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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-2017-8-1-0230</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-330</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>СОВРЕМЕННАЯ ГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>RECENT GEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>Рифты, орогены, кратоны и глобальная тектоника: введение в проблему</article-title><trans-title-group xml:lang="en"><trans-title>Rifts, orogens, cratons, and global tectonics: Introduction</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>Рассказов</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Rasskazov</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. геол.-мин. наук, профессор, зав. лабораторией Институт земной коры СО РАН;8664033, Иркутск, ул. Лермонтова, 128;</p><p> Иркутский государственный университет, геологический факультет 664003, Иркутск, ул. Ленина, 3;</p><p> Тел. (3952)511659;</p></bio><bio xml:lang="en"><p>Doctor of Geology and Mineralogy, Professor, Head of Laboratory Institute of the Earth’s Crust, Siberian Branch of RAS128 Lermontov street, Irkutsk 664033;</p><p>Irkutsk State University, Geological Faculty3 Lenin street, Irkutsk 664003;</p><p>Tel. +7(3952)511659;</p></bio><email xlink:type="simple">rassk@crust.irk.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт земной коры СО РАН&#13;
Иркутский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth’s Crust&#13;
Irkutsk State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2017</year></pub-date><pub-date pub-type="epub"><day>23</day><month>03</month><year>2017</year></pub-date><volume>8</volume><issue>1</issue><fpage>1</fpage><lpage>9</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Рассказов С.В., 2017</copyright-statement><copyright-year>2017</copyright-year><copyright-holder xml:lang="ru">Рассказов С.В.</copyright-holder><copyright-holder xml:lang="en">Rasskazov S.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/330">https://www.gt-crust.ru/jour/article/view/330</self-uri><abstract><p>В развитии теории Земли ключевую роль играют сравнительные исследования орогенов, рифтов и платформ в экваториальных, умеренных и высоких широтах Азии и сопредельной Арктики. Современная форма трехосного асимметричного кардиоидального эллипсоида на планете обусловлена ее новейшей (позднефанерозойской) геодинамической эволюцией, начавшейся в Арктике, а затем – в Азии. На новейшем геодинамическом этапе в Арктике был запущен механизм растяжения литосферы, в Азии – механизм сжатия, сочетающегося с растяжением. Cтатьи по этой тематике представлены в специальном выпуске журнала «Геодинамика и тектонофизика».</p></abstract><trans-abstract xml:lang="en"><p>A key role in developing the Earth theory is played by comparative studies of orogens, rifts, and platforms in the equatorial, middle and high latitudes of Asia and the adjacent Arctic regions. The modern shape of the planet’s triaxial asymmetrical cardioid ellipsoid results from its latest (Late Phanerozoic) geodynamic evolution that began in Arctic and then commenced in Asia. At this stage, mechanisms of the lithosphere extension and compression, combined with extension, were launched in Arctic and Asia, respectively. The special issue of Geodynamics &amp; Tectonophysics presents papers on this topic.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>ороген</kwd><kwd>рифт</kwd><kwd>мел</kwd><kwd>кайнозой</kwd><kwd>новейший геодинамический этап</kwd><kwd>Азия</kwd><kwd>Арктика</kwd><kwd>астеносфера</kwd><kwd>литосфера</kwd></kwd-group><kwd-group xml:lang="en"><kwd>orogen</kwd><kwd>rift</kwd><kwd>Cretaceous</kwd><kwd>Cenozoic</kwd><kwd>latest geodynamic stage</kwd><kwd>Asia</kwd><kwd>Arctic</kwd><kwd>asthenosphere</kwd><kwd>lithosphere</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Belousov V.V., Gerasimovsky V.I., Goryachev A.V., Dobrovolsky V.V., Kapitsa A.P., Logatchev N.A., Milanovsky E.E., Polyakov A.I., Rykunov L.N., Sedykh V.V., 1974. 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