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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="pmi" pub-id-type="custom">pmi-12418</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/12418</article-id>
      <article-categories>
        <subj-group subj-group-type="section-heading" xml:lang="ru">
          <subject>Без раздела</subject>
        </subj-group>
        <subj-group subj-group-type="section-heading" xml:lang="en">
          <subject>Without section</subject>
        </subj-group>
      </article-categories>
      <title-group>
        <article-title xml:lang="en">To the genesis of the Ural crustalenose pegmatites</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>К генезису хрусталеносных пегматитов Урала</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Nikitin</surname>
            <given-names>V. D.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Никитин</surname>
              <given-names>В. Д.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Nikitin</surname>
              <given-names>V. D.</given-names>
            </name>
          </name-alternatives>
          <email>pmi@spmi.ru</email>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
        <aff-alternatives id="aff1">
          <aff>
            <institution xml:lang="ru"> (Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en"> (Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Rudenko</surname>
            <given-names>S. A.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Руденко</surname>
              <given-names>С. А.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Rudenko</surname>
              <given-names>S. A.</given-names>
            </name>
          </name-alternatives>
          <email>pmi@spmi.ru</email>
          <xref ref-type="aff" rid="aff2"/>
        </contrib>
        <aff-alternatives id="aff2">
          <aff>
            <institution xml:lang="ru"> (Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en"> (Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Eshkin</surname>
            <given-names>V. Yu.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Эшкин</surname>
              <given-names>В. Ю.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Eshkin</surname>
              <given-names>V. Yu.</given-names>
            </name>
          </name-alternatives>
          <email>pmi@spmi.ru</email>
          <xref ref-type="aff" rid="aff3"/>
        </contrib>
        <aff-alternatives id="aff3">
          <aff>
            <institution xml:lang="ru"> (Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en"> (Russia)</institution>
          </aff>
        </aff-alternatives>
      </contrib-group>
      <pub-date pub-type="epub" iso-8601-date="1966-12-09">
        <day>09</day>
        <month>12</month>
        <year>1966</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>1967</year>
      </pub-date>
      <volume>52</volume>
      <issue>2</issue>
      <fpage>11</fpage>
      <lpage>19</lpage>
      <history>
        <date date-type="received" iso-8601-date="1966-08-26">
          <day>26</day>
          <month>08</month>
          <year>1966</year>
        </date>
        <date date-type="accepted" iso-8601-date="1966-10-03">
          <day>03</day>
          <month>10</month>
          <year>1966</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="1966-12-09">
          <day>09</day>
          <month>12</month>
          <year>1966</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>© V. D. Nikitin, S. A. Rudenko, V. Yu. Eshkin</copyright-statement>
        <copyright-year>1966</copyright-year>
        <copyright-holder xml:lang="ru">В. Д. Никитин, С. А. Руденко, В. Ю. Эшкин</copyright-holder>
        <copyright-holder xml:lang="en">V. D. Nikitin, S. A. Rudenko, V. Yu. Eshkin</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/12418">https://pmi.spmi.ru/pmi/article/view/12418</self-uri>
      <abstract xml:lang="ru">
        <p>Пегматитовые поля, приуроченные к зоне развития герцинских ин­трузий гранитоидов на восточном склоне Урала, изучаются, как известно, очень давно. В значительной мере эти пегматиты вошли в число тех при­родных объектов, на примере которых построена классическая теория генезиса пегматитовых образований ...</p>
      </abstract>
      <abstract xml:lang="en">
        <p>Pegmatite fields confined to the zone of development of Hercynian granitoid intrusions on the eastern slope of the Urals have been studied, as is known, for a very long time. To a large extent, these pegmatites are among those natural objects on the example of which the classical theory of the genesis of pegmatite formations is built ...</p>
      </abstract>
    </article-meta>
  </front>
  <body/>
  <back>
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  </back>
</article>
