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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">kaz29</journal-id><journal-title-group><journal-title xml:lang="ru">Вестник Казахстанско-Британского технического университета</journal-title><trans-title-group xml:lang="en"><trans-title>Herald of the Kazakh-British Technical University</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1998-6688</issn><issn pub-type="epub">2959-8109</issn><publisher><publisher-name>Казахстанско-Британский Технический Университет</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.55452/1998-6688-2025-22-3-340-346</article-id><article-id custom-type="elpub" pub-id-type="custom">kaz29-2135</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>НЕФТЕГАЗОВАЯ ИНЖЕНЕРИЯ И ГЕОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>OIL AND GAS ENGINEERING, GEOLOGY</subject></subj-group></article-categories><title-group><article-title>НЕФТЯНЫЕ БИОМАРКЕРЫ КАК ИНДИКАТОРЫ ПРОИСХОЖДЕНИЯ И СТЕПЕНИ ЗРЕЛОСТИ НЕФТИ В ЮГО-ВОСТОЧНОЙ ЧАСТИ ПРИКАСПИЙСКОЙ ВПАДИНЫ</article-title><trans-title-group xml:lang="en"><trans-title>PETROLEUM BIOMARKERS AS INDICATORS OF OIL ORIGIN AND MATURITY IN THE SOUTH-EASTERN PRECASPIAN BASIN</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-2900-9872</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Джарасова</surname><given-names>Т. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Jarassova</surname><given-names>T. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>PhD</p><p>г. Атырау</p></bio><bio xml:lang="en"><p>PhD </p><p>Atyrau</p></bio><email xlink:type="simple">t.jarassova@kmge.kz</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-3140-6682</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Алтунсой</surname><given-names>М.</given-names></name><name name-style="western" xml:lang="en"><surname>Altunsoy</surname><given-names>M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>д.т.н.</p><p>г. Анталья</p></bio><bio xml:lang="en"><p>Dr.Tech.Sc.</p><p>Antalya</p></bio><email xlink:type="simple">altunsoy@akdeniz.edu.tr</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">АФ ТОО «КМГ Инжиниринг»<country>Казахстан</country></aff><aff xml:lang="en">Atyrau Branch LLP “KMG Engineering”<country>Kazakhstan</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru">Университет Акдениз<country>Турция</country></aff><aff xml:lang="en">Akdeniz University<country>Turkey</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>27</day><month>09</month><year>2025</year></pub-date><volume>22</volume><issue>3</issue><fpage>340</fpage><lpage>346</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Джарасова Т.С., Алтунсой М., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Джарасова Т.С., Алтунсой М.</copyright-holder><copyright-holder xml:lang="en">Jarassova T.S., Altunsoy M.</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://vestnik.kbtu.edu.kz/jour/article/view/2135">https://vestnik.kbtu.edu.kz/jour/article/view/2135</self-uri><abstract><p>В данном исследовании изучается происхождение нефти юго-восточной части Прикаспийской впадины с помощью анализа биомаркеров пяти проб сырой нефти методом газовой хроматографии-массспектрометрии (ГХ-МС). Биомаркеры выступают в роли молекулярных отпечатков, позволяющих определить происхождение углеводородов, характеристики материнских пород и термическую историю. Анализ проб выявил: морские условия осадконакопления (соотношение C₂₆/C₂₅ терпанов = 0.59–0.79), преобладание карбонатных материнских пород (соотношение C₂₉/C₃₀ гопанов = 4.78-5.55), смешанное происхождение из отложений палеозоя (Карбон-Пермь) (соотношение C₂₈/C₂₉ стеранов = 0.44-0.57) и по соотношенииям Ts/Tm, C29Ts/ C29Tm и изомеризации C₂₉ стеранов пиковую и позднюю зону нефтеобразования. Полученные данные демонстрируют сложную историю генерации углеводородов в бассейне, при этом распределение биомаркеров указывает на поступление морского органического вещества в аноксидных условиях, карбонатно-эвапоритовые фации материнских пород и термическое равновесие, соответствующее основной фазе нефтеобразования. Результаты представляют ценные данные для разработки стратегий разведки в аналогичных бассейнах, позволяя снижать риски и оптимизировать освоение ресурсов. Дальнейшие исследования должны объединить эти геохимические данные со структурным и стратиграфическим анализами для уточнения моделей миграции.</p></abstract><trans-abstract xml:lang="en"><p>This study investigates the origin of oil from the south-eastern Precaspian Basin through biomarker analysis of five crude oil samples using gas chromatography-mass spectrometry (GC-MS). Biomarkers serve as molecular fingerprints to elucidate hydrocarbon origin, source rock characteristics, and thermal history. The analyzed samples revealed: a marine depositional environment (C₂₆/C₂₅ terpane ratios = 0.59–0.79), carbonate-dominated source rocks (C₂₉/C₃₀ hopane ratios = 4.78–5.55), sourcing from Paleozoic (Permo-Carboniferous) strata (C₂₈/C₂₉ sterane ratios = 0.44–0.57), and peak oil window – late maturation according to Ts/T, C29Ts/ C29Tm, C₂₉ sterane isomerization ratios. These findings demonstrate the basin's complex hydrocarbon generation history, with biomarker distributions indicating: marine organic matter input under anoxic conditions, carbonate-evaporitic source facies and thermal equilibrium consistent with primary oil generation. The results provide valuable insights for exploration strategies in similar frontier basins, with implications for reducing exploration risk and optimizing resource development. Future studies should combine these geochemical data with structural and stratigraphic analyses to refine migration models.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Прикаспийская впадина</kwd><kwd>анализ биомаркеров</kwd><kwd>органическая геохимия</kwd><kwd>стераны</kwd><kwd>терпаны</kwd><kwd>ГХ-МС</kwd><kwd>материнская порода</kwd><kwd>обстановка осадконакопления</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Precaspian Basin</kwd><kwd>biomarker analysis</kwd><kwd>organic geochemistry</kwd><kwd>sterane</kwd><kwd>terpane</kwd><kwd>GC-MS</kwd><kwd>source&#13;
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