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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-2014-5-3-0152</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-11</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>НЕОПРОТЕРОЗОЙСКАЯ ОСТРОВОДУЖНАЯ АССОЦИАЦИЯ ЗОЛОТОРУДНОГО ПОЛЯ МУКОДЕК (СЕВЕРНОЕ ПРИБАЙКАЛЬЕ)</article-title><trans-title-group xml:lang="en"><trans-title>THE NEOPROTEROZOIC ISLAND-ARC ASSOCIATION OF THE MUKODEK GOLD-ORE FIELD, NORTHERN BAIKAL AREA</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>аспирант Институт земной коры СО РАН 664033, Иркутск, ул. Лермонтова, 128, Россия Тел.: (3952)427117; факс: (3952)427000</p></bio><bio xml:lang="en"><p>post graduate student Institute of the Earth’s crust of SB RAS 128 Lermontov street, Irkutsk 664033, Russia Tel.: (3952)427117; fax: (3952)427000</p></bio><email xlink:type="simple">balagan-2000@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>Гладкочуб</surname><given-names>Д. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Gladkochub</surname><given-names>D. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. геол.-мин. наук, директор института Институт земной коры СО РАН 664033, Иркутск, ул. Лермонтова, 128, Россия </p></bio><bio xml:lang="en"><p>Doctor of Geology and Mineralogy, Director of the Institute Institute of the Earth’s Crust, Siberian Branch of RAS 128 Lermontov street, Irkutsk 664033, Russia</p></bio><email xlink:type="simple">dima@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>Донская </surname><given-names>Т. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Donskaya </surname><given-names>T. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, с.н.с. Институт земной коры СО РАН 664033, Иркутск, ул. Лермонтова, 128, Россия </p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Senior researcher Institute of the Earth’s Crust, Siberian Branch of RAS 128 Lermontov street, Irkutsk 664033, Russia</p></bio><email xlink:type="simple">tanlen@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, Иркутск, Россия </institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth's Crust of SB RAS, Irkutsk, Russia </institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2014</year></pub-date><pub-date pub-type="epub"><day>04</day><month>09</month><year>2015</year></pub-date><volume>5</volume><issue>3</issue><fpage>743</fpage><lpage>762</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ванин В.А., Гладкочуб Д.П., Донская  Т.В., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Ванин В.А., Гладкочуб Д.П., Донская  Т.В.</copyright-holder><copyright-holder xml:lang="en">Vanin V.A., Gladkochub D.P., Donskaya  T.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/11">https://www.gt-crust.ru/jour/article/view/11</self-uri><abstract/><trans-abstract xml:lang="en"><p>Metamorphosed volcanic rocks of the Ushmukan suite were studied in the Mukodek gold-ore field located in the Baikal-Muya belt in the Northern Baikal area, Russia. The Ushmukan suite shows interleaving of ortoschists which compositions are widely variable. Basalt-andesite-dacite series of normal alkalinity are the substrate of the studied metavolcanic rocks. Based on the set of geochemical characteristics, it is concluded that the rocks were formed in suprasubduction geodynamic conditions corresponding to a mature island arc. The proximity of the geological locations and the similarity of the geochemical characteristics of the volcanic rocks of the Ushmukan suite and rocks of the Kelyan suite (Neoproterozoic, 823 Ma), which have similar compositions, give grounds to consider these two rock suites as age peers. Specific features of gold distribution through the Mukodek gold-ore field are analyzed. Industrial gold contents are recorded only in berezite-listvenite metasomatic rocks of the gold-quartz-sulfide formation which were formed on metavolcanic rocks of the Ushmukan suite. It is concluded that the volcanic rocks, which are specific of the island-arc setting, could be a source of gold for deposits in the Mukodek gold-ore field.</p><p> </p></trans-abstract><kwd-group xml:lang="ru"><kwd>неопротерозой</kwd><kwd>вулканиты</kwd><kwd>островная дуга</kwd><kwd>Байкало-Муйский пояс</kwd><kwd>ушмуканская свита</kwd><kwd>метасоматиты</kwd><kwd>золото-кварц-сульфидная формация</kwd><kwd>золоторудное поле Мукодек</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Neoproterozoic</kwd><kwd>volcanic rocks</kwd><kwd>island arc</kwd><kwd>Baikal-Muya belt</kwd><kwd>Ushmukan suite</kwd><kwd>metasomatic rocks</kwd><kwd>gold-quartz-sulfide formation</kwd><kwd>Mukodek gold-ore field</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">Artemiev A.N., Tsypukov Yu.P., 1963. Report on geological survey works conducted by Orkolikan Party in 1962. 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