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    <journal-meta>
      <journal-id journal-id-type="issn">2411-3336</journal-id>
      <journal-id journal-id-type="eissn">2541-9404</journal-id>
      <journal-title-group>
        <journal-title xml:lang="ru">Записки Горного института</journal-title>
        <journal-title xml:lang="en">Journal of Mining Institute</journal-title>
      </journal-title-group>
      <publisher>
        <publisher-name xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины ΙΙ</publisher-name>
        <publisher-name xml:lang="en">Empress Catherine II Saint Petersburg Mining University</publisher-name>
      </publisher>
    </journal-meta>
    <article-meta>
      <article-id custom-type="edn" pub-id-type="custom">XCETNQ</article-id>
      <article-id custom-type="pmi" pub-id-type="custom">pmi-16641</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/16641</article-id>
      <article-categories>
        <subj-group subj-group-type="section-heading" xml:lang="ru">
          <subject>Геология</subject>
        </subj-group>
        <subj-group subj-group-type="section-heading" xml:lang="en">
          <subject>Geology</subject>
        </subj-group>
      </article-categories>
      <title-group>
        <article-title xml:lang="en">Diamondiferous garnet lherzolite from the V.Grib kimberlite pipe:  relationship between subduction, mantle metasomatism  and diamond formation</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Алмазоносный гранатовый лерцолит из кимберлитовой трубки им. В.Гриба: взаимосвязь субдукции, мантийного метасоматоза и образования алмаза</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Agasheva</surname>
            <given-names>Elena V.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Агашева</surname>
              <given-names>Е. В.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Agasheva</surname>
              <given-names>Elena V.</given-names>
            </name>
          </name-alternatives>
          <email>shchukinalena@igm.nsc.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0002-9396-8568</contrib-id>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
        <aff-alternatives id="aff1">
          <aff>
            <institution xml:lang="ru">Институт геологии и минералогии им. В.С.Соболева СО РАН (Новосибирск, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">V.S.Sobolev Institute of  Geology and Mineralogy SB RAS (Novosibirsk, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Gubanov</surname>
            <given-names>Nikolai V.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Губанов</surname>
              <given-names>Н. В.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Gubanov</surname>
              <given-names>Nikolai V.</given-names>
            </name>
          </name-alternatives>
          <email>goubanov97@gmail.com</email>
          <contrib-id contrib-id-type="orcid">0000-0002-0718-8021</contrib-id>
          <xref ref-type="aff" rid="aff2"/>
        </contrib>
        <aff-alternatives id="aff2">
          <aff>
            <institution xml:lang="ru">Институт геологии и минералогии им. В.С.Соболева СО РАН (Новосибирск, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">V.S.Sobolev Institute of Geology and Mineralogy SB RAS (Novosibirsk, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Zedgenizov</surname>
            <given-names>Dmitrii A.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Зедгенизов</surname>
              <given-names>Д. А.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Zedgenizov</surname>
              <given-names>Dmitrii A.</given-names>
            </name>
          </name-alternatives>
          <email>Director@igg.uran.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0002-5934-9122</contrib-id>
          <xref ref-type="aff" rid="aff3"/>
        </contrib>
        <aff-alternatives id="aff3">
          <aff>
            <institution xml:lang="ru">Институт геологии и геохимии им. академика А.Н.Заварицкого (Екатеринбург, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">A.N.Zavaritsky Institute of Geology and Geochemistry UB RAS (Ekaterinburg, Russia)</institution>
          </aff>
        </aff-alternatives>
      </contrib-group>
      <pub-date pub-type="epub" iso-8601-date="2025-09-04">
        <day>04</day>
        <month>09</month>
        <year>2025</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>2025</year>
      </pub-date>
      <volume>276</volume>
      <issue>2</issue>
      <fpage>140</fpage>
      <lpage>156</lpage>
      <history>
        <date date-type="received" iso-8601-date="2025-01-16">
          <day>16</day>
          <month>01</month>
          <year>2025</year>
        </date>
        <date date-type="accepted" iso-8601-date="2025-07-02">
          <day>02</day>
          <month>07</month>
          <year>2025</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2025-12-30">
          <day>30</day>
          <month>12</month>
          <year>2025</year>
        </date>
      </history>
      <permissions>
        <copyright-statement xml:lang="ru">© 2025 Е. В. Агашева, Н. В. Губанов, Д. А. Зедгенизов</copyright-statement>
        <copyright-statement xml:lang="en">© 2025 Elena V. Agasheva, Nikolai V. Gubanov, Dmitrii A. Zedgenizov</copyright-statement>
        <copyright-year>2025</copyright-year>
        <copyright-holder xml:lang="ru">Е. В. Агашева, Н. В. Губанов, Д. А. Зедгенизов</copyright-holder>
        <copyright-holder xml:lang="en">Elena V. Agasheva, Nikolai V. Gubanov, Dmitrii A. Zedgenizov</copyright-holder>
        <license license-type="open-access" xlink:href="http://creativecommons.org/licenses/by/4.0" xml:lang="ru">
          <license-p>Эта статья доступна по лицензии Creative Commons Attribution 4.0 International (CC BY 4.0)</license-p>
        </license>
        <license license-type="open-access" xlink:href="http://creativecommons.org/licenses/by/4.0" xml:lang="en">
          <license-p>This article is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0)</license-p>
        </license>
      </permissions>
      <self-uri xlink:type="simple" xlink:href="https://pmi.spmi.ru/pmi/article/view/16641">https://pmi.spmi.ru/pmi/article/view/16641</self-uri>
      <abstract xml:lang="ru">
        <p>Приведены результаты комплексного исследования алмазосодержащего лерцолита из кимберлитовой трубки им. В.Гриба. Состав породообразующих минералов (оливин, ортопироксен, Cr-диопсид, Cr-пироп) по главным элементам преимущественно соответствует минералам из включений в алмазах лерцолитовой ассоциации и алмазосодержащих лерцолитов мира. Повышенное модальное количество ортопироксена (18 об.%), а также концентрация FeO (7,5 мас.%) и значение отношения MgO/SiO2 (0,89) для лерцолита позволяют отнести его к обогащенным ортопироксеном лерцолитам. Особенности состава Cr-диопсида и Cr-пиропа по редким элементам свидетельствуют о том, что на момент захвата кимберлитом лерцолит сохранил признаки слабого воздействия мантийного метасоматоза. Результаты моделирования позволили предположить в качестве метасоматического агента магнезиокарбонатные и силикатные высокоплотные флюиды (HDF). Признаки влияния протокимберлитового расплава не обнаружены. Степень агрегации азота в алмазе (%В от 6 до 15) указывает на длительное пребывание в мантийных условиях, что исключает формирование незадолго до внедрения кимберлита. Экстремально легкие значения изотопного состава углерода (δ13С = –18,59 ‰) свидетельствуют о вовлечении в образование алмаза органического углерода субдукционной природы. Образование алмаза могло быть связано с древним метасоматическим событием, протекающим при ведущей роли низко-Mg силикатно-карбонатных HDF, источником которых были эклогиты и/или содержащие органический углерод субдуцированные осадочные отложения. Расчетные Р-Т параметры (3,7 ГПа, 814 °С) последнего равновесия минеральных фаз лерцолита указывают на его захват с глубины ~118 км, что соответствует участку литосферной мантии (примерно 95-120 км), в пределах которого ранее обнаружены породы, также имеющие признаки специфических преобразований под воздействием субдукционно-связанных флюидов.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>The article presents the results of a comprehensive study of diamondiferous lherzolite from the V.Grib kimberlite pipe. The composition of rock-forming minerals (olivine, orthopyroxene, Cr-diopside, Cr-pyrope) in terms of major elements mainly corresponds to minerals from inclusions in diamonds of the lherzolite association and diamondiferous lherzolites of the world. The elevated modal amount of orthopyroxene (18 vol.%) as well as the concentration of FeO (7.5 wt.%) and the value of MgO/SiO2 ratio (0.89) for lherzolite allow assigning it to orthopyroxene-enriched lherzolites. Specific features of the composition of Cr-diopside and Cr-pyrope in respect of rare elements indicate that at the time of capture by kimberlite, lherzolite retained the signs of a slight impact of mantle metasomatism. Modelling results allowed suggesting magnesiocarbonate and silicate high-density fluids (HDF) as the metasomatic agent. No signs of influence of proto-kimberlite melt were found. The degree of nitrogen aggregation in diamond (%B from 6 to 15) indicates a long stay in mantle conditions, which excludes formation shortly before the emplacement of kimberlite. Extremely light values of carbon isotope composition (δ13C = –18.59 ‰) indicate the involvement of organic carbon of subduction origin in diamond formation. Diamond formation could be associated with an ancient metasomatic event occurring with the leading role of low-Mg silicate-carbonate HDF, the source of which were eclogites and/or subducted sedimentary deposits containing organic carbon. The calculated P-T parameters (3.7 GPa, 814 °C) of the last equilibrium of mineral phases of lherzolite point to its capture from a depth of ~118 km, which corresponds to a section of the lithospheric mantle (approximately 95-120 km), within which rocks also demonstrating features of specific transformations under the influence of subduction-related fluids were earlier discovered.</p>
      </abstract>
      <kwd-group xml:lang="ru">
        <title>Ключевые слова</title>
        <kwd>алмаз</kwd>
        <kwd>субдукция</kwd>
        <kwd>геохимия</kwd>
        <kwd>мантийный метасоматоз</kwd>
        <kwd>литосферная мантия</kwd>
        <kwd>кимберлит</kwd>
      </kwd-group>
      <kwd-group xml:lang="en">
        <title>Keywords</title>
        <kwd>diamond</kwd>
        <kwd>subduction</kwd>
        <kwd>geochemistry</kwd>
        <kwd>mantle metasomatism</kwd>
        <kwd>lithospheric mantle</kwd>
        <kwd>kimberlite</kwd>
      </kwd-group>
      <funding-group>
        <funding-statement xml:lang="ru">Аналитические работы выполнены за счет гранта РНФ 20-77-10018. Отбор образца ксенолита осуществлен в рамках полевых работ по Государственному заданию ИГМ СО РАН № 122041400241-5.</funding-statement>
        <funding-statement xml:lang="en">The analytical work was carried out at the expense of the RSF grant 20-77-10018. Xenolith sample was collected as part of field work under the State assignment of IGM SB RAS N 122041400241-5.</funding-statement>
      </funding-group>
    </article-meta>
  </front>
  <body/>
  <back>
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</article>
