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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-2012-3-2-0064</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-154</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>МИОЦЕНОВЫЙ И ДЕВОНСКИЙ МАГМАТИЗМ В СОЧЛЕНЕНИИ ТУВИНО-МОНГОЛЬСКОГО МАССИВА И СИБИРСКОГО КРАТОНА: ОБЩИЙ КОМПОНЕНТ МАНТИЙНЫХ ИСТОЧНИКОВ И ЕГО ПРОИСХОЖДЕНИЕ</article-title><trans-title-group xml:lang="en"><trans-title>THE MIOCENE AND DEVONIAN MAGMATISM AT THE JUNCTION BETWEEN THE TUVA-MONGOLIAN MASSIF AND SIBERIAN CRATON: COMMON COMPONENT OF MANTLE SOURCES AND ITS ORIGIN</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>Сергей Васильевич</given-names></name><name name-style="western" xml:lang="en"><surname>Rasskazov</surname><given-names>Sergey V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. геол.-мин. наук, профессор, зав. лабораторией,</p><p>664033, Иркутск, ул. Лермонтова, 128;</p><p>геологический факультет, зав. кафедрой динамической геологии</p></bio><bio xml:lang="en"><p>Doctor of Geology and Mineralogy, Professor, Head of Laboratory,</p><p>664033, Irkutsk, Lermontov street, 128</p></bio><email xlink:type="simple">rassk@crust.irk.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>Ильясова</surname><given-names>Айгуль Маратовна</given-names></name><name name-style="western" xml:lang="en"><surname>Il'yasova</surname><given-names>Aigul M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, н.с.,</p><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Researcher,</p><p>664033, Irkutsk, Lermontov street, 128</p></bio><email xlink:type="simple">ila@crust.irk.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>Ясныгина</surname><given-names>Татьяна Александровна</given-names></name><name name-style="western" xml:lang="en"><surname>Yasnygina</surname><given-names>Tatiana A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, с.н.с.,</p><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Senior Researcher,</p><p>664033, Irkutsk, Lermontov street, 128</p></bio><email xlink:type="simple">ty@crust.irk.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>Фефелов</surname><given-names>Николай Николаевич</given-names></name><name name-style="western" xml:lang="en"><surname>Fefelov</surname><given-names>Nikolay N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, с.н.с.,</p><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Senior Researcher,</p><p>664033, Irkutsk, Lermontov street, 128</p></bio><xref ref-type="aff" rid="aff-2"/></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, Siberian Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><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 RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2012</year></pub-date><pub-date pub-type="epub"><day>23</day><month>09</month><year>2015</year></pub-date><volume>3</volume><issue>2</issue><fpage>77</fpage><lpage>102</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Рассказов С.В., Ильясова А.М., Ясныгина Т.А., Фефелов Н.Н., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Рассказов С.В., Ильясова А.М., Ясныгина Т.А., Фефелов Н.Н.</copyright-holder><copyright-holder xml:lang="en">Rasskazov S.V., Il'yasova A.M., Yasnygina T.A., Fefelov N.N.</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/154">https://www.gt-crust.ru/jour/article/view/154</self-uri><abstract><p>В структурном сочленении неопротерозойского Тувино-Монгольского массива с Сибирским кратоном пространственно совмещены между собой девонские дайки Урик-Бельского и Шагайтэ-Гол-Урикского поясов и миоценовые лавы Урикского вулканического поля. Первый дайковый пояс представлен базальтами-андезибазальтами толеитовой серии, второй – трахибазальтами-трахиандезибазальтами умереннощелочной серии с локальным распространением трахибазальтов-фонотефритов серии повышенной щелочности. Урикское вулканическое поле образуют трахибазальты-трахиандезибазальты умереннощелочной серии. Выявлено частичное сходство концентраций петрогенных оксидов, микроэлементов и изотопных отношений стронция и свинца разновозрастных магматических серий. С поправкой на возраст определен общий компонент магматических расплавов по сходящимся трендам его смешения с компонентами мантийной части литосферы и коры. Идентификация компонента послужила основой для расшифровки характера изотопно-геохимической гетерогенности разновозрастных магматических источников. Сделан вывод о том, что общий компонент характеризует либо модифицированный (обедненный) нижнемантийный резервуар, либо, что более вероятно, локальную область конвектирующей астеносферной мантии, подстилающей Тувино-Монгольский массив. В последней интерпретации допускается образование локального конвектирующего объема астеносферы в середине неопротерозоя, одновременно с заложением и развитием Окинской зоны массива, и накладываются ограничения на последующие существенные преобразования астеносферы под влиянием поднятия плюмового или погружения слэбового материала.</p></abstract><trans-abstract xml:lang="en"><p>Devonian dikes of the Urik-Belaya and Shagayte-Gol-Urik zones and Miocene lavas of the Urik volcanic field are spatially associated with each other at the structural junction between the Neoproterozoic Tuva-Mongolian massif and Siberian craton. The former dike belt is represented by basalts and basaltic andesites of tholeiitic series and the latter one by trachybasalts, trachyandesitic basalts of moderately alkaline series and trachybasalts, phonotephrites of highly alkaline one. The Urik volcanic field is composed of trachybasalts and trachyandesitic basalts of moderately alkaline series. A partial similarity between magmatic series of different age is found in terms of major oxides, trace elements, and Sr, Pb isotopes. The common component corrected for age was defined through its converging mixing trends with those of the lithospheric mantle and crust. The component identification was a basis for deciphering the nature of isotopic and geochemical heterogeneity of evolved magmatic sources. It was inferred that the common component characterizes either a modified (depleted) reservoir of the lower mantle or, more likely, a local region of the convecting asthenospheric mantle that underlies the Tuva-Mongolian massif. The latter interpretation assumes the formation of a locally convecting asthenosphere in the middle Neoproterozoic, along with the development of the Oka zone at the massif, and puts constrains on later sufficient processing of the asthenosphere due to rising plumes or subducting slabs.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Восточный Саян</kwd><kwd>девон</kwd><kwd>миоцен</kwd><kwd>дайки</kwd><kwd>базальты</kwd><kwd>литосфера</kwd><kwd>астеносфера</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Eastern Sayans</kwd><kwd>Devonian</kwd><kwd>Miocene</kwd><kwd>dikes</kwd><kwd>basalts</kwd><kwd>lithosphere</kwd><kwd>asthenosphere</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">ФЦП «Научные и научно-педагогические кадры инновационной России» на 2009–2013 годы», государственный контракт № П736</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">Anderson D.L., 1995. 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