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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">geolmsu</journal-id><journal-title-group><journal-title xml:lang="ru">ВЕСТНИК МОСКОВСКОГО УНИВЕРСИТЕТА. СЕРИЯ 4. ГЕОЛОГИЯ</journal-title><trans-title-group xml:lang="en"><trans-title>Moscow University Bulletin. Series 4. Geology</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0579-9406</issn><publisher><publisher-name>Издательский Дом МГУ</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.33623/0579-9406-2022-4-3-20</article-id><article-id custom-type="elpub" pub-id-type="custom">geolmsu-477</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></article-categories><title-group><article-title>Формы проявления мелового вулканизма и интрузивного магматизма в районе поднятия Менделеева (Арктический океан) по данным сейсморазведки</article-title><trans-title-group xml:lang="en"><trans-title>Cretaceous volcanism and intrusive magmatism features in the Mendeleev Rise region (Arctic Ocean) according to seismic data</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>Родина</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Rodina</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Елизавета Андреевна Родина</p><p>Москва</p></bio><bio xml:lang="en"><p>Elizaveta A. Rodina</p><p>Moscow</p></bio><email xlink:type="simple">rodina_liza@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>Никишин</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Nikishin</surname><given-names>A. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Анатолий Михайлович Никишин</p><p>Москва</p></bio><bio xml:lang="en"><p>Anatoly M. Nikishin</p><p>Moscow</p></bio><email xlink:type="simple">amnikishin@gmail.com</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>Старцева</surname><given-names>К. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Startseva</surname><given-names>K. F.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ксения Федоровна Старцева</p><p>Москва</p></bio><bio xml:lang="en"><p>Ksenia F. Startseva</p><p>Moscow</p></bio><email xlink:type="simple">kfstartseva@gmail.com</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>Посаментьер</surname><given-names>Г. У.</given-names></name><name name-style="western" xml:lang="en"><surname>Posamentier</surname><given-names>H. W.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Генри Уильям Посаментьер</p><p>25 Топсайд Роу Драйв, Те-Вудлендс, Техас 77380, США</p></bio><bio xml:lang="en"><p>Henry W. Posamentier</p><p>25 Topside Row Drive, the Woodlands, TX 77380</p></bio><email xlink:type="simple">hposamen1@gmail.com</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Консультант</institution><country>Соединённые Штаты Америки</country></aff><aff xml:lang="en"><institution>Consultant</institution><country>United States</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>15</day><month>12</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><fpage>3</fpage><lpage>20</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Родина Е.А., Никишин А.М., Старцева К.Ф., Посаментьер Г.У., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Родина Е.А., Никишин А.М., Старцева К.Ф., Посаментьер Г.У.</copyright-holder><copyright-holder xml:lang="en">Rodina E.A., Nikishin A.M., Startseva K.F., Posamentier H.W.</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://vestnik.geol.msu.ru/jour/article/view/477">https://vestnik.geol.msu.ru/jour/article/view/477</self-uri><abstract><p>. Работа основана на интерпретации сейсмических профилей МОВ ОГТ для Амеразийского бассейна. По результатам интерпретации сейсмических данных практически повсеместно в пределах поднятия Альфа-Менделеева и сопряженных с ним бассейнов в полуграбенах и впадинах выделен синрифтовый сейсмостратиграфический комплекс. На сейсмических профилях в составе синрифтового комплекса обнаружены различные проявления магматизма: платобазальты; силлы и дайки; рефлекторы, похожие на SDRs (Seaward Dipping Reflectors Sequences или последовательности рефлекторов, наклонных в сторону моря), и вулканы. Региональное растяжение и синхронный широко распространенный магматизм, вероятно, связаны с образованием в апт-альбское время Большой магматической провинции Высокой Арктики (HALIP, High Artic Large Igneous Province). С учетом данных о изотопном возрасте магматических пород для поднятия Менделеева сделано предположение, что кровля синрифтового сейсмостратиграфического комплекса имеет возраст приблизительно 100 млн лет, подошва — 125 млн. Повсеместность распространения синрифтового комплекса и его единый сейсмостратиграфический уровень позволяют предположить, что поднятие Альфа-Менделеева и сопряженные бассейны начали формирование синхронно в апте–альбе. Вдоль поднятия Альфа-Менделеева можно провести осевую линию. Западнее осевой линии высокоамплитудные рефлекторы, похожие на SDRs, падают в сторону бассейна Подводников, восточнее — в сторону бассейнов Толля, Менделеева, Наутилуса и Стефанссона. Рефлекторы сходятся в центральных частях бассейнов. Здесь проходят центральные оси растяжения. Поднятие Альфа-Менделеева — двусторонняя вулканическая пассивная континентальная окраина. Бассейны Подводников, Толля, Менделеева, Наутилус и Стефанссона — рифтовые бассейны с утоненной континентальной корой в основании. Их развитие было прервано до начала спрединга и образования океанической коры.</p></abstract><trans-abstract xml:lang="en"><p>The current paper is based primarily on the interpretation of 2D seismic lines for the Amerasian Basin. A synrift complex has been identified in half-grabens almost everywhere within the Alpha-Mendeleev Rise and conjugate basins according to the results of seismic data interpretation. Various magmatism features within the synrift complex have been identified on seismic profiles: plateau basalts; sills and dikes; reflections similar to SDRs (Seaward Dipping Reflectors Sequences) and volcanoes. Regional extension and synchronous widespread magmatism are probably associated with the formation of the High Artic Large Igneous Province (HALIP) in the Aptian-Albian. Considering the data on the isotope ages of igneous rocks for the Mendeleev Rise, it is assumed that the top of the synrift complex has an approximate age of 100 Ma and the bottom has an approximate age of 125 Ma. The Alpha-Mendeleev Rise was formed simultaneously with conjugate basins in the Aptian-Albian. An axial line can be drawn along the Alpha-Mendeleev Rise. To the west of the axial line, reflections similar to SDRs dip towards the Podvodnikov basin. To the east of the axial line, reflections dip towards the Toll, Mendeleev, Nautilus and Stefansson basins. The reflections converge in the central parts of the basins. The Alpha Mendeleev Rise is a double-sided volcanic passive continental margin. The Podvodnikov, Toll, Mendeleev, Nautilus, and Stefansson basins are rift basins with thinned continental crust at the base. Their development was interrupted before the start of spreading and the oceanic crust formation.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>сейсмостратиграфия</kwd><kwd>Арктический океан</kwd><kwd>Амеразийский бассейн</kwd><kwd>поднятие Менделеева</kwd><kwd>бассейн Подводников</kwd><kwd>бассейн Толля</kwd><kwd>поднятие Де-Лонга</kwd><kwd>SDRs</kwd><kwd>подводные вулканы</kwd><kwd>платобазальты</kwd><kwd>HALIP</kwd></kwd-group><kwd-group xml:lang="en"><kwd>seismostratigraphy</kwd><kwd>Arctic Ocean</kwd><kwd>Amerasian Basin</kwd><kwd>Mendeleev Rise</kwd><kwd>Podvodnikov Basin</kwd><kwd>Toll Basin</kwd><kwd>De Long High</kwd><kwd>SDRs</kwd><kwd>volcanoes</kwd><kwd>plateau basalts</kwd><kwd>HALIP</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при поддержке гранта РНФ (проект № 22-27-00160).</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">Гусев Е.А., Лукашенко Р.В., Попко А.О. и др. 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