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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">gtcrust</journal-id><journal-title-group><journal-title xml:lang="ru">Геодинамика и тектонофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Geodynamics &amp; Tectonophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2078-502X</issn><publisher><publisher-name>Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.5800/GT-2024-15-6-0802</article-id><article-id custom-type="edn" pub-id-type="custom">GMMZOW</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1943</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>ПАЛЕОГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>PALEOGEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>ОСОБЕННОСТИ ГЕОЛОГИЧЕСКОГО СТРОЕНИЯ И ПЕРСПЕКТИВЫ НЕФТЕГАЗОНОСНОСТИ РИФЕЙСКИХ И ВЕНДСКИХ ОСАДОЧНЫХ ТОЛЩ ЮГО-ВОСТОЧНОЙ ЧАСТИ КАМОВСКОГО СВОДА БАЙКИТСКОЙ АНТЕКЛИЗЫ</article-title><trans-title-group xml:lang="en"><trans-title>FEATURES OF GEOLOGICAL STRUCTURE AND PROSPECTS OF OIL-AND-GAS BEARING CAPACITY OF THE RIPHEAN AND VENDIAN DEPOSITS IN THE SOUTHEASTERN PART OF THE KAMO ARCH OF THE BAYKIT ANTICLISE</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>Фомин</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Fomin</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</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>Вахромеев</surname><given-names>А. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Vakhromeev</surname><given-names>A. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</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>Мотова</surname><given-names>З. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Motova</surname><given-names>Z. L.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</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>Струнов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Strunov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>105118, Москва, ш. Энтузиастов, 36</p></bio><bio xml:lang="en"><p>36 Rte Entuziastov, Moscow 105118</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>Машенькин</surname><given-names>Д. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Mashenkin</surname><given-names>D. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>660037, Красноярск, ул. Семафорная, 471</p></bio><bio xml:lang="en"><p>471 Semafornaya St, Krasnoyarsk 660037</p></bio><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Фомина</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Fomina</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119017, Москва, Пыжевский пер., 7, стр. 1</p></bio><bio xml:lang="en"><p>7-1 Pyzhevsky Ln, Moscow 119017</p></bio><xref ref-type="aff" rid="aff-4"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Плюснин</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Plusnin</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>423462, Альметьевск, ул. Советская, 186а, Татарстан</p></bio><bio xml:lang="en"><p>186a Sovetskaya St, Almetyevsk 423462, Republic of Tatarstan</p></bio><xref ref-type="aff" rid="aff-5"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт земной коры СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Всероссийский научно-исследовательский геологический нефтяной институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>All-Russian Scientific Research Geological Oil Institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>ООО «Газпром недра»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Gazprom Nedra LLC</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-4"><aff xml:lang="ru"><institution>Геологический институт РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geological Institute, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-5"><aff xml:lang="ru"><institution>Высшая школа нефти</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Petroleum High School</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>13</day><month>12</month><year>2024</year></pub-date><volume>15</volume><issue>6</issue><fpage>802</fpage><lpage>802</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Фомин В.А., Вахромеев А.Г., Мотова З.Л., Струнов А.В., Машенькин Д.В., Фомина В.В., Плюснин А.В., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Фомин В.А., Вахромеев А.Г., Мотова З.Л., Струнов А.В., Машенькин Д.В., Фомина В.В., Плюснин А.В.</copyright-holder><copyright-holder xml:lang="en">Fomin V.A., Vakhromeev A.G., Motova Z.L., Strunov A.V., Mashenkin D.V., Fomina V.V., Plusnin A.V.</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.gt-crust.ru/jour/article/view/1943">https://www.gt-crust.ru/jour/article/view/1943</self-uri><abstract><p>В работе представлены результаты комплексного исследования особенностей геологического строения юго-восточной части Камовского свода Байкитской антеклизы. Использованы опубликованные геолого-геофизические данные, а также новые данные, полученные авторами в ходе сейсморазведочных работ, проведенных методом общей глубинной точки (МОГТ 2D) и методом сейсмической локации бокового обзора (СЛБО). Проведенные исследования позволили уточнить современные представления о геологическом строении и условиях формирования наиболее перспективных на обнаружение промышленных залежей углеводородов (УВ) терригенно-карбонатных пород камовской серии нижнего рифея (мадринская, юрубченская и долгоктинская толщи) и венда (ванаварская и оскобинская свиты), распространенных в юго-восточной части Камовского свода Байкитской антеклизы. Интерпретация сейсмических данных (МОГТ 2D и СЛБО) позволила уточнить мощность наиболее перспективных на УВ терригенно-карбонатных пород нижнего рифея и построить прогнозную геологическую схему предвендской эрозионной поверхности, а также составить схемы толщин перспективных на УВ раннерифейских и вендских отложений. По аналогии с уже разведанными крупными месторождениями УВ центральной части Камовского свода Байкитской антеклизы приведенные в работе новые данные свидетельствуют о благоприятных структурно-тектонических условиях строения изученных нижнерифейских и вендских пород юго-восточного склона Камовского свода Байкитской антеклизы и указывают на их высокую перспективность.</p></abstract><trans-abstract xml:lang="en"><p>The paper presents the results of the integrated study of the features of geological structure of the southeastern Kamo arch of the Baikit anticlise. Use has been made of both already published and unpublished geological-geophysical data obtained through seismic survey using the common depth point (CDP 2D) and the side view seismic location (SVSL) methods. The conducted research made it possible to improve understanding of the geological structure and formation conditions of the terrigenous-carbonate rocks of the Lower Riphean (Madrа, Yurubchen and Dolgokit formations) and Vendian (Vanavara and Oskoba formations) Kamo Group in the southern Kamo arch of the Baykit anticlese in terms of the prospects for the discovery of hydrocarbon (HC) deposits therein. The interpretation of seismic data (CDP and SVSL) provided the possibility to specify the thickness of the Lower Riphean terrigenous-carbonate rocks, most promising for hydrocarbons, to generate the predictive geology map of the pre-Vendian erosion surface, and to map the HC-promising Early Riphean and Vendian deposit thickness. Along with the previously explored large HC deposits in the central Kamo arch of the Baykit anticlise, the new data presented here testify in favor of the structural-and tectonic conditions for the development of the Lower Riphean and Vendian rocks on the southeastern slope of the Kamo arch of the Baykit anticlise and imply their high potential.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Сибирская платформа</kwd><kwd>Камовский свод</kwd><kwd>Байкитская антеклиза</kwd><kwd>рифей</kwd><kwd>венд</kwd><kwd>нефть</kwd><kwd>газ</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Siberian Platform</kwd><kwd>Kamo arch</kwd><kwd>Baykit anticlise</kwd><kwd>Riphean</kwd><kwd>Vendian</kwd><kwd>oil</kwd><kwd>gas</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено за счет гранта Российского научного фонда № 23-17-00196, https://rscf.ru/project/23-17-00196/</funding-statement><funding-statement xml:lang="en">The study was conducted with the financial support of the Russian Science Foundation under grant agreement 23-17-00196, https://rscf.ru/project/23-17-00196/</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">Афанасенков А.П., Бухаров Н.Г., Мухаметзянов Р.Н. 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