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  <front>
    <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">PIANQZ</article-id>
      <article-id custom-type="pmi" pub-id-type="custom">pmi-16832</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/16832</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">The problem of identifying lower crustal garnet-clinopyroxene granulites and mantle eclogites: a case study of xenoliths from the V.Grib pipe</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Проблема идентификации нижнекоровых гранат-клинопироксеновых гранулитов и мантийных эклогитов на примере ксенолитов трубки им. В.Гриба</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Stetskaya</surname>
            <given-names>Ekaterina V.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Стецкая</surname>
              <given-names>Е. В.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Stetskaya</surname>
              <given-names>Ekaterina V.</given-names>
            </name>
          </name-alternatives>
          <email>yekaterina.logunova.02@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0009-0001-1547-8176</contrib-id>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
        <aff-alternatives id="aff1">
          <aff>
            <institution xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины II (Санкт-Петербург, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Empress Catherine ΙΙ Saint Petersburg Mining University (Saint Petersburg, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Salimgaraeva</surname>
            <given-names>Laysan I.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Салимгараева</surname>
              <given-names>Л. И.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Salimgaraeva</surname>
              <given-names>Laysan I.</given-names>
            </name>
          </name-alternatives>
          <email>fluoritecaf2@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0002-3285-847X</contrib-id>
          <xref ref-type="aff" rid="aff2"/>
        </contrib>
        <aff-alternatives id="aff2">
          <aff>
            <institution xml:lang="ru">Институт геологии и геохронологии докембрия РАН, (Санкт-Петербург, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Institute of Precambrian Geology and Geochronology RAS (Saint Petersburg, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Berezin</surname>
            <given-names>Aleksei V.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Березин</surname>
              <given-names>А. В.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Berezin</surname>
              <given-names>Aleksei V.</given-names>
            </name>
          </name-alternatives>
          <email>berezin-geo@ya.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0002-5324-5840</contrib-id>
          <xref ref-type="aff" rid="aff3"/>
        </contrib>
        <aff-alternatives id="aff3">
          <aff>
            <institution xml:lang="ru">Институт геологии и геохронологии докембрия РАН (Санкт-Петербург, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Institute of Precambrian geology and geochronology RAS (Saint Petersburg, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Ustinov</surname>
            <given-names>Viktor N.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Устинов</surname>
              <given-names>В. Н.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Ustinov</surname>
              <given-names>Viktor N.</given-names>
            </name>
          </name-alternatives>
          <email>agddiamond@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0002-6565-6575</contrib-id>
          <xref ref-type="aff" rid="aff4"/>
        </contrib>
        <aff-alternatives id="aff4">
          <aff>
            <institution xml:lang="ru">АО «АГД Даймондс» (Архангельск, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">AGD Diamonds JSC (Arkhangelsk, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Pendelyak</surname>
            <given-names>Roman N.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Пенделяк</surname>
              <given-names>Р. Н.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Pendelyak</surname>
              <given-names>Roman N.</given-names>
            </name>
          </name-alternatives>
          <email>rpendelyak@agddiamond.com</email>
          <contrib-id contrib-id-type="orcid">0009-0004-7798-2118</contrib-id>
          <xref ref-type="aff" rid="aff5"/>
        </contrib>
        <aff-alternatives id="aff5">
          <aff>
            <institution xml:lang="ru">АО «АГД Даймондс» (Архангельск, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">AGD Diamonds JSC (Arkhangelsk, Russia)</institution>
          </aff>
        </aff-alternatives>
      </contrib-group>
      <pub-date pub-type="epub" iso-8601-date="2026-04-03">
        <day>03</day>
        <month>04</month>
        <year>2026</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>2026</year>
      </pub-date>
      <volume>278</volume>
      <fpage>99</fpage>
      <lpage>114</lpage>
      <history>
        <date date-type="received" iso-8601-date="2025-10-16">
          <day>16</day>
          <month>10</month>
          <year>2025</year>
        </date>
        <date date-type="accepted" iso-8601-date="2025-12-24">
          <day>24</day>
          <month>12</month>
          <year>2025</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2026-02-01">
          <day>01</day>
          <month>02</month>
          <year>2026</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>© Ekaterina V. Stetskaya, Laysan I. Salimgaraeva, Aleksei V. Berezin, Viktor N. Ustinov, Roman N. Pendelyak</copyright-statement>
        <copyright-year>2026</copyright-year>
        <copyright-holder xml:lang="ru">Е. В. Стецкая, Л. И. Салимгараева, А. В. Березин, В. Н. Устинов, Р. Н. Пенделяк</copyright-holder>
        <copyright-holder xml:lang="en">Ekaterina V. Stetskaya, Laysan I. Salimgaraeva, Aleksei V. Berezin, Viktor N. Ustinov, Roman N. Pendelyak</copyright-holder>
        <license xlink:href="http://creativecommons.org/licenses/by/4.0">
          <license-p>CC BY 4.0</license-p>
        </license>
      </permissions>
      <self-uri xlink:type="simple" xlink:href="https://pmi.spmi.ru/pmi/article/view/16832">https://pmi.spmi.ru/pmi/article/view/16832</self-uri>
      <abstract xml:lang="ru">
        <p>Статья посвящена комплексному анализу минералогических и геохимических особенностей ксенолитов кимберлитовой трубки им. В.Гриба, которые представлены нижнекоровыми гранат-клинопироксеновыми гранулитами и мантийными эклогитами. Проводится сравнительная характеристика двух типов ксенолитов, поскольку в настоящее время отсутствуют четкие критерии, по которым их можно было бы разделить. В результате исследования выявлены несколько отличительных признаков, однозначно характеризующих мантийные эклогиты. Это повышенное содержание Cr (в гранатах &amp;gt;300 ppm, в клинопироксенах &amp;gt;1500 ppm), высокое содержание пиропового минала в гранате (больше 34 мол.%) и наличие признаков раннего метасоматоза, проявляющегося в виде метасоматического граната, губчатого клинопироксена, замещаемого паргаситом, а также флогопитовых кайм на контакте граната и клинопироксена. Оценка параметров давления и температуры ксенолитов трубки им. В.Гриба подтвердилa мантийную природу эклогитовых ксенолитов с условиями формирования в диапазоне Т = 800-1200 °С и Р = 30-50 кбар и не опровергла первоначальное предположение о нижнекоровом происхождении гранулитовых ксенолитов, характеризующихся Т = 750-800 °С и Р = 14-15 кбар. Для окончательного решения проблемы идентификации нижнекоровых гранат-клинопироксеновых гранулитов и мантийных эклогитов предложено провести комплексное сравнение изотопно-геохимических характеристик «эклогитового» и «гранулитового» циркона в дальнейшем.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>The article presents a comprehensive analysis of the mineralogical and geochemical features of xenoliths from the V.Grib kimberlite pipe, represented by lower crustal garnet-clinopyroxene granulites and mantle eclogites. A comparative characterization of the two xenolith types is conducted, as clear criteria for their distinction are currently lacking. The study identifies several distinctive features that unequivocally characterize mantle eclogites: elevated Cr contents (in garnets &amp;gt;300 ppm, in clinopyroxenes &amp;gt;1500 ppm), high pyrope content in garnet (&amp;gt;34 mol.%), and evidence of early metasomatism manifested as metasomatic garnet, spongy clinopyroxene replaced by pargasite, and phlogopite rims at garnet-clinopyroxene contacts. Evaluation of the pressure-temperature parameters of the V.Grib pipe xenoliths confirmed the mantle origin of eclogitic xenoliths formed at T = 800-1200 °C and P = 30-50 kbar, and did not refute the initial assumption of a lower crustal origin for granulitic xenoliths characterized by T = 750-800 °C and P = 14-15 kbar. To definitively resolve the issue of identifying lower crustal garnet-clinopyroxene granulites and mantle eclogites, a comprehensive comparison of the isotope-geochemical characteristics of “eclogitic” and “granulitic” zircon is proposed for future research.</p>
      </abstract>
      <kwd-group xml:lang="ru">
        <title>Ключевые слова</title>
        <kwd>трубка им. В.Гриба</kwd>
        <kwd>Р-Т параметры</kwd>
        <kwd>нижнекоровые гранулиты</kwd>
        <kwd>мантийные эклогиты</kwd>
        <kwd>гранаты</kwd>
        <kwd>клинопироксены</kwd>
        <kwd>ксенолиты</kwd>
      </kwd-group>
      <kwd-group xml:lang="en">
        <title>Keywords</title>
        <kwd>The V.Grib pipe</kwd>
        <kwd>P-T parameters</kwd>
        <kwd>lower crustal granulites</kwd>
        <kwd>mantle eclogites</kwd>
        <kwd>garnets</kwd>
        <kwd>clinopyroxenes</kwd>
        <kwd>xenoliths</kwd>
      </kwd-group>
      <funding-group>
        <funding-statement xml:lang="ru">Исследование выполнено при финансовой поддержке гранта РНФ № 24-27-00121.</funding-statement>
        <funding-statement xml:lang="en">The study was supported by the Russian Science Foundation Grant N 24-27-00121.</funding-statement>
      </funding-group>
    </article-meta>
  </front>
  <body/>
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