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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">10.24930/1681-9004-2022-22-5-624-643</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1729</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>Пермско-триасовые трапповые вулканиты в доюрском фундаменте арктической части Западно-Сибирской платформы</article-title><trans-title-group xml:lang="en"><trans-title>Permian-Triassic ﬂood basalts in the pre-Jurassic basement of the Arctic zone of the West Siberian 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>Берзин</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Berzin</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г Екатеринбург, ул. Акад. Вонсовского, 15</p></bio><bio xml:lang="en"><p>Stepan V. Berzin</p><p>15 Acad. Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">sbersin@yandex.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>Иванов</surname><given-names>К. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>K. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г Екатеринбург, ул. Акад. Вонсовского, 15</p></bio><bio xml:lang="en"><p>Kirill S. Ivanov</p><p>15 Acad. Vonsovsky st., Ekaterinburg 620110</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Панкрушина</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Pankrushina</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г Екатеринбург, ул. Акад. Вонсовского, 15</p></bio><bio xml:lang="en"><p>Elizaveta A. Pankrushina</p><p>15 Acad. Vonsovsky st., Ekaterinburg 620110</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Солошенко</surname><given-names>Н. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Soloshenko</surname><given-names>N. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г Екатеринбург, ул. Акад. Вонсовского, 15</p></bio><bio xml:lang="en"><p>Nataliya G. Soloshenko</p><p>15 Acad. Vonsovsky st., Ekaterinburg 620110</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Институт геологии и геохимии им. А.Н. Заварицкого 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><aff-alternatives id="aff-2"><aff xml:lang="ru">Институт геологии и геохимии им. А. Н. Заварицкого 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>2022</year></pub-date><pub-date pub-type="epub"><day>04</day><month>11</month><year>2022</year></pub-date><volume>22</volume><issue>5</issue><fpage>624</fpage><lpage>643</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Берзин С.В., Иванов К.С., Панкрушина Е.А., Солошенко Н.Г., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Берзин С.В., Иванов К.С., Панкрушина Е.А., Солошенко Н.Г.</copyright-holder><copyright-holder xml:lang="en">Berzin S.V., Ivanov K.S., Pankrushina E.A., Soloshenko N.G.</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/1729">https://www.lithosphere.ru/jour/article/view/1729</self-uri><abstract><sec><title>Объект исследования</title><p>Объект исследования. Пермско-триасовые трапповые вулканиты в фундаменте арктической части Западно-Сибирской платформы залегают преимущественно в грабен-рифтовых структурах. Трапповые вулканиты в данном регионе характеризуются наименьшей изученностью, по сравнению с другими районами их распространения, главным образом из-за значительной глубины залегания (4–6 км и более).</p></sec><sec><title>Материалы и методы</title><p>Материалы и методы. В ходе работы были иcследованы 36 образцов керна из 11 сверхглубоких и глубоких скважин. Изотопные отношения измерены на масс-спектрометрах NEPTUNE PLUS (Nd, Sm) и TRITON PLUS (Rb, Sr). Изучение битума производилось при помощи рамановского спектрометра LabRAM HR800 Evolution. Выполнена деконволюция рамановских спектров (процедуры “Peak ﬁtting”) и оценена температура преобразования битума.</p></sec><sec><title>Результаты</title><p>Результаты. Около половины образцов вулканитов подверглись метаморфизму пренит-пумпеллиитовой и местами зеленосланцевой фации или интенсивным низкотемпературным гидротермальным изменениям. По геохимическим характеристикам изученные базальты близки к типичным трапповым базальтам, но имеют некоторое сходство с островодужными вулканитами. Впервые найдены тонкие включения битума в миндалинах пермско-триасовых базальтов в сверхглубокой скважине Тюменская СГ-6 на глубине 7310.6 м. Показано высокое сходство изученных вулканитов по геохимическим характеристикам и изотопному составу Sr и Nd с траппами Сибирской платформы.</p></sec><sec><title>Выводы</title><p>Выводы. Наличие в некоторых проанализированных образцах отрицательной аномалии по Ta, Nb, Ti, а также отрицательной Ce-аномалии свидетельствует о возможной контаминации изученных базальтов островодужными вулканитами и вулканогенно-осадочными породами. Температура преобразования битума во включениях в базальтах из скв. Тюменская СГ-6, по данным рамановской спектроскопии, 150–300°C и в целом соответствует температуре метаморфизма вмещающей базальтовой толщи. Присутствие битума в миндалинах может быть свидетельством его миграции через базальтовую толщу углеводородов.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>Research subject</title><p>Research subject. Permian-Triassic ﬂood basalts in the basement of the Arctic zone of the West Siberian Platform locate mainly in graben-rift structures. Flood basalts in this region remain to be understudied in comparison with other areas of its distribution, mainly due to the signiﬁcant depth of their occurrence (4–6 km).</p></sec><sec><title>Materials and methods</title><p>Materials and methods. 36 core samples from 11 superdeep and deep boreholes were studied. Isotopic ratios were measured on mass spectrometers NEPTUNE PLUS (Nd, Sm) and TRITON PLUS (Rb, Sr). Bitumen were studied using a Raman spectrometer LabRAM HR800 Evolution. The Raman spectra were deconvoluted (“Peak ﬁtting” procedure), and the bitumen conversion temperature was estimated.</p></sec><sec><title>Results</title><p>Results. About half of the samples of volcanic rocks underwent metamorphism of the prehnite-pumpellite and locally greenschist facies or intense low-temperature hydrothermal alteration. The studied basalts are close to typical ﬂood basalts and are somewhat similar to island-arc volcanic rocks in terms of their geochemical characteristics. For the ﬁrst time, thin inclusions of bitumen were found in the amygdalae of Permian-Triassic basalts in the superdeep borehole Tyumenskaya SG-6 at a depth of 7310.6 m. A high similarity of the studied volcanics by geochemical characteristics and the isotopic composition of Sr and Nd with the ﬂood basalts of the Siberian platform is shown.</p></sec><sec><title>Conclusions</title><p>Conclusions. The presence of a negative Ta, Nb, Ti anomaly, as well as a negative Ce anomaly, in some of the analyzed samples indicates a possible contamination of the basalts by island arc volcanics and volcanogenic-sedimentary rocks. The temperature of transformation of bitumen in inclusions in basalts from the well Tyumenskaya SG-6 according to Raman spectroscopy is estimated at 150–300°C and generally corresponds to the temperature of metamorphism of the host basalts. The presence of bitumen in the amygdalae may indicate the migration of hydrocarbons through the basalts.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>трапповые базальты</kwd><kwd>триас</kwd><kwd>Западо-Сибирская платформа</kwd><kwd>доюрский фундамент</kwd><kwd>Арктика</kwd><kwd>сверхглубокие скважины</kwd><kwd>Ен-Яхинская СГ-7</kwd><kwd>Тюменская СГ-6</kwd><kwd>битум</kwd></kwd-group><kwd-group xml:lang="en"><kwd>ﬂood basalts</kwd><kwd>Triassic</kwd><kwd>West Siberian platform</kwd><kwd>pre-Jurassic basement</kwd><kwd>Arctic</kwd><kwd>superdeep boreholes</kwd><kwd>Yen-Yakhinskaya SG-7</kwd><kwd>Tyumenskaya SG-6</kwd><kwd>bitumen</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Исследования выполнялись в рамках государственного задания ИГГ УрО РАН, тема № АААА-А18-118052590032-6 с использованием оборудования ЦКП “Геоаналитик” ИГГ УрО РАН. Изотопные измерения и рамановская спектроскопия выполнены в рамках государственного задания ИГГ УрО РАН, тема АААА-А18-118053090045-8, с использованием оборудования ЦКП “Геоаналитик” ИГГ УрО РАН. Дооснащение и комплексное развитие ЦКП “Геоаналитик” ИГГ УрО РАН осуществляются при финансовой поддержке гранта Министерства науки и высшего образования Российской Федерации, cоглашение № 075-15-2021-680. Авторы признательны В.С. Бочкареву за предоставленные образцы вулканитов и аналитикам лаборатории ФХМИ ИГГ УрО РАН к.г.-м.н. Д.В. Киселевой, Т.Г. Окуневой, Н.П. Горбуновой, Н.В. Чередниченко.</funding-statement></funding-group><funding-group xml:lang="en"><funding-statement>The studies are carried out as a part of the IGG uB RAS State assignment (state registration No. АААА-А18-118052590032-6) using the “Geoanalitik” shared research facilities of the IGG uB RAS. Isotopic measurements and Raman spectroscopy are carried out as a part of the IGG uB RAS State assignment (state registration No. АААА-А18-118053090045-8) using the “Geoanalitik” shared research facilities of the IGG uB RAS. The re-equipment and comprehensive development of the “Geoanalitik” shared research facilities of the IGG uB RAS is ﬁnancially supported by the grant of the Ministry of Science and higher Education of the Russian Federation (Agreement No. 075-15-2021-680). The authors are grateful to V.S. Bochkarev for providing samples of volcanic rocks and to the analysts of the laboratory of the FKhMI IGG UB RAS Ph.D. D.V. Kiseleva, T.G. Okuneva, N.P. Gorbunova, N.V. Cherednichenko.</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">Альмухамедов А.И., Медведев А.Я., Золотухин В.В. 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