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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">10.31242/2618-9712-2022-27-4-486-498</article-id><article-id custom-type="elpub" pub-id-type="custom">resar-72</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. Общая и региональная геология, петрология и вулканология</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Earth sciences. General and regional geology, petrology and volcanology</subject></subj-group></article-categories><title-group><article-title>Геологическое строение и вещественный состав кимберлитовых трубок Хомпу-Майского поля (Центральная Якутия)</article-title><trans-title-group xml:lang="en"><trans-title>The geology and composition of the KhompuMay field kimberlite pipes (Central Yakutia, Russia)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-3019-1245</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Опарин</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Oparin</surname><given-names>N. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>ОПАРИН Николай Александрович, младший научный сотрудник, Author ID: 57035370200, Researcher ID: J-7673-2018</p><p>677980, г. Якутск, пр. Ленина, 39</p></bio><bio xml:lang="en"><p>OPARIN, Nikolay Alexandrovich, Junior researcher, Author ID: 57035370200, Researcher ID: J7673 2018</p><p>39 Lenina pr., Yakutsk 677980</p></bio><email xlink:type="simple">nik3256-1989@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/0000-0003-1010-7592</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Олейников</surname><given-names>О. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Oleinikov</surname><given-names>O. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>ОЛЕЙНИКОВ Олег Борисович, ведущий научный сотрудник, кандидат геолого-минералогических наук, Author ID: 8730610300, Researcher ID: K-1689-2048</p><p>677980, г. Якутск, пр. Ленина, 39</p></bio><bio xml:lang="en"><p>OLEINIKOV, Oleg Borisovich, Cand.Sci (Geology and Mineralogy), Leading Researcher, Author ID: 8730610300, Researcher ID: K16892048</p><p>39 Lenina pr., Yakutsk 677980</p></bio><email xlink:type="simple">olei-oleg@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии алмаза и благородных металлов СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Diamond and Precious Metal Geology Institute, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>09</day><month>09</month><year>2022</year></pub-date><volume>27</volume><issue>4</issue><fpage>486</fpage><lpage>498</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Опарин Н.А., Олейников О.Б., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Опарин Н.А., Олейников О.Б.</copyright-holder><copyright-holder xml:lang="en">Oparin N.A., Oleinikov O.B.</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://resar.elpub.ru/jour/article/view/72">https://resar.elpub.ru/jour/article/view/72</self-uri><abstract><p>Приведены результаты петрохимических и геохимических исследований кимберлитов трубок Хомпу-Майского поля (Центральная Якутия) и сравнение их микроэлементного состава с аналогами кимберлитовых провинций Якутской (Россия) и Кимберли (ЮАР). Представлены петрографический состав и результаты постмагматической карбонатизации кимберлитов трубок Манчары, им. А.П. Смелова и Дабан. В обобщенной модели верхней части трубок выделены три условных горизонта: нижний, сложенный наименее измененными порода ми; средний, кимберлитовые породы которого фрагментированы в результате процессов карбонатизации; верхний, выполненный интенсивно карбонатизированными породами с утраченными текстурно-структурными признаками. Полученные данные химического и микроэлементного составов пород трубок Хомпу-Майского поля отражают их вещественную специфику, предполагающую схожие условия формирования кимберлитов Центральной Якутии и Южной Африки.</p></abstract><trans-abstract xml:lang="en"><p>The paper presents the results of petro and geochemical studies of the kimberlite pipes within the KhompuMay field (Central Yakutia). Their trace element data were compared with the analogues from the Yakut Kimberlite Province, Russia and the Kimberly Kimberlite Province, RSA. We present the data on petrographic composition and results of postmagmatic carbonation of the Manchary, A.P. Smelov, and Daban pipes kimberlites. The generalized model of the upper parts of the pipes show three conventional horizons: the lower horizon of least altered rocks, the middle horizon of fragments of kimberlite carbonates, and the upper horizon of intensely carbonated rocks without recognizable tex tural and structural characteristics. The obtained data on chemical and trace element compositions of rocks from pipes of the KhompuMay field reflect their material specificity, suggesting similar conditions for formation of kimberlites in Central Yakutia and South Africa.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>кимберлит</kwd><kwd>трубка</kwd><kwd>карбонатизация</kwd><kwd>редкоземельные элементы</kwd><kwd>Хомпу-Майское поле</kwd></kwd-group><kwd-group xml:lang="en"><kwd>kimberlite</kwd><kwd>pipe</kwd><kwd>carbonation</kwd><kwd>rare earth elements</kwd><kwd>KhompuMay field</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках НИР ИГАБМ СО РАН.</funding-statement><funding-statement xml:lang="en">This study was carried out within the Research Project of the DPMGI SB RAS.</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">Смелов А.П., Белоусова Е.А., Зайцев А.И., Олейников О.Б., Павлушин А.Д., Опарин Н.А. 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