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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">10.24930/1681-9004-2022-22-4-448-471</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1687</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>Железисто-глиноземистые метапелиты Северо-Енисейского кряжа: палеообстановки формирования, природа и возраст протолита</article-title><trans-title-group xml:lang="en"><trans-title>Ferruginious-aluminous metapelites of the North Yenisei Ridge: Formation paleosettings, nature and age of protolith</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>Лиханов</surname><given-names>И. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Likhanov</surname><given-names>I. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>СО РАН</p><p>Институт геологии и минералогии</p><p>630090</p><p>просп. Акад. Коптюга, 3</p><p>Новосибирск</p></bio><bio xml:lang="en"><p>Igor I. Likhanov</p><p>SB RAS</p><p>V. S. Sobolev Institute of Geology and Mineralogy</p><p>630090</p><p>3 Akad. Koptyug аv.</p><p>Novosibirsk</p></bio><email xlink:type="simple">likh@igm.nsc.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Козлов</surname><given-names>П. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Kozlov</surname><given-names>P. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>УрО РАН</p><p>Институт геологии и геохимии</p><p>620110</p><p>ул. Акад. Вонсовского, 15</p><p>Екатеринбург</p></bio><bio xml:lang="en"><p>Pavel S. Kozlov</p><p>UB RAS</p><p>620110</p><p>15 Akad. Vonsovsky st.</p><p>Ekaterinburg</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>Попов</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Popov</surname><given-names>N. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>СО РАН</p><p>Институт нефтегазовой геологии и геофизики</p><p>630090</p><p>просп. Акад. Коптюга, 3</p><p>Новосибирск</p></bio><bio xml:lang="en"><p>Nikolai V. Popov</p><p>SB RAS</p><p>A. A. Trofimuk Institute of Petroleum Geology and Geophysics</p><p>630090</p><p>3 Akad. Koptyug аv.</p><p>Novosibirsk</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">РАН<country>Россия</country></aff><aff xml:lang="en">RAS<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>02</day><month>09</month><year>2022</year></pub-date><volume>22</volume><issue>4</issue><fpage>448</fpage><lpage>471</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лиханов И.И., Козлов П.С., Попов Н.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Лиханов И.И., Козлов П.С., Попов Н.В.</copyright-holder><copyright-holder xml:lang="en">Likhanov I.I., Kozlov P.S., Popov N.V.</copyright-holder><license 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/1687">https://www.lithosphere.ru/jour/article/view/1687</self-uri><abstract><sec><title>   Предмет исследования</title><p>   Предмет исследования. Изучались неоднородные по Р-Т условиям метаморфизма железисто-глиноземистые метапелиты тейского, гаревского и приангарского комплексов Северо-Енисейского кряжа (западная окраина Сибирского кратона).</p></sec><sec><title>   Методы исследования</title><p>   Методы исследования. На основании анализа новых геохронологических (U-Pb SHRIMP-II датирование по цирконам) и геохимических данных по распределению главных и редких элементов в породах проведена реконструкция состава, условий формирования и возраста их протолита.</p></sec><sec><title>   Результаты</title><p>   Результаты. Железисто-глиноземистые метапелиты Северо-Енисейского кряжа представляют собой переотложенные и метаморфизованные продукты докембрийских кор выветривания преимущественно каолинитового, а не латеритного типа, как считалось ранее. Химическое выветривание пород в раннем протерозое на Енисейском кряже не достигало глубокой стадии латеритизации с образованием зон конечного разложения алюмосиликатов, а ограничивалось формированием продуктов выветривания преимущественно каолинитллит-монтмориллонит-кварцевого состава.</p></sec><sec><title>   Выводы</title><p>   Выводы. Петро- и геохимические характеристики изученных метапелитов обусловлены главным образом особенностями осадконакопления при формировании протолита, образование которого могло происходить за счет размыва нижнепротерозойских микрогнейсов Сибирского кратона с возрастами в диапазоне 2043–1962 млн лет с примесью материала кислых и основных пород (сухопитская серия) и последующего накопления в окраинно-континентальных мелководных бассейнах в условиях гумидного климата и спокойного тектонического режима. Полученные выводы о природе и составе протолита этих пород согласуются с данными литолого-фациального анализа и геодинамическими реконструкциями эволюции геологических комплексов Северо-Енисейского кряжа в докембрии.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>   Research subject</title><p>   Research subject. Fe- and Al-rich metapelites of the Teya, Garevka and Angara complexes of the North Yenisei Ridge (western margin of the Siberian craton) were studied.</p></sec><sec><title>   Research methods</title><p>   Research methods. Recently-obtained geochronologic (SHRIMP II U-Pb zircon dating) and geochemical data on the distribution of major and trace elements were used to reproduce the composition and age of the protolith, along with the paleofacies formation conditions.</p></sec><sec><title>   Results</title><p>   Results. The ferruginous-aluminous metapelites of the North Yenisei Ridge consitute redeposited and metamorphosed products of Precambrian weathering crusts predominantly of the kaolinite rather than lateritic type, as was previously thought. The chemical weathering of rocks in the Early Proterozoic on the Yenisei Ridge did not reach the deep stage of lateritization with the formation of zones of final decomposition of aluminosilicates; however, this process was limited to the formation of weathering products of predominantly kaolinite-illite-montmorillonite-quartz composition.</p></sec><sec><title>   Conclusions</title><p>   Conclusions. The petro- and geochemical characteristics of the studied metapelites are mainly due to the features of sedimentation during the formation of the protolith, which could have been formed due to the erosion of the Lower Proterozoic microgneisses of the Siberian craton with ages in the range of 1962-2043 Ma with the involvement of granitoid and volcanic admixture of mafic rocks into the erosion area and subsequent accumulation in marginal continental shallow basins under the conditions of a humid climate and a calm tectonic regime. These results are consistent with the data of lithofacies analysis and geodynamic reconstructions of the Precambrian evolution of geological complexes in the North Yenisei Ridge.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>метапелиты</kwd><kwd>геохимия</kwd><kwd>палеообстановки</kwd><kwd>протолиты</kwd><kwd>U-Pb датирование циркона</kwd><kwd>Северо-Енисейский кряж</kwd></kwd-group><kwd-group xml:lang="en"><kwd>metapelites</kwd><kwd>geochemistry</kwd><kwd>protoliths</kwd><kwd>paleosettings</kwd><kwd>U-Pb zircon dating</kwd><kwd>North Yenisei Ridge</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Работа выполнена за счет средств гранта Российского научного фонда (проект № 21-77-20018) с частичной поддержкой полевых работ по госзаданиям ИГМ СО РАН и ИГГ УрО РАН (АААА-А18-118052590032-6)</funding-statement></funding-group><funding-group xml:lang="en"><funding-statement>This research was funded by Russian Science Foundation (RSF), grant No. 21-77-20018 with additional support of field works in the framework of the state tasks of the Institute of Geology and Mineralogy (Novosibirsk) and Institute of Geology and Geochemistry (Ekaterinburg) (АААА-А18-118052590032-6)</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">Балашов Ю. 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