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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-2011-2-3-0046</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-136</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>НОВЫЕ ПАЛЕОМАГНИТНЫЕ ДАННЫЕ ПО СИЛУРИЙСКИМ И ДЕВОНСКИМ ВУЛКАНИТАМ ЧИНГИЗСКОЙ ОСТРОВНОЙ ДУГИ КАЗАХСТАНА И ИХ ВКЛАД В ПРЕДСТАВЛЕНИЯ О ТЕКТОНИЧЕСКОЙ ЭВОЛЮЦИИ УРАЛО-МОНГОЛЬСКОГО ПОЯСА</article-title><trans-title-group xml:lang="en"><trans-title>PALEOMAGNETISM OF SILURIAN AND DEVONIAN VOLCANICS FROM THE CHINGIZ ISLAND ARC, KAZAKHSTAN, AND ITS BEARING ON TECTONIC EVOLUTION OF THE URAL-MONGOL BELT</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>Левашова</surname><given-names>Наталья Михайловна</given-names></name><name name-style="western" xml:lang="en"><surname>Levashova</surname><given-names>Natalia M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.мин. наук, н. с.,</p><p>119017, Москва, Пыжевский пер., 7</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Senior Researcher,</p><p>119017, Moscow, Pyzhevsky Lane, 7</p></bio><email xlink:type="simple">namile2007@rambler.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>Баженов</surname><given-names>Михаил Львович</given-names></name><name name-style="western" xml:lang="en"><surname>Bazhenov</surname><given-names>Mikhail L.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. геол.мин. наук, зав. лаб. палеомагнетизма,</p><p>119017, Москва, Пыжевский пер., 7</p></bio><bio xml:lang="en"><p>Doctor of Geology and Mineralogy, Head of Palaeomagnetism Laboratory,</p><p>119017, Moscow, Pyzhevsky Lane, 7</p></bio><email xlink:type="simple">mibazh@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>Ван дер Во</surname><given-names>Роб</given-names></name><name name-style="western" xml:lang="en"><surname>Van der Voo</surname><given-names>Rob</given-names></name></name-alternatives><bio xml:lang="ru"><p>профессор геологии,</p><p>481091005, Энн Эрбор, Мичиган</p></bio><bio xml:lang="en"><p>Frank H.T. Rhodes Professor of Geological Sciences,</p><p>481091005, Ann Arbor, Michigan</p></bio><email xlink:type="simple">voo@umich.edu</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Абражевич</surname><given-names>Александра Владимировна</given-names></name><name name-style="western" xml:lang="en"><surname>Abrajevitch</surname><given-names>Alexandra V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ph.D,</p><p>ACT 0200, 11, Канберра</p></bio><bio xml:lang="en"><p>Ph.D.,</p><p>ACT 0200, 11, Canberra</p></bio><email xlink:type="simple">alexandra.abrajevitch@gmail.com</email><xref ref-type="aff" rid="aff-4"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Геологический институт РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geological Institute of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Геологический Институт РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geological Institute of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Департамент геологических наук Мичиганского университета</institution><country>Соединённые Штаты Америки</country></aff><aff xml:lang="en"><institution>Department of Geological Sciences, University of Michigan</institution><country>United States</country></aff></aff-alternatives><aff-alternatives id="aff-4"><aff xml:lang="ru"><institution>Исследовательская школа наук о Земле, Австралийский национальный университет</institution><country>Австралия</country></aff><aff xml:lang="en"><institution>Research School of Earth Sciences, The Australian National University</institution><country>Australia</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2011</year></pub-date><pub-date pub-type="epub"><day>20</day><month>09</month><year>2015</year></pub-date><volume>2</volume><issue>3</issue><fpage>266</fpage><lpage>288</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Левашова Н.М., Баженов М.Л., Ван дер Во Р., Абражевич А.В., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Левашова Н.М., Баженов М.Л., Ван дер Во Р., Абражевич А.В.</copyright-holder><copyright-holder xml:lang="en">Levashova N.M., Bazhenov M.L., Van der Voo R., Abrajevitch A.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/136">https://www.gt-crust.ru/jour/article/view/136</self-uri><abstract><p>Тектоническая эволюция Урало-Монгольского подвижного пояса (УМП) многие десятилетия является предметом исследования огромного количества авторов. Однако, несмотря на все усилия, тектонические реконструкции разных авторов различаются самым радикальным образом, а во многом являются взаимоисключающими. Один из способов прояснить ситуацию – получить последовательности разновозрастных палеомагнитных определений и на их основе оценить кинематику ключевых структур УМП. При палеомагнитных исследованиях среднепалеозойских вулканитов Чингизской палеоостровной дуги на северо-востоке Казахстана в андезитах середины силура была выделена первичная компонента намагниченности, что подтверждается положительным тестом галек для внутриформационного конгломерата. В двух среднедевонских объектах также была выделена первичная намагниченность, для которой тест складки и тест обращения положительны. Объединив все имеющиеся данные по этому региону, мы получили последовательность палеомагнитных определений в интервале с позднего кембрия до поздней перми, что позволило уверенно определить, в каком полушарии находилась Чингизская палеодуга. Сделан вывод, что эта структура устойчиво смещалась к северу и пересекла экватор в силуре. Имеющиеся данные так же уверенно указывают на вторичную природу изгиба вулканических поясов Казахстана, имеющих подковообразные очертания. Сравнение этих данных с кривой кажущейся миграции полюса Сибирской платформы позволяет говорить о том, что большую часть палеозоя Чингизская палеодуга двигалась согласованно с Сибирской платформой, что накладывает жесткие ограничения на эволюцию УМП.</p></abstract><trans-abstract xml:lang="en"><p>The tectonic and paleogeographic evolution of the Ural-Mongol belt between the cratons of Baltica, Siberia, and Tarim is the key to the formation of the Eurasian supercontinent during Paleozoic time, but the views on this complicated process remain very disparate and sometimes controversial. Three volcanic formations of the Middle Silurian, LowertoMiddle Devonian and Middle Devonian age from the southwestern boundary of the Chingiz Range (NE Kazakhstan) yields what are interpreted as primary paleomagnetic directions that help clarify the evolution of the belt. A singlepolarity characteristic component in midSilurian andesites yields a positive intraformational conglomerate test, whereas dualpolarity prefolding components are isolated from the two Devonian collections. These new data were evaluated together with previously published paleomagnetic results from Paleozoic rocks in the Chingiz Range, and allow us to establish with confidence the hemisphere in which the area was located at a given time. We conclude that NE Kazakhstan was steadily moving northward crossing the equator in Silurian time. These new paleomagnetic data from the Chingiz range also agree with and reinforce the hypothesis that the strongly curved volcanic belts of Kazakhstan underwent oroclinal bending between Middle Devonian and Late Carboniferous time. A comparison of the Chingiz paleolatitudes with those of Siberia shows similarities between the northward motion and rotational history of the Chingiz unit and those of Siberia, which imposes important constraints on the evolving paleogeography of the Ural-Mongol belt.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Урало-Монгольский пояс</kwd><kwd>Казахстан</kwd><kwd>Чингизская островная дуга</kwd><kwd>средний палеозой</kwd><kwd>палеомагнетизм</kwd><kwd>ороклинальное изгибание</kwd><kwd>кинематика Сибири и Балтии</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Ural-Mongol belt</kwd><kwd>Kazakhstan</kwd><kwd>Chingiz island arc</kwd><kwd>Middle Paleozoic</kwd><kwd>paleomagnetism</kwd><kwd>oroclinal bending</kwd><kwd>kinematics of Siberia and Baltica</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Научная станции РАН в Бишкеке, Н.Я. Дворов, А.В. Шацилло, В.Э. Павлов, А.Н. Диденко, А.В.Осетров; РФФИ, Отделение наук о Земле РАН, Национальный научный фонд США</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">Бекжанов Г.Р., Кошкин В.Я., Никитченко И.И., Скринник Л.И., Азизов Т.И., Тимуш А.В. Геологическое строение Казахстана. Алматы: Минво природных ресурсов Казахстана, 2000. 395 с.</mixed-citation><mixed-citation xml:lang="en">Бекжанов Г.Р., Кошкин В.Я., Никитченко И.И., Скринник Л.И., Азизов Т.И., Тимуш А.В. Геологическое строение Казахстана. Алматы: Минво природных ресурсов Казахстана, 2000. 395 с.</mixed-citation></citation-alternatives></ref><ref id="cit2"><label>2</label><citation-alternatives><mixed-citation xml:lang="ru">Богданов А.А. Тектоническое положение палеозоид Центрального Казахстана и ТяньШаня // Бюлл. МОИП. Геол. секция. 1965. Т. XL. № 5, C. 40–68.</mixed-citation><mixed-citation xml:lang="en">Богданов А.А. 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