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    <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="edn" pub-id-type="custom">JPUKCM</article-id>
      <article-id custom-type="pmi" pub-id-type="custom">pmi-16249</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/16249</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">Assessment of the influence of lithofacies conditions on the distribution of organic carbon in the Upper Devonian “Domanik” deposits of the Timan-Pechora Province</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Оценка влияния литолого-фациальных условий на распределение органического углерода в «доманиковых» верхнедевонских отложениях Тимано-Печорской провинции</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Prishchepa</surname>
            <given-names>Oleg M.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Прищепа</surname>
              <given-names>О. М.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Prishchepa</surname>
              <given-names>Oleg M.</given-names>
            </name>
          </name-alternatives>
          <email>omp2007_61@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0001-8404-7073</contrib-id>
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          <aff>
            <institution xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины II (Санкт-Петербург, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Empress Catherine II Saint Petersburg Mining University (Saint Petersburg, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Sinitsa</surname>
            <given-names>Nikita V.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Синица</surname>
              <given-names>Н. В.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Sinitsa</surname>
              <given-names>Nikita V.</given-names>
            </name>
          </name-alternatives>
          <email>omp2007_61@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0009-0001-9508-0749</contrib-id>
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        </contrib>
        <aff-alternatives id="aff2">
          <aff>
            <institution xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины II (Санкт-Петербург, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Empress Catherine II Saint Petersburg Mining University (Saint Petersburg, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Ibatullin</surname>
            <given-names>Aidar Kh.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Ибатуллин</surname>
              <given-names>А. Х.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Ibatullin</surname>
              <given-names>Aidar Kh.</given-names>
            </name>
          </name-alternatives>
          <email>raida785@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0001-6591-2957</contrib-id>
          <xref ref-type="aff" rid="aff3"/>
        </contrib>
        <aff-alternatives id="aff3">
          <aff>
            <institution xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины II (Санкт-Петербург, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Empress Catherine II Saint Petersburg Mining University (Saint Petersburg, Russia)</institution>
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      <pub-date pub-type="epub" iso-8601-date="2024-06-20">
        <day>20</day>
        <month>06</month>
        <year>2024</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>2024</year>
      </pub-date>
      <volume>268</volume>
      <fpage>535</fpage>
      <lpage>551</lpage>
      <history>
        <date date-type="received" iso-8601-date="2023-05-21">
          <day>21</day>
          <month>05</month>
          <year>2023</year>
        </date>
        <date date-type="accepted" iso-8601-date="2024-05-02">
          <day>02</day>
          <month>05</month>
          <year>2024</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2024-08-26">
          <day>26</day>
          <month>08</month>
          <year>2024</year>
        </date>
      </history>
      <permissions>
        <copyright-statement xml:lang="ru">© 2024 О. М. Прищепа, Н. В. Синица, А. Х. Ибатуллин</copyright-statement>
        <copyright-statement xml:lang="en">© 2024 Oleg M. Prishchepa, Nikita V. Sinitsa, Aidar Kh. Ibatullin</copyright-statement>
        <copyright-year>2024</copyright-year>
        <copyright-holder xml:lang="ru">О. М. Прищепа, Н. В. Синица, А. Х. Ибатуллин</copyright-holder>
        <copyright-holder xml:lang="en">Oleg M. Prishchepa, Nikita V. Sinitsa, Aidar Kh. Ibatullin</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/16249">https://pmi.spmi.ru/pmi/article/view/16249</self-uri>
      <abstract xml:lang="ru">
        <p>Изучение высокоуглеродистых формаций вызвано как сокращением сырьевой базы нефти в результате ее добычи, так и успехами освоения низкопроницаемых сланцевых толщ, в первую очередь в США, Австралии и Китае. Наиболее значимы формации, распространенные в традиционных районах добычи углеводородов, – в Западно-Сибирской, Волго-Уральской и Тимано-Печорской, Северо-Предкавказской и Лено-Тунгусской нефтегазоносных провинциях. Особенности высокоуглеродистой формации позднедевонско-раннекаменно-угольного времени, сформировавшейся в восточной краевой части Восточно-Европейской платформы, – неоднородность разреза, обусловленная интенсивной проградацией карбонатной платформы в направлении с запада на восток; последовательная смена литолого-фациальных обстановок, определивших неравномерность первичного накопления и вторичного распределения содержания органического вещества (ОВ); возможность эмиграции или сохранения в толще генерации на этапах погружения подвижных частей битумидов, определивших перспективы нефтегазоносности. Изучались закономерности распределения текущего содержания ОВ в зависимости от литолого-фациальных условий и литологического состава пород в верхнедевонско-турнейских отложениях «доманикового типа» Тимано-Печорской провинции (ТПП), степень его преобразованности для приведения к начальному содержанию органического углерода и дальнейшей оценке доли сохраненной «подвижной нефти» в нефтегазоматеринской формации. Исследование выполнено на основе анализа массива данных содержания органического углерода образцов керна и естественных обнажений Ухтинского района доманиково-турнейской части разреза, включающего более 5000 определений, представленных в отчетах и публикациях ВНИГРИ и ВНИГНИ, дополненных проведенными пиролитическими, битуминологическими анализами, увязанными с результатами микротомографического, макро- и литологического изучения и описаниями шлифов, выполненных в Санкт-Петербургском горном университете. Для каждой тектонической зоны ТПП в пределах изученных высокоуглеродистых интервалов установлено содержание суммарных объемов органического углерода. Полученные данные позволят оценить остаточную массу подвижных битумоидов в низкопроницаемой матрице высокоуглеродистой формации.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>The study of high-carbon formations was instigated both by the decreasing raw material base of oil as a result of its extraction, and by the progress in development of low-permeability shale strata, primarily in the USA, Australia, and China. The most valuable formations occur in traditional hydrocarbon production areas – the West Siberian, Volga-Ural and Timan-Pechora, North Pre-Caucasian and Lena-Tunguska oil and gas provinces. Specific features of the Late Devonian-Early Carboniferous high-carbon formation occurring in the eastern marginal part of the East European Platform are: heterogeneous section due to intense progradation of the carbonate platform from west to east; succession of lithofacies environments that determined the unevenness of the primary accumulation and secondary distribution of organic matter (OM); possible migration or preservation in the source strata during the subsidence stages of the moving parts of bitumides, which determined the prospects for oil and gas potential. The distribution pattern of the present OM content was investigated depending on lithofacies conditions and lithological composition of rocks in the “Domanik type” Upper Devonian-Tournaisian deposits in the Timan-Pechora Province (TPP), its transformation degree to bring it to the initial content of organic carbon and further estimation of the share of stored “mobile oil” in oil and gas source formation. The study was based on the analysis of the data set on organic carbon content in core samples and natural exposures in the Ukhta Region in the Domanik-Tournaisian part of the section including more than 5,000 determinations presented in reports and publications of VNIGRI and VNIGNI and supplemented by pyrolytic and bituminological analyses associated with the results of microtomographic, macro- and lithological studies and descriptions of thin sections made at the Saint Petersburg Mining University. For each tectonic zone of the TPP within the investigated high-carbon intervals, the content of total volumes of organic carbon was determined. The data obtained allow estimating the residual mass of mobile bitumoids in a low-permeability matrix of the high-carbon formation.</p>
      </abstract>
      <kwd-group xml:lang="ru">
        <title>Ключевые слова</title>
        <kwd>отложения доманикового типа</kwd>
        <kwd>фация</kwd>
        <kwd>формация</kwd>
        <kwd>органическое вещество</kwd>
        <kwd>осадочный бассейн</kwd>
        <kwd>литологический тип</kwd>
        <kwd>углеводороды</kwd>
        <kwd>нефть</kwd>
        <kwd>газ</kwd>
      </kwd-group>
      <kwd-group xml:lang="en">
        <title>Keywords</title>
        <kwd>Domanik type deposits</kwd>
        <kwd>facies</kwd>
        <kwd>formation</kwd>
        <kwd>organic matter</kwd>
        <kwd>sedimentary basin</kwd>
        <kwd>lithological type</kwd>
        <kwd>hydrocarbons</kwd>
        <kwd>oil</kwd>
        <kwd>gas</kwd>
      </kwd-group>
    </article-meta>
  </front>
  <body/>
  <back>
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