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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">10.24930/1681-9004-2020-20-6-751-770</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1365</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>Категории водосборов-источников тонкой алюмосиликокластики для отложений серебрянской и сылвицкой серий венда (Средний Урал)</article-title><trans-title-group xml:lang="en"><trans-title>Categories of Vendian catchments – sources of fine-grained aluminosiliciclastic materials for the Serebryanka and Sylvitsa group deposits (Middle Urals)</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>Маслов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Maslov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"><p>15 Akad. Vonsovsky st., Ekaterinburg 620016</p></bio><email xlink:type="simple">amas2004@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Институт геологии и геохимии УрО РАН<country>Россия</country></aff><aff xml:lang="en">A.N. Zavaritsky Institute of Geology and Geochemistry, UB RAS<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>28</day><month>12</month><year>2020</year></pub-date><volume>20</volume><issue>6</issue><fpage>751</fpage><lpage>770</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Маслов А.В., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Маслов А.В.</copyright-holder><copyright-holder xml:lang="en">Maslov A.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/1365">https://www.lithosphere.ru/jour/article/view/1365</self-uri><abstract><sec><title>Объект исследований</title><p>Объект исследований. В статье рассмотрен ряд геохимических особенностей (распределение лантаноидов и Th, значения (La/Yb)N и Eu/Eu*) тонкозернистых обломочных/глинистых пород различных региоярусов венда западного склона Среднего Урала. Для интерпретации результатов привлечены также данные о составе водосборов ряда современных рек и сведения о распределении тех же характеристик во взвеси и поверхностных донных осадках системы “нижнее течение р. Сев. Двина–Белое море”.</p></sec><sec><title>Материалы и методы</title><p>Материалы и методы. Материалом для исследований послужили данные о содержании La, Sm, Eu, Gd, Yb и Th в почти 200 образцах глинистых сланцев и аргиллитов серебрянской и сылвицкой серий. Методом исследований являлся анализ локализации индивидуальных и средних точек состава глинистых пород лапландского, редкинского, беломорского и котлинского региоярусов на парных диаграммах (La/Yb)N–Eu/Eu* и (La/Yb)N–Th, разработанных на основе аналитических данных о составе донных осадков приустьевых частей разных категорий/классов современных рек.</p></sec><sec><title>Результаты</title><p> Результаты. Показано, что осадочные последовательности западного склона Среднего Урала в основном сложены тонкозернистым обломочным материалом, относящимся к категориям 1 (осадки крупных рек/world’s major rivers) и 2 (осадки рек, дренирующих осадочные образования/rivers draining “mixed/sedimentary” formations). Этот материал поступал в область осадконакопления, вероятно, с востока, из разрушавшегося кадомского Варангер-Канино-Тиманского складчато-надвигового пояса/Тиманского орогена, и/или с запада (рифейские осадочные последовательности Камско-Бельского авлакогена). Определенный вклад вносили, возможно, также магматические и метаморфические породы фундамента Восточно-Европейской платформы, слагавшие структуры, которые в рамках современной классификации можно отнести к категории “igneous/metamorphic terranes”.</p></sec><sec><title>Выводы</title><p>Выводы. Полученные результаты не противоречат выводам, сделанным ранее в результате минералого-петрографических исследований конгломератов и песчаников серебрянской и сылвицкой серий, а также данным ранее выполненного геохимического анализа глинистых пород.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>Research subject</title><p>Research subject. The article discusses a number of geochemical features (distribution of lanthanides and Th, values of (La/Yb)N and Eu/Eu*) of fine-grained clastic/clay rocks of various Vendian regional stages of the western slope of the Middle Urals. The results were interpreted in the context of data on the composition of the catchment areas of a number of modern rivers and information on the distribution of the same characteristics in suspended matter and modern bottom sediments of the “downstream North Dvina River–White Sea”.</p></sec><sec><title>Methods and materials</title><p>Methods and materials. The content of La, Sm, Eu, Gd, Yb, and Th in as many as 200 samples of shales and mudstones of the Serebryanka and Sylvitsa groups served as a research material. The research method was an analysis of the localization of individual and average data points of clayey rocks of the Laplandian, Redkinian, Belomorian and Kotlinian regional stages on paired diagrams (La/Yb)N–Eu/Eu* and (La/Yb)N–Th developed on the basis of analytical data on the composition of bottom sediments of estuarine parts of different categories/classes of modern rivers.</p></sec><sec><title>Results</title><p> Results. It was shown that the sedimentary sequences of the western slope of the Middle Urals are mainly composed of fine-grained clastic material belonging to categories 1 (sediments of world major rivers) and 2 (sediments of rivers draining sedimentary/mixed sedimentary formations). This material is likely to have entered the sedimentation area from the east, from the growing Kadomian Varanger-Kanin-Timan folded-thrust belt/Timan orogen, or/and from the west (Riphean sedimentary sequences of Kama-Belsk aulacogen). In addition, the igneous and metamorphic rocks of the East European Platform basement composing the structures, which could be classified as “igneous/metamorphic terranes” under modern classification, were likely to have made a certain contribution.</p></sec><sec><title>Conclusions</title><p> Conclusions. The obtained results agree well with the conclusions obtained earlier as a result of mineralogical and petrographic studies of the conglomerates and sandstones of the Serebryanka and Sylvitsa groups, as well as with the data from a previous geochemical analysis of clay rocks.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>венд</kwd><kwd>западный склон Среднего Урала</kwd><kwd>распределение лантаноидов и Th</kwd><kwd>категории водосборов</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Vendian</kwd><kwd>western slope of the Middle Urals</kwd><kwd>distribution of lanthanides and Th</kwd><kwd>categories of catchments</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Аблизин Б.Д., Клюжина М.Л., Курбацкая Ф.А., Курбацкий А.М. (1982) Верхний рифей и венд западного склона Среднего Урала. 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