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<article 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" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Geotectonics</journal-id><journal-title-group><journal-title xml:lang="en">Geotectonics</journal-title><trans-title-group xml:lang="ru"><trans-title>Геотектоника</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0016-853X</issn><issn publication-format="electronic">3034-4972</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">11563</article-id><article-id pub-id-type="doi">10.31857/S0016-853X2019127-43</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Comparative geodynamics of Aleutian and Izu-Bonin-Mariana island-arc systems</article-title><trans-title-group xml:lang="ru"><trans-title>Сравнительная геодинамика формирования Алеутской и Идзу-Бонин-Марианской островодужных систем</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Chekhovich</surname><given-names>V. D.</given-names></name><name xml:lang="ru"><surname>Чехович</surname><given-names>В. Д.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vadim@ilran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Sukhov</surname><given-names>A. N.</given-names></name><name xml:lang="ru"><surname>Сухов</surname><given-names>А. Н.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vadim@ilran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Kononov</surname><given-names>M. V.</given-names></name><name xml:lang="ru"><surname>Кононов</surname><given-names>М. В.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vadim@ilran.ru</email><xref ref-type="aff" rid="aff2"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Sheremet</surname><given-names>O. G.</given-names></name><name xml:lang="ru"><surname>Шеремет</surname><given-names>О. Г.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vadim@ilran.ru</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Geological Institute, Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Геологический институт РАН</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">Shirshov Institute of Oceanology, Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Институт океанологии им. П.П. Ширшова РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2019-04-01" publication-format="electronic"><day>01</day><month>04</month><year>2019</year></pub-date><issue>1</issue><issue-title xml:lang="en"/><issue-title xml:lang="ru"/><fpage>27</fpage><lpage>43</lpage><history><date date-type="received" iso-8601-date="2019-04-01"><day>01</day><month>04</month><year>2019</year></date><date date-type="accepted" iso-8601-date="2019-04-01"><day>01</day><month>04</month><year>2019</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2019, Russian Academy of Sciences</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2019, Российская академия наук</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="en">Russian Academy of Sciences</copyright-holder><copyright-holder xml:lang="ru">Российская академия наук</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/0016-853X/article/view/11563">https://journals.eco-vector.com/0016-853X/article/view/11563</self-uri><abstract xml:lang="en"><p>Fulfilled comparative analysis of the Aleutian and Izu-Bonin-Marian island-arc systems structure and geodynamic development. Izu-Bonin-Maian island-arc systems situated along сontinental margin of Eurasia in the West of Pacific Ocean. The Aleutian island-arc system is situated between the North American and Eurasian continents. Aleutian and Izu-Bonin-Marian island-arc systems appeared to be of the same age. Both island-arc systems form autonomous Philippine and Beringia small lithospheric plates. Izu-Bonin-Marianas island-arc system formed on exclusively geodynamic interaction of oceanic plate and back-arc basins, with the main role of the Pacific subduction. Aleutian system at the initial stage was formed as a result from separation of the part of Pacific Cretaceous crust by Aleutian subduction zone.</p> <p>The subsequent process of Aleutian system development was caused by geodynamics of movement of North American and Eurasian lithospheric plates. Pacific plate constant oblique subduction led to expansion of Aleutian island-arc system in the Western direction.</p></abstract><trans-abstract xml:lang="ru"><p>Проведен сравнительный анализ геологического строения и геодинамического развития практически одновозрастных Идзу-Бонин-Марианской и Алеутской островодужных систем, первая из которых входит в систему окраинных островодужных систем на западе Тихого океана, вторая — межконтинентальная, располагается между континентальными плитами Евразии и Северной Америки. Обе островодужные системы образуют самостоятельные малые литосферные плиты — Филиппинскую и Берингия. Показано, что Идзу-Бонин-Марианская система возникла под влиянием геодинамического взаимодействия исключительно океанических, включая окраинноморские, плит с основной ролью Тихоокеанской субдукции. Формирование Алеутской системы произошло на начальном этапе за счет отделения Алеутской дугой части меловой коры Пацифики и в результате последующих процессов внутри островодужной системы, связанных с геодинамикой перемещения Североамериканской и Евразийской континентальных плит и косой субдукцией Тихоокеанской плиты.</p></trans-abstract><kwd-group xml:lang="en"><kwd>subduction</kwd><kwd>lithospheric plates</kwd><kwd>geodynamics</kwd><kwd>Aleutian and Izu-Bonin-Mariana island-arc systems</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>субдукция</kwd><kwd>островодужные системы</kwd><kwd>литосферные плиты</kwd><kwd>геодинамика</kwd><kwd>Идзу-Бонин-Марианская и Алеутская системы</kwd></kwd-group><funding-group><award-group><funding-source><institution-wrap><institution xml:lang="en">Geological Institute, Russian Academy of Sciences</institution></institution-wrap><institution-wrap><institution xml:lang="ru">Геологический институт РАН</institution></institution-wrap></funding-source><award-id></award-id></award-group><award-group><funding-source><institution-wrap><institution xml:lang="en">Russian Foundation for Basic Research</institution></institution-wrap><institution-wrap><institution xml:lang="ru">Российский фонд фундаментальных исследований</institution></institution-wrap></funding-source><award-id></award-id></award-group><award-group><funding-source><institution-wrap><institution xml:lang="en">Russian Science Foundation</institution></institution-wrap><institution-wrap><institution xml:lang="ru">Российский научный фонд</institution></institution-wrap></funding-source><award-id></award-id></award-group><funding-statement xml:lang="ru">Финансирование проводилось за счет субсидии ГИН РАН (г. Москва) по теме № 0135-2016-0022. Исследование поддержано грантом РФФИ № 16-05-00199 и грантом РНФ, проект № 14–50–00095.</funding-statement></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Богданов Н.А. Глубоководные впадины запада Тихого океана // М.: Недра, 1990. 189 с.</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>Богданов Н.А., Непрочнов Ю.П. Геология глубоководных впадин Берингова моря // 27-й МГК. История происхождения окраинных и внутренних морей. Симпозиум SW-06.2.3. Доклады. М.: Наука, 1984. Т. 6. Ч. 2. С. 4–11.</mixed-citation></ref><ref id="B3"><label>3.</label><mixed-citation>Богданов Н.А., Вишневская В.С., Сухов А.Н., Федорчук А.В., Чехович В.Д. Океаническая олистострома западного побережья Алеутской впадины (Берингово море) // Геотектоника. 1982. № 5. 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