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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-2018-9-3-0368</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-621</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>ТЕКТОНОФИЗИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>TECTONOPHYSICS</subject></subj-group></article-categories><title-group><article-title>ЗОНЫ КОНЦЕНТРИРОВАННОЙ ДЕФОРМАЦИИ (СТРУКТУРЫ ЦВЕТКА): НАТУРНЫЕ НАБЛЮДЕНИЯ И ДАННЫЕ МОДЕЛИРОВАНИЯ</article-title><trans-title-group xml:lang="en"><trans-title>ZONES OF CONCENTRATED DEFORMATION (FLOWER STRUCTURES): FIELD OBSERVATIONS AND MODELING DATA</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5311-0877</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Леонов</surname><given-names>М. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Leonov</surname><given-names>M. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Михаил Георгиевич Леонов, докт. геол.-мин. наук, зав. лабораторией119017, Москва, Пыжевский пер., 7</p></bio><bio xml:lang="en"><p>Mikhail G. Leonov, Doctor of Geology and Mineralogy, Head of Laboratory7 Pyzhevsky Lane 7, Moscow 119017</p></bio><email xlink:type="simple">mgleonov@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>Морозов</surname><given-names>Ю. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Morozov</surname><given-names>Yu. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Юрий Алексеевич Морозов, докт. геол.-мин. наук, член-корреспондент РАН, зав. лабораторией123242, ГСП-5, Москва Д-242, ул. Большая Грузинская, 10</p></bio><bio xml:lang="en"><p>Yuri A. Morozov, Doctor of Geology and Mineralogy, Corresponding Member of RAS, Head of Laboratory</p><p>10 Bol’shaya Gruzinskaya street, Moscow D-242 123242, GSP-5</p></bio><email xlink:type="simple">moro49@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-2004-955X</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Стефанов</surname><given-names>Ю. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Stefanov</surname><given-names>Yu. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Юрий Павлович Стефанов, докт. физ.-мат. наук630090, Новосибирск, пр. Академика Коптюга, 3,</p></bio><bio xml:lang="en"><p>Yuri P. Stefanov, Doctor of Physics and Mathematics3 Academician Koptug ave., Novosibirsk 630090</p></bio><email xlink:type="simple">yu_st@mail.ru</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5367-9211</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Бакеев</surname><given-names>Р. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bakeev</surname><given-names>R. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Рустам Альфредович Бакеев, канд. физ.-мат. наук634055, Томск, Академический проспект, 2/4</p></bio><bio xml:lang="en"><p>Rustam A. Bakeev, Candidate of Physics and Mathematics2/4 Akademicheskii ave., Tomsk 634055</p></bio><email xlink:type="simple">bakeev@ispms.ru</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>Институт физики Земли им. О.Ю. Шмидта РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>O.Yu. Schmidt Institute of Physics of the Earth of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Институт нефтегазовой геологии и геофизики им. А.А. Трофимука СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-4"><aff xml:lang="ru"><institution>Институт физики прочности и материаловедения СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Strength Physics and Materials Science, Siberian Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>08</day><month>10</month><year>2018</year></pub-date><volume>9</volume><issue>3</issue><fpage>693</fpage><lpage>670</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Леонов М.Г., Морозов Ю.А., Стефанов Ю.П., Бакеев Р.А., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Леонов М.Г., Морозов Ю.А., Стефанов Ю.П., Бакеев Р.А.</copyright-holder><copyright-holder xml:lang="en">Leonov M.G., Morozov Y.A., Stefanov Y.P., Bakeev R.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/621">https://www.gt-crust.ru/jour/article/view/621</self-uri><abstract><p>В настоящее время большое внимание уделяется изучению узких линейных зон, которые, пронизывая земную кору на разную глубину, характеризуются сложной инфраструктурой и интенсивной в сравнении с фоновой тектонической переработкой горных масс. Такие структуры получили название «структуры цветка» или «зоны концентрированной деформации». Изучение натурных объектов вкупе с данными тектонофизического и расчетного моделирования, дополненное анализом литературного материала, позволило сделать следующие выводы: ЗКД в эксперименте и в природных объектах обнаруживают сходство, иногда тождество, по морфологии, инфраструктуре, этапности эволюции; ЗКД отражают преимущественно обстановки транспрессии, и их формирование сопровождается 3D пластическим сдвиговым течением вещества и дилатансией деформируемого объема; возникновение ЗКД может быть связано с развитием системы «фундамент – чехол», но может определяться и внутричехольным тектогенезом, не затрагивающим фундамент; ЗКД обладают пространственно-регулярным расположением и определяют тектоническую делимость земной коры и литосферы.</p><p> </p></abstract><trans-abstract xml:lang="en"><p>Our study was focused on narrow linear zones that penetrate to different depths the crust and have complex infrastructure. Rocks in such zones are more intensively tectonically altered in comparison with the background. ‘Flower structures’ and ‘zones of concentrated deformation’ (ZCD) are the terms to describe these zones. The field study results combined with the data of tectonophysical and computational modeling data and supplemented by the literature analysis gave grounds for the following conclusions. In the experiments, as well as in nature, ZCDs show similar and, in some cases, identical morphological and infrastructural features and have similar stages of their evolution. A ZCD is mainly a reflection of the transpression setting. Its formation is accompanied by 3D plastic shear flow of matter and dilatancy of the deformed volume. A ZCD may be associated with the development of the ‘basement – cover’ system. It may also occur due to the intra-cover tectogenesis that does not influence the basement. Locations of ZCDs are spatially regular and predetermine the tectonic divisibility of the crust and lithosphere.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>деформация</kwd><kwd>осадочный чехол</kwd><kwd>структура цветка</kwd><kwd>тектоническое течение</kwd><kwd>тектонофизика</kwd><kwd>транспрессия</kwd><kwd>фундамент</kwd><kwd>численный эксперимент</kwd></kwd-group><kwd-group xml:lang="en"><kwd>deformation</kwd><kwd>sedimentary cover</kwd><kwd>flower structure</kwd><kwd>tectonic flow</kwd><kwd>tectonophysics</kwd><kwd>transpression</kwd><kwd>basement</kwd><kwd>computational modeling</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">Alvarez P., Maurin J.C., 1991. 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