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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-2024-24-3-479-506</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-2097</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>Особенности вещественного состава верхнекаменноугольно-нижнепермских пород лосиноостровской свиты и роль внебассейновых источников в их формировании (Приполярный Урал)</article-title><trans-title-group xml:lang="en"><trans-title>Composition features of the Upper Carboniferous-Lower Permian rocks of the Losinoostrov Fm. and the role of extrabasin sources in their formation (Subpolar 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>Инкина</surname><given-names>Н. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Inkina</surname><given-names>N. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167000, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>54 Pervomaiskaya st., Syktyvkar 167000</p></bio><email xlink:type="simple">nsinkina@geo.komisc.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>Салдин</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Saldin</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>167000, г. Сыктывкар, ул. Первомайская, 54</p></bio><bio xml:lang="en"><p>54 Pervomaiskaya st., Syktyvkar 167000</p></bio><email xlink:type="simple">litgeo@geo.komisc.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии ФИЦ Коми НЦ УрО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>N.P. Yushkin Institute of Geology, FRC Komi SC UB 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>07</day><month>07</month><year>2024</year></pub-date><volume>24</volume><issue>3</issue><fpage>479</fpage><lpage>506</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Инкина Н.С., Салдин В.А., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Инкина Н.С., Салдин В.А.</copyright-holder><copyright-holder xml:lang="en">Inkina N.S., Saldin V.A.</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/2097">https://www.lithosphere.ru/jour/article/view/2097</self-uri><abstract><p>Объектом исследований являются верхнекаменноугольно-нижнепермские породы лосиноостровской свиты Бельско-Елецкой структурно-формационной зоны, вскрытые на левом берегу р. Кожим в районе устья руч. Нортничаель западного склона Приполярного Урала. Методы оптико- и электронно-микроскопические (в т.ч. катодолюминесценция), анализы химический силикатный, карбонатный и рентгенодифракционный. Результаты и выводы. Изученные породы отнесены к трем основным группам: микстолитам (породам смешанного состава), карбонатолитам и силицитолитам, внутри каждой группы выделены разновидности. Микстолиты состоят из четырех главных компонентов: карбонатного, алевритистого, глинистого и кремнистого. Изменчивое соотношение породообразующих компонентов микстолитов отчетливо отразилось на дискриминационной модульной диаграмме ГМ–(Na2O + K2O), где ГМ = (Al2O3 + TiO2 + Fe2O3 + FeO + MnO)/SiO2). Обособились поля преимущественно кремнисто-алевритистых (кластер I), глинистых (кластер III), а также переходных (кластер II) микстолитов. Среди карбонатолитов выделены относительно чистые и алевритисто-глинисто-кремнистые известняки. Чистые известняки по форменным элементам разделены на биокластовые и пелоидно-микритовые. Силицитолиты представлены: 1) радиоляритами и радиоляриевыми спонголитами; 2) алевритисто-глинистыми силицитолитами и 3) вторичными кремнистыми образованиями. Количественные соотношения породообразующих компонентов показали, что более половины изученных микстолитов в основном сложены материалом внебассейнового происхождения. Относительно повышенные содержания внебассейного тонкого материала в карбонатолитах указывают на периодические ослабления гидродинамического режима во время накопления верхней части свиты. Изученные отложения, вероятно, формировались в обстановках дистального и проксимального рампов.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. The Upper Carboniferous-Lower Permian rocks of the Losinoostrov Formation of the Belsk-Eletsk structural-formational zone, exposed on the left bank of the Kozhim river, near the mouth of the stream Northnichael of the western slope of the Subpolar Urals. Methods. Optical and electron microscopic methods (including cathodoluminescence), chemical silicate, carbonate and X-ray diffraction analyses. Results and conclusions. The studied rocks are assigned to three main groups: mixtolites (rocks of mixed composition), carbonatoliths, and silicytolites with varieties.  Mixtoliths consist of three and four main components: carbonate, silty, argillaceous and siliceous. The variable ratio of rock-forming components of mixtolites was clearly reflected in the discriminative modular diagram. Here, fields of predominantly siliceous and silty mixolites (cluster I), predominantly argillaceous (cluster III), as well as transitional mixolites (cluster II) are identified. Relatively pure and silty-argillaceous-siliceous limestones were distinguished among carbonatoliths. According to the formed elements, pure limestones are divided into bioclastic and peloid-micritic. Silicytolites are represented by (1) radiolarites and radiolarian spongoliths; (2) silty-argillaceous silicytolites and (3) cherts (secondary siliceous formations). The established quantitative ratios of rock-forming components showed that more than half of the studied mixtoliths are composed mainly of the material of extrabasinal origin. Relatively high contents of extrabasinal fine material in carbonatoliths indicate a periodic decrement of the hydrodynamic regime during the accumulation of the upper part of the formation. The studied deposits were probably formed in distal and proximal ramp settings.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Приполярный Урал</kwd><kwd>верхнекаменноугольно-нижнепермские породы</kwd><kwd>лосиноостровская свита</kwd><kwd>микстолиты</kwd><kwd>карбонатолиты</kwd><kwd>силицитолиты</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Subpolar Urals</kwd><kwd>Upper Carboniferous-Lower Permian rocks</kwd><kwd>Losinoostrov Formation</kwd><kwd>mixtoliths</kwd><kwd>carbonate rocks</kwd><kwd>cherts</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа проводилась в рамках государственного задания ИГ ФИЦ Коми НЦ УрО РАН (№ 122040600013-9, FUUU-2022-0054)</funding-statement><funding-statement xml:lang="en">The work was carried out within the framework of the state task of the IG FIC Komi Scientific Center of the Ural Branch of the Russian Academy of Sciences (No. 122040600013-9)</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">Анищенко Л.А., Клименко С.С., Рябинкина Н.Н., Рябинкин С.В., Малышев Н.А., Куплевич И.Л., Захаров А.А., Прозоров С.Ф., Антонов В.И., Иванов В.В., Кузнецов Н.И., Юдин В.М. 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