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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-2022-13-5-0669</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1580</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>ИСТОЧНИКИ СНОСА И ОГРАНИЧЕНИЕ ВОЗРАСТА РИФЕЙСКИХ ПЕСЧАНИКОВ ИВАНОВСКОГО ГРАБЕНА КОЛЬСКОГО ПОЛУОСТРОВА ПО РЕЗУЛЬТАТАМ U-Pb LA-ICP-MS ДАТИРОВАНИЯ И РАМАНОВСКОЙ СПЕКТРОСКОПИИ ОБЛОМОЧНОГО ЦИРКОНА</article-title><trans-title-group xml:lang="en"><trans-title>PROVENANCE AND AGE CONSTRAINTS OF THE RIPHEAN SANDSTONES FROM THE IVANOVSKY GRABEN (THE KOLA PENINSULA) BASED ON THE U-Pb LA-ICP-MS DATING AND RAMAN SPECTROSCOPY OF DETRITAL ZIRCON</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>Чистякова</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Chistyakova</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119991, Москва, Ленинские горы, 1</p><p>123242, Москва, ул. Большая Грузинская, 10, стр. 1</p></bio><bio xml:lang="en"><p>1 Leninskie Gory, Moscow 119991</p><p>10-1 Bolshaya Gruzinskaya St, Moscow 123242</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>Веселовский</surname><given-names>Р. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Veselovskiy</surname><given-names>R. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119991, Москва, Ленинские горы, 1</p><p>123242, Москва, ул. Большая Грузинская, 10, стр. 1</p></bio><bio xml:lang="en"><p>1 Leninskie Gory, Moscow 119991</p><p>10-1 Bolshaya Gruzinskaya St, Moscow 123242</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>Семёнова</surname><given-names>Д. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Semenova</surname><given-names>D. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет им. М.В. Ломоносова; Институт физики Земли им. О.Ю. Шмидта РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University; Schmidt Institute of Physics of the Earth, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт геологии и минералогии им. В.С. Соболева СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Sobolev Institute of Geology and Mineralogy, Siberian 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>10</day><month>12</month><year>2022</year></pub-date><volume>13</volume><issue>5</issue><fpage>669</fpage><lpage>669</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Чистякова А.В., Веселовский Р.В., Семёнова Д.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Чистякова А.В., Веселовский Р.В., Семёнова Д.В.</copyright-holder><copyright-holder xml:lang="en">Chistyakova A.V., Veselovskiy R.V., Semenova D.V.</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/1580">https://www.gt-crust.ru/jour/article/view/1580</self-uri><abstract><p>Приводятся первые результаты U-Pb LA-ICP-MS изотопного датирования 150 зерен обломочного циркона из докембрийских (рифейских?) песчаников кильдинской серии губы Ивановской северо-востока Кольского полуострова. По группе из трех самых молодых зерен получено нижнее ограничение на время накопления песчаников – 1179±45 млн лет. В распределении возрастов зерен циркона доминируют три максимума – 1.9, 2.4 и 2.7 млрд лет. Авторы рассматривают два взаимодополняющих варианта интерпретации полученных данных. Первый вариант предполагает вклад удаленных источников сноса – гранитоидов Лапландско-Кольского орогена (~1.9 млрд лет) и сопряженных с ними областей Карельско-Кольского региона (~2.7 млрд лет), Имандра-Варзугской структуры (~2.4 млрд лет), Свеконорвежского пояса (~1.2 млрд лет); вероятны также и внебалтийские (гренландские?) источники. Согласно второму варианту, в Ивановский грабен циркон поступал, в том числе, из проксимальных источников – сиалических комплексов, сформированных при плавлении гранитогнейсов верхней коры Мурманского кратона в ходе эпизодов масштабного базитового магматизма 1.86, 2.50 и 2.68 млрд лет назад. Методом рамановской спектроскопии показано, что примерно 25 % проанализированных зерен обломочного циркона около 1.4 млрд лет назад испытали воздействие термального события, не приведшего к потерям Pb, но частично восстановившего кристаллическую структуру циркона. Этот результат может использоваться как дополнительное ограничение при проведении детального анализа питающих провинций осадочных бассейнов северо-восточной части Восточно-Европейской платформы и указывает на масштабность проявления магматических событий около 1.4 млрд лет назад, связанных с распадом суперконтинента Нуна.</p></abstract><trans-abstract xml:lang="en"><p>The results of U-Pb LA-ICP-MS dating of 150 detrital zircon grains from the Precambrian (Riphean?) sandstones of the Kildin group on the coast of the Ivanovka Bay (northeastern Kola Peninsula) are presented. A group of three youngest grains yielded constraint on the sandstone maximum depositional age of 1179±45 Ma. Detrital zircon age distribution is dominated by three maximums of 1.9, 2.4 and 2.7 Ga. The authors consider two complementary scenarios of interpretation of the data obtained. The first scenario involves the contribution of distant provenance out of granitoids in the Lapland-Kola orogen (~1.9 Ga) and adjacent areas of the Kola-Karelia region (~2.7 Ga), Imandra-Varzuga structure (~2.4 Ga), and Sveconorwegian belt (~1.2 Ga); the off-Baltic (Greenland?) sources of the detrital zircon also cannot be excluded. According to the second scenario, the Ivanovsky graben received zircons also from the proximal sources – sialic complexes formed upon melting of granite-gneiss substratum of the upper crust of the Murmansk craton during largescale episodic mafic magmatism 1.86, 2.50 and 2.68 Ga. The Raman spectroscopy showed that about 25 % of the analyzed detrital zircon grains experienced a 1.4-Ga-old thermal effect which did not lead to Pb losses but partially restored the crystalline structure of zircon. This result can be used as an additional constraint in the detailed provenance analysis of the northeastern East European Platform sedimentary basins and is indicative of 1.4-Ga-old large-scale magmatic events related to the breakup of the supercontinent Nuna.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>обломочный (детритовый) циркон</kwd><kwd>U-Pb геохронология</kwd><kwd>рифей</kwd><kwd>Кольский полуостров</kwd><kwd>Ивановский грабен</kwd><kwd>питающие провинции</kwd><kwd>стратиграфическая корреляция</kwd><kwd>спектроскопия комбинационного рассеяния</kwd><kwd>рамановская спектроскопия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>detrital zircon</kwd><kwd>U-Pb geochronology</kwd><kwd>Riphean</kwd><kwd>the Kola Peninsula</kwd><kwd>Ivanovsky graben</kwd><kwd>provenance</kwd><kwd>stratigraphic correlation</kwd><kwd>Raman spectroscopy</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследования выполнены при поддержке грантов Президента РФ МД-1116.2018.5 и РНФ 16-17-10260-П, а также в рамках НИР по государственному заданию ИФЗ РАН и геологического факультета МГУ имени М.В. Ломоносова. Лабораторные исследования проведены с использованием оборудования и инфраструктуры ЦКП «Петрофизика, геомеханика и палеомагнетизм» ИФЗ РАН.</funding-statement><funding-statement xml:lang="en">The study was supported by the RF President’s grant MD-1116.2018.5 and RSF grant 16-17-10260-P, and carried out as part of research projects by state assignment of IPE RAS and Faculty of Geology of Lomonosov Moscow State University. The laboratory researches were conducted using equipment of Shared Research Facilities "Petrophysics, geomechanics and paleomagnetism" IPE RAS.</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">Andreichev V.L., Soboleva A.A., Khubanov V.B., Sobolev I.D., 2018. U-Pb (LA-ICP-MS) Age of Detrital Zircons from Meta-Sedimentary Rocks of the Upper Precambrian Section of Northern Timan. Bulletin of Moscow Society of Naturalists. 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