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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-2025-16-3-0826</article-id><article-id custom-type="edn" pub-id-type="custom">hwnufq</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-2039</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>МЕЗОЗОЙСКО-КАЙНОЗОЙСКИЕ ВНУТРИГОРНЫЕ ВПАДИНЫ ТЯНЬ-ШАНЯ   И ЗАПАДНОГО ЗАБАЙКАЛЬЯ: СРАВНИТЕЛЬНАЯ ХАРАКТЕРИСТИКА И КОРРЕЛЯЦИЯ СОБЫТИЙ СТАТЬЯ 1. ПОСТАНОВКА ВОПРОСА. ВНУТРИГОРНЫЕ ВПАДИНЫ ГИССАРО-АЛАЯ И ЦЕНТРАЛЬНОГО ТЯНЬ-ШАНЯ</article-title><trans-title-group xml:lang="en"><trans-title>MESOZOIC-CENOZOIC INTRAMOUNTAIN BASINS OF THE TIEN SHAN AND WESTERN TRANSBAIKALIA:  COMPARATIVE CHARACTERISTICS AND CORRELATION OF EVENTS ARTICLE 1. QUESTION FORMULATION. INTRAMOUNTAIN BASINS OF THE GISSAR-ALAI  AND CENTRAL TIEN SHAN</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>Леонов</surname><given-names>М. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Leonov</surname><given-names>M. G.</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-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Пржиялговский</surname><given-names>Е. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Przhiyalgovskii</surname><given-names>E. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119017, Москва, Пыжевский пер., 7, стр. 1</p></bio><bio xml:lang="en"><p>Evgeny S. Przhiyalgovskii</p><p>7-1 Pyzhevsky Ln, Moscow 119017</p></bio><email xlink:type="simple">prz4@yandex.ru</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>Морозов</surname><given-names>Ю. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Morozov</surname><given-names>Yu. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>123242, Москва, ул. Большая Грузинская, 10, стр. 1</p></bio><bio xml:lang="en"><p>10-1 Bolshaya Gruzinskaya St, Moscow 123242</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>Лунина</surname><given-names>О. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Lunina</surname><given-names>O. V.</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-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мазукабзов</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Mazukabzov</surname><given-names>A. M.</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-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Никитин</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Nikitin</surname><given-names>А. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>394018, Воронеж, Университетская площадь, 1</p></bio><bio xml:lang="en"><p>1 Universitetskaya Sq, Voronezh 394018</p></bio><xref ref-type="aff" rid="aff-4"/></contrib></contrib-group><aff-alternatives id="aff-1"><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-2"><aff xml:lang="ru"><institution>Институт физики Земли им. О.Ю. Шмидта РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Schmidt Institute of Physics of the Earth, Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><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-4"><aff xml:lang="ru"><institution>Воронежский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Voronezh State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>18</day><month>06</month><year>2025</year></pub-date><volume>16</volume><issue>3</issue><fpage>826</fpage><lpage>826</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Леонов М.Г., Пржиялговский Е.С., Морозов Ю.А., Лунина О.В., Мазукабзов А.М., Никитин А.В., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Леонов М.Г., Пржиялговский Е.С., Морозов Ю.А., Лунина О.В., Мазукабзов А.М., Никитин А.В.</copyright-holder><copyright-holder xml:lang="en">Leonov M.G., Przhiyalgovskii E.S., Morozov Y.A., Lunina O.V., Mazukabzov A.M., Nikitin А.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/2039">https://www.gt-crust.ru/jour/article/view/2039</self-uri><abstract><p>Отрицательные структуры земной коры, включая межгорные и внутригорные впадины, являются ключевыми источниками информации о развитии континентальной коры на плитном и орогенном этапах ее формирования. Цель работы заключается в сравнительном описании мезозойско­кайнозойских впадин Евразийского внутриконтинентального орогена и выявлении региональных особенностей геодинамического развития его различных сегментов. Объектом исследования являются мезозойско­кайнозойские внутригорные впадины Гиссаро­Алайской горной системы (Западный Тянь­Шань), Центрального Тянь­Шаня и Западного Забайкалья. Методика исследования включала сравнительный геологический анализ, структурно­тектоническое исследование, геокартирование ключевых участков, описание литологических разрезов, тектонофизические экспериментальные работы, магнитотеллурическое зондирование и другое. В первой статье цикла показано, что в течение мезозоя и кайнозоя территория Западного и Центрального Тянь­Шаня представляла собой зону рассредоточенного сдвигового течения. В этих условиях сформировалась и эволюционировала система внутригорных впадин и разделяющих их поднятий. Установлено, что движения горных масс в системе «впадина/ поднятие» были обусловлены перераспределением масс горных пород в процессе их реидной деформации в условиях вертикальной и латеральной реологической неоднородности коры. Во второй статье цикла будет представлено описание впадин Западного Забайкалья и проведено обсуждение материала, будут сформулированы выводы по обозначенной проблеме.</p></abstract><trans-abstract xml:lang="en"><p>Negative structures of the Earth’s crust, including intermountain and intramountain basins, are key sources of information on the formation of the continental crust through plate tectonic and orogenic cycles. The aim of the work is to give a comparative description of the Mesozoic-Cenozoic basins of the Eurasian intracontinental orogen and to identify regional features of the geodynamic development of its various segments. The object of the study is the Mesozoic-Cenozoic intramountain basins of the Gissar-Alai mountain system (Western Tien Shan), Central Tien Shan, and Western Transbaikalia. The research methodology included comparative geological analysis, structural and tectonic research, geomapping of key areas, description of lithological sections, experimental tectonophysics, magnetotelluric sounding, etc. The first article of the series shows that the Mesozoic and Cenozoic territory of the Western and Central Tien Shan was a zone of dispersed shear flow. These were the conditions in which a system of intramountain depressions and their separating uplifts was formed and evolved. It has been found that the movements of rock masses in the "depres­sion/uplift" system were caused by the redistribution of rock masses during their rheid deformation under conditions of vertical and lateral rheological heterogeneity of the crust. The second article of the series will present a description of the depressions in Western Transbaikalia, discuss the material, and formulate conclusions on the research problem.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>мезозой</kwd><kwd>кайнозой</kwd><kwd>внутригорные впадины</kwd><kwd>тектоническая эволюция</kwd><kwd>седиментация</kwd><kwd>реидная деформация</kwd><kwd>транстенсия</kwd><kwd>транспрессия</kwd><kwd>Тянь­Шань</kwd><kwd>Гиссаро­Алай</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Mesozoic</kwd><kwd>Cenozoic</kwd><kwd>intramountain basins</kwd><kwd>tectonic evolution</kwd><kwd>sedimentation</kwd><kwd>rheid deformation</kwd><kwd>transtension</kwd><kwd>transpression</kwd><kwd>Tien Shan</kwd><kwd>Gissar-Alai</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследования проведены в рамках госзаданий Геологического института РАН, Института физики Земли им. О.Ю. Шмидта РАН, Института земной коры СО РАН, Воронежского государственного уни­верситета.</funding-statement><funding-statement xml:lang="en">The study was carried out on the state assignments of the Geological Institute RAS, Schmidt Institute of Physics of the Earth RAS, Institute of the Earth’s Crust SB RAS, and Voronezh State University.</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">Абдрахматов К.Е., Джанабилова С.О. Новейшая разломно-блоковая структура Северного Тянь-Шаня и сейсмичность // Вестник Института сейсмологии НАН КР. 2016. № 1 (7). С. 8‒16.</mixed-citation><mixed-citation xml:lang="en">Abdrakhmatov K.E., Dzhanabilova S.O., 2016. Modern Fault-Block Structure of the Northern Tien Shan and Seis­micity. 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