FINAL CONSOLIDATION AGE OF THE SOUTHERN PART OF THE SIBERIAN CRATON

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

Авторы: Donskaya T.V., Gladkochub D.P., Sergeev S.A., Khubanov V.B., Mazukabzov A.M., Motova Z.L.
Журнал: Geodynamics & Tectonophysics
Том: 14
Номер: 6
Год издания: 2023
Издательство: Федеральное государственное бюджетное учреждение науки Институт земной коры Сибирского отделения РАН
Местоположение издательства: Иркутск
Первая страница: 0727
Последняя страница: 0727
DOI: 10.5800/gt-2023-14-6-0727
Аннотация: 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 Al O , Th, Sr, Ba, low concentrations of K O, Nb, Y, Yb, a highly fractionated rare earth elements pattern (La /Yb =284), and the 23absence of europium anomaly. U-Pb geochronological studies of zircon from cataclastic granodiorite were carried out in- dependently 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.
Добавил в систему: Хубанов Валентин Борисович

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