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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-11989</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/11989</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 morphology of growth and dissolution bodies of crystals</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>К морфологии тел роста и растворения кристаллов</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Voytsekhovsky</surname>
            <given-names>V. N.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Войцеховский</surname>
              <given-names>В. Н.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Voytsekhovsky</surname>
              <given-names>V. 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 contrib-type="author">
          <name name-style="eastern">
            <surname>Mokievsky</surname>
            <given-names>V. A.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Мокиевский</surname>
              <given-names>В. А.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Mokievsky</surname>
              <given-names>V. 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-group>
      <pub-date pub-type="epub" iso-8601-date="1967-11-15">
        <day>15</day>
        <month>11</month>
        <year>1967</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>1967</year>
      </pub-date>
      <volume>54</volume>
      <issue>2</issue>
      <fpage>25</fpage>
      <lpage>37</lpage>
      <history>
        <date date-type="received" iso-8601-date="1967-08-10">
          <day>10</day>
          <month>08</month>
          <year>1967</year>
        </date>
        <date date-type="accepted" iso-8601-date="1967-10-15">
          <day>15</day>
          <month>10</month>
          <year>1967</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="1967-11-15">
          <day>15</day>
          <month>11</month>
          <year>1967</year>
        </date>
      </history>
      <permissions>
        <copyright-statement xml:lang="ru">© 1967 В. Н. Войцеховский, В. А. Мокиевский</copyright-statement>
        <copyright-statement xml:lang="en">© 1967 V. N. Voytsekhovsky, V. A. Mokievsky</copyright-statement>
        <copyright-year>1967</copyright-year>
        <copyright-holder xml:lang="ru">В. Н. Войцеховский, В. А. Мокиевский</copyright-holder>
        <copyright-holder xml:lang="en">V. N. Voytsekhovsky, V. A. Mokievsky</copyright-holder>
        <license license-type="open-access" xlink:href="http://creativecommons.org/licenses/by/4.0" xml:lang="ru">
          <license-p>Эта статья доступна по лицензии Creative Commons Attribution 4.0 International (CC BY 4.0)</license-p>
        </license>
        <license license-type="open-access" xlink:href="http://creativecommons.org/licenses/by/4.0" xml:lang="en">
          <license-p>This article is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0)</license-p>
        </license>
      </permissions>
      <self-uri xlink:type="simple" xlink:href="https://pmi.spmi.ru/pmi/article/view/11989">https://pmi.spmi.ru/pmi/article/view/11989</self-uri>
      <abstract xml:lang="ru">
        <p>По закону образования тел растворения кристаллов, сформулированному В. Гольдшмидтом и Ф. Райтом [Goldschmidt, Wright. 1904], углы и вершины на теле растворения кристалла соответствуют полюсам граней, присут­ствующих при его росте; ребра зонам граней. Этот закон приводит А. Е. Фер­сман [1955] в качестве правила, по которому следует отличать формы роста кристаллов от форм их растворения. В 1958 г. Ф. Франк показал, что если скорость растворения (роста) есть функция только ориентации его поверхности, то при растворении (росте) кристалла точка на по­верхности данной ориентации имеет прямоли­нейную траекторию, направленную перпенди­кулярно к поверхности полярной диаграммы обратных скоростей растворения (роста) кри­сталла в соответствующей точке.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>According to the law of formation of crystal dissolution bodies formulated by W. Goldschmidt and F. Wright [Goldschmidt, Wright. 1904], the angles and vertices on the dissolution body of a crystal correspond to the poles of the faces present during its growth; the edges to the zones of the faces. This law is cited by A. E. Fersman [1955] as a rule by which the forms of crystal growth should be distinguished from the forms of dissolution. In 1958, F. Frank showed that if the dissolution (growth) rate is a function only of the orientation of its surface, then during dissolution (growth) of a crystal, a point on the surface of a given orientation has a rectilinear trajectory directed perpendicular to the surface of the polar diagram of inverse dissolution (growth) rates of the crystal at the corresponding point.</p>
      </abstract>
    </article-meta>
  </front>
  <body/>
  <back>
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