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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-11649</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/11649</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">Lithologic and paleophytologic substantiation of dissection of Lower Permian deposits of the Minusinsk basin</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Литолого-палеофитологическое обоснование расчленения нижнепермских отложений Минусинского бассейна</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Beresneva</surname>
            <given-names>D. I.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Береснева</surname>
              <given-names>Д. И.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Beresneva</surname>
              <given-names>D. I.</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"/>
          </aff>
          <aff>
            <institution xml:lang="en"/>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Oshurkova</surname>
            <given-names>M. V.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Ошуркова</surname>
              <given-names>М. В.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Oshurkova</surname>
              <given-names>M. V.</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"/>
          </aff>
          <aff>
            <institution xml:lang="en"/>
          </aff>
        </aff-alternatives>
      </contrib-group>
      <pub-date pub-type="epub" iso-8601-date="1973-02-01">
        <day>01</day>
        <month>02</month>
        <year>1973</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>1973</year>
      </pub-date>
      <volume>65</volume>
      <issue>2</issue>
      <fpage>111</fpage>
      <lpage>119</lpage>
      <history>
        <date date-type="received" iso-8601-date="1972-08-04">
          <day>04</day>
          <month>08</month>
          <year>1972</year>
        </date>
        <date date-type="accepted" iso-8601-date="1972-10-14">
          <day>14</day>
          <month>10</month>
          <year>1972</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="1973-02-01">
          <day>01</day>
          <month>02</month>
          <year>1973</year>
        </date>
      </history>
      <permissions>
        <copyright-statement xml:lang="ru">© 1973 Д. И. Береснева, М. В. Ошуркова</copyright-statement>
        <copyright-statement xml:lang="en">© 1973 D. I. Beresneva, M. V. Oshurkova</copyright-statement>
        <copyright-year>1973</copyright-year>
        <copyright-holder xml:lang="ru">Д. И. Береснева, М. В. Ошуркова</copyright-holder>
        <copyright-holder xml:lang="en">D. I. Beresneva, M. V. Oshurkova</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/11649">https://pmi.spmi.ru/pmi/article/view/11649</self-uri>
      <abstract xml:lang="ru">
        <p>Литолого-палеофитологическое обоснование расчленения нижне­пермских угленосных отложений Минусинского бассейна произведено на основании детального литолого-фациального и палеофитологического описания разреза по Изыхскому месторождению, где продуктивная толща (мощностью 1750 м) развита наиболее полно и где прослежи­ваются осадки в возрастном диапазоне от карбона до перми.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>The lithologic-paleophytologic substantiation of the Lower Permian coal-bearing sediments of the Minusinsk basin was made on the basis of a detailed lithologic-facial and paleophytologic description of the section of the Izikhskoye field, where the productive stratum (1750 m thick) is most fully developed and where sediments in the age range from Carboniferous to Permian are traced.</p>
      </abstract>
    </article-meta>
  </front>
  <body/>
  <back>
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      <ref id="ref1">
        <label>1</label>
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        <mixed-citation xml:lang="ru">Педан И. С. и др. Минусинский угольный бассейн. — В кн.: Геология месторождений угля и горючих сланцев СССР. Т. 8. Недра, 1964.</mixed-citation>
        <mixed-citation xml:lang="en">Pedan I. S. et al. Minusinsky coal basin. - In the book: Geology of Coal and Oil Shale Deposits of the USSR. V. 8. Nedra, 1964.</mixed-citation>
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        <mixed-citation xml:lang="ru">Радченко Г. П. Критерии и методы палеогеографических реконструкций прежних условий в областях древней суши по палеонтологическим данным. — В сб.: Методы палеогеографических исследований. Недра, 1964.</mixed-citation>
        <mixed-citation xml:lang="en">Radchenko G. P. Criteria and methods of paleogeographic reconstructions of former conditions in the areas of ancient land by paleontological data. - In the collection: Methods of Paleogeographic Studies. Nedra, 1964.</mixed-citation>
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  </back>
</article>
