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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">litosphere</journal-id><journal-title-group><journal-title xml:lang="ru">Литосфера</journal-title><trans-title-group xml:lang="en"><trans-title>LITHOSPHERE (Russia)</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1681-9004</issn><issn pub-type="epub">2500-302X</issn><publisher><publisher-name>A.N. Zavaritsky Institute of Geology and Geochemistry</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24930/1681-9004-2023-23-4-603-621</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1916</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>U-Pb (LA-ICP-MS) возраст детритовых цирконов из песчаников кратерной части кимберлитовой трубки им. В. Гриба и магматического объекта KL-01, Архангельская алмазоносная провинция (север Восточно-Европейской платформы)</article-title><trans-title-group xml:lang="en"><trans-title>U-Pb (LA-ICP-MS) age of detrital zircons from sandstones of the crater part of the V. Grib kimberlite pipe and KL-01 magmatic object, Arkhangelsk diamondiferous province (north of the East European Platform)</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>Агашева</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Agasheva</surname><given-names>E. 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>Elena V. Agasheva.</p><p>3 Academician Koptyug av., Novosibirsk 630090</p></bio><email xlink:type="simple">shchukinalena@igm.nsc.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><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>V.S. Sobolev Institute of Geology and Mineralogy, SB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>06</day><month>09</month><year>2023</year></pub-date><volume>23</volume><issue>4</issue><fpage>603</fpage><lpage>621</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Агашева Е.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Агашева Е.В.</copyright-holder><copyright-holder xml:lang="en">Agasheva E.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.lithosphere.ru/jour/article/view/1916">https://www.lithosphere.ru/jour/article/view/1916</self-uri><abstract><p>Объект исследования. Обломочные цирконы из песчаников, не содержащих какую-либо примесь магматического (туфогенного) материала, отобранных из кратерных частей высокоалмазоносной кимберлитовой трубки им. В. Гриба и магматического объекта KL-01. Оба объекта расположены на севере Восточно-Европейской платформы, в пределах Архангельской алмазоносной провинции, на расстоянии ≈100 км друг от друга. Цель. Получить первые данные по составу U-Pb изотопной системы обломочных цирконов из песчаников магматических объектов Архангельской алмазоносной провинции для возрастных оценок их источников сноса и установления корреляций с известными тектонотермальными событиями в континентальной коре региона. Материалы и методы. Методом LA-ICP-MS получены данные по составу U-Pb изотопной системы 52 зерен цирконов из песчаников трубки им. В. Гриба и 143 зерен цирконов из песчаников объекта KL-01. Результаты. Для изученных цирконов установлены разновозрастные источники сноса - от архейских до неопротерозойских, но с преобладанием мезопротерозойских, которым отвечают 63 и 65% зерен из трубки им. В. Гриба и объекта KL-01 соответственно. Для цирконов из песчаников трубки им. В. Гриба отмечается большее количество зерен мезо- и неоархейского (≈15%) и меньшее палеопротерозойского (≈14%) возраста по сравнению с таковыми из объекта KL-01 (≈7 и 20% соответственно). Для двух объектов установлено отсутствие цирконов, возраст которых соответствует интервалу 900-700 млн лет. Минимальный возраст цирконов из песчаников кратера трубки им. В. Гриба (557 ± 9 млн лет) и объекта KL-01 (609 ± 9 млн лет) согласуется с определенным возрастом формирования вендских песчаников в районе трубок Архангельской алмазоносной провинции. Выводы. Полученные U-Pb возрастные оценки для изученных обломочных цирконов в целом коррелируют с выявленными ранее этапами тектонотермальных событий в континентальной коре северных территорий Восточно-Европейской платформы, за исключением мезопротерозойского периода 1.7-1.4 и 1.3-1.0 млрд лет назад, которому соответствует преобладающая часть U-Pb возрастных значений изученных цирконов.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. Detrital zircons from sandstones that contain no admixtures of magmatic material, sampled from the crater parts of the highly diamondiferous V. Grib kimberlite pipe and KL-01 magmatic object. Both objects are located in the north of the East European Platform, within the Arkhangelsk diamondiferous province, at a distance of ≈100 km from each other. Aim. To obtain the first data on the composition of the U-Pb isotope system of detrital zircons from sandstones of magmatic objects of the Arkhangelsk diamondiferous province in order to evaluate the ages of their sources and reveal correlations with known tectono-thermal events in the continental crust of the region. Materials and methods. Using the LA-ICP-MS method, data were obtained on the composition of the U-Pb isotopic system of 52 zircon grains from the sandstones of the V. Grib pipe and 143 zircon grains from the KL-01 sandstones. Results. Sources of various ages from Archean to Neoproterozoic were established for the studied zircons. However, the majority zircons have Mesoproterozoic age, namely 63 and 65% of grains from the V. Grib pipe and KL-01 object, respectively. The sandstones of the V. Grib pipe contain a larger amount of Meso- and Neo-Archean zircons (≈15%) and a smaller amount of Paleoproterozoic grains (≈14%) compared to those from the KL-01 object ≈7 and 20%, respectively. The population of zircons with the U-Pb ages of 900-700 Ma is absent in the two objects. The minimum age of zircons from sandstones of the crater of the V. Grib pipe (557 ± ± 9 Ma) and KL-01 object (609 ± 9 Ma) is consistent with that of formation of the Vendian sandstones in the area of the pipes of the Arkhangelsk diamondiferous province. Conclusions. The obtained U-Pb age for the studied detrital zircons generally correlate with the previously identified stages of tectono-thermal events in the continental crust of the northern territories of the East European Platform, with the exception of the Mesoproterozoic period 1.7-1.4 and 1.3-1.0 Ga ago, which corresponds to the predominant part U-Pb age values of the studied zircons.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>кимберлитовая трубка</kwd><kwd>кратер</kwd><kwd>восточно-европейская платформа</kwd><kwd>песчаник</kwd><kwd>циркон</kwd><kwd>континентальная кора</kwd><kwd>магматизм</kwd><kwd>седиментация</kwd></kwd-group><kwd-group xml:lang="en"><kwd>kimberlite pipe</kwd><kwd>crater part</kwd><kwd>East European platform</kwd><kwd>sandstone</kwd><kwd>zircon</kwd><kwd>continental crust</kwd><kwd>magmatism</kwd><kwd>sedimentation</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Все аналитические работы выполнены при поддержке Российского научного фонда, грант № 20-77-10018. Отбор образцов песчаников из кратерной части кимберлитовой трубки им. в. Гриба и магматического объекта Kl-01 выполнен по государственному заданию ИГМ СО РАН (№ 122041400157-9)</funding-statement><funding-statement xml:lang="en">All analytical works were supported by the Russian Science Foundation (grant No. 20-77-10018, https://rscf.ru/project/20-77-10018). Sampling of sandstones from the crater parts of the V. Grib kimberlite pipe and the Kl-01 magmatic object was carried out due to the state assignment of IGM SB RAS (No. 122041400157-9)</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">Агашев А.М., Кулигин С.С., Орихаши Ю., Похиленко Н.П., Вавилов М.А., Кларк Д. (2008) Цирконы из осадочного коллектора долины реки Блюфиш (северо-западные территории Канады) и возможный возраст кимберлитового магматизма площади Лена-Вест. Докл. 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