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<article 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" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Geotectonics</journal-id><journal-title-group><journal-title xml:lang="en">Geotectonics</journal-title><trans-title-group xml:lang="ru"><trans-title>Геотектоника</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0016-853X</issn><issn publication-format="electronic">3034-4972</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">660394</article-id><article-id pub-id-type="doi">10.31857/S0016853X24030023</article-id><article-id pub-id-type="edn">FGNTZW</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Geological position of the Junggar terrane (Southern Kazakhstan) in the structure of Rodinia supercontinent: results of research of the late-precambrian metasedimentary complexes</article-title><trans-title-group xml:lang="ru"><trans-title>Положение Джунгарского террейна (Южный Казахстан) в структуре супреконтинента Родиния; результаты изучения позднекембрийских метаосадочных комплексов</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Kanygina</surname><given-names>N. A.</given-names></name><name xml:lang="ru"><surname>Каныгина</surname><given-names>Н. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Tretyakov</surname><given-names>A. A.</given-names></name><name xml:lang="ru"><surname>Третьяков</surname><given-names>А. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Degtyarev</surname><given-names>K. E.</given-names></name><name xml:lang="ru"><surname>Дегтярев</surname><given-names>К. Е.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Dubenskiy</surname><given-names>A. S.</given-names></name><name xml:lang="ru"><surname>Дубенский</surname><given-names>А. С.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Erofeeva</surname><given-names>K. G.</given-names></name><name xml:lang="ru"><surname>Ерофеева</surname><given-names>К. Г.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Sheshukov</surname><given-names>V. S.</given-names></name><name xml:lang="ru"><surname>Шешуков</surname><given-names>В. С.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Chervyakovskiy</surname><given-names>V. S.</given-names></name><name xml:lang="ru"><surname>Червяковский</surname><given-names>В. С.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff2"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Chervyakovskaya</surname><given-names>M. V.</given-names></name><name xml:lang="ru"><surname>Червяковская</surname><given-names>М. В.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>kanygina.nadia@gmail.com</email><xref ref-type="aff" rid="aff2"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Geological Institute, Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Геологический институт РАН</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">A.N. Zavaritsky Institute of Geology and Geochemistry, Urals Branch of the Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Институт геологии и геохимии им. академика А.Н. Заварицкого УрО РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2024-06-15" publication-format="electronic"><day>15</day><month>06</month><year>2024</year></pub-date><issue>3</issue><fpage>30</fpage><lpage>54</lpage><history><date date-type="received" iso-8601-date="2025-02-22"><day>22</day><month>02</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2024, Russian Academy of Sciences</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2024, Российская академия наук</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="en">Russian Academy of Sciences</copyright-holder><copyright-holder xml:lang="ru">Российская академия наук</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/0016-853X/article/view/660394">https://journals.eco-vector.com/0016-853X/article/view/660394</self-uri><abstract xml:lang="en"><p>The results of studying of the Precambrian metasedimentary sequences of the Junggar terrane located in South Kazakhstan are given in the article. In the structure of the Junggar terrane, we studied the rocks of the Sarychebyn group and Kosagash formation. Petrogeochemical data combined with the results of U‒Pb and Lu‒Hf isotope-geochronological studies of the detrital zircons showed that the Sarychebyn Group and the Kosagash formation represent a similar stratigraphic level that accumulation occurred in the Late Mesoproterozoic to Early Neoproterozoic (~1026‒~920 Ma). The main sources of the detrital zircon age populations were the Mesoproterozoic and Paleoproterozoic complexes. Among these complexes can be identified metabasites and metapelites of intermediate and high metamorphic grades, as well as felsic igneous rocks formed with the participation of various sources, can be distinguished. The Junggar terrane exhibits a close tectonic affinity with the Aktau-Mointy, Yili, Issyk-Kul, Chinese Central Tien-Shan, and the Northern Kazakhstan terranes in the Late Precambrian. They were probably located near the Sveconorwegian orogen in the western Baltica within the Rodinia supercontinent structure.</p></abstract><trans-abstract xml:lang="ru"><p>В статье представлены результаты изучения докембрийских метаосадочных комплексов Джунгарского террейна, расположенного в пределах Южного Казахстана. В структуре Джунгарского террейна нами были изучены породы сарычабынской серии и косагашской свиты. Петрогеохимические данные в сочетании с полученными результатами U–Pb и Lu–Hf изотопно-геохронологического узучения обломочных цирконов показали, что породы сарычабынской серии и косагашской свиты представляют собой единый стратиграфический уровень, накопление которого происходило в конце мезопротерозоя‒начале неопротерозоя (~1026–920 млн лет). Основными источниками сноса для данных толщ являлись комплексы мезопротерозойского и палеопротерозойского возраста. Среди источников сноса можно выделить метабазиты и метапелиты умеренных и высоких ступеней метаморфизма, а также кислые магматические породы, сформированные при участии различных источников. Позднедокембрийская история развития Джунгарского террейна имеет сходство с тектоно-магматической эволюцией Актау-Моинтинского, Илийского, Иссыккульского, Китайского Центрального Тянь-Шаня террейнов, а также террейнов Северного Казахстана. В это время террейны представляли собой единый континентальный блок, который располагался вблизи Свеконорвежского орогена на западе палеоконтинента Балтики при образовании суперконтинента Родиния.</p></trans-abstract><kwd-group xml:lang="en"><kwd>Junggar terrane</kwd><kwd>paleoreconstruction</kwd><kwd>Rodinia supercontinent</kwd><kwd>Neoproterozoic</kwd><kwd>provenance</kwd><kwd>detrital zircons</kwd><kwd>U–Pb dating</kwd><kwd>Lu–Hf isotopes</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>Джунгарский террейн</kwd><kwd>палеореконструкция</kwd><kwd>суперконтинент Родиния</kwd><kwd>неопротерозой</kwd><kwd>источники сноса</kwd><kwd>обломочные цирконы</kwd><kwd>U–Pb-датирование</kwd><kwd>Lu–Hf изотопия</kwd></kwd-group><funding-group><award-group><funding-source><institution-wrap><institution xml:lang="ru">Российский научный фонд</institution></institution-wrap><institution-wrap><institution xml:lang="en">Russian Science Foundation</institution></institution-wrap></funding-source><award-id>22-77-00082</award-id></award-group></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Алексеев Д.В., Дегтярев К.Е., Третьяков А.А., Каныгина Н.А. Ранненеопротерозойские (~920 млн лет) гранито-гнейсы Джунгарского Алатау, южный Казахстан: обоснование возраста по результатам U–Th–Pb (SIMS)-датирования // ДАН. 2021. Т. 496. № 1. С. 17–21.</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>Алексеев Д.В., Худолей A.К., Дюфрейн С.Э. Палеопротерозойские и неопротерозойские кварциты Киргизского Северного Тянь-Шаня: обоснование возраста по результатам датирования обломочных цирконов // ДАН. Науки о Земле. 2020. T. 491. № 2. С. 5‒9.</mixed-citation></ref><ref id="B3"><label>3.</label><mixed-citation>Барчан Г.Н., Дубровский А.Г., Керн К.В. и др. Геологическая карта Текелийского рудного района. ‒ М-б 1 : 50 000. ‒ Объяснительная записка. ‒ М.: Мингео СССР, 1985. 180 с.</mixed-citation></ref><ref id="B4"><label>4.</label><mixed-citation>Беспалов В.Ф., Костенко Н.Н. Геологическая карта Казахской ССР. ‒ М-б 1 : 500 000. ‒ Южно-Казахстанская серия. ‒ Объяснительная записка. ‒ Алма-Ата: Мингео СССР, 1981. 248 с.</mixed-citation></ref><ref id="B5"><label>5.</label><mixed-citation>Гвоздик Н.И. Некоторые результаты литологического изучения протерозойских сланцево-кварцитовых толщ Актау-Моинтинского антиклинория. ‒ Кн.1. ‒ Проблемы геологии Центрального Казахстана. ‒ Под ред. Ю.А. Зайцева ‒ М.: МГУ, 1980. С. 41‒55.</mixed-citation></ref><ref id="B6"><label>6.</label><mixed-citation>Геология Северного Казахстана. ‒ Под ред. М.А. Абдулкабирова ‒ Алма-Ата: Наука, 1987. 224 с.</mixed-citation></ref><ref id="B7"><label>7.</label><mixed-citation>Дегтярев К.Е., Ковач В.П., Третьяков А.А., Котов А.Б., Ван K.-Л. Возраст и источники докембрийских циркон-рутиловых россыпей Кокчетавского сиалического массива (Северный Казахстан) // ДАН. 2015. Т. 464. № 5. С. 584–588.</mixed-citation></ref><ref id="B8"><label>8.</label><mixed-citation>Дегтярев К.Е. Положение Актау-Джунгарского микроконтинента в структуре палеозоид Центрального Казахстана // Геотектоника. 2003. № 4. С. 14–34.</mixed-citation></ref><ref id="B9"><label>9.</label><mixed-citation>Дегтярев К.Е., Шатагин К.Н., Кузнецов Н.Б., Астраханцев О.В. Палеогеография позднего докембрия–раннего палеозоя Северной Евразии. ‒ Под ред. … ‒ Екатеринбург: Изд-во, 1998. С. 159–166.</mixed-citation></ref><ref id="B10"><label>10.</label><mixed-citation>Каныгина Н.А., Третьяков А.А., Дегтярев К.Е., Пан К.-Н., Ван K.-Л., Ли Х.-Ян, Плоткина Ю. В. Первые результаты U–Pb-изучения обломочных цирконов из докембрийских кварцито-сланцевых толщ Чуйского блока (южный Казахстан) // ДАН. 2019. Т. 489. № 1. С. 52–56.</mixed-citation></ref><ref id="B11"><label>11.</label><mixed-citation>Каныгина Н.А., Третьяков А.А., Дегтярев К.Е., Ковач В.П., Плоткина Ю.В., Pang K.-N., Wang K.-L., Lee H.-Y. Кварцито-сланцевые толщи Актау-Моинтинского массива (Центральный Казахстан): структурное положение, источники сноса, основные этапы формирования континентальной коры в докембрии // Геотектоника. 2020. № 2. С. 75–93.</mixed-citation></ref><ref id="B12"><label>12.</label><mixed-citation>Козаков И.К. Ранний докембрий Центрально-Азиатского складчатого пояса. ‒ Под ред. И.К. Козакова. ‒ СПб.: Наука, 1993. 270 с.</mixed-citation></ref><ref id="B13"><label>13.</label><mixed-citation>Лыдка К., Филатова Л.И. Главные черты литостратиграфии кокчетавской серии протерозоя Кокчетавского массива // Литология и полезные ископаемые. 1982. № 4. С. 130–136.</mixed-citation></ref><ref id="B14"><label>14.</label><mixed-citation>Моссаковский А.А., Руженцев С.В. Самыгин С.Г., Хераскова Т.Н. Центрально-Азиатский складчатый пояс: геодинамическая эволюция и история формирования// Геотектоника. 1993. Т. 1. № 6. С. 3‒32.</mixed-citation></ref><ref id="B15"><label>15.</label><mixed-citation>Никитин И.Ф., Цай Д.Т., Шлыгин А.Е. Рудовмещающие толщи Коксу-Текелийского рудного района // Отечественная геология 1993. № 3. С. 33–41.</mixed-citation></ref><ref id="B16"><label>16.</label><mixed-citation>Никитченко И.И. Стратиграфия докембрия и нижнего палеозоя Джунгарского Алатау // Изв. АН КазССР. Сер. геол. 1978. № 5. С. 1‒14.</mixed-citation></ref><ref id="B17"><label>17.</label><mixed-citation>Попов Н.В., Добрецов Г.Л. Петрология полихронных плутонов (на примере Джунгарского Алатау). ‒ Под ред. Э.П. Изоха. ‒ Новосибирск: Наука, 1982. 133 с.</mixed-citation></ref><ref id="B18"><label>18.</label><mixed-citation>Спиридонов Э.М. О толщах кварцитов среднего и верхнего рифея Северного Казахстана // Бюлл. МОИП. Отд. геол. 1987. Т. 62. В. 2. С. 71–77.</mixed-citation></ref><ref id="B19"><label>19.</label><mixed-citation>Тейлор С.Р., МакЛеннан С.М. Континентальная кора и ее состав и эволюция. ‒ Под ред. Л.С. Бородина. ‒ М.: Мир, 1988. 379 с.</mixed-citation></ref><ref id="B20"><label>20.</label><mixed-citation>Третьяков А.А., Дегтярев К.Е., Каныгина Н.А., Летникова Е.Ф., Журавлев А.Н., Третьякова К.А. Эволюция Улутауского террейна (Центральный Казахстан) в палеопротерозое–эдиакарии. ‒ В кн.: Геодинамическая эволюция литосферы Центрально-Азиатского подвижного пояса (от океана к континенту). ‒ Мат-лы науч. конф., Иркутск (17–20 октября 2023 года) – Иркутск: ИЗК СО РАН, 2023. С. 252‒254.</mixed-citation></ref><ref id="B21"><label>21.</label><mixed-citation>Третьяков А.А., Дегтярев К.Е., Котов А.Б., Сальникова Е.Б., Шатагин К.Н., Яковлева С.З., Анисимова И.В., Плоткина Ю.В. Среднерифейский гнейсограниты Кокчетавского массива (Северный Казахстан): структурное положение и обоснование возраста // ДАН. 2011b. Т. 440. № 4. С. 511–515.</mixed-citation></ref><ref id="B22"><label>22.</label><mixed-citation>Третьяков А.А., Дегтярев К.Е., Сальникова Е.Б., Шатагин К.Н., Котов А.Б., Рязанцев А.В., Пилицына А.В., Яковлева С.З., Толмачева Е.В, Плоткина Ю.В. Палеопротерозойские анорогенные гранитоиды Жельтавского сиалического массива (Южный Казахстан): структурное положение и обоснование возраста // ДАН. 2016. Т. 466. № 2. С. 196–201.</mixed-citation></ref><ref id="B23"><label>23.</label><mixed-citation>Третьяков А.А., Дегтярев К.Е., Шатагин К.Н., Котов А.Б., Сальникова Е.Б., Анисимова И.В. Неопротерозойская анорогенная риолит-гранитная вулкано-плутоническая ассоциация Актау-Моинтинского массива (Центральный Казахстан): возраст, источники и палеотектоническая позиция // Петрология. 2015. Т. 23. № 1. С. 26–49.</mixed-citation></ref><ref id="B24"><label>24.</label><mixed-citation>Третьяков А.А., Котов А.Б., Дегтярев К.Е., Сальникова Е.Б., Шатагин К.Н., Яковлева С.З., Анисимова И.В. Среднерифейский вулканогенный комплекс Кокчетавского массива (Северный Казахстан): структурное положение и обоснование возраста // ДАН. 2011а. Т. 438. № 5. С. 644–648.</mixed-citation></ref><ref id="B25"><label>25.</label><mixed-citation>Туркина О.М., Летников Ф.А., Левин А.В. Мезопротерозойские гранитоиды фундамента Кокчетавского микроконтинента // ДАН. 2011. Т. 436. № 4. С. 499–503.</mixed-citation></ref><ref id="B26"><label>26.</label><mixed-citation>Филатова Л.И. Стратиграфия и историко-геологический анализ метаморфических толщ докембрия Центрального Казахстана. М.: Недра, 1983. 160 с.</mixed-citation></ref><ref id="B27"><label>27.</label><mixed-citation>Филатова Л.И., Гвоздик Н.И., Зубаткина Г.М. К стратиграфии протерозоя Центрального Казахстана. ‒ В кн.: Геология и полезные ископаемые Центрального Казахстана. ‒ Под ред. Е.Е. Милановского. ‒ М.: Наука, 1988. С. 15–29.</mixed-citation></ref><ref id="B28"><label>28.</label><mixed-citation>Червяковская М.В., Вотяков С.Л., Червяковский В.С. Изучение Lu/Hf изотопного состава цирконов с помощью многоколлекторного масс-спектрометра с индуктивно-связанной плазмой Neptune Plus и приставки для лазерной абляции NWR 213 // Аналитика и контроль. 2021. Т. 25. № 3. С. 212‒221.</mixed-citation></ref><ref id="B29"><label>29.</label><mixed-citation>Геология Чу-Илийского региона. ‒ Под ред. А. А. Абдулина ‒ Алма-Ата: Наука, 1980. 504 с.</mixed-citation></ref><ref id="B30"><label>30.</label><mixed-citation>Ярмолюк В.В., Дегтярев К.Е. Докембрийские террейны Центрально-Азиатского орогенного пояса: сравнительная характеристика, типизация и особенности тектонической эволюции // Геотектоника. 2019. № 1. С. 3‒43.</mixed-citation></ref><ref id="B31"><label>31.</label><mixed-citation>Alexeiev D.V., Ryazantsev A.V., Kröner A., Tretyakov A.A., Xia, X., Liu, D.Y. Geochemical data and zircon ages for rocks in a high-pressure belt of Chu-Yili Mountains, southern Kazakhstan: Implications for the earliest stages of accretion in Kazakhstan and the Tianshan // J. Asian Earth Sci. 2011. V. 42. P. 805–820.</mixed-citation></ref><ref id="B32"><label>32.</label><mixed-citation>Bingen B., Nordgulen Ø., Sigmond E.M.O., Tucker R.D., Mansfeld J., Högdahl K. Relations between 1.19‒1.13 Ga continental magmatism, sedimentation and metamorphism, Sveconorwegian province, South Norway // Precambrian Research. 2003. V. 124. P. 215‒241.</mixed-citation></ref><ref id="B33"><label>33.</label><mixed-citation>Bingen B., Skår Ø., Marker M., Sigmond E.M.O., Nordgulen Ø., Raganhildstveit J., Mansfeld J., Tucker R.D., Liégeois J.-P. Timing of continental building in the Sveconorwegian orogen, SW Scandinavia // Norw. J. Geol. 2005. V. 85. P. 87–116.</mixed-citation></ref><ref id="B34"><label>34.</label><mixed-citation>Blichert-Toft J., Albarиde F. The Lu–Hf isotope geochemistry of chondrites and the evolution of the mantle–crust system // Earth and Planet. Sci. Lett. 1997. V. 148. P. 243–258.</mixed-citation></ref><ref id="B35"><label>35.</label><mixed-citation>Boynton W.V. Geochemistry of the rare earth elements: Meteorite studies. In: Rare Earth Element Geochemistry. ‒ Ed. by P. Henderson, (Elsevier, NY, USA. 1984), P. 63‒114.</mixed-citation></ref><ref id="B36"><label>36.</label><mixed-citation>Cawood P.A., Strachan R.A., Pisarevsky S.A., Gladkochub D.P., Murphy J. B. Linking collisional and accretionary orogens during Rodinia assembly and breakup: Implications for models of supercontinent cycles // Earth and Planet. Sci. Lett. 2016. V. 449. P. 118–126.</mixed-citation></ref><ref id="B37"><label>37.</label><mixed-citation>Cawood P.A., Pisarevsky S.A. Laurentia-Baltica-Amazonia relations during Rodinia assembly // Precambrian Research. 2017. V. 292. P. 386–397.</mixed-citation></ref><ref id="B38"><label>38.</label><mixed-citation>Cawood P.A., Strachan R., Cutts K., Kinny P.D., Hand M., Pisarevsky S. Neoproterozoic orogeny along the margin of Rodinia: Valhalla orogen, North Atlantic // Geology. 2010. V. 38. P. 99–102.</mixed-citation></ref><ref id="B39"><label>39.</label><mixed-citation>Cawood P.A., Strachan R.A., Merle R.E., Millar I.L., Loewy S.L., Dalziel I.W.D., Kinny P.D., Jourdan F., Nemchin A.A., Connelly J.N. Neoproterozoic to early Paleozoic extensional and compressional history of East Laurentian margin sequences: The Moine supergroup, Scottish Caledonides // GSA. Bull. 2015. V. 127. P. 349–371.</mixed-citation></ref><ref id="B40"><label>40.</label><mixed-citation>Cawood P.A., Strachan R.A., Pisarevsky S.A., Gladkochub D.P., Murphy J.B. Linking collisional and accretionary orogens during Rodinia assembly and breakup: Implications for models of supercontinent cycles // Earth Planet. Sci. Lett. 2016. V. 449. P. 118–126.</mixed-citation></ref><ref id="B41"><label>41.</label><mixed-citation>Cawood P.A., Wang Y., Xu Y., Zhao G. Locating South China in Rodinia and Gondwana: a fragment of greater India lithosphere? // Geology. 2013. V. 41. P. 903–906.</mixed-citation></ref><ref id="B42"><label>42.</label><mixed-citation>Condie K.C. Chemical composition and evolution of the upper continental crust: Contrasting results from surface samples and shales // Chem. Geol. 1993. V. 104. P. 1‒37.</mixed-citation></ref><ref id="B43"><label>43.</label><mixed-citation>Cullers R.L. The chemical signature of source rocks in size fractions of Holocene stream sediment derived from metamorphic rocks in the Wet Mountains region, Colorado, USA // Chem. Geol. 1994. V. 113. P. 327–343.</mixed-citation></ref><ref id="B44"><label>44.</label><mixed-citation>Cullers R.L. The geochemistry of shales, siltstones, and sandstones of Pennsylvanian‒Permian age, Colorado, USA: Implications for provenance and metamorphic studies // Lithos. 2000. V. 51. P. 181–203.</mixed-citation></ref><ref id="B45"><label>45.</label><mixed-citation>Degtyarev K., Yakubchuk A., Tretyakov A., Kotov A., Kovach V. Precambrian geology of the Kazakh Uplands and Tien Shan: An overview // Gondwana Research. 2017. V. 47. P. 44–75.</mixed-citation></ref><ref id="B46"><label>46.</label><mixed-citation>Gao J., Wang X.-S., Klemd R., Jiang T., Qian Q., Mu L.-X., Ma Y.-Z. Record of assembly and breakup of Rodinia in the southwestern Altaids: Evidence from Neoproterozoic magmatism in the Chinese Western Tianshan orogen // J. Asian Earth Sci. 2015. V. 113. P. 173–193.</mixed-citation></ref><ref id="B47"><label>47.</label><mixed-citation>Gehrels G. Introduction to detrital zircon studies of Paleozoic and Triassic strata in Western Nevada and Northern California // GSA. Spec. Pap. 2000. V. 347. P. 1–17.</mixed-citation></ref><ref id="B48"><label>48.</label><mixed-citation>Gehrels G.E. Detrital zircon U‒Pb geochronology: Current methods and new opportunities. ‒ In: Tectonics of Sedimentary Basins: Recent Advances. ‒ Ed. by C. Busby, A. Azor, (Wiley-Blackwell, Chichester, UK. 2012). P. 47–62.</mixed-citation></ref><ref id="B49"><label>49.</label><mixed-citation>Glorie S., Zhimulev F.I., Buslov M.M., Andersen T., Plavsa D., Izmer A., Vanhaecke F., De Grave J. Formation of the Kokchetav subduction‒collision zone (Northern Kazakhstan): Insights from zircon U‒Pb and Lu‒Hf isotope systematics // Gondwana Research. 2015. V. 27. P. 424-438.</mixed-citation></ref><ref id="B50"><label>50.</label><mixed-citation>Griffin W.L., Wang X., Jackson S.E., Pearson N.J., O′Reilly S.Y., Xu X., Zhou X. Zircon chemistry and magma mixing, SE China: In-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes // Lithos. 2002. V. 61. P. 237–269.</mixed-citation></ref><ref id="B51"><label>51.</label><mixed-citation>He J., Zhu W., Zheng B., Wu H., Cui X., Lu Y. Neoproterozoic diamictite-bearing sedimentary rocks in the northern Yili Block and their constraints on the Precambrian evolution of microcontinents in the western Central Asian Orogenic Belt // Tectophysics. 2015b. V. 665. P. 23–36.</mixed-citation></ref><ref id="B52"><label>52.</label><mixed-citation>He J.W., Zhu W.B., Ge R.F. New age constraints on Neoproterozoic diamicites in Kuruktag, NW China and Precambrian crustal evolution of the Tarim Craton // Precambrian Research. 2014a. V. 241. P. 44–60.</mixed-citation></ref><ref id="B53"><label>53.</label><mixed-citation>He J.W., Zhu W.B., Ge R.F., Zheng B.H., Wu H.L. Detrital zircon U–Pb ages and Hf isotopes of Neoproterozoic strata in the Aksu area, northwestern Tarim Craton: implications for supercontinent reconstruction and crustal evolution // Precambrian Research. 2014b. V. 254. P. 194–209.</mixed-citation></ref><ref id="B54"><label>54.</label><mixed-citation>Herron M.M. Geochemical classification of terrigenous sands and shales from core or log data // J. Sediment. Petrol. 1988. V. 58. P. 820–829.</mixed-citation></ref><ref id="B55"><label>55.</label><mixed-citation>Hoskin P.W.O., Schaltegger U. The composition of zircon and igneous and metamorphic petrogenesis // Rev. Mineral. Geochem. 2003. V. 53. P. 27–62.</mixed-citation></ref><ref id="B56"><label>56.</label><mixed-citation>Hu A.Q., Wei G.J., Jahn B.M., Zhang J.B., Deng W.F., Chen L.L. Formation of the 0.9 Ga Neoproterozoic granitoids in the Tianshan Orogen, NW China: constraints from the SHRIMP zircon age determination and its tectonic significance // Geochimica. 2010. V. 39. № 3. Р. 197–212 (in Chinese with English abstract).</mixed-citation></ref><ref id="B57"><label>57.</label><mixed-citation>Huang B.T., He Z.Y., Zhang Z.M., Klemd R., Zong K.Q., Zhao Z.D. Early Neoproterozoic granitic gneisses in the Chinese Eastern Tianshan: Petrogenesis and tectonic implications // J. Asian Earth Sci. 2015a. V. 113. № 1. P. 339–352.</mixed-citation></ref><ref id="B58"><label>58.</label><mixed-citation>Huang H., Cawood P.A., Hou M.C., Xiong F.H., Ni S.J., Gong T.T. Provenance of latest Mesoproterozoic to early Neoproterozoic (meta)-sedimentary rocks and implications for paleographic reconstruction of the Yili Block // Gondwana Research. 2019. V. 72. P. 120–138.</mixed-citation></ref><ref id="B59"><label>59.</label><mixed-citation>Huang Z., Long X., Kröner A., Yuan C., Wang Y., Chen B., Zhang Y. Neoproterozoic granitic gneisses in the Chinese Central Tianshan block: Implications for tectonic affinity and Precambrian crustal evolution // Precambrian Research. 2015b. V. 269. P. 73–89.</mixed-citation></ref><ref id="B60"><label>60.</label><mixed-citation>Huang Z., Long X., Yuan C., Sun M., Wang Y., Zhang Y., Chen B. Detrital zircons from Neoproterozoic sedimentary rocks in the Yili block: Constraints on the affinity of microcontinents in the southern Central Asian orogenic belt // Gondwana Research. 2016. V. 37. P. 39–52.</mixed-citation></ref><ref id="B61"><label>61.</label><mixed-citation>Huang Z., Yuan C., Long X., Zhang Y., Du L. From breakup of Nuna to assembly of Rodinia: A link between the Chinese Central Tianshan block and Fennoscandia // Tectonics. 2019. V. 38. P. 4378–4398.</mixed-citation></ref><ref id="B62"><label>62.</label><mixed-citation>Kanygina N., Tretyakov A., Alexeiev D., Degtyarev K., Skoblenko A., Soloshenko N., Ermolaev B. Early Neoproterozoic granite-gneisses of the Junggar Alatau (Southeastern Kazakhstan): Age, petrogenesis and tectonic implications // Acta Geologica Sinica. 2024. V. 98. № 1. P. 67–82.</mixed-citation></ref><ref id="B63"><label>63.</label><mixed-citation>Kanygina N., Tretyakov A., Degtyarev K., Kovach V., Skuzovatov S., Pang K.-N., Wang K.-L., Lee H.-Y. Late Mesoproterozoic–early Neoproterozoic quartzite–schist sequences of the Aktau–Mointy terrane (Central Kazakhstan): Provenance, crustal evolution, and implications for paleotectonic reconstruction // Precambrian Research. 2021. V. 354. Art. 106040.</mixed-citation></ref><ref id="B64"><label>64.</label><mixed-citation>Kelemen P.B., Hanghøj K., Greene A.R. One view on the geochemistry of subduction-related magmatic arcs, with an emphasis of primitive andesite and lower crust // Treat. Geochem. 2014. P. 749–806.</mixed-citation></ref><ref id="B65"><label>65.</label><mixed-citation>Kovach V., Degtyarev K., Tretyakov A., Kotov A., Tolmacheva E.,Wang K.-L., Chung S.-L., Lee H.-Y., Jahn B.-M. Sources and provenance of the Neoproterozoic placer deposits of the Northern Kazakhstan: Implication for continental growth of the western Central Asian orogenic belt // Gondwana Research. 2017. V. 47. P. 28–43.</mixed-citation></ref><ref id="B66"><label>66.</label><mixed-citation>Kröner A., Alexeiev D.V., Hegner E., Rojas-Agramonte Y., Corsini M., ChaoY., Wong J., Windley B.F., Liu D., Tretyakov A.A. Zircon and muscovite ages, geochemistry and Nd‒Hf isotopes for the Aktyuz metamorphic terrane: evidence for an Early Ordovician collision belt in the northern Tianshan of Kyrgyzstan // Gondwana Research. 2012. V. 21. P. 901–927.</mixed-citation></ref><ref id="B67"><label>67.</label><mixed-citation>Kröner A., Alexeiev D.V., Kovach V.P., Rojas-Agramonte Y., Tretyakov A.A., Mikolaichuk A.V., Xie H., So- bel E.R. Zircon ages, geochemistry and Nd isotopic systematics for the Palaeoproterozoic 2.3 to 1.8 Ga Kuilyu complex, East Kyrgyzstan – the oldest continental basement fragment in the Tianshan orogenic belt // J. Asian Earth Sci. 2017. V. 135. P. 122–135.</mixed-citation></ref><ref id="B68"><label>68.</label><mixed-citation>Kröner A., Alexeiev D.V., Rojas-Agramonte Y. Hegner E., Wong J., Xia X., Belousova E., Mikolaichuk A.V., Seltmann R., Liu D., Kiselev V.V. Mesoproterozoic (Grenville age) terranes in the Kyrgyz North Tianshan: Zircon ages and Nd‒Hf isotopic constraints on the origin and evolution of basement blocks in the southern Central Asian orogen // Gondwana Research. 2013. V. 23. P. 272–295.</mixed-citation></ref><ref id="B69"><label>69.</label><mixed-citation>Kröner A., Windley B.F., Badarch G., Tomurtogoo O., Hegner E., Jahn B.M., Gruschka S., Khain E.V., Demoux A., Wingate M.T.D. Accretionary growth and crust formation in the Central Asia orogenic belt and comparison with the Arabian‒Nubian shield // GSA Bull. 2007. V. 200. P. 1–29.</mixed-citation></ref><ref id="B70"><label>70.</label><mixed-citation>Liu C., Zhao G., Liu F., Shi J. Detrital zircon U‒Pb and Hf isotopic and whole-rock geochemical study of the Bayan Obo group, northern margin of the North China craton: Implications for Rodinia reconstruction // Precambrian Research. 2017. V. 303. P. 372–391.</mixed-citation></ref><ref id="B71"><label>71.</label><mixed-citation>Liu H.S., Wang B., Shu L.S., Jahn B.M., Lizuka Y., Chen Y. Detrital zircon ages of Proterozoic meta-sedimentary rocks and Paleozoic sedimentary cover of the northern Yili block: Implications for the tectonics of microcontinents in the Central Asian orogenic belt // Precambrian Research. 2014. V. 252. P. 209–222.</mixed-citation></ref><ref id="B72"><label>72.</label><mixed-citation>Ludwig K.R. Isoplot v. 4.15. Geochronological Toolkit for Microsoft Excel // Berkeley Geochron. Center. Spec. Publ. 2008. V. 4. P. 76.</mixed-citation></ref><ref id="B73"><label>73.</label><mixed-citation>McLennan S.M., Hemming S.R., McDaniel D.K., Hanson G.N. Geochemical approaches to sedimentation, provenance, and tectonics. ‒ In: Processes Controlling the Composition of Clastic Sediments. ‒ Ed. by M.J. Johnson, A. Basu, (GSA Spec. Pap. 1993. V. 284), P. 21–40.</mixed-citation></ref><ref id="B74"><label>74.</label><mixed-citation>Meinhold G. Rutile and its application in Earth sciences // Earth Sci. Rev. 2010. V. 102. P. 1‒28.</mixed-citation></ref><ref id="B75"><label>75.</label><mixed-citation>Nesbitt H.W., Young G.M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites // Nature. 1982. V. 299. P. 715‒717.</mixed-citation></ref><ref id="B76"><label>76.</label><mixed-citation>Rogers J.W., Santosh M. Configuration of Columbia, a Mesoproterozoic Supercontinent // Gondwana Research. 2002. V. 5. No. 1. P. 5‒22.</mixed-citation></ref><ref id="B77"><label>77.</label><mixed-citation>Sengör A.M.C., Natal′In B.A., Burtman V.S. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia // Nature. 1993. V. 364. P. 299‒307.</mixed-citation></ref><ref id="B78"><label>78.</label><mixed-citation>Sheshukov V.S., Kuzmichev A.B., Dubenskiy A.S., Okina O.I., Degtyarev K.E., Kanygina N.A., Kuznetsov N.B., Romanjuk T.V., Lyapunov S.M. U‒Pb zircon dating by LA-SF-ICPMS at Geological Institute GIN RAS (Moscow). ‒ Proc. 10th Int. conference “Analysis of Geological and Environmental Materials,” (Sydney, Australia. 2018. Abstr.), p. 63.</mixed-citation></ref><ref id="B79"><label>79.</label><mixed-citation>Sun S.S., McDonough W.F. Chemical and isotopic systematic of oceanic basalts: Implications for mantle composition and processes. ‒ In: Magmatism in the Ocean Basins. ‒ Ed.by A.D. Saunders, M.J. Norry, (Geol. Soc. London. Spec. Publ. 1989. V. 42), P. 313–345.</mixed-citation></ref><ref id="B80"><label>80.</label><mixed-citation>Taylor S.R., McLennan S.M. The Continental Crust: Its Composition and Evolution. ‒ (Blackwell, Oxford, UK. 1985), 312 p.</mixed-citation></ref><ref id="B81"><label>81.</label><mixed-citation>Tomkins H.S., Powell R., Ellis D.J. The pressure dependence of the zirconium-in-rutile thermometer // J. Metamorph. Geol. 2007. V. 25. P. 703–713.</mixed-citation></ref><ref id="B82"><label>82.</label><mixed-citation>Triebold S., von Eynatten H., Zack T. A recipe for the use of rutile in sedimentary provenance analysis // Sedimentary Geology. 2012. V. 282. P. 268–275.</mixed-citation></ref><ref id="B83"><label>83.</label><mixed-citation>Van Achterbergh E., Ryan C.G., Jackson S.E., Griffin W.L. LA-ICP-MS in the Earth sciences – appendix 3, data reduction software for LA-ICP-MS. ‒ In: Short Course Mineralogical Assoc. ‒ Ed.by PJ. Sylvester, (St. John′s Publ., Ottawa, Canada, 2001. V. 29), P. 239–243.</mixed-citation></ref><ref id="B84"><label>84.</label><mixed-citation>Vermeesch P. Isoplot R: A free and open toolbox for geochronology // Geosci. Frontiers. 2018. V. 9. P. 1479–1493.</mixed-citation></ref><ref id="B85"><label>85.</label><mixed-citation>Wang L.X., Huang H., Hou M.C., Kneller B., Xiong F. H., Luo H.W., Zhu S.X. Reconstruction of microcontinents during the assembly of Rodinia: A case study from the Central Tianshan block // Precambrian Research. 2024. V. 400. Art. 107270.</mixed-citation></ref><ref id="B86"><label>86.</label><mixed-citation>Wang B., Liu H., Shu L., Jahn B., Chung S., Zhai Y., Liu D. Early Neoproterozoic crustal evolution in northern Yili Block: Insights from migmatite, orthogneiss and leucogranite of the Wenquan metamorphic complex in the NW Chinese Tianshan // Precambrian Research. 2014a. V. 242. P. 58–81.</mixed-citation></ref><ref id="B87"><label>87.</label><mixed-citation>Wang B., Shu L., Liu H., Gong H., Ma Y., Mu L., Zhong L. First evidence for ca. 780 Ma intra-plate magmatism and its implications for Neoproterozoic rifting of the North Yili block and tectonic origin of the continental blocks in SW of Central Asia // Precambrian Research. 2014b. V. 254. P. 258–272.</mixed-citation></ref><ref id="B88"><label>88.</label><mixed-citation>Watson E. B., Wark D. A., Thomas J. B. Crystallization thermometers for zircon and rutile // Contrib. Mineral. Petrol. 2006. V. 151. P. 413–433.</mixed-citation></ref><ref id="B89"><label>89.</label><mixed-citation>Windley B.F., Alexeiev D., Xiao W., Kröner A., Badarch G. Tectonic models for accretion of the Central Asian orogenic belt // J. Geol. Soc. London. 2007. V. 164. P. 31–47.</mixed-citation></ref><ref id="B90"><label>90.</label><mixed-citation>Yang T.N., Li J.Y., Sun G.H., Wang Y.B. Mesoproterozoic continental arc type granite in the Central Tianshan Mountains: zircon SHRIMP U–Pb dating and geochemical analyses // Acta Geol. Sin. 2008. V. 82. P. 117–125.</mixed-citation></ref><ref id="B91"><label>91.</label><mixed-citation>Zack T., Moraes R., Kronz A. Temperature dependence of Zr in rutile: Empirical calibration of a rutile thermometer // Contrib. Mineral. Petrol. 2004a. V. 148. № 4. P. 471–488.</mixed-citation></ref><ref id="B92"><label>92.</label><mixed-citation>Zhao G. C., Cawood P. A., Wilde S. A., Sun M. Review of global 2.1–1.8 Ga orogens implications for a pre-Rodinia supercontinent // Earth Sci. Rev. 2002. V. 59. P. 125–162.</mixed-citation></ref><ref id="B93"><label>93.</label><mixed-citation>Zhao G. C., Sun M., Wilde S. A., Li S. Z. A Paleo-Mesoproterozoic supercontinent: Assembly, growth and breakup // Earth Sci. Rev. 2004. V. 67. № 1-2. P. 91–123.</mixed-citation></ref><ref id="B94"><label>94.</label><mixed-citation>Zheng B.H., Zhu W.B., Ge R., Wu H., He J., Lu Y. Proterozoic tectonic evolution of the Tarim craton: New insights from detrital zircon U‒Pb and Lu‒Hf isotopes of metasediments in the Kuruktag area // Precambrian Research. 2020. V. 346. Art. 105788.</mixed-citation></ref><ref id="B95"><label>95.</label><mixed-citation>Zhu W., Zheng B., Shu L., Ma D., Wu H., Li Y., Huang W., Yu J. Neoproterozoic tectonic evolution of the Precambrian Aksu blue-schist terrane, Northwestern Tarim, China: Insights from LA-ICP-MS zircon U–Pb ages and geochemical data // Precambrian Research. 2011. V. 185. P. 215–230</mixed-citation></ref><ref id="B96"><label>96.</label><mixed-citation>Zhu X., Wang B., Cluzel D., He Z., Zhou Y., Zhong L. Early Neoproterozoic gneissic granitoids in the southern Yili block (NW China): Constraints on microcontinent provenance and assembly in the SW Central Asian orogenic belt // Precambrian Research. 2019. V. 325. P. 111‒131.</mixed-citation></ref><ref id="B97"><label>97.</label><mixed-citation>Zhu X., Wang B., Sun Z., Liu J., He Z., Zhong L. Detrital zircon ages of the Mesoproterozoic metasedimentary rocks in the southern Yili block: Implications for tectonic affinities of the microcontinents in SW Central Asian orogenic belt // Precambrian Research. 2020. V. 350. Art. 105926.</mixed-citation></ref><ref id="B98"><label>98.</label><mixed-citation>Zonenshain L.P., Kuzmin M.I., Natapov L.M. Geology of the USSR: a plate-tectonic synthesis. ‒ In: Geology of the USSR. ‒ Ed.by B.M. Page, (AGU, Washington, DC, USA. 1990. V.21), 242 p.</mixed-citation></ref></ref-list></back></article>
