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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.2021.1.4</article-id><article-id custom-type="elpub" pub-id-type="custom">geores-214</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>ГЕОХИМИЧЕСКИЕ ИССЛЕДОВАНИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOCHEMICAL STUDIES</subject></subj-group></article-categories><title-group><article-title>Ароматические соединения в битумоидах баженовской свиты севера Хантейской гемиантеклизы</article-title><trans-title-group xml:lang="en"><trans-title>Aromatic compounds in bitumoids of the Bazhenov Formation in the North of the Khantey hemiantheclise</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>Сотнич</surname><given-names>И. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Sotnich</surname><given-names>I. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Инга Сергеевна Сотнич – научный сотрудник лаборатории проблем геологии, разведки и разработки месторождений трудноизвлекаемой нефти; научный сотрудник лаборатории геохимии нефти и газа</p><p>630090, Новосибирск, пр. ак. Коптюга, д. 3</p></bio><bio xml:lang="en"><p>Inga S. Sotnich – Researcher, Laboratory of the Problems of Geology, Exploration and Development of hard-to-recover oil fields; Researcher of the Laboratory of Petroleum Geochemistry</p><p>3, Ak. Koptyug ave., Novosibirsk, 630090</p></bio><email xlink:type="simple">SotnichIS@ipgg.sbras.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>Костырева</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kostyreva</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Елена Анатольевна Костырева – канд. геол.-мин. наук, старший научный сотрудник лаборатории геохимии нефти и газа</p><p>630090, Новосибирск, пр. ак. Коптюга, д. 3</p></bio><bio xml:lang="en"><p>Elena A. Kostyreva – Cand. Sci. (Geology and Mineralogy), Senior Researcher of the Laboratory of Petroleum Geochemistry</p><p>3, Ak. Koptyug ave., Novosibirsk, 630090</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт нефтегазовой геологии и геофизики им. А.А.Трофимука СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Trofimuk Institute of Petroleum Geology and Geophysics of Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>20</day><month>04</month><year>2024</year></pub-date><volume>23</volume><issue>1</issue><fpage>42</fpage><lpage>51</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Сотнич И.С., Костырева Е.А., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Сотнич И.С., Костырева Е.А.</copyright-holder><copyright-holder xml:lang="en">Sotnich I.S., Kostyreva E.A.</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/214">https://www.geors.ru/jour/article/view/214</self-uri><abstract><p>Рассмотрены основные черты геохимии индивидуальных ароматических соединений (фенантренов, дибензотиофенов, моно- и триароматических стероидов) в битумоидах, экстрагированных хлороформом из открытого (из образцов регулярной формы и грубого дробления (≥0,5 см)) и закрытого (из образцов мелкого дробления (0,25 мм)) порового пространства пород баженовской свиты. Различия в распределении ароматических соединений органического вещества баженовской свиты на севере Хантейской гемиантеклизы (Сургутский район, Ханты-Мансийский автономный округ, Западная Сибирь) связаны, главным образом, со степенью его катагенетической преобразованности. Установлено, что степень преобразованности аквагенного органического вещества баженовской свиты на территории исследования уменьшается в юго-западном направлении. Показано, что наиболее чувствительны к вариациям зрелости органического вещества в пределах одной градации катагенеза параметры: CPI, Ts/Tm, 1/Ki ((н-С17+н-С18)/(Pr+Ph)), MDR (4-МДБТ/1-МДБТ), ДБТИ ((2+3-MДБТ)/ДБТ) и ТАСИ (ТАС I/(TAC I+TAС II)). Замечена отчетливая тенденция к снижению и выравниванию значений некоторых показателей (ФИ, MPI, PP-1, MDR, ДБТИ и др.) в битумоидах закрытых пор по сравнению с битумоидами из открытого порового пространства, что, по-видимому, связано с удалением наиболее преобразованной, легкой и миграционно-способной части органического вещества из породы при извлечении битумоидов открытых пор.</p></abstract><trans-abstract xml:lang="en"><p>The main features of the geochemistry of individual aromatic compounds (phenanthrenes, dibenzothiophenes, monoand triaromatic steroids) in chloroform extracts (bitumoids) from the open (regular form and coarse-crushed (≥0.5 cm) samples) and closed (fine-crushed (0.25 mm) samples) pore space of the Bazhenov Formation have been determined. The differences in the aromatic compounds distribution of organic matter of the Bazhenov Formation in the North of the Khantey hemiantheclise (Surgut region, KhantyMansiysk Autonomous District, Western Siberia) are mainly related to its stage of thermal maturity which decreases in the south-west direction within the studying area. The most sensitive to maturity variations at the same catagenesis gradation are the parameters: CPI, Ts/Tm, 1/Ki ((n-C17 + n-C18)/(Pr + Ph)), MDR (4-MDBT/1- MDBT), DBTI ((2+3-MDBT)/DBT) and TASI (TAS I/(TAS I + TAS II)). Based on some indicators (PI, MPI, PP-1, MDR, DBTI etc.), it is possible to notice the decrease and equalization of its values in bitumoids from closed pores compared with those from open ones. It seems to be associated with the removal of the most transformed, light and migratory-capable part of bitumoids during their extraction from the open pore space of rocks.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>органическое вещество</kwd><kwd>битумоиды</kwd><kwd>баженовская свита</kwd><kwd>ароматические соединения</kwd><kwd>катагенез</kwd><kwd>фенантрены</kwd><kwd>дибензотиофены</kwd><kwd>ароматические стероиды</kwd></kwd-group><kwd-group xml:lang="en"><kwd>organic matter</kwd><kwd>bitumoids (chloroform extracts)</kwd><kwd>Bazhenov Formation</kwd><kwd>aromatic compounds</kwd><kwd>сatagenesis</kwd><kwd>phenanthrenes</kwd><kwd>dibenzothiophenes</kwd><kwd>aromatic steroids</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при поддержке проектов ФНИ № 0331- 2019-0022 «Органическая геохимия и история геологического развития доминантных нефтегазовых систем верхнего протерозоя и фанерозоя Сибири» и № 0266-2019-0006 «Разработка методик оценки ресурсов, разведки и подсчета запасов залежей трудноизвлекаемой нефти в углеродистых карбонатно-глинисто-кремнистых, карбонатных и засолоненных песчаных коллекторах».</funding-statement><funding-statement xml:lang="en">This work was supported by the Basic Scientific Research Projects No. 0331-2019-0022 «Organic geochemistry and the history of geological development of the dominant oil and gas systems of the Upper Proterozoic and Phanerozoic of Siberia» and No. 0266-2019-0006 «Development of resource assessment methodologies, exploration and calculation of reserves of hard-torecover oil in carbonate-argillaceous-siliceous, carbonate and saline sand reservoirs».</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">движных компонентов рассеянного органического вещества в поровой системе пород. 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