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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-15290</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/15290</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">Different solubility of facets and its manifestation in the mineral kingdom</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Различная растворимость граней и ее проявление в минеральном царстве</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Fedorov</surname>
            <given-names>Ye. S.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Федоров</surname>
              <given-names>Е. С.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Fedorov</surname>
              <given-names>Ye. S.</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="1908-06-01">
        <day>01</day>
        <month>06</month>
        <year>1908</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>1908</year>
      </pub-date>
      <volume>1</volume>
      <issue>2</issue>
      <fpage>160</fpage>
      <lpage>163</lpage>
      <history>
        <date date-type="received" iso-8601-date="1907-12-08">
          <day>08</day>
          <month>12</month>
          <year>1907</year>
        </date>
        <date date-type="accepted" iso-8601-date="1908-02-16">
          <day>16</day>
          <month>02</month>
          <year>1908</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="1908-06-01">
          <day>01</day>
          <month>06</month>
          <year>1908</year>
        </date>
      </history>
      <permissions>
        <copyright-statement>© Ye. S. Fedorov</copyright-statement>
        <copyright-year>1908</copyright-year>
        <copyright-holder xml:lang="ru">Е. С. Федоров</copyright-holder>
        <copyright-holder xml:lang="en">Ye. S. Fedorov</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/15290">https://pmi.spmi.ru/pmi/article/view/15290</self-uri>
      <abstract xml:lang="ru">
        <p>Различие это проявляется в передвижении растворенного вещества в слое раствора, разделяющем различные грани кристалла того вещества, из которого получен и раствор. Если бы возникло сомнение в одинаковости в этом отношении свойств натуральной грани и напр. плоскости спайности, ей параллельной, то упомянутый прием дает в руки средство его разрешить.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>This difference is manifested in the movement of the dissolved substance in the layer of solution separating the different faces of the crystal of the substance from which the solution is obtained. If there were any doubt about the similarity in this regard of the properties of a natural edge and, for example, a plane of cleavage parallel to it, then the mentioned technique provides a means of resolving it.</p>
      </abstract>
    </article-meta>
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        <label>1</label>
        <mixed-citation xml:lang="ru">-</mixed-citation>
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