gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2026-17-2-0884GAKYPXgtcrust-2244Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSК ВОПРОСУ ОБ ИСТОЧНИКАХ ОБЛОМОЧНОГО ЦИРКОНА ПЕСЧАНИКОВ АЙСКОЙ И БОЛЬШЕИНЗЕРСКОЙ СВИТ (СТРАТОТИП РИФЕЯ, ЮЖНЫЙ УРАЛ)DETRITAL ZIRCON PROVENANCES FOR SANDSTONES OF THE AI AND BOL’SHOI INZER FORMATIONS (RIPHEAN STRATOTYPE, SOUTHERN URALS)https://orcid.org/0000-0003-4902-5789МасловА. В.MaslovA. V.

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

20110, Екатеринбург, ул. Академика Вонсовского, 15

7-1 Pyzhevsky Ln, Moscow 119017 

15 Academician Vonsovsky St, Ekaterinburg 620110

amas2004@mail.ruhttps://orcid.org/0000-0002-9661-1708ЕршоваВ. Б.ErshovaV. B.

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

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

7-1 Pyzhevsky Ln, Moscow 119017 

7/9 Universitetskaya Emb, Saint Petersburg 199034 

https://orcid.org/0000-0003-0050-3495МельничукО. Ю.MelnichukO. Yu.

620110, Екатеринбург, ул. Академика Вонсовского, 15 

15 Academician Vonsovsky St, Ekaterinburg 620110

https://orcid.org/0000-0002-5698-450XДубС. А.DubS. A.

620110, Екатеринбург, ул. Академика Вонсовского, 15

15 Academician Vonsovsky St, Ekaterinburg 620110

https://orcid.org/0000-0002-9067-4804КрупенинМ. Т.KrupeninM. T.

620110, Екатеринбург, ул. Академика Вонсовского, 15

15 Academician Vonsovsky St, Ekaterinburg 620110

https://orcid.org/0000-0003-0078-6923БадидаЛ. В.BadidaL. V.

620110, Екатеринбург, ул. Академика Вонсовского, 15

15 Academician Vonsovsky St, Ekaterinburg 620110

Геологический институт РАН ; Институт геологии и геохимии им. акад. А.Н. Заварицкого УрО РАНРоссияGeological Institute, Russian Academy of Sciences ; Zavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of SciencesRussian FederationГеологический институт РАН ; Санкт-Петербургский государственный университетРоссияGeological Institute, Russian Academy of Sciences ; Saint Petersburg UniversityRussian FederationИнститут геологии и геохимии им. акад. А.Н. Заварицкого УрО РАНРоссияZavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of SciencesRussian Federation202617042026172884884Copyright © Маслов А.В., Ершова В.Б., Мельничук О.Ю., Дуб С.А., Крупенин М.Т., Бадида Л.В., 20262026Маслов А.В., Ершова В.Б., Мельничук О.Ю., Дуб С.А., Крупенин М.Т., Бадида Л.В.Maslov A.V., Ershova V.B., Melnichuk O.Y., Dub S.A., Krupenin M.T., Badida L.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/2244

Сопоставление максимумов на кривых относительной плотности вероятности возрастов обломочного циркона песчаников базальных уровней стратотипа рифея (айская и большеинзерская свиты, Южный Урал) и временных интервалов формирования потенциальных источников такого циркона на Восточно-Европейском и Сибирском кратонах, располагавшихся ~1.7 млрд лет назад непосредственно к западу и востоку от области накопления исходных для названных свит осадков, показало их существенное сходство. Это позволяет предполагать, что поставщиками обломочного материала для базальных толщ стратотипа рифея могли быть комплексы пород обоих названных кратонов. Все сказанное представляет собой, на наш взгляд, пример так называемой параллельной тектономагматической эволюции кратонов и привлекает внимание исследователей к возможной многовариантности моделей формирования популяций обломочного циркона песчаников, основанных только на данных о его U-Th-Pb изотопном возрасте.

When the maxima on the relative probability density curves of age of detrital zircons from the basal sandstones of the of the Riphean prototype (Ai and Bol’shoi Inzer formations, Southern Urals) are compared with the time intervals of formation of potential detrital zircon sources in the East European and Siberian cratons, ~1.7 Ga ago located immediately west and east of the area of accumulation of sediments originally comprising these formations, it is apparent that they are substantially similar to each other. This suggests that the detritus in the basal strata of the Riphean stratotype could be derived from rock complexes of both cratons. All of the aforesaid may represent an example of the so-called parallel tectonomagmatic evolution of cratons and draw the attention of researchers to the possibility of obtaining multivariate models for the formation of detrital zircon populations in sandstones based solely on U-Th-Pb isotopic dating of detrital zircons.

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