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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">46978</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Native iron in Miocene sediments</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Native iron in Miocene sediments</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Pechersky</surname>
       <given-names>D M</given-names>
      </name>
      <name xml:lang="en">
       <surname>Pechersky</surname>
       <given-names>D M</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Nurgaliev</surname>
       <given-names>D K</given-names>
      </name>
      <name xml:lang="en">
       <surname>Nurgaliev</surname>
       <given-names>D K</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Trubikhin</surname>
       <given-names>V M</given-names>
      </name>
      <name xml:lang="en">
       <surname>Trubikhin</surname>
       <given-names>V M</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-3"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Geological Faculty, Kazan State University, Kazan, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Geological Faculty, Kazan State University, Kazan, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-3">
    <aff>
     <institution xml:lang="ru">Geological Institute, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Geological Institute, Russian Academy of Sciences, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>10</volume>
   <issue>6</issue>
   <fpage>1</fpage>
   <lpage>11</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-11-10T18:25:36+03:00">
     <day>10</day>
     <month>11</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46978/view">https://rjes.ru/en/nauka/article/46978/view</self-uri>
   <abstract xml:lang="ru">
    <p>With the aid of thermomagnetic analysis up to 800o C we studied the detailed pattern of how native iron is distributed in Miocene sediments of two sections, Khalats Turkmenia and Kvirinaki Georgia, which are more than 1500nbsp;km apart. Out main result is that enrichment by native iron particles was synchronous in both sections. This phenomenon is of extraterrestrial origin and does not depend upon local conditions of deposition. The length of iron-enriched interval from 12.6 to 12.2nbsp;Ma over a vast area cannot result from a single impact event.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>With the aid of thermomagnetic analysis up to 800o C we studied the detailed pattern of how native iron is distributed in Miocene sediments of two sections, Khalats Turkmenia and Kvirinaki Georgia, which are more than 1500nbsp;km apart. Out main result is that enrichment by native iron particles was synchronous in both sections. This phenomenon is of extraterrestrial origin and does not depend upon local conditions of deposition. The length of iron-enriched interval from 12.6 to 12.2nbsp;Ma over a vast area cannot result from a single impact event.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>cosmic metallic iron</kwd>
    <kwd>sediments</kwd>
    <kwd>themomagnetic analysis</kwd>
    <kwd>Curie point.</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>cosmic metallic iron</kwd>
    <kwd>sediments</kwd>
    <kwd>themomagnetic analysis</kwd>
    <kwd>Curie point.</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
 <back>
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</article>
