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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">NZMXJC</article-id>
      <article-id custom-type="pmi" pub-id-type="custom">pmi-16253</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/16253</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">Velocity structure of the Earth’s crust and upper mantle in the Pechenga ore region and adjacent areas in the northwestern part of the Lapland-Kola orogen by the receiver function technique</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Скоростное строение земной коры и верхней мантии Печенгского рудного района и сопредельных территорий в северо-западной части Лапландско-Кольского орогена методом функций приемника</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Goev</surname>
            <given-names>Andrei G.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Гоев</surname>
              <given-names>А. Г.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Goev</surname>
              <given-names>Andrei G.</given-names>
            </name>
          </name-alternatives>
          <email>andr.goev@gmail.com</email>
          <contrib-id contrib-id-type="orcid">0000-0001-9477-5963</contrib-id>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
        <aff-alternatives id="aff1">
          <aff>
            <institution xml:lang="ru">Институт динамики геосфер имени академика М.А.Садовского РАН (Москва, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Sadovsky Institute of Geosphere Dynamics, RAS (Moscow, Russia)</institution>
          </aff>
        </aff-alternatives>
      </contrib-group>
      <pub-date pub-type="epub" iso-8601-date="2024-04-09">
        <day>09</day>
        <month>04</month>
        <year>2024</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>2024</year>
      </pub-date>
      <volume>266</volume>
      <fpage>188</fpage>
      <lpage>198</lpage>
      <history>
        <date date-type="received" iso-8601-date="2023-05-31">
          <day>31</day>
          <month>05</month>
          <year>2023</year>
        </date>
        <date date-type="accepted" iso-8601-date="2023-12-27">
          <day>27</day>
          <month>12</month>
          <year>2023</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2024-04-25">
          <day>25</day>
          <month>04</month>
          <year>2024</year>
        </date>
      </history>
      <permissions>
        <copyright-statement xml:lang="ru">© 2024 А. Г. Гоев</copyright-statement>
        <copyright-statement xml:lang="en">© 2024 Andrei G. Goev</copyright-statement>
        <copyright-year>2024</copyright-year>
        <copyright-holder xml:lang="ru">А. Г. Гоев</copyright-holder>
        <copyright-holder xml:lang="en">Andrei G. Goev</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/16253">https://pmi.spmi.ru/pmi/article/view/16253</self-uri>
      <abstract xml:lang="ru">
        <p>Представлено исследование земной коры и верхней мантии Печенгского рудного района, а также сопредельных территорий северо-западной части Кольского региона. Методом функций приемника, по данным новой и двух постоянных широкополосных сейсмических станций получены одномерные модели распределения сейсмических скоростей до глубины 300 км. Станции расположены в северных частях Финляндии и Норвегии, а также в Печенгском районе Российской Федерации. Несмотря на близкое (не более 100 км) расположение станций скоростные модели существенно разнятся, что свидетельствует о гетерогенности строения литосферы. Так для станции, расположенной в Финляндии, выявлен градиентный коро-мантийный переход, не прослеживающийся в двух других моделях. На глубинах около 150 км обнаружена зона пониженных скоростей, связанная со средне-литосферной неоднородностью, которая не обнаружена под Печенгским рудным районом. Также в строении земной коры Печенгского района выявлены аномально высокие значения параметра Vp/Vs до глубины около 20 км. С учетом того, что сейсмическая станция установлена в непосредственной близости от крупнейших медно-никелевых месторождений, эта аномалия может интерпретироваться как реликт протерозойской плюмовой активности.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>The article presents a study of the Earth’s crust and upper mantle in the Pechenga ore region, as well as areas adjacent to it in the northwestern part of the Kola region. Applying the receiver function technique to data acquired by three broadband seismic stations, we obtained one-dimensional seismic velocity distribution models to a depth of 300 km. The stations are located in the northern parts of Finland and Norway, as well as in the Pechenga region of the Russian Federation. Despite the stations being in relatively close proximity (within 100 km of each other), the velocity models turned out to be significantly different, which indicates structural discontinuity within the lithosphere. Thus, Finland station data set revealed a gradient crust-mantle transition, which is not present in the other two models. At depths of about 150 km, a low-velocity zone was discovered, associated with mid-lithospheric discontinuity, which was not found beneath the Pechenga ore region. Furthermore, the crustal structure of the Pechenga region has an anomalously high Vp/Vs ratio to a depth of about 20 km. Considering the fact that the Pechenga (Nikel) seismic station was installed in close proximity to major copper-nickel deposits, this anomaly can be interpreted as a relic of Proterozoic plume activity.</p>
      </abstract>
      <kwd-group xml:lang="ru">
        <title>Ключевые слова</title>
        <kwd>Кольский полуостров</kwd>
        <kwd>Лапландско-Кольский ороген</kwd>
        <kwd>литосфера</kwd>
        <kwd>мантия</kwd>
        <kwd>метод функции приемника</kwd>
        <kwd>рудоносность</kwd>
        <kwd>плюм</kwd>
      </kwd-group>
      <kwd-group xml:lang="en">
        <title>Keywords</title>
        <kwd>Kola Peninsula</kwd>
        <kwd>Lapland-Kola orogen</kwd>
        <kwd>lithosphere</kwd>
        <kwd>mantle</kwd>
        <kwd>receiver function</kwd>
        <kwd>ore deposits</kwd>
        <kwd>plume</kwd>
      </kwd-group>
      <funding-group>
        <funding-statement xml:lang="ru">Работа выполнена за счет средств Российского научного фонда, грант № 21-17-00161, кроме обзора тектонической истории всего Фенноскандинавского щита, осуществленного в соответствии с темой 122040400015-5.</funding-statement>
        <funding-statement xml:lang="en">The work was supported by the Russian Science Foundation, grant N 21-17-00161, part  of the review of the tectonic history of the entire Fennoscandian Shield carried out in accordance with topic 122040400015-5.</funding-statement>
      </funding-group>
    </article-meta>
  </front>
  <body/>
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