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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">resar</journal-id><journal-title-group><journal-title xml:lang="ru">Природные ресурсы Арктики и Субарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Subarctic Natural Resources</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2618-9712</issn><issn pub-type="epub">2686-9683</issn><publisher><publisher-name>Академия наук Республики Саха (Якутия)</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.31242/2618-9712-2025-30-4-572-588</article-id><article-id custom-type="elpub" pub-id-type="custom">resar-1079</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>Науки о Земле. Геология и полезные ископаемые</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Earth sciences. Geology and mineral resources</subject></subj-group></article-categories><title-group><article-title>Вещественный состав и U-Pb возраст магматических пород   Эвотинского массива (Южная Якутия, Алдано-Становой щит)</article-title><trans-title-group xml:lang="en"><trans-title>Сomposition and U-Pb age of igneous rocks of the Evotinsky massif (Southern Yakutia, Aldan-Stanovoy shield)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-0204-1653</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Иванов</surname><given-names>М. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>M. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Иванов Мичил Спартакович, младший научный сотрудник</p><p>ResearcherID: AAL 7447-2021</p><p>Scopus Author ID: 57212410522</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Yakutsk</p></bio><email xlink:type="simple">ivanov.michil@bk.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-5485-3127</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Иванов</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>A. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Иванов Алексей Иванович, кандидат геолого-минералогических наук, старший научный сотрудник</p><p>ResearcherID: JBR-7954-2023</p><p>Scopus Author ID: 57674640500</p><p> г. Якутск</p></bio><bio xml:lang="en"><p>Ivanov, Michil Spartakovich, Junior Researcher</p><p>ResearcherID: AAL-7447-2021Scopus Author ID: 57212410522</p><p>Yakutsk</p></bio><email xlink:type="simple">aiivanov@diamond.ysn.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-0115-5146</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Журавлев</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Zhuravlev</surname><given-names>A. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p> Журавлев Анатолий Иванович, младший научный сотрудник</p><p>ResearcherID: AAC-6095-2019</p><p>Scopus Author ID: 57200217371</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Ivanov, Alexey Ivanovich, Cand. Sci. (Geol. and Mineral.), Senior Researcher</p><p>ResearcherID: JBR-7954-2023</p><p>Scopus Author ID: 57674640500</p><p>Yakutsk</p></bio><email xlink:type="simple">ai.zhuravlevgeo@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7491-1067</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Лоскутов</surname><given-names>Е. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Loskutov</surname><given-names>E. E.</given-names></name></name-alternatives><bio xml:lang="ru"><p> Лоскутов Евгений Евгеньевич, кандидат геолого-минералогических наук, старший научный сотрудник</p><p>ResearcherID: AAO-4823-2021</p><p>Scopus Author ID: 57205150102</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Zhuravlev, Anatolii Ivanovich, Junior Researcher</p><p>ResearcherID: AAC-6095-2019Scopus Author ID: 57200217371</p><p>Yakutsk</p></bio><email xlink:type="simple">Loskutov@diamond.ysn.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-9767-6610</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Кравченко</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kravchenko</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кравченко Александр Александрович , кандидат геолого-минералогических наук, старший научный сотрудник</p><p>Scopus Author ID: 15750892800</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Kravchenko, Alexander Alexanderovich , Cand. Sci. (Geol. and Mineral.), Senior Researcher</p><p>Scopus Author ID: 15750892800</p><p>Yakutsk</p></bio><email xlink:type="simple">freshrock@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-3288-7999</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Гузев</surname><given-names>В. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Guzev</surname><given-names>V. E.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Гузев Владислав Евгеньевич, кандидат геолого-минералогических наук, ведущий геолог</p><p>Scopus Author ID: 57355951700</p><p>г. Санкт-Петербург</p></bio><bio xml:lang="en"><p>Guzev, Vladislav Evgenievich, Cand. Sci. (Geol. and Mineral.), Leading Geologist</p><p>Scopus Author ID: 57355951700</p><p>St. Petersburg</p></bio><email xlink:type="simple">lector10@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-2001-1391</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Терехов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Terekhov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Терехов Артем Валерьевич, кандидат геолого-минералогических наук, зав. отделом</p><p>Scopus Author ID: 57215378338</p><p>г. Санкт-Петербург</p></bio><bio xml:lang="en"><p>Terekhov, Artem Valerievich, Cand. Sci. (Geol. and Mineral.), Head of Department</p><p>Scopus Author ID: 57215378338</p><p>St. Petersburg</p></bio><email xlink:type="simple">artem_terekhov@vsegei.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Институт геологии алмаза и благородных металлов СО РАН<country>Россия</country></aff><aff xml:lang="en">Diamond and Precious Metal Geology Institute, Siberian Branch of the Russian Academy of Sciences<country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru">Всероссийский научно-исследовательский геологический институт им. А.П. Карпинского<country>Россия</country></aff><aff xml:lang="en">Russian Geological Research Institute (VSEGEI)<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>13</day><month>01</month><year>2026</year></pub-date><volume>30</volume><issue>4</issue><fpage>572</fpage><lpage>588</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Иванов М.С., Иванов А.И., Журавлев А.И., Лоскутов Е.Е., Кравченко А.А., Гузев В.Е., Терехов А.В., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Иванов М.С., Иванов А.И., Журавлев А.И., Лоскутов Е.Е., Кравченко А.А., Гузев В.Е., Терехов А.В.</copyright-holder><copyright-holder xml:lang="en">Ivanov M.S., Ivanov A.I., Zhuravlev A.I., Loskutov E.E., Kravchenko A.A., Guzev V.E., Terekhov A.V.</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://resar.elpub.ru/jour/article/view/1079">https://resar.elpub.ru/jour/article/view/1079</self-uri><abstract><p>Проблемы определения металлогенической специализации магматических пород рудных районов всегда ак туальны и дискуссионны. В решении этих задач ключевой момент – комплексное изучение отдельно взятых объектов с целью выявления особенностей петрографического и петро-геохимического составов магматических пород, а также геохронологические исследования во взаимосвязи с условиями образования и металлогенической оценкой последних, позволяющие получить объективную картину. Одним из таких образований яв ляется Эвотинский массив, пространственно входящий в одноименный рудно-россыпной район центральной части Алдано-Станового щита. При исследовании магматических образований главных фаз массива были использованы образцы пород, отобранные в ходе полевых работ 2018–2020 гг., с последующей обработкой и определением основных компонентов методами силикатного, многоэлементного анализов в отделе физикохимических методов анализа Института геологии алмаза и благородных металлов СО РАН и масс-спектрометрии в лаборатории ООО «ХАЦ Плазма», г. Томск. Геохронологические исследования U-Pb методом (SIMS, SHRIMP-II) по цирконам проводились в Центре изотопных исследований Всероссийского научно-исследова тельского геологического института им. А.П. Карпинского. В результате изучения и интерпретации аналитического материала получены следующие результаты и выводы: Эвотинский массив имеет антидромное строение. Установлены две фазы внедрения: первая – амфиболовые кварцевые сиениты, вторая – амфибол-пироксеновые кварцевые монцониты. Породы принадлежат к высококалиевой известково-щелочной петрохимической серии и соответствуют производным шошонит-латитового ряда. Установлен вклад в формирование массива как мантийных, так и коровых источников. По петрогеохимическим параметрам, соотношению редких элементов Rb, Y, Yb, Ta породы массива близки составам вулканитов окраинно-континентальных и островных дуг. U-Pb воз раст по циркону (SHRIMP II) амфиболовых кварцевых сиенитов – 119 ± 1 млн лет, амфибол-пироксеновых кварцевых монцонитов – 117 ± 1 млн лет (аптский век раннего мела). Один из основных выводов состоит в том, что образование Эвотинского массива происходило в условиях задугового растяжения на заключительных стадиях закрытия Монголо-Охотского океана, а также показан минерагенический потенциал Эвотинского массива на золотую минерализацию.</p></abstract><trans-abstract xml:lang="en"><p>Determining the metallogenic specialization of igneous rocks in ore districts remains a pressing and often controversial challenge. Addressing this issue requires a comprehensive approach, that integrates petrographic and petrogeochemical data with geochronological studies of individual formations. Such integrated analysis, when contextualized within specific formation conditions and metallogenic assessments, provides a robust framework for interpretation. The Evotinsky massif, located within the eponymous Evotinsky placer ore region in the central Aldan-Stanovoy shield, represents one such critical formation. This study investigates its petrogenesis based on rock samples collected during fieldwork from 2018 to 2020, focusing on the massif’s main phases. Subsequent processing and major element analysis were performed using silicate and multielement techniques at the Department of Physicochemical Analysis Methods of the Diamond and Precious Metals Geology Institute SB RAS (Yakutsk). Trace element concentrations were determined by mass spectrometry at the САС Plasma LLC laboratory (Tomsk). Finally, geochronological U-Pb dating of zircons was conducted using SIMS (SHRIMP-II) at the Center for Isotope Research of the Karpinsky Russian Geological Research Institute (VSEGEI). The Evotinsky massif displays an antidromous structure and comprises two intrusive phases: an earlier phase of amphibole quartz syenites and a later phase of amphibole-pyroxene quartz monzonites. The rocks are classified within the high potassium calc-alkaline series, corresponding to derivatives of the shoshonite-latite series. Geochemical data indicate a mixed mantle and crustal source for the magmas. Petrochemical parameters and trace element ratios (Rb, Y, Yb, Ta) show compositions analogous to volcanic rocks from continental margins and island arcs. U-Pb zircon geochronology (SHRIMP II) constrains the emplacement of the amphibole quartz syenites to 119 ± 1 Ma and the amphibole-pyroxene quartz monzonites to 117 ± 1 Ma (Aptian, Early Cretaceous). In conclusion, the Evotinsky massif formed under back-arc extensional conditions during the final stages of the Mongol-Okhotsk Ocean closure. Furthermore, these findings demonstrate the massif’s significant potential for gold mineralization.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Алдано-Становой щит</kwd><kwd>Эвотинский рудно-россыпной район</kwd><kwd>магматизм</kwd><kwd>U-Pb возраст цир кона</kwd><kwd>кварцевые сиениты</kwd><kwd>кварцевые монцониты</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Aldan-Stanovoy shield</kwd><kwd>Evotinsky gold-bearing region</kwd><kwd>magmatism</kwd><kwd>U-Pb age from zircons</kwd><kwd>quartz syen ites</kwd><kwd>quartz monzonites</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Работа выполнена в рамках госзадания ИГАБМ СО РАН (проект № FUFG-2024-0005).Авторы выражают благодарность за проведение аналитических работ сотрудникам ИГАБМ  СО РАН Л.Т. Галенчиковой и С.Ю. Коркиной</funding-statement></funding-group><funding-group xml:lang="en"><funding-statement>This study was conducted within the framework of the state assignment for the Diamond and Precious Metals Geology Institute SB RAS (project No. FUFG-2024-0005).The authors are grateful to L.T. Galenchikova and S.Yu. Korkina from the Diamond and Pre cious Metals Geology Institute SB RAS for conducting the analytical work.</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">Тектоника, геодинамика и металлогения территории Республики Саха (Якутия). Отв. редакторы: д.г.-м.н. Л.М. Парфенов, чл.-корр. РАН М.И. Кузьмин. М.: МАИК “Наука/Интерпериодика”; 2001. 571 с.</mixed-citation><mixed-citation xml:lang="en">Tectonics, geodynamics and metallogeny of the territory of the Republic of Sakha (Yakutia). Responsible editors: doctor of geological and mineralogical sciences L.M. 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