020.105778.Rud’ko S., Kuznetsov N., Shatsillo A., Rud’ko D., Malyshev S., Dubensky A., Sheshukov V., Kanygina N., Romanyuk T., 2020. Sturtian Glaciation in Siberia: Evidence of Glacial Origin and U-Pb Dating of the Diamictites of the Chivida Formation in the North Yenisei Ridge. Precambrian Research 345, 105778. https://doi.org/10.1016/j.precamres.2020.105778.Самсонов A.В., Служеникин С.Ф., Ларионова Ю.О., Ларионов А.Н., Ерофеева К.Г., Полозов А.Г. Активная окраина 870 млн лет в северо-западной части Сибирского кратона: данные по ксенолитам из раннетриасовой эксплозивной Масловской диатремы, Норильский район // Тектоника и геодинамика земной коры и мантии: фундаментальные проблемы-2022: Материалы LIII Тектонического совещания (1–5 февраля 2022 г.). М.: ГЕОС, 2022. Т. 2. С. 168–171.Samsonov A.V., Sluzhenikin S.F., Larionova Yu.O., Larionov A.N., Erofeeva K.G., Polozov A.G., 2022. Active Margin 870 Ma in the Northwestern Siberian Craton: Data from Xenoliths in the Early Triassic Explosive Maslovskaya Diatreme, Norilsk Region. In: Problems of Tectonics and Geodynamics of the Earth’s Crust and Mantle. Proceedings of the LIII Tectonic Meeting (February 1–5, 2022). Vol. 2. GEOS, Moscow, p. 168–171 (in Russian).Семенова Д.В., Владимиров В.Г., Кармышева И.В., Яковлев В.А. Возраст раннеколлизионных гранитоидов Западного Сангилена (Юго-Восточная Тува): значение для оценки длительности орогенеза на окраине Тувино-Монгольского массива // Геодинамика и тектонофизика. 2024. Т. 15. № 4. 0767. https://doi.org/10.5800/GT-2024-15-4-0767.Semenova D.V., Vladimirov V.G., Karmysheva I.V., Yakovlev V.A., 2024. The Age of Early Collisional Granitoids of Western Sangilen (SE Tuva): Implications for Estimating the Duration of Orogeny at the Margin of the Tuva-Mongolian Massif. Geodynamics & Tectonophysics 15 (4), 0767 (in Russian). https://doi.org/10.5800/GT-2024-15-4-0767.Советов Ю.К. Седиментология и стратиграфическая корреляция вендских отложений на юго-западе Сибирской платформы: выдающийся вклад внешнего источника кластического материала в образование осадочных систем // Литосфера. 2018. Т. 18. № 1. С. 20–45. https://doi.org/10.24930/1681-9004-2018-18-1-020-045.Sovetov J.K., 2018. Sedimentology and Stratigraphic Correlation of Vendian Deposits in the Southwestern Siberian Platform: Major Contribution of an Exocratonic Clastic Source to Sedimentary Systems. Lithosphere 18 (1), 20–45 (in Russian). https://doi.org/10.24930/1681-9004-2018-18-1-020-045.Государственная геологическая карта Российской Федерации масштаба 1:200000. Серия Тунгусско-Туруханская. Лист Q-45-IX, X (Полой): Объяснительная записка. СПб.: ВСЕГЕИ, 2001. 84 с.State Geological Map of the Russian Federation, 2001. Tunguska-Turukhanskaya Series. Scale of 1:200000. Sheet Q-45-IX, X (Poloy). Explanatory Note. VSEGEI, Saint Petersburg, 84 p. (in Russian).Государственная геологическая карта Российской Федерации. Масштаб 1:1000000. Серия Таймыро-Североземельская. Лист S-46 (Тарея): Объяснительная записка. СПб.: ВСЕГЕИ, 2016. 115 с.State Geological Map of the Russian Federation, 2016. Taimyro-Severozemelskaya Series. Scale of 1:1000000. Sheet S-46 (Tareya). Explanatory Note. VSEGEI, Saint Petersburg, 115 p. (in Russian).Государственная геологическая карта Российской Федерации. Серия Норильская. Масштаб 1:1000000. Лист Q-45 (Игарка): Объяснительная записка. СПб.: ВСЕГЕИ, 2018. 389 с.State Geological Map of the Russian Federation, 2018. Norilsk Series. Scale of 1:1000000. Sheet Q-45 (Igarka). Explanatory Note. VSEGEI, Saint Petersburg, 389 p. (in Russian).Vermeesch P., 2012. On the Visualization of Detrital Age Distribution. Chemical Geology 312–313, 190–194. https://doi.org/10.1016/j.chemgeo.2012.04.021.Vermeesch P., 2012. On the Visualization of Detrital Age Distribution. Chemical Geology 312–313, 190–194. https://doi.org/10.1016/j.chemgeo.2012.04.021.Vernikovskaya A., Vernikovsky V.A., Matushkin N., Kadilnikov P., Metelkin D.V., Romanova I., Li Z.-X., Bogdanov E., 2020. Early Ediacaran Magmatism in the Yenisei Ridge and Evolution of the Southwestern Margin of the Siberian Craton. Minerals 10, 565. https://doi.org/10.3390/min10060565.Vernikovskaya A., Vernikovsky V.A., Matushkin N., Kadilnikov P., Metelkin D.V., Romanova I., Li Z.-X., Bogdanov E., 2020. Early Ediacaran Magmatism in the Yenisei Ridge and Evolution of the Southwestern Margin of the Siberian Craton. Minerals 10, 565. https://doi.org/10.3390/min10060565.Vernikovskaya A.E., Vernikovsky V.A., Matushkin N., Kadilnikov P., Wingate M.T.D., Bogdanov E.A., Travin A.V., 2023. Cryogenian A-type Granites of the Yenisei Ridge – Indicators of Tectonic Transformation in the Southwestern Margin of the Siberian Craton. Russian Geology and Geophysics 64 (6), 647–668. https://doi.org/10.2113/RGG20224532.Vernikovskaya A.E., Vernikovsky V.A., Matushkin N., Kadilnikov P., Wingate M.T.D., Bogdanov E.A., Travin A.V., 2023. Cryogenian A-type Granites of the Yenisei Ridge – Indicators of Tectonic Transformation in the Southwestern Margin of the Siberian Craton. Russian Geology and Geophysics 64 (6), 647–668. https://doi.org/10.2113/RGG20224532.Vernikovsky V.A., Vernikovskaya A.E., Chernykh A.I., Sal’nikova E.B., Kotov A.B., Kovach V.P., Yakovleva S.Z., Fedoseenko A.M., 2001. Porozhnaya Granitoids of the Enisei Ophiolite Belt: Indicators of Neoproterozoic Events on the Enisei Ridge. Doklady Earth Science 381A (9), 1043–1046.Vernikovsky V.A., Vernikovskaya A.E., Chernykh A.I., Sal’nikova E.B., Kotov A.B., Kovach V.P., Yakovleva S.Z., Fedoseenko A.M., 2001. Porozhnaya Granitoids of the Enisei Ophiolite Belt: Indicators of Neoproterozoic Events on the Enisei Ridge. Doklady Earth Science 381A (9), 1043–1046.Vishnevskaya I.A., Letnikova E.F., Vetrova N.I., Kochnev B.B., Dril S.I., 2017. Chemostratigraphy and Detrital Zircon Geochronology of the Neoproterozoic Khorbusuonka Group, Olenek Uplift, Northeastern Siberian Platform. Gondwana Research 51, 255–271. https://doi.org/10.1016/j.gr.2017.07.010.Vishnevskaya I.A., Letnikova E.F., Vetrova N.I., Kochnev B.B., Dril S.I., 2017. Chemostratigraphy and Detrital Zircon Geochronology of the Neoproterozoic Khorbusuonka Group, Olenek Uplift, Northeastern Siberian Platform. Gondwana Research 51, 255–271. https://doi.org/10.1016/j.gr.2017.07.010.Вотах О.А. Тектоника докембрия западной окраины Сибирской платформы. М.: Наука, 1968. 138 с.Votakh O.A., 1968. The Precambrian Tectonics of the Western Margin of the Siberian Platform. Nauka, Moscow, 138 p. (in Russian).

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