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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">geolmsu</journal-id><journal-title-group><journal-title xml:lang="ru">ВЕСТНИК МОСКОВСКОГО УНИВЕРСИТЕТА. СЕРИЯ 4. ГЕОЛОГИЯ</journal-title><trans-title-group xml:lang="en"><trans-title>Moscow University Bulletin. Series 4. Geology</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0579-9406</issn><publisher><publisher-name>Издательский Дом МГУ</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.33623/0579-9406-2018-3-3-11</article-id><article-id custom-type="elpub" pub-id-type="custom">geolmsu-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>Статьи</subject></subj-group></article-categories><title-group><article-title>ВУЛКАНОГЕННЫЕ КОЛЧЕДАННЫЕ МЕСТОРОЖДЕНИЯ БОГАТЫХ ЗОЛОТОМ РУД</article-title><trans-title-group xml:lang="en"><trans-title>VOLCANOGENIC MASSIVE SULFIDE DEPOSITS ENRICHED IN GOLD</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>Дергачев</surname><given-names>A. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Dergachev</surname><given-names>A. L.</given-names></name></name-alternatives><bio xml:lang="ru"/><email xlink:type="simple">alderg@geol.msu.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>Еремин</surname><given-names>Н. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Eremin</surname><given-names>N. I.</given-names></name></name-alternatives><bio xml:lang="ru"/><email xlink:type="simple">eremin@geol.msu.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московский государственный университет имени М.В. Ломоносова</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>28</day><month>06</month><year>2018</year></pub-date><volume>0</volume><issue>3</issue><fpage>3</fpage><lpage>11</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Дергачев A.Л., Еремин Н.И., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Дергачев A.Л., Еремин Н.И.</copyright-holder><copyright-holder xml:lang="en">Dergachev A.L., Eremin N.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://vestnik.geol.msu.ru/jour/article/view/154">https://vestnik.geol.msu.ru/jour/article/view/154</self-uri><abstract><p>В рудах вулканогенных колчеданных месторождений содержатся не только Cu, Zn, Pb, но и Sb, Bi, Te, Se, Ag, Co и другие металлы, а также переменное количество Ag и Au. В некоторых из них запасы Au превышают 100 т, а среднее содержание может достигать десятков г/т. На основе оригинальной базы данных предложены статистические критерии для выделения месторождений с крупными запасами и (или) аномально высоким содержанием Au в рудах. Исследованы некоторые особенности месторождений богатых Au руд, в том числе распределение в геологическом времени и между важнейшими колчеданоносными провинциями, а также ассоциация с палеовулканическими структурами, геохимические и минералогические особенности руд и причины их обогащения золотом.</p></abstract><trans-abstract xml:lang="en"><p>Volcanogenic massive sulfide deposits contain Cu, Zn, Pb, Sb, Bi, Te, Se, Ag, Co and variable amounts of Ag and Au. In some of them gold reserves exceed 100 t while gold grades reach several dozens ppm. Original data base was used to establish statistically meaningful criteria for identification of deposits with large gold reserves and/or anomalously enriched in gold. Some peculiar features of deposits with high Au grades were investigated including distribution in geological history and among the principal metallogenic provinces, association with volcanogenic formations and paleovolcanic structures, geochemical and mineralogical features and factors that caused enrichment in gold.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>золото</kwd><kwd>вулканогенные колчеданные месторождения</kwd><kwd>цветные металлы</kwd><kwd>месторождения богатых золотом руд</kwd></kwd-group><kwd-group xml:lang="en"><kwd>gold</kwd><kwd>base metals</kwd><kwd>volcanogenic massive sulfide deposits</kwd><kwd>deposits of rich gold ores</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">Дергачев А.Л., Еремин Н.И., Сергеева Н.Е. Разномасштабные тенденции в эволюции состава руд вулканогенных колчеданных месторождений // Вестн. Моск. ун-та. Сер. 4. 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