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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">76143</article-id>
   <article-id pub-id-type="doi">10.2205/2024ES000895</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>25-летие Russian Journal of Earth Sciences</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>25th anniversary of the Russian Journal of Earth Sciences</subject>
    </subj-group>
    <subj-group>
     <subject>25-летие Russian Journal of Earth Sciences</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">The Polymetallic Deposits of the Western European Plate and Structure of the Earth's Crust According to GOCE Gravity Data</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>The Polymetallic Deposits of the Western European Plate and Structure of the Earth's Crust According to GOCE Gravity Data</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-8122-9282</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Галямов</surname>
       <given-names>А. Л.</given-names>
      </name>
      <name xml:lang="en">
       <surname>Galyamov</surname>
       <given-names>A. L.</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-6628-8823</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Волков</surname>
       <given-names>А. В.</given-names>
      </name>
      <name xml:lang="en">
       <surname>Volkov</surname>
       <given-names>A. V.</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-8153-2775</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Лобанов</surname>
       <given-names>К. В.</given-names>
      </name>
      <name xml:lang="en">
       <surname>Lobanov</surname>
       <given-names>K. V.</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Институт геологии рудных месторождений, петрографии минералогии и геохимии (ИГЕМ) Российской академии наук</institution>
    </aff>
    <aff>
     <institution xml:lang="en">The Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences</institution>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2024-02-29T00:00:00+03:00">
    <day>29</day>
    <month>02</month>
    <year>2024</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2024-02-29T00:00:00+03:00">
    <day>29</day>
    <month>02</month>
    <year>2024</year>
   </pub-date>
   <volume>24</volume>
   <issue>1</issue>
   <fpage>1</fpage>
   <lpage>17</lpage>
   <history>
    <date date-type="received" iso-8601-date="2023-10-15T00:00:00+03:00">
     <day>15</day>
     <month>10</month>
     <year>2023</year>
    </date>
    <date date-type="accepted" iso-8601-date="2024-01-15T00:00:00+03:00">
     <day>15</day>
     <month>01</month>
     <year>2024</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/76143/view">https://rjes.ru/en/nauka/article/76143/view</self-uri>
   <abstract xml:lang="ru">
    <p>For the first time, the results of modern studies of the earth's crust based on gravity data from the GOCE satellite Project are used for a comparative regional metallogenic analysis of the geodynamic settings of the formation of polymetallic deposits in Western Europe and the Mediterranean segment of the Tethys belt. It is shown that exhalative sulfide deposits (SEDEX) and cuprous sandstones and shales (SSC) are mainly located in the earth's crust with a predominant development of the lower “basalt” layer of the earth's crust. Pyrite copper and lead-zinc deposits in volcanogenic rocks (VMS), as well as some occurrences of the SEDEX type, are found in supra-subduction island-arc and accretionary crustal settings with a predominant development of the middle “granite” layer. Lead-zinc ores of the Mississippi type (MVT) are localized in deep pericratonic sedimentary basins with petroleum-bearing specialization on the shelf and continental slope, regardless of the stratification of the earth's crust. The results obtained can be used for regional forecasting and metallogenic constructions, prospecting and assessment of new deposits.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>For the first time, the results of modern studies of the earth's crust based on gravity data from the GOCE satellite Project are used for a comparative regional metallogenic analysis of the geodynamic settings of the formation of polymetallic deposits in Western Europe and the Mediterranean segment of the Tethys belt. It is shown that exhalative sulfide deposits (SEDEX) and cuprous sandstones and shales (SSC) are mainly located in the earth's crust with a predominant development of the lower “basalt” layer of the earth's crust. Pyrite copper and lead-zinc deposits in volcanogenic rocks (VMS), as well as some occurrences of the SEDEX type, are found in supra-subduction island-arc and accretionary crustal settings with a predominant development of the middle “granite” layer. Lead-zinc ores of the Mississippi type (MVT) are localized in deep pericratonic sedimentary basins with petroleum-bearing specialization on the shelf and continental slope, regardless of the stratification of the earth's crust. The results obtained can be used for regional forecasting and metallogenic constructions, prospecting and assessment of new deposits.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Western Europe</kwd>
    <kwd>Tethys</kwd>
    <kwd>lithosphere</kwd>
    <kwd>Earth's crust</kwd>
    <kwd>base metal</kwd>
    <kwd>deposit</kwd>
    <kwd>SEDEX</kwd>
    <kwd>MVT</kwd>
    <kwd>VMS</kwd>
    <kwd>SSC</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Western Europe</kwd>
    <kwd>Tethys</kwd>
    <kwd>lithosphere</kwd>
    <kwd>Earth's crust</kwd>
    <kwd>base metal</kwd>
    <kwd>deposit</kwd>
    <kwd>SEDEX</kwd>
    <kwd>MVT</kwd>
    <kwd>VMS</kwd>
    <kwd>SSC</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">The work was supported in terms of the State assignment of IGEM RAS.</funding-statement>
    <funding-statement xml:lang="en">The work was supported in terms of the State assignment of IGEM RAS.</funding-statement>
   </funding-group>
  </article-meta>
 </front>
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