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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-2019-10-4-0455</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-944</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>СОВРЕМЕННАЯ ГЕОДИНАМИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>RECENT GEODYNAMICS</subject></subj-group></article-categories><title-group><article-title>ГЕОДИНАМИЧЕСКИЕ И ГИДРОДИНАМИЧЕСКИЕ УСЛОВИЯ УРНЕНСКОГО И УСТЬ‐ТЕГУССКОГО НЕФТЯНЫХ МЕСТОРОЖДЕНИЙ</article-title><trans-title-group xml:lang="en"><trans-title>GEODYNAMIC AND HYDRODYNAMIC CONDITIONS OF THE URNA AND UST‐TEGUS OIL FIELDS</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-4747-058X</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Курчиков</surname><given-names>А. Р.</given-names></name><name name-style="western" xml:lang="en"><surname>Kurchikov</surname><given-names>A. R.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. геол.-мин. наук, профессор, член-корреспондент РАН, директор, 625026, Тюмень, ул. Таймырская, 74;</p><p>625000, Тюмень, ул. Володарского, 38</p></bio><bio xml:lang="en"><p>Doctor of Geology and Mineralogy, Professor, Corresponding member of RAS, Director, 74 Taymyrskaya street, Tyumen 625026;</p><p>38 Volodarsky street, Tyumen 625000</p></bio><email xlink:type="simple">Kurchikov.d@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/0000-0001-8099-4874</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Плавник</surname><given-names>А. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Plavnik</surname><given-names>A. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>докт. техн. наук, г.н.с., 625026, Тюмень, ул. Таймырская, 74;</p><p>625000, Тюмень, ул. Володарского, 38</p></bio><bio xml:lang="en"><p>Doctor of Technical Sciences, Chief Researcher, 74 Taymyrskaya street, Tyumen 625026;</p><p>38 Volodarsky street, Tyumen 625000</p></bio><email xlink:type="simple">plavnikag@ipgg.sbras.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/0000-0002-3796-0596</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Курчиков</surname><given-names>Д. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kurchikov</surname><given-names>D. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>канд. геол.-мин. наук, н.с., 625026, Тюмень, ул. Таймырская, 74;</p><p>625000, Тюмень, ул. Володарского, 38</p></bio><bio xml:lang="en"><p>Candidate of Geology and Mineralogy, Researcher, 74 Taymyrskaya street, Tyumen 625026;</p><p>38 Volodarsky street, Tyumen 625000</p></bio><email xlink:type="simple">Kurchikov.d@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Западно‐Сибирский филиал Института нефтегазовой геологии и геофизики	&#13;
им. А.А. Трофимука СО РАН;&#13;
Тюменский индустриальный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>West Siberian Division of A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of RAS;&#13;
Tyumen Industrial University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>10</day><month>12</month><year>2019</year></pub-date><volume>10</volume><issue>4</issue><fpage>1011</fpage><lpage>1027</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Курчиков А.Р., Плавник А.Г., Курчиков Д.А., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Курчиков А.Р., Плавник А.Г., Курчиков Д.А.</copyright-holder><copyright-holder xml:lang="en">Kurchikov A.R., Plavnik A.G., Kurchikov D.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.gt-crust.ru/jour/article/view/944">https://www.gt-crust.ru/jour/article/view/944</self-uri><abstract><p>В работе рассматриваются особенности строения и фильтрационно‐емкостных свойств продуктивных отложений Урненского и Усть‐Тегусского месторождений Западной Сибири, обусловленные воздействием геодинамических процессов. Эти процессы привели к формированию многочисленных трещиноватых зон в осадочных отложениях юрского комплекса, по которым происходило активное движение подземных вод и сопутствующее гидротермальное преобразование порового пространства осадочных отложений. Представленные в работе данные свидетельствуют о проявлении этих процессов в современных гидрогеохимических и геотермических условиях юрско‐меловых отложений рассматриваемых месторождений и прилегающих районов. Следствием комплексного воздействия отмеченных процессов является существенная неоднородность коллекторских свойств продуктивных отложений рассматриваемых месторождений, что подтверждается петрофизическими исследованиями керна и результатами гидродинамических исследований в скважинах. Анализ проведенных трассерных исследований свидетельствует о том, что, несмотря на существенное влияние геодинамического фактора, не прослеживается явной пространственной согласованности в наличии или отсутствии гидродинамической связи между скважинами с расположением зон трещиноватости и динамически напряженных зон. В работе предложен и апробирован метод, основанный на анализе морфоструктурных показателей строения опорных горизонтов, который может служить дополнительным инструментом для анализа связи тектонических и гидродинамических условий на месторождениях.</p></abstract><trans-abstract xml:lang="en"><p>This paper discusses the productive beds of the Urna and Ust‐Tegus oil fields (West Siberia, Russian) and permeability and capacity properties that are influenced by geodynamic processes. Strong tectonic processes, accompanied by periodic magma intrusions, produced numerous fractures and faults in the Jurassic sediments, which act as conduits for groundwater flows, and thus led to the hydrothermal alteration of rocks and changes in the pore space. The data presented in the paper testify to the manifestation of these processes in the modern hydrogeochemical and geothermal conditions of the Jurassic‐Cretaceous sediments within the two oil fields and their vicinity. The petrophysical studies of the core samples and the hydrodynamic studies in the wells confirm that the reservoir properties of the productive strata are considerably heterogeneous. Despite the significant effect of the geodynamic factors, the analysis of the tracer data has not revealed any apparent spatial consistency of the presence (or absence) of a hydrodynamic connection between the wells and the locations of fractured and dynamically stressed zones. In our study, we have proposed and tested a method based on the analysis of morphotectonic features detectable in the depth maps of reference surfaces. This method is a useful additional tool for discovering and analyzing the relationships between the tectonic and hydrodynamic conditions of oil and gas fields.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>геодинамические условия</kwd><kwd>юрский комплекс</kwd><kwd>палеозойский фундамент</kwd><kwd>интрузия</kwd><kwd>фильтрационно‐емкостные свойства</kwd><kwd>неоднородность</kwd><kwd>Урненское и Усть‐Тегусское месторождения</kwd></kwd-group><kwd-group xml:lang="en"><kwd>geodynamics</kwd><kwd>magmatism</kwd><kwd>Paleozoic basement</kwd><kwd>Jurassic reservoir</kwd><kwd>reservoir properties</kwd><kwd>heterogeneity</kwd><kwd>Urna and Ust‐Tegus oil fields</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">Афонин Д.Г. 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