References

gtcrust

Геодинамика и тектонофизика

Geodynamics & Tectonophysics

2078-502X

Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch

10.5800/GT-2023-14-6-0727

gtcrust-1757

Research Article

ПАЛЕОГЕОДИНАМИКА

PALEOGEODYNAMICS

ВОЗРАСТ ФИНАЛЬНОЙ КОНСОЛИДАЦИИ СТРУКТУРЫ СИБИРСКОГО КРАТОНА

FINAL CONSOLIDATION AGE OF THE SOUTHERN PART OF THE SIBERIAN CRATON

Донская

Т. В.

Donskaya

T. V.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

Гладкочуб

Д. П.

Gladkochub

D. P.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

Сергеев

С. А.

Sergeev

S. A.

199106, Санкт-Петербург, пр-т Средний, 74

74 Sredny Ave, Saint Petersburg, 199106

Хубанов

В. Б.

Khubanov

V. B.

670047, Улан-Удэ, ул. Сахьяновой, 6а, Республика Бурятия

6а Sakhyanova St, Ulan-Ude 670047, Republic of Buryatia

Мазукабзов

А. М.

Mazukabzov

A. M.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

Мотова

З. Л.

Motova

Z. L.

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 Federation

Всероссийский научно-исследовательский геологический институт им. А.П. КарпинскогоРоссияKarpinsky Russian Geological Research InstituteRussian Federation

Геологический институт им. Н.Л. Добрецова СО РАНРоссияDobretsov Geological Institute, Siberian Branch of the Russian Academy of SciencesRussian Federation

2023

14122023

146727727

2023

Донская Т.В., Гладкочуб Д.П., Сергеев С.А., Хубанов В.Б., Мазукабзов А.М., Мотова З.Л.

Donskaya T.V., Gladkochub D.P., Sergeev S.A., Khubanov V.B., Mazukabzov A.M., Motova Z.L.

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/1757

Проведены петрографические, геохимические и U-Pb геохронологические исследования катаклазированных гранитоидов юго-восточной части Иркутного блока Шарыжалгайского выступа фундамента Сибирской платформы, который, согласно большинству тектонических схем, является южной частью Тунгусского супертеррейна. По своим геохимическим характеристикам исследованный представительный образец этих гранитоидов соответствует гранодиориту и обнаруживает повышенные содержания Al2O3, Th, Sr, Ba, низкие концентрации K2O, Nb, Y, Yb, сильно фракционированный спектр распределения редкоземельных элементов (Lan/Ybn=284) и отсутствие европиевой аномалии. U-Pb геохронологические исследования циркона из катаклазированного гранодиорита выполнены независимо двумя методами: SIMS и LA-ICP-MS, показавшими хорошую сходимость полученных результатов. U-Pb возраст центральных частей кристаллов циркона, имеющих магматическую зональность, соответствует значениям 2893±19 млн лет (метод SIMS) и 2889±16 млн лет (метод LA-ICP-MS). Эти результаты датирования могут быть проинтерпретированы как возраст архейского протолита гранодиорита. Для краевых оболочек кристаллов циркона, имеющих архейские ядра, и отдельных кристаллов циркона с параллельной зональностью были установлены значения возраста 1855±6 млн лет (метод SIMS) и 1864±5 млн лет (метод LA-ICP-MS), которые фиксируют время преобразований гранодиорита. Оценка возраста около 1.86 млрд лет соответствует основному раннепротерозойскому этапу метаморфизма, мигматизации и сопряженного магматизма, которые широко проявлены в Шарыжалгайском выступе фундамента. Эта оценка возраста совместно с опубликованными ранее значениями возраста метаморфических и синхронных с ними магматических событий в Шарыжалгайском выступе позволила сделать вывод о присоединении Тунгусского супертеррейна к ранее сформированному ядру Сибирского кратона на временном рубеже 1.85–1.88 млрд лет. Финальным этапом становления Сибирского кратона является формирование пород Южно-Сибирского постколлизионного магматического пояса, пересекающего все уже объединенные в единую структуру крупные раннедокембрийские блоки южной части Сибирского кратона.

Petrographic, geochemical and U-Pb geochronological research studies are done into cataclastic granitoids of the southeastern part of the Irkutsk block of the Sharyzhalgay basement uplift of the Siberian craton – the uplift which is considered southern part of the Tungus superterrane according to most of tectonic schemes. The representative sample of these granitoids corresponds to granodiorite in its geochemical properties and is characterized by high contents of Al2O3, Th, Sr, Ba, low concentrations of K2O, Nb, Y, Yb, a highly fractionated rare earth elements pattern (Lan/Ybn=284), and the absence of europium anomaly. U-Pb geochronological studies of zircon from cataclastic granodiorite were carried out independently by two methods: SIMS and LA-ICP-MS, which showed good consistency of the results. The U-Pb age of the cores of zircon grains with magmatic zoning corresponds to 2893±19 Ma (SIMS method) and 2889±16 Ma (LA-ICP-MS method). These results can be interpreted as the age of the Archean granodiorite protolith. The rims of zircon crystals with the Archean cores, as well as the individual zircon crystals with parallel zoning, yielded ages of 1855±6 Ma (SIMS method) and 1864±5 Ma (LA-ICP-MS method), which record the time of granodiorite transformations. The age of about 1.86 Ga corresponds to the main Early Proterozoic stage of metamorphism, migmatization and magmatism, which show their widespread occurrence in the Sharyzhalgay basement uplift. This age estimate together with the previously published ages for metamorphic and their synchronous magmatic events in the Sharyzhalgay uplift allowed concluding that the Tungus superterrane joined the earlier formed core of the Siberian craton in the time interval 1.85–1.88 Ga. The final stage in the Siberian craton formation is the development of the South Siberian post-collisional magmatic belt, intersecting all large Early Precambrian blocks of the southern part of the Siberian craton, already united into a single structure.

гранодиоритцирконU-Pb возрастранний протерозойСибирский кратон

granodioritezirconU-Pb ageEarly ProterozoicSiberian craton

Исследования выполнены при поддержке Российского научного фонда (грант № 23-17-00196) и Правительства Российской Федерации (грант № 075-15-2022-1100). В работе задействовалось оборудование ЦКП «Геодинамика и геохронология» ИЗК СО РАН в рамках гранта № 075-15-2021-682. U-Pb изотопно-геохронологические исследования методом LA-ICP-MS выполнены в ЦКП «Геоспектр» ГИН СО РАН, г. Улан-Удэ (в рамках базовых проектов, № гос. рег. АААА-А21-121011390002-2 и АААА-А21-121011890029-4)

The study was supported by the Russian Science Foundation (grant 23-17-00196) and the Russian Government (grant 075-15-2022-1100). The work was conducted using equipment and infrastructure of the Centre for Geodynamics and Geochronology at the Institute of the Earth's Crust SB RAS (grant 075-15-2021-682). U-Pb isotope-geochronological studies involving the LA-ICP-MS method were carried out using Shared Research Facilities "Geospectr" of the GIN SB RAS, Ulan-Ude (basic projects, State Registration AAAA-A21-121011390002-2 and AAAA-A21-121011890029-4)

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