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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">geores</journal-id><journal-title-group><journal-title xml:lang="ru">Георесурсы</journal-title><trans-title-group xml:lang="en"><trans-title>Georesources</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1608-5043</issn><issn pub-type="epub">1608-5078</issn><publisher><publisher-name>Georesursy LLC</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.18599/grs.2023.2.12</article-id><article-id custom-type="elpub" pub-id-type="custom">geores-68</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>СТАТЬИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>RESEARCH ARTICLES</subject></subj-group></article-categories><title-group><article-title>Источники нефтей Красноленинского месторождения</article-title><trans-title-group xml:lang="en"><trans-title>Oil sources of the Krasnoleninskoe field</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Осипов</surname><given-names>К. О.</given-names></name><name name-style="western" xml:lang="en"><surname>Osipov</surname><given-names>K. O.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Константин Олегович Осипов – научный сотрудник кафедры геологии и геохимии горючих ископаемых</p><p>119234, Москва, ул. Ленинские горы, д. 1</p></bio><bio xml:lang="en"><p>Konstantin O. Osipov – PhD student, Researcher, Petroleum Geology Department</p><p>1, Leninskie gory, Moscow, 119234</p></bio><email xlink:type="simple">k.osipov@oilmsu.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Большакова</surname><given-names>М. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bolshakova</surname><given-names>M. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Мария Александровна Большакова – кандидат геол.- мин. наук, ведущий научный сотрудник кафедры геологии и геохимии горючих ископаемых</p><p>119234, Москва, ул. Ленинские горы, д. 1</p></bio><bio xml:lang="en"><p>Maria A. Bolshakova – PhD (Geology and Mineralogy), Leading Researcher, Petroleum Geology Department</p><p>1, Leninskie gory, Moscow, 119234</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Абля</surname><given-names>Э. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Ablya</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Энвер Алексеевич Абля – кандидат геол.-мин. наук, доцент кафедры геологии и геохимии горючих ископаемых</p><p>119234, Москва, ул. Ленинские горы, д. 1</p></bio><bio xml:lang="en"><p>Enver A. Ablya – PhD (Geology and Mineralogy), Assistant Professor, Petroleum Geology Department</p><p>1, Leninskie gory, Moscow, 119234</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Краснова</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Krasnova</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Елизавета Андреевна Краснова – кандидат геол.-мин. наук, старший научный сотрудник кафедры геологии и геохимии горючих ископаемых;</p><p>старший научный сотрудник</p><p>119234, Москва, Ленинские горы, д. 1</p></bio><bio xml:lang="en"><p>Elizaveta A. Krasnova – PhD (Geology and Mineralogy), Senior Researcher, Petroleum Geology Department;</p><p>Senior Researcher</p><p>1, Leninskie gory, Moscow, 119234</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Сауткин</surname><given-names>Р. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Sautkin</surname><given-names>R. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Роман Сергеевич Сауткин – кандидат геол.-мин. наук, старший научный сотрудник кафедры геологии и геохимии горючих ископаемых</p><p>119192, Москва, Ломоносовский пр-т, д. 27, к.1</p></bio><bio xml:lang="en"><p>Roman S. Sautkin – PhD (Geology and Mineralogy), Senior Researcher, Petroleum Geology Department</p><p>1, Leninskie gory, Moscow, 119234</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Суслова</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Suslova</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Анна Анатольевна Суслова – кандидат геол.-мин. наук, ведущий научный сотрудник кафедры геологии и геохимии горючих ископаемых</p><p>119192, Москва, Ломоносовский пр-т, д. 27, к.1</p></bio><bio xml:lang="en"><p>Anna A. Suslova – PhD (Geology and Mineralogy), Leading Researcher, Petroleum Geology Department</p><p>1, Leninskie gory, Moscow, 119234</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Калмыков</surname><given-names>А. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Kalmykov</surname><given-names>A. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Антон Георгиевич Калмыков – кандидат хим. наук, старший научный сотрудник кафедры геологии и геохимии горючих ископаемых</p><p>119234, Москва, ул. Ленинские горы, д. 1</p></bio><bio xml:lang="en"><p>Anton G. Kalmykov – PhD (Chemistry), Senior Researcher, Petroleum Geology Department</p><p>1, Leninskie gory, Moscow, 119234</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Тихонова</surname><given-names>М. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Tikhonova</surname><given-names>M. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Маргарита Станиславовна Тихонова – инженер кафедры геологии и геохимии горючих ископаемых</p><p>119192, Москва, Ломоносовский пр., д. 27, к.1</p></bio><bio xml:lang="en"><p>Margarita S. Tikhonova – Engineer of the Petroleum Geology Department</p><p>1, Leninskie gory, Moscow, 119234</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова;&#13;
Института геохимии и аналитической химии им. В.И. Вернадского РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University;&#13;
Vernadsky Institute of Geochemistry and Analytical Chemistry of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>11</day><month>04</month><year>2024</year></pub-date><volume>25</volume><issue>2</issue><fpage>161</fpage><lpage>182</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Осипов К.О., Большакова М.А., Абля Э.А., Краснова Е.А., Сауткин Р.С., Суслова А.А., Калмыков А.Г., Тихонова М.С., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Осипов К.О., Большакова М.А., Абля Э.А., Краснова Е.А., Сауткин Р.С., Суслова А.А., Калмыков А.Г., Тихонова М.С.</copyright-holder><copyright-holder xml:lang="en">Osipov K.O., Bolshakova M.A., Ablya E.A., Krasnova E.A., Sautkin R.S., Suslova A.A., Kalmykov A.G., Tikhonova M.S.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://www.geors.ru/jour/article/view/68">https://www.geors.ru/jour/article/view/68</self-uri><abstract><p>В настоящее время не существует единого мнения о роли различных нефтегазоматеринских толщ (НГМТ) в формировании Красноленинского месторождения. Основная верхнеюрско-раннемеловая НГМТ Западной Сибири представлена на Красноленинском своде тутлеймской свитой (J3tt–K1v). Кроме нее нефтегазоматеринские прослои также расположены во фроловской (K1v–K1a), абалакской (J2cl–J3km), тюменской (J2a-b), шеркалинской (J1 ) свитах и, возможно, в доюрских отложениях. В работе определены источники нефти Красноленинского месторождения путем сопоставления нефтей с НГМТ и установлены условия формирования состава нефти. На основе обзора известных геохимических параметров и результатов статистического анализа предложены новые молекулярные параметры определения типа и зрелости органического вещества (ОВ). Сделано предположение о вторичном преобразовании нефтей викуловской свиты Каменной вершины, которое связано с миграцией углеводородов (УВ) из свиты в вышележащие отложения или на дневную поверхность в прошлом. Показано, что нефти викуловской свиты Каменной вершины образовались из НГМТ, находящейся во время генерации УВ на градации МК2 , а нефти юрских и доюрских отложений – конец МК2 – начало МК3 . Установлено аквагенное происхождение исходного ОВ нефтей Каменной вершины, пород тутлеймской и части пород тюменской НГМТ. По критериям типа и зрелости источник нефтей Каменной вершины определить не удается, поэтому для проведения корреляции нефть – НГМТ выявлены генетические признаки различия аквагенного ОВ тюменской и тутлеймской свит. Эти признаки позволили оценить источник нефтей разных частей Красноленинского месторождения: для Каменной вершины – тутлеймская свита, для Талинской площади – тюменская свита, для Ем-Еговской площади – тюменская и тутлеймская свиты. Оценка вклада шеркалинской и абалакской НГМТ в формирование скоплений УВ выходит за рамки текущей работы.</p></abstract><trans-abstract xml:lang="en"><p>There is no consensus on the role of different source rocks (SRs) in the formation of the Krasnoleninskoe field. The main Upper Jurassic-Early Cretaceous SR of Western Siberia is represented on the Krasnoleninsky arch by the Tutleim formation (fm) (J3tt–K1v). It is overlain by argillaceous rocks of the Frolov fm (K1v–K1a), underlain by the Abalak (J2cl–J3km), Tyumen (J2a-b), Sherkalin (J1 ) formations and folded pre-Jurassic basement. All these formations potentially contain SR layers. The purpose of the article is to determine the sources of oil in the Krasnoleninskoe field by comparing oils with SRs and to determine of the history of oil composition formation. Based on a review of known geochemical parameters and the results of statistical analysis new molecular parameters for determining the type of organic matter (OM) and its maturity are proposed. A secondary processes of the oils of the Vikulov fm of the Kamennaya crest has been established, which is associated with the migration of hydrocarbons from the Vikulov fm to the overlying deposits. It is shown that the oils of the Vikulov fm of Kamennaya crest were formed from the SR, which was at the MC2 substage during the generation of hydrocarbons, and the oils of the Jurassic and pre-Jurassic deposits were formed on the end of MC2 -beginning of MC3 substages. It was determined that the oils of Kamennaya crest have aquatic initial OM, aquatic OM was found in the Tutleim and Tyumen SRs. According to the criteria of OM type and its maturity, the source of Kamennaya crest oils cannot be determined; therefore, genetic features of the difference between the aquatic OM of the Tyumen and Tutleim formations were found. These features made it possible to estimate the source of oils for different parts of the Krasnoleninskoe field: for Kamennaya crest the Tutleim fm, for the Talinskaya area the Tyumen fm, for the Em-Egovskaya area, the Tyumen and Tutleim formations. Estimation of the contribution of the Sherkalin and Abalak SRs to the formation of hydrocarbon accumulations is beyond the scope of current work.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Западная Сибирь</kwd><kwd>Красноленинское месторождение</kwd><kwd>геохимические параметры</kwd><kwd>зрелость органического вещества</kwd><kwd>тип органического вещества</kwd><kwd>источник нефти</kwd><kwd>тюменская свита</kwd><kwd>тутлеймская свита</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Western Siberia</kwd><kwd>Krasnoleninsky field</kwd><kwd>geochemical (molecular</kwd><kwd>isotopic</kwd><kwd>pyrolytic) parameters</kwd><kwd>maturity of organic matter</kwd><kwd>type of organic matter</kwd><kwd>oil source</kwd><kwd>Tyumen formation</kwd><kwd>Tutleim formation</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Атлас «Геология и нефтегазоносность Ханты-Мансийского автономного округа» (2004). 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