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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">litosphere</journal-id><journal-title-group><journal-title xml:lang="ru">Литосфера</journal-title><trans-title-group xml:lang="en"><trans-title>LITHOSPHERE (Russia)</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1681-9004</issn><issn pub-type="epub">2500-302X</issn><publisher><publisher-name>A.N. Zavaritsky Institute of Geology and Geochemistry</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24930/1681-9004-2023-23-5-820-843</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1954</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>Articles</subject></subj-group></article-categories><title-group><article-title>Геологическое строение и мезозойско-кайнозойская тектоническая эволюция Неня-Чумышского прогиба (Южный Салаир, юг Западной Сибири)</article-title><trans-title-group xml:lang="en"><trans-title>Geological structure and Mesozoic-Cenozoic tectonic evolution of the Nenya-Chumysh basin (Southern Salair, southern Western Siberia)</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>Жимулев</surname><given-names>Ф. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Zhimulev</surname><given-names>F. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, г. Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptuga av., Novosibirsk 630090</p></bio><email xlink:type="simple">zhimulev@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Котляров</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kotlyarov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, г. Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptuga av., Novosibirsk 630090</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>Новиков</surname><given-names>И. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Novikov</surname><given-names>I. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, г. Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptuga av., Novosibirsk 630090</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>Сенников</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Sennikov</surname><given-names>N. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, г. Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptuga av., Novosibirsk 630090</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>Колесов</surname><given-names>К. К.</given-names></name><name name-style="western" xml:lang="en"><surname>Kolesov</surname><given-names>K. K.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, г. Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptuga av., Novosibirsk 630090</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии и минералогии им. В.С. Соболева СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.S. Sobolev Institute of Geology and Mineralogy, SB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт нефтегазовой геологии и геофизики СО РАН им. А.А. Трофимука</institution><country>Россия</country></aff><aff xml:lang="en"><institution>A.A. Trofimuk Institute of Petroleum Geology and Geophysics, SB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>03</day><month>11</month><year>2023</year></pub-date><volume>23</volume><issue>5</issue><fpage>820</fpage><lpage>843</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Жимулев Ф.И., Котляров А.В., Новиков И.С., Сенников Н.В., Колесов К.К., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Жимулев Ф.И., Котляров А.В., Новиков И.С., Сенников Н.В., Колесов К.К.</copyright-holder><copyright-holder xml:lang="en">Zhimulev F.I., Kotlyarov A.V., Novikov I.S., Sennikov N.V., Kolesov K.K.</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.lithosphere.ru/jour/article/view/1954">https://www.lithosphere.ru/jour/article/view/1954</self-uri><abstract><p>Объект исследования. Неня-Чумышский прогиб – длительно развивавшийся внутриконтинентальный мезозойский осадочный бассейн, приуроченный к зоне регионального разрывного нарушения, отделяющего Салаир от структур Горного Алтая, Горной Шории и Кузнецкого прогиба. Цель. Геологическая и структурно-кинематическая характеристика импульсов внутриконтинентального орогенеза, имевших место в течение мезозоя и кайнозоя на территории СЗ части Алтае-Саянской складчатой области. Материалы и методы. Использовались геологические карты района, геофизические данные о положении подошвы палеозойского фундамента, спутниковые снимки и цифровые модели рельефа. Осадочное выполнение бассейна рассмотрено как летопись тектонических движений СЗ части Алтае-Саянской складчатой области на внутриконтинентальном этапе развития. Результаты. Выделяются раннеюрский, раннемеловой, позднемеловой-палеогеновый и неоген-четвертичный тектонические этапы развития Неня-Чумышского прогиба. В раннеюрское время Неня-Чумышский прогиб представлял собой бассейн пулл-апарт в зоне левого сдвига. С данным этапом связано накопление грубообломочных терригенных отложений глушинской свиты, мощность которых в Неня-Чумышском прогибе достигает около 1900 м. В раннемеловое время в результате изменения поля напряжений Неня-Чумышский прогиб был преобразован в принадвиговый бассейн, сложенный терригенными отложениями илекской свиты, образующими осадочный бассейн клиновидной формы, характерной для форландовых прогибов, например, кайнозойских межгорных принадвиговых впадин Тянь-Шаня. Неотектоническая структура Неня-Чумышского прогиба, сформированная в поле напряжений Индо-Евроазиатской коллизии, наследует более древний структурный план в общих чертах, но отличается от него деталями. Новообразованной структурой является поперечное неотектоническое поднятие Сары-Чумышского вала. Выводы. Раннеюрский этап обусловлен закрытием Палеотетиса и коллизией серии киммерийских террейнов с южной окраиной Евразии, раннемеловой этап – закрытием Монголо-Охотского океана и коллизией Евразии с Северо-Китайским континентом, кайнозойский этап происходил на фоне продолжающейся Индо-Евроазиатской коллизии. Геологическая эволюция континентальных осадочных бассейнов, контролируемых региональными разломами, может использоваться как источник информации об интенсивности и кинематической картине импульсов внутриконтинентального орогенеза в геологическом прошлом.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. The Nenya-Chumysh basin is a long-term Mesozoic intracontinental sedimentary basin confined to the zone of a regional fault separating the Salair from the structures of Gorny Altai, Gornaya Shoria, and the Kuznetsk basin. Aim. To establish the geological and structural-kinematic characteristics of impulses of intracontinental orogeny that took place during the Mesozoic and Cenozoic in the territory of the northwestern part of the Altai-Sayan Folded Area. Materials and Methods. Geological maps of the area, geophysical data on the position of the base of the Paleozoic basement, satellite images and digital elevation models were used. The sedimentary filling of the basin is considered as a chronicle of tectonic movements in the NW part of the Altai-Sayan Folded Area at the intracontinental stage of development. Results. The Early Jurassic, Early Cretaceous, Late Cretaceous-Paleogene, and Neogene-Quaternary tectonic stages of the development of the Nenya-Chumysh basin were distinguished. In the Early Jurassic, the Nenya-Chumysh basin was a pull-apart basin in a left-hand strike-slip zone. This stage is associated with the accumulation of coal-bearing deposits of the Glushinskaya Formation, the thickness of which in the Nenya-Chumysh basin reaches about 1900 m. In the Early Cretaceous, as a result of changes in the stress field, the Nenya-Chumysh basin was transformed into a thrust basin, composed of terrigenous deposits of the Ilek Formation, forming a wedge-shaped sedimentary basin characteristic of foreland troughs. The neotectonic structure of the Nenya-Chumysh basin, formed in the stress field of the Indo-Eurasian collision, inherits an older structural plan in general terms, although differing in details. A non-inherited structure is the transverse neotectonic uplift of the Sary-Chumysh swell. Conclusions. The Early Jurassic stage is related with the closure of the Paleo-Tethys and the collision of a series of Cimmerian terranes with the southern margin of Eurasia, Early Cretaceous stage is caused with Mongol-Okhotsk collision, and the Cenozoic stage proceeds with the ongoing Indo-Eurasian collision. The geological evolution of continental sedimentary basins controlled by regional faults can be used as a source of information about the intensity and kinematic pattern of impulses of intracontinental orogeny in the geological past.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>осадочные бассейны</kwd><kwd>коррелятные отложения</kwd><kwd>внутриконтинентальный орогенез</kwd><kwd>Западная Сибирь</kwd><kwd>Центрально-Азиатский складчатый пояс</kwd><kwd>мезозой</kwd><kwd>сдвиги</kwd><kwd>бассейны пулл-апарт</kwd></kwd-group><kwd-group xml:lang="en"><kwd>sedimentary basins</kwd><kwd>correlative deposits</kwd><kwd>intracontinental orogeny</kwd><kwd>Western Siberia</kwd><kwd>Central Asian orogenic belt</kwd><kwd>Mesozoic</kwd><kwd>strike-slip</kwd><kwd>pull-apart basins</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена по государственному заданию ИГМ СО РАН (проекты 122041400057-2, 122041400214-9). Работа Н.В. Сенникова проделана в рамках государственного задания РАН (проект FW ZZ-2022-0003). Авторы благодарны Е.С. Жимулевой за помощь в подготовке рукописи.</funding-statement><funding-statement xml:lang="en">The work was carried out within the state assignment of IGM SB RAS (projects 122041400057-2, 122041400214-9). The work of N.V. Sennikov was supported in the framework of the state assignment of the Russian Academy of Sciences (project FW ZZ-2022-0003). The authors are grateful to E.S. Zhimuleva for assistance in editing the text.</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">Адаменко О.М. (1974) Мезозой и кайнозой Степного Алтая. Новосибирск: Наука, 168 с.</mixed-citation><mixed-citation xml:lang="en">Adamenko O.M. (1974) Mesozoic and Cenozoic of the Steppe Altai. Novosibirsk, Nauka Publ., 168 p. 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