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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-2017-8-4-0316</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-470</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>АМПЛИТУДЫ ДИЗЪЮНКТИВНЫХ НАРУШЕНИЙ ФЛАНГОВ ХРЕБТА КНИПОВИЧА (СЕВЕРНАЯ АТЛАНТИКА) КАК ИНДИКАТОР СОВРЕМЕННОЙ ГЕОДИНАМИКИ РЕГИОНА</article-title><trans-title-group xml:lang="en"><trans-title>AMPLITUDES OF DISJUNCTIVE DISLOCATIONS IN THE KNIPOVICH RIDGE FLANKS (NORTHERN ATLANTIC) AS AN INDICATOR OF MODERN REGIONAL GEODYNAMICS</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>Соколов</surname><given-names>С. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Sokolov</surname><given-names>S. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Соколов Сергей Юрьевич, канд. физ.-мат. наук, в.н.с.</p><p>119017, Москва, Пыжевский пер., 7</p></bio><bio xml:lang="en"><p>Sokolov, Sergey Yu., Candidate of Physics and Mathematics, Lead Researcher </p><p>7 Pyzhevsky Lane, Moscow 119017, Russia</p></bio><email xlink:type="simple">sysokolov@yandex.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>Абрамова</surname><given-names>А. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Abramova</surname><given-names>A. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Абрамова Анастасия Сергеевна, м.н.с. </p><p>119017, Москва, Пыжевский пер., 7</p></bio><bio xml:lang="en"><p>Abramova, Anastasia S., Junior Researcher </p><p>7 Pyzhevsky Lane, Moscow 119017, Russia</p></bio><email xlink:type="simple">abramanastas@gmail.com</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>Мороз</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Moroz</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Мороз Евгений Андреевич, канд. геол.-мин. наук, н.с. </p><p>119017, Москва, Пыжевский пер., 7</p></bio><bio xml:lang="en"><p>Moroz, Evgenii A., Researcher </p><p>7 Pyzhevsky Lane, Moscow 119017, Russia</p></bio><email xlink:type="simple">morozzea@gmail.com</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>Зарайская</surname><given-names>Ю. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Zaraiskaya</surname><given-names>Yu. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Зарайская Юлия Андреевна, канд. геол.-мин. наук, н.с. </p><p>119017, Москва, Пыжевский пер., 7</p></bio><bio xml:lang="en"><p>Zarayskaya, Yulia A., Junior Researcher </p><p>7 Pyzhevsky Lane, Moscow 119017, Russia</p></bio><email xlink:type="simple">geozar@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></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><pub-date pub-type="collection"><year>2017</year></pub-date><pub-date pub-type="epub"><day>18</day><month>12</month><year>2017</year></pub-date><volume>8</volume><issue>4</issue><elocation-id>769–789</elocation-id><permissions><copyright-statement>Copyright &amp;#x00A9; Соколов С.Ю., Абрамова А.С., Мороз Е.А., Зарайская Ю.А., 2017</copyright-statement><copyright-year>2017</copyright-year><copyright-holder xml:lang="ru">Соколов С.Ю., Абрамова А.С., Мороз Е.А., Зарайская Ю.А.</copyright-holder><copyright-holder xml:lang="en">Sokolov S.Y., Abramova A.S., Moroz E.A., Zaraiskaya Y.A.</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/470">https://www.gt-crust.ru/jour/article/view/470</self-uri><abstract><p>Впервые представлена карта вертикальных амплитуд современных дизъюнктивных нарушений в глубоководной части океана по смещениям фаз отраженных волн высокочастотной сейсмоакустической записи. Полученное распределение амплитуд имеет мозаичный характер с чередованием областей сжатия и растяжения на флангах рифтовой системы Книповича. Два сдвиговых смещения формируют современную структуру хребта Книповича как локальный рифт в обстановке пулл-апарт. Асимметрия напряжений и наличие сжатия на флангах хребта подтверждаются распределением механизмов очагов сильных землетрясений взбросового типа. Наблюдается тектоническая активизация юго-восточного фланга хребта Книповича, выраженная в асимметрии эпицентров слабых землетрясений.</p></abstract><trans-abstract xml:lang="en"><p>This article presents the first map showing the vertical amplitudes of modern disjunctive dislocations inNorthern Atlantic, based on the estimated phase shifts of reflected waves recorded by high-frequency seismic acoustic surveys. The amplitude distribution pattern is mosaic with alternating areas of compression and extension in the flanks of the Knipovich rift system. The modern structure of the Knipovich Ridge, including two strike-slip faults, represents a local rift in the pull-apart setting. The asymmetry of stresses and the presence of compression in the ridge flanks is evidenced by the distribution of the focal mechanisms of strong earthquakes related to reverse faults. In the southeastern Knipovich Ridge, tectonic activity is marked by the asymmetric pattern of the epicenters of small earthquakes.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>геодинамика</kwd><kwd>амплитуды дизъюнктивных нарушений</kwd><kwd>осадочный чехол</kwd><kwd>сейсмоакустика</kwd><kwd>хребет Книповича</kwd><kwd>землетрясение</kwd><kwd>механизмы очагов</kwd></kwd-group><kwd-group xml:lang="en"><kwd>geodynamics</kwd><kwd>amplitudes of disjunctive dislocations</kwd><kwd>sedimentary cover</kwd><kwd>seismoacoustics</kwd><kwd>Knipovich Ridge</kwd><kwd>earthquake</kwd><kwd>earthquake focal mechanisms</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">Abramova A.S., Sokolov S.Yu., Moroz E.A., 2016. Mapping of neotectonic elements in the mid-ocean ridge based on high-frequency profiling data. In: D.E. 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