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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">reggeomet</journal-id><journal-title-group><journal-title xml:lang="ru">Региональная геология и металлогения</journal-title><trans-title-group xml:lang="en"><trans-title>Regional Geology and Metallogeny</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0869-7892</issn><publisher><publisher-name>(ФГБУ "Институт Карпинского")</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">reggeomet-212</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>МЕТАЛЛОГЕНИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>METALLOGENY</subject></subj-group></article-categories><title-group><article-title>Золото-сульфидная вкрапленная минерализация месторождения Гадир (Малый Кавказ, Азербайджан)</article-title><trans-title-group xml:lang="en"><trans-title>Gold-sulphide disseminated mineralization of the Gadir deposit (Lesser Caucasus, Azerbaijan)</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>Байрамов</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bayramov</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>аспирант</p></bio><bio xml:lang="en"><p>PhD Student</p></bio><email xlink:type="simple">geoloq_aydin@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Азербайджанский государственный университет нефти и промышленности (АГУНП)<country>Россия</country></aff><aff xml:lang="en">Azerbaijan State Oil and Industry University (ASOIU)<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>19</day><month>06</month><year>2025</year></pub-date><volume>0</volume><issue>82</issue><elocation-id>103–112</elocation-id><permissions><copyright-statement>Copyright &amp;#x00A9; Байрамов А.А., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Байрамов А.А.</copyright-holder><copyright-holder xml:lang="en">Bayramov A.A.</copyright-holder><license 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://reggeomet.elpub.ru/jour/article/view/212">https://reggeomet.elpub.ru/jour/article/view/212</self-uri><abstract><p>Золото-сульфидное месторождение Гадир располагается в северо-западной части Гедабекского месторождения в Йогундагской эпитермальной системе. Рудовмещающие толщи представлены вулканогенно- и вулканогенно-осадочными отложениями средней юры, сформировавшимися в обстановке вулканизма базальт-андезит-дацит-риолитовой формации. Минералогия, минерализация золота и содержание металлов в этом месторождении были изучены в ходе текущих исследований с целью определения геологических условий, временных и пространственных связей с определенными минеральными сообществами и ассоциациями. Минералогия рудных тел в основном состоит из пирита, халькопирита, сфалерита, галенита, магнетита, самородного золота. Самородное золото наблюдалось в халькопирите, что, вероятно, связано со второй стадией отложения руды.</p></abstract><trans-abstract xml:lang="en"><p>The Gadir gold-sulfide deposit is located in the northwestern part of the Gedabek deposit in the Yogundag epithermal system. Ore-bearing strata are represented by Middle Jurassic volcanic and volcanic-sedimentary rocks formed under conditions of basalt-andesite-dacite-rhyolite volcanism formation. Mineralogy, gold mineralization, and metal content in the Gadir deposit have been investigated during ongoing studies to determine geological setting, temporal and spatial relationships with specific mineral assemblages and associations. Mine ralogy of ore bodies is mainly characterzed by pyrite, chalcopyrite, sphalerite, galena, magnetite, and native gold. Native gold was recorded in chalcopyrite that is probably related to the second stage of ore deposition.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>самородное золото</kwd><kwd>стадии минерализации</kwd><kwd>Гадир</kwd><kwd>Гедабек</kwd></kwd-group><kwd-group xml:lang="en"><kwd>native gold</kwd><kwd>mineralization stages</kwd><kwd>Gadir</kwd><kwd>Gedabek</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">Гусейнов Г. С. Распределение благородных металлов (Аu, Ag) в рудах Гедабекского золотомедно-колчеданного месторождения (Малый Кавказ) // Отечественная геология. – 2017. – № 6. – С. 67–71.</mixed-citation><mixed-citation xml:lang="en">Guseynov G. S. The distribution of precious metals (Au, Ag) in the ores of the Gadabek gold-copper-pyrite deposit (Lesser Caucasus). Otechestvennaya geologiya. 2017. No 6, pp. 67–71. 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