gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2025-16-3-0827hsphpegtcrust-2040Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSПОЗДНЕНЕОПРОТЕРОЗОЙСКИЕ РЕДКОМЕТАЛЛЬНЫЕ ЛЕЙКОГРАНИТЫ ХАРИУСИХИНСКОГО МАССИВА ЕНИСЕЙСКОГО КРЯЖА: ОСОБЕННОСТИ ГЕНЕЗИСА И СВЯЗЬ С МАГМАТИЗМОМ КРУПНОЙ ИЗВЕРЖЕННОЙ ПРОВИНЦИИLATE NEOPROTEROZOIC RARE-METAL LEUCOGRANITE FROM THE KHARIUSIKHA MASSIF OF YENISEI RIGDE: GENESIS AND RELATIONSHIP TO MAGMATISM OF A LARGE IGNEOUS PROVINCEНожкинА. Д.NozhkinA. D.

630090, Новосибирск, пр-т Академика Коптюга, 3

 3 Academician Koptyug Ave, Novosibirsk 630090 

ТуркинаО. М.TurkinaO. M.

630090, Новосибирск, пр-т Академика Коптюга, 3

 Olga M. Turkina 

 3 Academician Koptyug Ave, Novosibirsk 630090 

turkina@igm.nsc.ruИнститут геологии и минералогии им. В.С. Соболева СО РАНРоссияSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesRussian Federation202518062025163827827Copyright © Ножкин А.Д., Туркина О.М., 20252025Ножкин А.Д., Туркина О.М.Nozhkin A.D., Turkina O.M.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/2040

Приводится петрогеохимический состав и U-Pb (SHRIMP-II) возраст (753±6 млн лет) субщелочных лейкогранитов и сиенитов Хариусихинского массива Енисейского кряжа, содержащих редкометалльную минерализацию. Повышенные концентрации редких элементов (в %) – Nb (0.5–0.7), Ta (0.12–0.16), РЗЭ (0.08–0.24), Y (0.06–0.10), Zr (2.3–2.6), Hf (0.10–0.12), U (0.05–0.10) и Th (0.08–0.10) – приурочены к альбитизированным гранитам. Синтез имеющейся информации по возрасту и составу риолитов бимодальных вулканических ассоциаций Верхневороговского и Глушихинского прогибов и субсинхронных гранитоидов Заангарья Енисейского кряжа показывает их принадлежность к А-типу гранитоидов. Их образование ограничено интервалом 750–720 млн лет и коррелирует по времени с формированием поздненеопротерозойской крупной изверженной провинции, ультрабазит-/базитовый магматизм которой локализован вдоль современного южного фланга Сибирской платформы. Рассматриваемые вулканические и интрузивные породы характеризуются широким диапазоном концентраций высокозарядных элементов и значениями εNd(t) от –9.2 до +0.7. Доминирующими для большинства кислых магматических пород являются коровые источники. О вероятном вкладе мантийного вещества в генерацию кислых магм свидетельствует более радиогенный изотопный состав Nd и обогащение высокозарядными элементами, прежде всего Nb для гранитов и сиенитов Хариусихинского массива, а также сходство базальтов Верхневороговского прогиба с OIB.

The paper deals with the petrogeochemical composition and U-Pb (SHRIMP-II) age (753±6 Ma) of subalkaline leucogranites and syenites from the Khariusikha massif of the Yenisei Ridge, which contain rare-metal mineralization. High trace-element concentrations (%) – Nb (0.5–0.7), Ta (0.12–0.16), REE (0.08–0.24), Y (0.06–0.10), Zr (2.3–2.6), Hf (0.10–0.12), U (0.05–0.10) and Th (0.08–0.10) – are confined to albitized granites. Synthesis information on age and composition of rhyolites of the bimodal volcanic associations of the Upper Vorogovka and Glushikha troughs and subsynchronous granitoids of the Trans-Angarian Yenisei Ridge indicates A-type granitoids. Their formation is limited to 750–720 Ma interval and is temporally correlated with the formation of a Late Neoproterozoic large igneous province whose ultrabasite-basite magmatism is localized along the present-day southern flank of the Siberian Platform. The considered volcanic and intrusive rocks are characterized by wide-range high field strength element concentrations and εNd(t) values ranging from –9.2 to +0.7. Crustal sources are dominant for most of the felsic magmatic rocks. A probable contribution of the mantle source to felsic magmas generation is evidenced by more radiogenic Nd isotope composition and enrichment of the Khariusikha massif granites and syenites in high field strength elements, as well as by the similarity of the Upper Vorogovka trough basalts with OIB.

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