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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">gtcrust</journal-id><journal-title-group><journal-title xml:lang="ru">Геодинамика и тектонофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Geodynamics &amp; Tectonophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2078-502X</issn><publisher><publisher-name>Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.5800/GT-2022-13-4-0652</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1547</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>ПАЛЕОГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>PALEOGEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>ВОЗРАСТ И ГЕОДИНАМИЧЕСКИЕ ОБСТАНОВКИ ФОРМИРОВАНИЯ МИАСКИТ-ПЕГМАТИТОВ, КАРБОНАТИТОВ И Nb-Zr МИНЕРАЛИЗАЦИИ ИЛЬМЕНО-ВИШНЕВОГОРСКОГО ЩЕЛОЧНОГО КОМПЛЕКСА, ЮЖНЫЙ УРАЛ (U-Pb И Rb-Sr ИЗОТОПНЫЕ ДАННЫЕ)</article-title><trans-title-group xml:lang="en"><trans-title>AGE AND GEODYNAMIC SETTINGS OF MIASKITE-PEGMATITES, CARBONATITES, AND Nb-Zr MINERALIZATION OF THE ILMENO-VISHNEVOGORSKY ALKALINE COMPLEX, SOUTH URAL (U-Pb AND Rb-Sr ISOTOPE DATA)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Недосекова</surname><given-names>И. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Nedosekova</surname><given-names>I. L.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620016, Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>15 Academician Vonsovsky St, Ekaterinburg 620016</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Червяковский</surname><given-names>В. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Chervyakovsky</surname><given-names>V. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620016, Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>15 Academician Vonsovsky St, Ekaterinburg 620016</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Червяковская</surname><given-names>М. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Chervyakovskaya</surname><given-names>M. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620016, Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>15 Academician Vonsovsky St, Ekaterinburg 620016</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Булатов</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bulatov</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620016, Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>15 Academician Vonsovsky St, Ekaterinburg 620016</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии и геохимии им. А.Н. Заварицкого УрО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Zavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>12</day><month>10</month><year>2022</year></pub-date><volume>13</volume><issue>4</issue><fpage>652</fpage><lpage>652</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Недосекова И.Л., Червяковский В.С., Червяковская М.В., Булатов В.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Недосекова И.Л., Червяковский В.С., Червяковская М.В., Булатов В.А.</copyright-holder><copyright-holder xml:lang="en">Nedosekova I.L., Chervyakovsky V.S., Chervyakovskaya M.V., Bulatov V.A.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://www.gt-crust.ru/jour/article/view/1547">https://www.gt-crust.ru/jour/article/view/1547</self-uri><abstract><p>Ильмено-Вишневогорский миаскит-фенит-карбонатитовый комплекс (ИВК), расположенный в Уральской складчатой области, является представителем карбонатитовых комплексов «линейного типа», с которым связаны Nb-Zr месторождения. Рудный потенциал карбонатитовых комплексов «линейного типа», время и продолжительность рудообразующих процессов, геодинамическая обстановка их формирования остаются предметом дискуссий. С целью оценки возраста и продолжительности процессов рудообразования в ИВК проведено U-Pb-датирование циркона (метод LA-ICP-MS) из миаскит-пегматитов, а также Rb-Sr-датирование рудоносных (пирохлорсодержащих) разностей миаскит-пегматитов и карбонатитов (ID-TIMS по минералам и валу породы). U-Pb-датирование циркона миаскит-пегматитов ИВК показало пермский возраст (280±8 млн лет, P1 – возраст основной генерации циркона). Rb-Sr-минеральная изохрона для миаскит-пегматита с близким возрастом – 274±5 млн лет (Р1) – подтверждает результаты датирования миаскит-пегматитов U-Pb-методом. Rb-Sr-датирование пирохлоровых разностей карбонатитов (сёвитов II) показало возраст 250±3 млн лет (Т1). Результаты Rb-Sr- и U-Pb-датирования свидетельствуют о том, что процессы пегматито- и карбонатитообразования и связанного с ними Zr-Nb-рудообразования в ИВК происходили на поздне- и постколлизионной стадии развития Уральской складчатой области. На основании полученных данных предложена геодинамическая модель формирования ИВК.</p></abstract><trans-abstract xml:lang="en"><p>The Ilmeno-Vishnevogorsky miaskite-phenite-carbonatite complex (IVС), located in the Urals folded region, is a representative of "linear type" carbonatite complexes, with which Nb-Zr deposits are associated. The ore potential of linear carbonatite complexes, the time and duration of ore-forming processes, and the geodynamic setting remain the subject of discussion. In order to estimate the age and duration of ore formation processes in the IVC, the U-Pb dating of zircon (LA-ICP-MS) from miaskite-pegmatites, as well as Rb-Sr dating of ore-bearing (pyrochlore-bearing) varieties of miaskite-pegmatites and carbonatites (ID-TIMS) were carried out. The U-Pb dating of zircon from the IVC miaskite-pegmatites showed the Permian age (280±8 Ma, P1 – age of the main zircon generation). The Rb-Sr-mineral isochron of miaskite-pegmatite showed a close age of 274±5 Ma (P1), confirming the results of U-Pb-dating of miaskite-pegmatites. The Rb-Sr dating of pyrochlore carbonatite varieties (sovites II) showed an age of 250±3 Ma (T1). The results of Rb-Sr- and U-Pb dating indicate that the processes of pegmatite- and carbonatite formation and the associated Zr-Nb ore formation in IVC occurred at the late collisional and postcollisional stage of development of the Ural folded region. Based on the data obtained, the geodynamic model for the IVC formation was proposed.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>карбонатиты</kwd><kwd>миаскит-пегматиты</kwd><kwd>U-Pb и Rb-Sr-датирование</kwd><kwd>Ильмено-Вишневогорский комплекс</kwd><kwd>Урал</kwd></kwd-group><kwd-group xml:lang="en"><kwd>сarbonatites</kwd><kwd>miaskite-pegmatites</kwd><kwd>U-Pb and Rb-Sr dating</kwd><kwd>Ilmeno-Vishnegorsky complex</kwd><kwd>the Urals</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследования выполнены в рамках государственного задания ИГГ УрО РАН, тема № AAAA-А18-118052590028-9, с использованием оборудования ЦКП «Геоаналитик» ИГГ УрО РАН. Дооснащение и комплексное развитие ЦКП «Геоаналитик» ИГГ УрО РАН осуществляется при финансовой поддержке Министерства науки и высшего образования РФ (Соглашение № 075-15-2021-680). Авторы выражают благодарность Т.Б. Баяновой,  А.Ю. Кисину, П.А. Серову, Б.В. Беляцкому и коллективу  ФХМИ ИГГ УрО РАН за поддержку, консультации и помощь в проведении аналитических работ.</funding-statement><funding-statement xml:lang="en">The research was carried out within the framework of the State Assignment of the Institute of Geology, the Ural Branch of the Russian Academy of Sciences, theme AAAA-A18-118052590028-9, using the equipment of the Shared Research Facilities "Geoanalyst" of the Institute of Geology, the Ural Branch of the Russian Academy of Sciences. The retrofitting and integrated development of the Shared Research Facilities "Geoanalyst" of the Institute of Geology and Geochemistry of the Ural Branch of the Russian Academy of Sciences is financially supported by the grant from the Ministry of Science and Higher Education of the Russian Federation (Agreement 075-15-2021-680).</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Abramov S.S., Rass I.T., Kononkova N.N., 2020. Fenites of the Miaskite–Carbonatite Complex in the Vishnevye Mountains, Southern Urals, Russia: Origin of the Metasomatic Zoning and Thermodynamic Simulations of the Processes. Petrology 28, 263–286. https://doi.org/10.1134/S0869591120030029.</mixed-citation><mixed-citation xml:lang="en">Abramov S.S., Rass I.T., Kononkova N.N., 2020. 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