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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-2023-14-2-0689</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1660</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>ТЕКТОНОФИЗИКА</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>TECTONOPHYSICS</subject></subj-group></article-categories><title-group><article-title>АНАЛИЗ РАЗЛОМНО-БЛОКОВОЙ СТРУКТУРЫ И НАПРЯЖЕННОГО СОСТОЯНИЯ ОСАДОЧНОГО ЧЕХЛА НА ГАЗОКОНДЕНСАТНЫХ МЕСТОРОЖДЕНИЯХ: ОСНОВЫ ТЕКТОНОФИЗИЧЕСКОГО ПОДХОДА</article-title><trans-title-group xml:lang="en"><trans-title>ANALYSIS OF THE FAULT-BLOCK STRUCTURE AND STRESS STATE OF THE SEDIMENTARY COVER IN GAS-CONDENSATE DEPOSITS: BASICS OF THE TECTONOPHYSICAL APPROACH</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7607-0417</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Семинский</surname><given-names>К. Ж.</given-names></name><name name-style="western" xml:lang="en"><surname>Seminsky</surname><given-names>K. Zh.</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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-9955-0314</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Бурзунова</surname><given-names>Ю. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Burzunova</surname><given-names>Yu. P.</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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-5119-1092</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Борняков</surname><given-names>С. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bornyakov</surname><given-names>S. 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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-2749-8825</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мирошниченко</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Miroshnichenko</surname><given-names>A. I.</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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-9953-6627</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Черемных</surname><given-names>А. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Cheremnykh</surname><given-names>A. S.</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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-6309-2235</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Семинский</surname><given-names>А. К.</given-names></name><name name-style="western" xml:lang="en"><surname>Seminsky</surname><given-names>A. K.</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"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-5204-9530</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Буддо</surname><given-names>И. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Buddo</surname><given-names>I. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, Иркутск, ул. Лермонтова, 128</p><p>664074, Иркутск, ул. Лермонтова, 83</p></bio><bio xml:lang="en"><p>128 Lermontov St, Irkutsk 664033</p><p>83 Lermontov St, Irkutsk 664074</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>Смирнов</surname><given-names>А. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Smirnov</surname><given-names>A. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>625003, Тюмень ул. Перекопская, 19</p></bio><bio xml:lang="en"><p>19 Perekopskaya St, Tyumen 625003</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>Горлов</surname><given-names>И. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Gorlov</surname><given-names>I. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>625003, Тюмень ул. Перекопская, 19</p></bio><bio xml:lang="en"><p>19 Perekopskaya St, Tyumen 625003</p></bio><xref ref-type="aff" rid="aff-3"/></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>Институт земной коры СО РАН; Иркутский национальный исследовательский технический университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences; Irkutsk National Research Technical University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>ООО «Газпром ВНИИГАЗ»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Gazprom VNIIGAZ LLC</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>18</day><month>04</month><year>2023</year></pub-date><volume>14</volume><issue>2</issue><fpage>689</fpage><lpage>689</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Семинский К.Ж., Бурзунова Ю.П., Борняков С.А., Мирошниченко А.И., Черемных А.С., Семинский А.К., Буддо И.В., Смирнов А.С., Горлов И.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Семинский К.Ж., Бурзунова Ю.П., Борняков С.А., Мирошниченко А.И., Черемных А.С., Семинский А.К., Буддо И.В., Смирнов А.С., Горлов И.В.</copyright-holder><copyright-holder xml:lang="en">Seminsky K.Z., Burzunova Y.P., Bornyakov S.A., Miroshnichenko A.I., Cheremnykh A.S., Seminsky A.K., Buddo I.V., Smirnov A.S., Gorlov 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.gt-crust.ru/jour/article/view/1660">https://www.gt-crust.ru/jour/article/view/1660</self-uri><abstract><p>Рассмотрено содержание тектонофизического подхода к реконструкции механизмов структурообразования и напряженнодеформированного состояния пород на месторождениях углеводородов, локалиующихся в платформенном чехле, который отличается сложным строением в плане реологической расслоенноти и нарушенности разноранговыми разрывами. На примере крупнейшего Ковыктинского газоконденсатного месторождения в Восточной Сибири показаны основные приемы и способы использования современных достижений тектонофизики для интерпретации уникальной по объему и значимости геологогеофизической информации, полученной для верхней и нижней части осадочного чехла при проведении геологоразведочных работ. Закономерности напряженнодеформированного состояния пород, установленные в ходе исследований, объединены в тектонофизическую модель, которая может использоваться в качестве базовой для других месторождений углеводородного сырья. Основу модели составляют представления о зонноблоковой структуре платформенного чехла, которую образует сеть субвертикальных и субгоризонтальных разломных зон, разделяющих его на менее нарушенные блоки. Дизъюнктивные структуры являются зонами повышенной трещиноватости и сгущения сравнительно мелких малоамплитудных разрывов, т.е. представляют ранние стадии разломообразования. Зонноблоковая структура формируется главным образом под действием сил тектонической и гравитационной природы, причем в первом случае этапность и характер разрывообразования трансформируются на платформу со стороны окружающих подвижных поясов, а во втором – определяются наличием в разрезе пластичных пород, способных к гравитационному скольжению. Графической составляющей тектонофизической модели являются 3D объемы информации, отражающие зонноблоковую структуру и напряженное состояние пород для место рождения с той степенью детальности, которую обеспечивают ключевые геофизические материалы, и прежде всего данные сейсморазведки. При помощи современных ГИС эта информация может оперативно извлекаться для любого по размеру участка изучаемого породного массива и затем использоваться в качестве основы для решения производственных вопросов, связанных с разработкой залежей в трещиннопоровых коллекторах, или для анализа общих проблем их образования и динамики.</p></abstract><trans-abstract xml:lang="en"><p>Consideration is being given to the tectonophysical approach to the reconstruction of structure formation mechanisms and stress-strain state of rocks in hydrocarbon deposits localized in the platform cover, which has a complex structure in terms of rheological layering and disturbance by different-rank fractures. With the Kovykta gas condensate field, largest in Eastern Siberia, there were shown the main methods and ways of using modern achievements in tectonophysics for interpreting geological and geophysical information on the upper and lower parts of the sedimentary cover, unique in terms of volume and significance, that was obtained during geological exploration therein. Regularities of changes in the stress-strain state of rocks, found during the research, are combined into a tectonophysical model, which can be used as a base for other hydrocarbon deposits. The model is based on the concept of a zone-block structure of the platform cover, which is formed by a network of subvertical and subhorizontal fault zones that divide it into less faulted blocks. Disjunctive structures are highly fractured zones with concentration of relatively small low-amplitude faults, i.e. represent the early stages of faulting. The zone-block structure is formed mainly by tectonic or gravitational forces; in the first case, the stages and fracture characteristics are transformed onto the platform from the surrounding mobile belts, and in the second case they are determined by the presence of ductile rocks in the section capable of gravitational sliding. The graphic component of the tectonophysical model is 3D datasets that show the zone-block structure and stress state of rocks for the deposit with the degree of detail provided by key geophysical materials and, primarily, by seismic data. By modern GIS, this information can be quickly retrieved for any-size area of the studied rock mass and then used as a basis for solving production issues related to the development of deposits in fracture-pore reservoirs, or for analyzing general problems of their formation and dynamics.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>тектонофизический подход</kwd><kwd>разломная зона</kwd><kwd>поле напряжений</kwd><kwd>зонноблоковая структура</kwd><kwd>осадочный чехол</kwd><kwd>моделирование</kwd><kwd>Ковыктинское газоконденсатное месторождение</kwd></kwd-group><kwd-group xml:lang="en"><kwd>tectonophysical approach</kwd><kwd>fault zone</kwd><kwd>stress field</kwd><kwd>zoneblock structure</kwd><kwd>sedimentary cover</kwd><kwd>modeling</kwd><kwd>Kovykta gas condensate field</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Обобщение материалов выполнено в рамках госзадания ИЗК СО РАН на 2021–2025 гг. «Современная геодинамика, механизмы деструкции литосферы и опасные геологические процессы в Центральной Азии» (шифр научной темы FWEF20210009). В работе задействовалось оборудование и инфраструктура ЦКП «Геодинамика и геохронология» ИЗК СО РАН в рамках гранта No 075152021682. Авторы благодарны директору Института земной коры СО РАН, чл.корр. РАН Д.П. Гладкочубу и генеральному директору ООО «СИГМАГЕО», к.т.н. Ю.А. Агафонову за всестороннюю поддержку исследования на всех этапах его реализации, а также А.В. Черемных, А.Г. Вахромееву, В.В. Огибенину, В.А. Санькову, А.А. Боброву, С.А. Сверкунову, Н.В. Мисюркеевой, И.А. Шелохову и А.В. Парфеевец за помощь в сборе и обработке комплекса геолого геофизических данных по Ковыктинскому ГКМ.</funding-statement><funding-statement xml:lang="en">The generalization was performed on the materials as part of the 2021–2025 state assignment for the IEC SB RAS "Modern geodynamics, mechanism of lithosphere destruction and geologic hazards in the Central Asia" (scientific code FWEF-2021-0009). The work was conducted using equipment and infrastructure of the Centre for Geodynamics and Geochronology at the Institute of the IEC SB RAS (grant 075-15-2021-682).</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">Aarre V., Astratti D., Dayyni T.N.A.A., Mahmoud S.L., Clark A.B.S., Stellas M.J., Stringer J.W., Toelle B.Е., Vejbak O.V., White G., 2012. Seismic Detection of Subtle Faults and Fractures. Oilfield Review 24 (2), 28–43.</mixed-citation><mixed-citation xml:lang="en">Aarre V., Astratti D., Dayyni T.N.A.A., Mahmoud S.L., Clark A.B.S., Stellas M.J., Stringer J.W., Toelle B.Е., Vejbak O.V., White G., 2012. Seismic Detection of Subtle Faults and Fractures. 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