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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-2022-13-1-0575</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1428</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>НАЛОЖЕННЫЕ ДЕФОРМАЦИИ ГЕРЦИНСКОГО ВРЕМЕНИ В СТРУКТУРЕ МЕСТОРОЖДЕНИЯ ГОЛЕЦ ВЫСОЧАЙШИЙ (БАЙКАЛО-ПАТОМСКИЙ ПОЯС), 40AR/39AR ДАННЫЕ</article-title><trans-title-group xml:lang="en"><trans-title>THE HERCYNIAN IMPOSED DEFORMATIONS IN THE GOLETS VYSOCHAISHII DEPOSIT STRUCTURE (BAIKAL-PATOM BELT), 40AR/39AR DATA</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>Ванин</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Vanin</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>Vadim A. Vanin</p><p>128 Lermontov St, Irkutsk 664033</p></bio><email xlink:type="simple">vanin_geo@mail.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>Мазукабзов</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Mazukabzov</surname><given-names>A. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Юдин</surname><given-names>Д. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Yudin</surname><given-names>D. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Блинов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Blinov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Фаворского, 1а664074, Иркутск, ул. Лермонтова, 83</p></bio><bio xml:lang="en"><p>1а Favorsky St, Irkutsk 664033</p></bio><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Тарасова</surname><given-names>Ю. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Tarasova</surname><given-names>Yu. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Фаворского, 1а664074, Иркутск, ул. Лермонтова, 83</p></bio><bio xml:lang="en"><p>1а Favorsky St, Irkutsk 664033</p></bio><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт земной коры СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт геологии и минералогии им. В.С. Соболева СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Институт геохимии им. А.П. Виноградова СО РАН; Иркутский национальный исследовательский технический университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>22</day><month>03</month><year>2022</year></pub-date><volume>13</volume><issue>1</issue><fpage>575</fpage><lpage>575</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ванин В.А., Мазукабзов А.М., Юдин Д.С., Блинов А.В., Тарасова Ю.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Ванин В.А., Мазукабзов А.М., Юдин Д.С., Блинов А.В., Тарасова Ю.И.</copyright-holder><copyright-holder xml:lang="en">Vanin V.A., Mazukabzov A.M., Yudin D.S., Blinov A.V., Tarasova Y.I.</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/1428">https://www.gt-crust.ru/jour/article/view/1428</self-uri><abstract><p>В работе приведены результаты детального структурного анализа и изотопно-геохронологического 40Ar/39Ar датирования деформаций, проявленных на территории месторождения Голец Высочайший. В ходе выполнения геолого-структурных работ установлена последовательность проявления складчатых деформаций от крупных лежачих складок через формирование кливажа осевой поверхности и кренуляционного кливажа до разрывных нарушений, заполненных кварцевым материалом. С помощью 40Ar/39Ar датирования синтектонического серицита удалось установить возраст двух тектонических импульсов герцинского этапа – 340 и 320 млн лет. Этот этап характеризуется последовательным осложнением покровно-складчатой структуры района, сформированной на раннепалеозойском этапе, известном по литературным данным предшественников. Проанализированы четыре пробы, отобранные в различных местах и характеризующиеся различным набором деформационных структур. 40Ar/39Ar возраст 340 млн лет отражает формирование мелкой складчатости в результате межслоевых скольжений и скольжений по плоскостям кливажа осевой поверхности. 40Ar/39Ar возраст 320 млн лет отражает формирование дискретно проявленного кренуляционного кливажа и слабозолотоносных, малосульфидных кварцевых жил, занимающих секущее положение по отношению к элементам слоистости и кливажа осевой поверхности.</p></abstract><trans-abstract xml:lang="en"><p>The paper presents the results of the detailed structural analysis and 40Ar/39Ar dating of the deformations in the Golets Vysochaishii deposit area. The geological and structural studies showed the folded-deformation sequence from large lying folds through axial-plane cleavage formation and cleavage to quartz-filled fractures. The 40Ar/39Ar dating of syntectonic sericite yielded the ages of two Hercynian tectonic impulses – 340 and 320 Ma. This stage is characterized by the earlier-known successive complication of the Early Paleozoic fold-nappe structure of the area. Analysis has been made on four samples taken from different sites and characterized by different sets of deformational structures. The 40Ar/39Ar age of 340 Ma reflects the formation of small-size folds as a result of interlayer sliding and sliding along the cleavage axial planes. The 40Ar/39Ar age of 320 Ma reflects the formation of discretely manifested crenulation cleavage and low-Au, low-sulfidation quartz veins oriented obliquely to the elements of bedding and axial-plane cleavage.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>40Ar/39Ar данные</kwd><kwd>золото</kwd><kwd>месторождение Голец Высочайший</kwd><kwd>разрывное нарушение</kwd><kwd>кливаж осевой поверхности</kwd><kwd>кренуляционный кливаж</kwd><kwd>складчатость</kwd><kwd>деформация</kwd></kwd-group><kwd-group xml:lang="en"><kwd>40Ar/39Ar data</kwd><kwd>gold</kwd><kwd>Golets Vysochaishii deposit</kwd><kwd>fault</kwd><kwd>axial-plane cleavage</kwd><kwd>crenulation cleavage</kwd><kwd>folding</kwd><kwd>deformation</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено при финансовой поддержке РФФИ и Правительства Иркутской области в рамках научного проекта № 20-45-380025.</funding-statement><funding-statement xml:lang="en">The work has been done under financial support of RFBR and the Irkutsk Region Administration as part of research project 20-45-380025.</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">Baksi A.K., Archibald D.A., Farrar E., 1996. 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