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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">10.24930/2500-302X-2024-24-3-507-525</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-2098</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>Кварциты хобеинской свиты Приполярного Урала: вещественный состав, возрастные ограничения и возможные источники сноса терригенного материала</article-title><trans-title-group xml:lang="en"><trans-title>Quartzites of the Khobeinskaya suite of the Subpolar Urals: Material composition, age limitations and possible sources of terrigenous material</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>Попвасев</surname><given-names>К. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Popvasev</surname><given-names>K. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>54 Pervomayskaya st., 167982 Syktyvkar</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>Пыстин</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Pystin</surname><given-names>A. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>54 Pervomayskaya st., 167982 Syktyvkar</p></bio><email xlink:type="simple">pystin.48@mail.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>Гракова</surname><given-names>О. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Grakova</surname><given-names>O. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>54 Pervomayskaya st., 167982 Syktyvkar</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>Пыстина</surname><given-names>Ю. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Pystina</surname><given-names>Yu. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>54 Pervomayskaya st., 167982 Syktyvkar</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>Кушманова</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kushmanova</surname><given-names>E. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167982, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>54 Pervomayskaya st., 167982 Syktyvkar</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>Хубанов</surname><given-names>В. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Khubanov</surname><given-names>V. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>670047, г. Улан-Удэ, ул. Сахьяновская, 6а</p></bio><bio xml:lang="en"><p>6a Sakhyanovskaya st., 670047 Ulan-Ude</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии им. Н.П. Юшкина ФИЦ Коми НЦ УрО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>N.P. Yushkin Institute of Geology, FRC Komi Science Center, UB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Геологический институт им. Н.Л. Добрецова СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>N.L. Dobretsov Geological Institute SB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>08</day><month>07</month><year>2024</year></pub-date><volume>24</volume><issue>3</issue><fpage>507</fpage><lpage>525</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Попвасев К.С., Пыстин А.М., Гракова О.В., Пыстина Ю.И., Кушманова Е.В., Хубанов В.Б., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Попвасев К.С., Пыстин А.М., Гракова О.В., Пыстина Ю.И., Кушманова Е.В., Хубанов В.Б.</copyright-holder><copyright-holder xml:lang="en">Popvasev K.S., Pystin A.M., Grakova O.V., Pystina Y.I., Kushmanova E.V., Khubanov V.B.</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/2098">https://www.lithosphere.ru/jour/article/view/2098</self-uri><abstract><p>Объект исследований. Кварциты, слагающие гребневую часть хр. Росомаха в северной части Ляпинского мегантиклинория на Приполярном Урале. Материал и методы. Из кварцитов выделены детритовые цирконы и выполнены оптические и изотопно-геохронологические U-Pb (LA-SF-ICP-MS) исследования. На основе химических анализов пород с использованием индикаторных соотношений и коэффициентов установлены условия образования отложений. Результаты. Определена стратиграфическая позиция кварцитов хр. Россомаха. Уточнены время и условия формирования хобеинской свиты. Дана оценка роли полиметаморфических комплексов Приполярного Урала как возможных источников сноса терригенного материала при формировании верхнедокембрийского разреза Приполярного Урала. Выводы. Установлена принадлежность кварцитов хр. Росомаха к хобеинской свите, возраст которой ограничивается интервалом 850–800 млн лет (инзерский уровень). Показано, что источниками сноса терригенного материала могли быть кристаллические комплексы Фенноскандии и Среднерусского орогена, а также полиметаморфические комплексы кристаллического фундамента Тимано-Североуральской окраины Восточно-Европейской платформы.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. Quartzites that make up the ridge part of the ridge Rosomaha in the northern part of the Lyapinsky meganticlinorium in the Subpolar Urals. Material and methods. Detrital zircons were isolated from quartzites and their optical and isotope-geochronological U-Pb (LA-SF-ICP-MS) studies were performed. On the basis of chemical analyzes of rocks using indicator ratios and coefficients, the conditions for the formation of deposits were established. Results. The stratigraphic position of the quartzite ridge Rosomaha was determined. The time and conditions for the formation of the Khobeinskaya formation were specified. The role of polymetamorphic complexes of the Subpolar Urals as possible sources of terrigenous material removal during the formation of the Upper Precambrian section of the Subpolar Urals was estimated. Conclusions. It was established that the quartzites belong to the ridge Rosomaha to the Khobeinskaya formation, whose age is limited to the interval of 850–800 Ma (Inzersky level). It is shown that the crystalline complexes of Fennoscandia and the Central Russian orogen, as well as polymetamorphic complexes of the crystalline basement of the Timan-Severoural margin of the East European Platform, could be sources of terrigenous material.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Приполярный Урал</kwd><kwd>рифей</kwd><kwd>хобеинская свита</kwd><kwd>кварциты</kwd><kwd>источники сноса</kwd><kwd>циркон</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Subpolar Urals</kwd><kwd>Riphean</kwd><kwd>Khobeinskaya formation</kwd><kwd>quartzites</kwd><kwd>provenances</kwd><kwd>zircon</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при финансовой поддержке РНФ. Проект № 22-27-00119</funding-statement><funding-statement xml:lang="en">The work was supported by the Russian Science Foundation. 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