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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-10943</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/10943</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">On the influence of mineral composition of mudstones of the Razvedochninskaya Formation of the Talibskoye field on well wall stability</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>О влиянии минерального состава аргиллитов Разведочнинской свиты Талибского месторождения на устойчивость стенок скважин</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"> (Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en"> (Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Chaschinov</surname>
            <given-names>Yu. M.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Чащинов</surname>
              <given-names>Ю. М.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Chaschinov</surname>
              <given-names>Yu. M.</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="1981-07-09">
        <day>09</day>
        <month>07</month>
        <year>1981</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>1981</year>
      </pub-date>
      <volume>86</volume>
      <fpage>95</fpage>
      <lpage>95</lpage>
      <history>
        <date date-type="received" iso-8601-date="1980-09-29">
          <day>29</day>
          <month>09</month>
          <year>1980</year>
        </date>
        <date date-type="accepted" iso-8601-date="1980-11-08">
          <day>08</day>
          <month>11</month>
          <year>1980</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="1981-07-09">
          <day>09</day>
          <month>07</month>
          <year>1981</year>
        </date>
      </history>
      <permissions>
        <copyright-statement xml:lang="ru">© 1981 Д. И. Береснева, Ю. М. Чащинов</copyright-statement>
        <copyright-statement xml:lang="en">© 1981 D. I. Beresneva, Yu. M. Chaschinov</copyright-statement>
        <copyright-year>1981</copyright-year>
        <copyright-holder xml:lang="ru">Д. И. Береснева, Ю. М. Чащинов</copyright-holder>
        <copyright-holder xml:lang="en">D. I. Beresneva, Yu. M. Chaschinov</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/10943">https://pmi.spmi.ru/pmi/article/view/10943</self-uri>
      <abstract xml:lang="ru">
        <p>Проходка аргиллитов разведочнинской свиты Талнахского месторождения часто осложняется обрушением стенок скважин. Сильная тектоническая нарушенность района и высокое горное давление, обусловленное большими глуби­нами (2000 м) залегания свиты, полностью не объясняют это явление, по­скольку в равных условиях зафиксированы как аварийные, так и безаварийные скважины ...</p>
      </abstract>
      <abstract xml:lang="en">
        <p>Borehole penetration of mudstones of the Exploration Formation of the Talnakhskoye field is often complicated by collapse of borehole walls. The strong tectonic disturbance of the area and high rock pressure due to the great depth (2000 m) of the formation do not fully explain this phenomenon, since both emergency and accident-free wells have been recorded in equal conditions ...</p>
      </abstract>
    </article-meta>
  </front>
  <body/>
  <back>
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</article>
