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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">gtcrust</journal-id><journal-title-group><journal-title xml:lang="ru">Геодинамика и тектонофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Geodynamics &amp; Tectonophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2078-502X</issn><publisher><publisher-name>Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.5800/GT-2021-12-3-0533</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1234</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>ТЕКТОНОФИЗИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>TECTONOPHYSICS</subject></subj-group></article-categories><title-group><article-title>РАЗВИТИЕ МОДЕЛИ ВЕРХНЕМАНТИЙНОЙ КОНВЕКЦИИ, СОПРЯЖЕННОЙ С ЗОНОЙ СУБДУКЦИИ, С ПРИЛОЖЕНИЯМИ К МЕЛ-КАЙНОЗОЙСКОЙ ГЕОДИНАМИКЕ ЦЕНТРАЛЬНО-ВОСТОЧНОЙ АЗИИ И АРКТИКИ</article-title><trans-title-group xml:lang="en"><trans-title>UPPER MANTLE CONVECTION RELATED TO SUBDUCTION ZONE AND APPLICATION OF THE MODEL TO INVESTIGATE THE CRETACEOUS-CENOZOIC GEODYNAMICS OF CENTRAL EAST ASIA AND THE ARCTIC</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>Лобковский</surname><given-names>Л. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Lobkovsky</surname><given-names>L. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Москва, пр-т Нахимовский, 36</p><p>141701, Долгопрудный, Институтский пер., 9</p></bio><bio xml:lang="en"><p>36 Nahimovskiy Ave, Moscow 117997</p><p>9 Institutskiy Ln, Dolgoprudny 141701</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>Рамазанов</surname><given-names>М. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Ramazanov</surname><given-names>M. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>367030, Махачкала, пр-т И. Шамиля, 39а, Республика Дагестан</p></bio><bio xml:lang="en"><p>39а Shamil Ave, Makhachkala 367030, Republic of Dagestan</p></bio><email xlink:type="simple">mukamay-ipg@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Котелкин</surname><given-names>В. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Kotelkin</surname><given-names>V. D.</given-names></name></name-alternatives><bio xml:lang="ru"><p>117997, Москва, пр-т Нахимовский, 36</p><p>119991, Москва, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>36 Nahimovskiy Ave, Moscow 117997</p><p>1 Leninskie Gory, Moscow 119991</p></bio><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт океанологии им. П.П. Ширшова РАН; Московский физико-технический институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Shirshov Institute of Oceanology, Russian Academy of Sciences; Moscow Institute of Physics and Technology</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт проблем геотермии и возобновляемой энергетики, филиал Объединенного института высоких температур РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute for Geothermal Research and Renewable Energy, Branch of Joint Institute for High Temperatures of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Институт океанологии им. П.П. Ширшова РАН; Московский государственный университет им. М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Shirshov Institute of Oceanology, Russian Academy of Sciences; Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>17</day><month>09</month><year>2021</year></pub-date><volume>12</volume><issue>3</issue><fpage>455</fpage><lpage>470</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лобковский Л.И., Рамазанов М.М., Котелкин В.Д., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Лобковский Л.И., Рамазанов М.М., Котелкин В.Д.</copyright-holder><copyright-holder xml:lang="en">Lobkovsky L.I., Ramazanov M.M., Kotelkin V.D.</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.gt-crust.ru/jour/article/view/1234">https://www.gt-crust.ru/jour/article/view/1234</self-uri><abstract><p>Рассматривается математическое обоснование геодинамической модели верхнемантийной конвекции, сопряженной с Тихоокеанской зоной субдукции, в приложении к мел-кайнозойской эволюции Центрально-Восточной Азии (ЦВА) и Арктики. Приводится решение двухмерной стационарной задачи термической конвекции в слое верхней мантии при различных числах Рэлея с учетом влияния процесса субдукции и движения литосферного слоя вдоль подошвы верхней мантии. Описываются результаты 3D-моделирования нестационарной конвекции в верхней мантии, сопряженной с зоной субдукции. Полученные результаты позволяют объяснить весь спектр наблюдаемых тектономагматических процессов, развивающихся в пределах ЦВА в кайнозое и Арктики в верхнем мелу и кайнозое, а именно сочетание общего смещения литосферы ЦВА и Арктики в сторону Тихоокеанской зоны субдукции с наличием отдельных магматических провинций и рифтовых зон как следствие существования длинной горизонтально вытянутой конвективной ячейки (создающей эффект конвейерного волочения литосферы), осложненной внутренними изометричными ячейками (создающими эффект верхнемантийных плюмов).</p></abstract><trans-abstract xml:lang="en"><p>A geodynamic model of upper mantle convection related to the Pacific subduction zone is mathematically substantiated and applied to investigate the Cretaceous-Cenozoic evolution of Central East Asia (CEA) and the Arctic. We present a solution for the two-dimensional stationary problem of thermal convection in the upper mantle layer, considering different Rayleigh numbers and taking into account the influence of the subduction process and lithospheric movements along the upper mantle base. We describe the results of 3D modeling of nonstationary upper mantle convection in a subduction zone. Our data give grounds to propose explanations for the entire spectrum of tectonic-magmatic processes developing within CEA in the Cenozoic and the Arctic in the Upper Cretaceous and Cenozoic. We discuss the reasons why the lithosphere in CEA and the Arctic is generally shifting towards the Pacific subduction zone, considering the presence of separate magmatic provinces and rift zones. In our opinion, this is due to the existence of a large horizontally elongated convective cell, which interior is composed of smaller isometric cells. This long cell creates the effect of conveyor dragging of the lithosphere, while its internal cells produce the effect of upper mantle plumes.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>литосфера</kwd><kwd>зона субдукции</kwd><kwd>верхняя мантия</kwd><kwd>тепловая конвекция</kwd><kwd>двухмерная модель конвекции</kwd><kwd>3D моделирование</kwd><kwd>мел-кайнозойская эволюция</kwd><kwd>Центрально-Восточная Азия</kwd><kwd>Арктика</kwd><kwd>Байкальская рифтовая зона</kwd></kwd-group><kwd-group xml:lang="en"><kwd>lithosphere</kwd><kwd>subduction zone</kwd><kwd>upper mantle</kwd><kwd>thermal convection</kwd><kwd>2D convection model</kwd><kwd>3D modeling</kwd><kwd>Cretaceous-Cenozoic evolution</kwd><kwd>Central East Asia</kwd><kwd>Arctic</kwd><kwd>Baikal rift zone</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках госзадания Института океанологии им. П.П. Ширшова РАН № 0128-2021-0004 и частично по теме гранта РФФИ «Арктика» № 18-05-70012.</funding-statement><funding-statement xml:lang="en">The study was performed under the state assignment of Shirshov Institute of Oceanology (project 0128- 2021-0004) and partially supported by the Russian Foundation for Basic Research (project 18-05-70012 – Arctic).</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">Altamimi Z., Rebischung P., Metivier L., Collilieux X., 2016. ITRF2014: A New Release of the International Terrestrial Reference Frame Modeling Nonlinear Station Motions. Journal of Geophysical Research: Solid Earth 121 (8), 6109–6131. http://doi.org/10.1002/2016JB013098.</mixed-citation><mixed-citation xml:lang="en">Altamimi Z., Rebischung P., Metivier L., Collilieux X., 2016. 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