Mesoproterozoic (ca. 1.26 Ga) Srednecheremshansk mafic–ultramafic intrusion in the southern Siberia: Signature of the Mackenzie event in Siberia

Гладкочуб, Д.П.; Donskaya, T. V.; Pisarevsky, Sergei; Kotov, A. B.; Сальникова, Е. Б.; Мехоношин, А. С.; Sklyarov, E. V.; Demonterova, Е. I.; Мазукабзов, А. М.; Stepanova, A. V.; Константинов, К. М.

doi:10.1016/j.precamres.2023.107038

Cited by 2 publications

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“…Метаморфические породы всех блоков Шарыжалгайского выступа прорваны постколлизионными гранитоидами, реже -габброидами и долеритами с возрастом 1.84-1.87 млрд лет, входящими в состав Южно-Сибирского постколлизионного магматического пояса [Donskaya et al, 2002[Donskaya et al, , 2005Levitskii et al, 2002;Didenko et al, 2005;Turkina et al, 2006;Gladkochub et al, 2013;Ernst et al, 2016;Turkina, Kapitonov, 2017Ivanov et al, 2019;Donskaya, Gladkochub, 2021;Turkina, Izokh, 2023], а также мезопротерозойскими и неопротерозойскими дайками долеритов [Gladkochub et al, 2007[Gladkochub et al, , 2019[Gladkochub et al, , 2023Donskaya et al, 2018]. Geological Map…, 2009;Turkina, 2023]).…”

Section: краткий геологический очеркunclassified

Final Consolidation Age of the Southern Part of the Siberian Craton

Donskaya,

Gladkochub,

Sergeev

et al. 2023

Geodin. tektonofiz.

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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.

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