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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-15500</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/15500</article-id>
      <article-categories/>
      <title-group>
        <article-title xml:lang="en">Changes in the side rocks of the Zyryanovskoe field</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Изменения в боковых породах Зыряновского месторождения</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Zavaritskii</surname>
            <given-names>A. N.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Заварицкий</surname>
              <given-names>А. Н.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Zavaritskii</surname>
              <given-names>A. N.</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-group>
      <pub-date pub-type="epub" iso-8601-date="1912-12-01">
        <day>01</day>
        <month>12</month>
        <year>1912</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>1912</year>
      </pub-date>
      <volume>3</volume>
      <fpage>176</fpage>
      <lpage>185</lpage>
      <history>
        <date date-type="received" iso-8601-date="1912-06-05">
          <day>05</day>
          <month>06</month>
          <year>1912</year>
        </date>
        <date date-type="accepted" iso-8601-date="1912-08-19">
          <day>19</day>
          <month>08</month>
          <year>1912</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="1912-12-01">
          <day>01</day>
          <month>12</month>
          <year>1912</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>© A. N. Zavaritskii</copyright-statement>
        <copyright-year>1912</copyright-year>
        <copyright-holder xml:lang="ru">А. Н. Заварицкий</copyright-holder>
        <copyright-holder xml:lang="en">A. N. Zavaritskii</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/15500">https://pmi.spmi.ru/pmi/article/view/15500</self-uri>
      <abstract xml:lang="ru">
        <p>Все имеющиеся образцы в большем или меньшем количестве содержат вкрапления рудных минералов: пирита, цинковой обманки и частью свинцового блеска. Это ясно указывает, что они взяты в непосредственном соседстве с рудной толщей. Расположение в пространстве этих образцов ясно из приложенной схемы. Как известно, Зыряновское месторождение представляет довольно неправильно разветвляющуюся желеобразную массу.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>All available samples contain inclusions of ore minerals in greater or lesser quantities: pyrite, zinc blende and partly lead luster. This clearly indicates that they were taken in the immediate vicinity of the ore sequence. The spatial location of these samples is clear from the attached diagram. As is known, the Zyryanovskoe deposit is a rather irregularly branched jelly-like mass.</p>
      </abstract>
    </article-meta>
  </front>
  <body/>
  <back>
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</article>
