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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">10.24930/1681-9004-2020-20-6-771-790</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1366</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>Структуры Алайской и Кичи-Каракольской впадин и обстановки новейших деформаций в их горном обрамлении (Южный Тянь-Шань)</article-title><trans-title-group xml:lang="en"><trans-title>The structures of the Alai and Kichi-Karakol depressions and the latest deformations in their mountainous surroundings (Southern 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>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"/><bio xml:lang="en"><p>7 Pyzhevsky line, 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>Лаврушина</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Lavrushina</surname><given-names>E. V.</given-names></name></name-alternatives><bio xml:lang="ru"/><bio xml:lang="en"><p>7 Pyzhevsky line, Moscow 119017</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Геологический институт (ГИН) РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Geological Institute (GIN) RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>29</day><month>12</month><year>2020</year></pub-date><volume>20</volume><issue>6</issue><fpage>771</fpage><lpage>790</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Пржиялговский Е.С., Лаврушина Е.В., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Пржиялговский Е.С., Лаврушина Е.В.</copyright-holder><copyright-holder xml:lang="en">Przhiyalgovskii E.S., Lavrushina E.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.lithosphere.ru/jour/article/view/1366">https://www.lithosphere.ru/jour/article/view/1366</self-uri><abstract><sec><title>Объект исследований</title><p>Объект исследований. Изучались структуры Алайской и Кичи-Каракольской внутригорных впадин (Южный Тянь-Шань) и обстановки новейших деформаций во впадинах и их горном обрамлении. Целью работы являлось определение основных параметров напряженно-деформированного состояния (НДС) в ключевой области сочленения складчатых сооружений Тянь-Шаня и Памира.</p></sec><sec><title>Материалы и методы</title><p>Материалы и методы. Комплекс исследований включал в себя изучение морфологии и ориентировки деформационных структур осадочного чехла и структурных несогласий на основе детального геологического картирования; статистически значимые замеры ориентировок линейных и плоскостных элементов (тектонических борозд, зеркал скольжения) в зонах динамического влияния активных разломов; обработку комплекса кинематических индикаторов с помощью апробированных методик и расчетных программ (Расцветаев, 1987; Delvaux, Sperner, 2003). Помимо этого, проводился анализ структурно-геологических данных предшествующих работ. Результаты. 1. Определены возрастные интервалы и кинематические обстановки главных фаз структурной перестройки рассмотренного сегмента Тянь-Шаня на альпийском этапе тектогенеза. 2. Показано, что на территории Алайского хребта наиболее значимая деформация и альпийская активизация структур палеозойского фундамента произошли на рубеже неогена и квартера. Заключение. Получены аргументы в пользу того, что на современном этапе район исследований представляет собой относительно единый монолитный блок, не испытывающий существенной деформации, связанной с надвиганием с юга верхнекоровых комплексов Северного Памира.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>Research subject</title><p>Research subject. A series of research studies was conducted in the Alai Range area, at the junction of the folded Tien Shan and Pamir provinces with the purpose of investigating the morphological structure of alpine deformations in the Paleozoic basement and Mesozoic–Cenozoic sediment cover.</p></sec><sec><title>Materials and Methods</title><p>Materials and Methods. Structural and geological observations were carried out in the Alai and Kichi-Karakol inter-mountain depressions and their mountainous surroundings. These investigations included an analysis of the morphology and orientation of the deformation structures of the sedimentary cover and structural inconsistencies based on detailed geological mapping; measurements of the orientations of tectonic slickenlines and slickensides in the zones of active faults; processing the entire complex of data in terms of kinematic strain indicators using proven methods and calculation programs in order to determine the main parameters of the stress-strain state of the upper crustal rock complexes.</p></sec><sec><title>Results</title><p>Results. The age intervals and kinematic conditions of the main phases of structural transformation of the Southern Tien Shan at the Alpine stage of tectogenesis were determined based new structural and geological data, as well as materials published in previous works. It was demonstrated that, in the territory of Alai, the most significant deformations and activation of the Paleozoic basement faults occurred at the Neogene-Quarter boundary.</p></sec><sec><title>Conclusions</title><p> Conclusions. At the present stage, the area under study constitutes a relatively stable block, which does not experience significant deformations associated with the encroachment of the upper crustal rock complexes of the Northern Pamir from the south.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>Тянь-Шань</kwd><kwd>фундамент</kwd><kwd>осадочный чехол</kwd><kwd>Алайская впадина</kwd><kwd>Кичи-Каракольская впадина</kwd><kwd>напряженно-деформированонное состояние</kwd><kwd>кайнозой</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Tien Shan</kwd><kwd>basement</kwd><kwd>cover</kwd><kwd>Alai depression</kwd><kwd>Kichi-Karakol depression</kwd><kwd>deformations</kwd><kwd>stress-strain state</kwd><kwd>Cenozoic</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">Баженов М.Л., Миколайчук А.В. 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