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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.2026.1.9</article-id><article-id custom-type="elpub" pub-id-type="custom">geores-524</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>Тектонические нарушения в доплитном комплексе и платформенного чехла Северного Каспия: причины и следствия</article-title><trans-title-group xml:lang="en"><trans-title>Tectonic Faults of the Pre-Plate Complex and Platform Cover of the Northern Caspian: Causes and Consequences</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>Попков</surname><given-names>В. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Popkov</surname><given-names>V. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Василий Иванович Попков – доктор геол.-минерал. наук, профессор</p><p>350049, Краснодар, ул. ставропольская, 149 </p></bio><bio xml:lang="en"><p>Vasily I. Popkov – Dr. Sci. (Geology and Mineralogy), Professor,</p><p>149 Stavropolskaya Av., Krasnodar, 350049</p></bio><email xlink:type="simple">geoskubsu@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-2386-6611</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Попков</surname><given-names>И. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Popkov</surname><given-names>I. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Иван Васильевич Попков – кандидат геолого-минерал. наук, доцент</p><p>350049, Краснодар, ул. ставропольская, 149 </p></bio><bio xml:lang="en"><p>Ivan V. Popkov – Cand. Sci. (Geology and Mineralogy), Associate Professor</p><p>149 Stavropolskaya Av., Krasnodar, 350049</p></bio><email xlink:type="simple">iv-popkov@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Кубанский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kuban State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2026</year></pub-date><pub-date pub-type="epub"><day>27</day><month>03</month><year>2026</year></pub-date><volume>28</volume><issue>1</issue><fpage>78</fpage><lpage>85</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Попков В.И., Попков И.В., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Попков В.И., Попков И.В.</copyright-holder><copyright-holder xml:lang="en">Popkov V.I., Popkov I.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.geors.ru/jour/article/view/524">https://www.geors.ru/jour/article/view/524</self-uri><abstract><p>Исследованы тектонические дислокации доплитного пермско-триасового комплекса и в перекрывающем его платформенном чехле северной части Каспийского моря. В результате анализа материалов сейсморазведки и глубокого бурения установлена тектоническая расслоенность доплитного комплекса, обусловленная развитием в его разрезе пологих надвигов и тектонических пластин. Их формирование связано с коллизионными процессами, сопровождавшими закрытие остаточных бассейнов океана Палеотетис. В последующем своем развитии молодая платформа периодически испытывала горизонтальное сжатие, приводившее к возобновлению подвижек по погребенным надвигам, что сопровождалось формированием в отложениях чехла характерных дислокаций. Важным следствием этих процессов является резко выраженная дисгармоничная складчатость, при которой структурный план платформенного чехла кардинально отличается от строения глубинных слоев. учитывая развитие тектонических пластин в доплитном комплексе, поиск ловушек нефти и газа в нем нужно вести отдельно по каждому структурному уровню (пластине). Помимо данного типа структур в отложениях мелового возраста впервые выявлены послойные тектонические срывы. Источником тангенциальных напряжений, обусловивших тектоническую расслоенность платформенного чехла, является стресс, транслирующийся в пределы платформы из области альпийской коллизионной зоны Кавказа. Наиболее крупные из срывов, трансформируясь в головных частях пластин в наклонные разрывы, проникают в вышележащие кайнозойские отложения, разрывая осадочный чехол на всю его мощность. Послойные срывы сопровождаются зонами катаклазированных пород, обладающих повышенными емкостными и фильтрационными параметрами. В соответствии с этим они могут служить путями латеральной миграции углеводородов, а в пределах продуктивных интервалов разреза при разработке месторождений обеспечивать более высокие дебиты флюидов.</p></abstract><trans-abstract xml:lang="en"><p>Tectonic dislocations of the pre-plate PermianTriassic complex and the overlying platform cover of the northern Caspian Sea have been studied. Analysis of seismic survey and deep drilling data has revealed tectonic layering of the pre-plate complex due to the development of gentle thrusts and tectonic plates in its section. Their formation is associated with collision processes that accompanied the closure of the residual basins of the Paleotethys Ocean. In its subsequent development, the young platform periodically experienced horizontal compression, which resulted in the resumption of movements along the buried thrusts, which led to the formation of characteristic dislocations in the cover deposits, confined to their frontal parts. In addition to this type of structure, rootless layered tectonic faults were revealed for the first time in Cretaceous deposits. The source of tangential stresses that caused the tectonic stratification of the platform cover is stress transmitted to the platform from the region of the Alpine collision zone of the Caucasus. The largest of the faults, transforming in the head parts of the plates into inclined ruptures, penetrates into the overlying Cenozoic deposits, tearing the sedimentary cover to its full thickness. The results obtained indicate the important role of horizontal tectonic movements in the formation of the modern structure of this region, which belongs to the Scythian-Turanian young platform. The results of the research provide an opportunity to take a new approach to solving a number of applied problems in prospecting and exploration of hydrocarbon deposits. Considering the development of the tectonic plate in the preplate complex, the search for oil and gas traps in it should be carried out separately for each structural level (plate). Layered detachments are accompanied by zones of cataclastic rocks with increased capacity and filtration parameters. Accordingly, they can serve as paths for lateral migration of hydrocarbons, and within the productive intervals of the section during field development, provide higher fluid flow rates. </p></trans-abstract><kwd-group xml:lang="ru"><kwd>доплитный комплекс</kwd><kwd>платформенный чехол</kwd><kwd>тектоническая расслоенность</kwd><kwd>складчато-надвиговые дислокации</kwd><kwd>послойные срывы</kwd><kwd>тангенциальное сжатие</kwd><kwd>нефтегазоносность</kwd></kwd-group><kwd-group xml:lang="en"><kwd>preplate complex</kwd><kwd>platform cover</kwd><kwd>tectonic stratification</kwd><kwd>fold-thrust dislocations</kwd><kwd>tangential compression</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Авторы выражают благодарность рецензентам за ценные замечания и предложения, которые способствовали улучшению работы.</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">Анисимов Л.А. 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