gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2024-15-5-0784SKLFQIgtcrust-1920Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSВОЗРАСТ И ГЕОДИНАМИЧЕСКИЕ ОБСТАНОВКИ ФОРМИРОВАНИЯ КАРБОНАТИТОВЫХ КОМПЛЕКСОВ И СВЯЗАННЫХ С НИМИ РЕДКОМЕТАЛЛЬНЫХ МЕСТОРОЖДЕНИЙ ЮЖНОГО УРАЛАAGE AND GEODYNAMIC SETTINGS FOR FORMATION OF CARBONATITE COMPLEXES AND ASSOCIATED RARE METAL DEPOSITS OF THE SOUTH URALhttps://orcid.org/0000-0001-7952-0639НедосековаИ. Л.NedosekovaI. L.

620110, Екатеринбург, ул. Академика Вонсовского, 15

15 Academician Vonsovsky St, Ekaterinburg 620110

nedosekova@igg.uran.ruИнститут геологии и геохимии им. А.Н. Заварицкого УрО РАНРоссияZavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of SciencesRussian Federation202418102024155784784Copyright © Недосекова И.Л., 20242024Недосекова И.Л.Nedosekova I.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/1920

Ильмено-Вишневогорский и Булдымский карбонатитовые комплексы Южного Урала являются представителями деформированных карбонатитовых комплексов линейного типа. Их происхождение, возраст и геодинамическая обстановка формирования остаются предметом дискуссий. С целью определения возраста и длительности этапов щелочно-карбонатитового магматизма и связанного с ним редкометалльного рудообразования были использованы как изохронные методы (Rb-Sr, Sm-Nd, TIMS), так и локальное U-Pb-датирование цирконов (SHRIMP II, LA-ICP MS) этих комплексов. Установлен U-Pb-возраст циркона ранних фаз миаскитов – 420.7±11 (S2) и карбонатитов – 417±2.8 (D1) млн лет. В поздних фазах миаскитов и карбонатитов ранние цирконы резорбированы, имеют нарушенные изотопные системы, а более поздние генерации образуют кластер 386±7.6 млн лет (D2). В поздних карбонатитах и миаскит-пегматитах определен нижнепермский U-Pb-возраст циркона: 280±8 млн лет (P1). Изохронное датирование поздних рудоносных разностей карбонатитов также показало возраст от нижней перми до раннего триаса (P1–T1): 254±18 млн лет, Sm-Nd, и 247±4 млн лет, Rb-Sr (ИВК); 280±53 млн лет, Sm-Nd (Булдымский комплекс). Генерация и внедрение щелочных магм на Урале происходили ~420 млн лет назад (S2–D1), синхронно с формированием островодужных комплексов, и связаны с процессами пассивного рифтогенеза на формирующихся континентальных окраинах. Этап тектонической активности и формирования щелочных пород и карбонатитов фиксируется в среднем девоне (~380 млн лет, D2) и коррелирует с аккреционно-коллизионным этапом развития Урала. На этапе «жесткой» коллизии (~280 млн лет, P1) Ильмено-Вишневогорский и Булдымский комплексы были пластически деформированы, подверглись плавлению и внедрены субсогласно коллизионно-сдвиговым тектоническим структурам. Перекристаллизация пород и минералов, пластические и хрупкие деформации, процессы пегматито-, карбонатито- и редкометалльного рудообразования связаны с палингенно-метасоматическими процессами преобразований рифтогенных щелочных комплексов ордовик-силурийского возраста на коллизионном и постколлизионном (~250 млн лет, P3–T1) этапах развития Урала.

The Ilmen-Vishnevogorsky and Buldym carbonatite complexes occurring in the Southern Urals represent linear deformed carbonatite complexes. Their origin, as well as the age and geodynamic conditions remain the subject of debate. The isochron methods (Rb-Sr, Sm-Nd, TIMS) and local U-Pb-dating of zircons (SHRIMP II and LA-ICP MS) of these carbonatite complexes were employed to determine the age and duration of the stages of alkali-carbonatite magmatism and associated rare-metal ore formation. The Silurian-Devonian U-Pb zircon ages of the early phases of Ilmen-Vishnevogorsky miaskites and carbonatites were determined as 420.7±11 Ma (S2) and 417±2.8 Ma (D1), respectively. In the later phases of miaskites and carbonatites, early zircons are resorbed, they have broken isotope systems, and later zircon generations form a cluster of 386±7.6 Ma (D2). The Lower Permian U-Pb age of zircon 280±8 Ma (P1) was determined in the miaskite-pegmatite and late carbonatite. The isochron dating of late ore-bearing varieties of carbonatites provided the ages from the Lower Permian to the Early Triassic (P1–T1): 254±18 Ma, Sm-Nd and 247±4 Ma, Rb-Sr, IVC; 280±53 Ma, Sm-Nd, Buldym complex. Thus, the generation and intrusion of alkaline magmas in the Urals occurred ~420 Ma (S2–D1), synchronously with the formation of island-arc complexes. They are related to rifting on the emerging continental margins. The tectonic activity and formation of alkaline rocks and carbonatites proceeded in the Middle Devonian (~380 Ma, D2); it correlates with the accretion-collision stage of the Urals development. At the stage of "hard" collision (~280 Ma, P1), the Ilmen-Vishnevogorsky and Buldym complexes were plastically deformed, underwent melting and emplaced conformably with collision-slip tectonic structures. Recrystallization of rocks and minerals, plastic and brittle deformations, processes of pegmatitic, carbonatitic and rare-metal ore formation are associated with palingenic-metasomatic transformation of rifting alkaline complexes of Silurian-Devonian age at the collision and post-collision (~250 Ma, P3–T1) stages of the Urals emplacement.

карбонатитовые комплексы линейного типаU-Pb-Rb-Sr-Sm-Nd-изотопный возрастгеодинамические обстановкиИльмено-Вишневогорский и Булдымский комплексыЮжный Уралlinear сarbonatite complexesU-Pb-Rb-Sr-Sm-Nd-isotope agegeodynamic conditionsIlmenVishnevogorsk and Buldym complexesSouthern UralsИсследования выполнены в рамках государственного задания ИГГ УрО РАН, тема № 123011800011-2 «Рудообразующие процессы и закономерности размещения месторождений полезных ископаемых во внутриплитных коллизионно-складчатых поясах».The research was carried out within the framework of the State assignment of the Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Sciences, topic No. 123011800011-2 "Ore-forming processes and patterns of distribution of mineral deposits in intraplate collision-fold belts".ReferencesAbramov S.S., Rass I.T., Kononkova N.N., 2020. 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The authors declare that there are no conflicts of interest present.