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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-2019-10-2-0420</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-847</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>ПАЛЕОГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>PALEOGEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>СВЯЗЬ СУБДУКЦИОННОГО И ПЛЮМОВОГО МАГМАТИЗМА НА АКТИВНЫХ ГРАНИЦАХ ЛИТОСФЕРНЫХ ПЛИТ В ЗОНЕ ВЗАИМОДЕЙСТВИЯ СИБИРСКОГО КОНТИНЕНТА И ПАЛЕОАЗИАТСКОГО ОКЕАНА В НЕОПРОТЕРОЗОЕ И ПАЛЕОЗОЕ</article-title><trans-title-group xml:lang="en"><trans-title>RELATIONSHIP BETWEEN SUBDUCTION‐RELATED AND PLUME MAGMATISM AT THE ACTIVE BOUNDARIES OF LITHOSPHERIC PLATES IN THE INTERACTION ZONE OF THE SIBERIAN CONTINENT AND PALEOASIAN OCEAN IN THE NEOPROTEROZOIC AND PALEOZOIC</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-2890-1105</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Гордиенко</surname><given-names>И. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Gordienko</surname><given-names>I. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Иван Власович Гордиенко - член-корреспондент РАН, доктор геолого-минералогических наук, главный научный сотрудник</p><p>670047, Улан-Удэ, ул. Сахьяновой, 6а</p></bio><bio xml:lang="en"><p>Ivan V. Gordienko - Corresponding Member of RAS, Doctor of Geology and Mineralogy, Chief Researcher</p><p>6a Sakhyanova street, Ulan-Ude 670047</p></bio><email xlink:type="simple">gord@pres.bscnet.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Геологический институт СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geological Institute, Siberian Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>24</day><month>06</month><year>2019</year></pub-date><volume>10</volume><issue>2</issue><fpage>405</fpage><lpage>457</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Гордиенко И.В., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Гордиенко И.В.</copyright-holder><copyright-holder xml:lang="en">Gordienko I.V.</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/847">https://www.gt-crust.ru/jour/article/view/847</self-uri><abstract><p>На основе анализа известных моделей конвекции в астеносфере и мантии Земли, субдукционного и плюмового магматизма кайнозойских активных окраин западно‐тихоокеанского и калифорнийского типа и собственных материалов многолетних исследований Центрально‐Азиатского складчатого пояса (ЦАСП) рассматривается взаимосвязь плейт‐ и плюмтектонических процессов при формировании неопроте‐ розойских и венд‐палеозойских островодужных систем и активных континентальных окраин в зоне взаимо‐ действия Сибирского континента и Палеоазиатского океана (ПАО). Показано, что субдукционный магматизм активных окраин Палеоазиатского океана невозможно рассматривать отдельно от плюмового. Эти процессы взаимосвязаны и играли основную роль в истории формирования ЦАСП. В результате анализа выполненных палеогеодинамических реконструкций неопротерозоя, венда – раннего и среднего палеозоя охарактеризова‐ но 25 островодужных систем ПАО, с которыми связано формирование более 30 ареалов плюмового магматизма. Кроме того, в пределах активной окраины Сибирского континента описаны многочисленные поля разномасштабного проявления внутриплитного магматизма в рифтогенных структурах, не связанных с зо‐ нами субдукции, особенно на заключительном позднепалеозойском этапе. Все переломные этапы в истории развития ЦАСП, включая кембро‐ордовикский коллизионный, четко сопоставляются с активностью мантийных плюмов. Такое сочетание островных дуг и ареалов плюмового магматизма указывает на то, что вся эта огромная неопротерозой‐палеозойская область Центральной Азии, несомненно, была связана с деятельностью мантийных плюмов.</p></abstract><trans-abstract xml:lang="en"/><kwd-group xml:lang="ru"><kwd>Сибирский континент</kwd><kwd>Центрально‐Азиатский складчатый пояс</kwd><kwd>Палеоазиатский океан</kwd><kwd>активная окраина</kwd><kwd>конвекция</kwd><kwd>зона субдукции</kwd><kwd>мантийный плюм</kwd><kwd>островодужный и внутриплитный магматизм</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Siberian continent</kwd><kwd>Central Asian Orogenic Belt</kwd><kwd>Paleoasian Ocean</kwd><kwd>active margin</kwd><kwd>convection</kwd><kwd>subduction zone</kwd><kwd>mantle plume</kwd><kwd>island‐arc and intraplate magmatism</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при финансовой поддержке Отделения наук о Земле РАН по программе IX.124.1. «Глубинная геодинамика и эволюция литосферы: закономерности проявления мантийных плюмов и плитотектонических процессов, динамика осадочных бассейнов» (координатор акад. РАН Н.Л. Добрецов), бюджетной темы лаборатории геодинамики ГИН СО РАН IX.124.1.3. (гос. номер АААА-А17-117011650013-4) и РФФИ (проекты № 15-05-01633а, 16-55-44008 Монг_а, 19-05-00312а) (руководитель работ чл.-к. РАН И.В. Гордиенко)</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">Al’mukhamedov A.I., Gordienko I.V., Kuzmin M.I., Tomurtogoo O., Tomurkhuu D., 1996. The Dzhida Zone: A fragment of the Paleoasian Ocean. Geotectonics 30 (4), 279–294.</mixed-citation><mixed-citation xml:lang="en">Al’mukhamedov A.I., Gordienko I.V., Kuzmin M.I., Tomurtogoo O., Tomurkhuu D., 1996. The Dzhida Zone: A fragment of the Paleoasian Ocean. 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