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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-2022-13-2s-0617</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1488</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>ВЫСОКОБАРИЧЕСКИЕ МЕТАМОРФИЧЕСКИЕ ПОРОДЫ ЧАРСКОГО ОФИОЛИТОВОГО ПОЯСА (ЦАСП): ВОЗРАСТ И ОБСТАНОВКИ ЭКСГУМАЦИИ ПОРОД</article-title><trans-title-group xml:lang="en"><trans-title>HIGH-PRESSURE METAMORPHIC ROCKS OF THE CHARA OPHIOLITE BELT (CAOB): AGE AND EXHUMATION CONDITIONS</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>Здрокова</surname><given-names>М. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Zdrokova</surname><given-names>M. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, 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>Владимиров</surname><given-names>В. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Vladimirov</surname><given-names>V. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3; 630090, Новосибирск, ул. Пирогова, 1</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090; 1 Pirogov St, 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>Травин</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Travin</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3; 630090, Новосибирск, ул. Пирогова, 1</p></bio><bio xml:lang="en"><p>3 Academician Koptyug Ave, Novosibirsk 630090; 1 Pirogov St, Novosibirsk 630090</p><p> </p></bio><xref ref-type="aff" rid="aff-2"/></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>Sobolev Institute of Geology and Mineralogy, 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 геологии и минералогии им. В.С. Соболева СО РАН; &#13;
Новосибирский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; &#13;
Novosibirsk State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>14</day><month>06</month><year>2022</year></pub-date><volume>13</volume><issue>2</issue><fpage>617</fpage><lpage>617</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Здрокова М.С., Владимиров В.Г., Травин А.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Здрокова М.С., Владимиров В.Г., Травин А.В.</copyright-holder><copyright-holder xml:lang="en">Zdrokova M.S., Vladimirov V.G., Travin A.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/1488">https://www.gt-crust.ru/jour/article/view/1488</self-uri><abstract><p>Критическим элементом при построении тектонических моделей эксгумации базальтов, претерпевших высокобарический метаморфизм, является диагностика синхронности и генетической связи между деформациями и высокобарическими метаморфогенными изменениями. В настоящем сообщении данные вопросы обсуждаются на примере метабазальтов Чарского офиолитового пояса. В подошве блока базальтов с отдельностью подушечных лав, вблизи фермы Буршабулак, обнаружены и проанализированы трещинно-жильные системы с высокобарическими минеральными ассоциациями, что прямо указывает на их тектоническое происхождение. Показано, что условия образования подобных жильных минеральных ассоциаций отвечают эклогитовой фации (P=18.5 кбар, T – не более 520 °C). Возраст высокобарического метаморфизма базальтов, синхронного с деформациями по данным 40Ar/39Ar изотопного датирования амфиболов, не может быть моложе рубежа 452±14 млн лет.</p></abstract><trans-abstract xml:lang="en"><p>A critical element in the construction of tectonic models of exhumation of basalts that have undergone high-pressure metamorphism is the diagnosis of synchronicity and the genetic relationship between deformations and high-pressure metamorphic changes. In this report, these issues are discussed on the example of the metabasalts of the Chara ophiolite belt. In the bottom of the basalt block with the separation of pillow lavas near the Burshabulak farm, crack-vein systems with high-pressure mineral associations were discovered and analyzed, which directly indicates their tectonic origin. It is shown that the conditions for the formation of such vein mineral associations correspond to eclogite-like rocks (P=18.5 kbar temperatures of no more than 520 °C). The age of the high-pressure metamorphism basalts of the synchronous type with deformations according to 40Ar/39Ar isotope dating of amphiboles cannot be younger than the boundary of 452±14 million years.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>высокобарический метаморфизм</kwd><kwd>эксгумация</kwd><kwd>базальты</kwd><kwd>Ar/Ar изотопное датирование</kwd><kwd>Чарский офиолитовый пояс</kwd></kwd-group><kwd-group xml:lang="en"><kwd>high-pressure metamorphism</kwd><kwd>exhumation</kwd><kwd>basalts</kwd><kwd>Ar/Ar dating</kwd><kwd>Chara ophiolite belt</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено по государственному заданию ИГМ СО РАН. Аналитические работы выполнены в ЦКП Многоэлементных и изотопных исследований СО PAН.</funding-statement><funding-statement xml:lang="en">The study was conducted in the framework of state assignment for the IGM SB RAS. Analytical work was carried out at Analytical Center for multi-elemental and isotope research SB RAS.</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">Беляев С.Ю. Тектоника Чарской зоны (Восточный Казахстан) // Труды Института геологии и геофизики СО АН СССР. Вып. 650. Новосибирск, 1985. 119 с.</mixed-citation><mixed-citation xml:lang="en">Belyaev S.Yu., 1985. Tectonics of Chara Zone (East Kazakhstan). Proceedings of the Institute of Geology and Geophysics of the USSR Academy of Sciences. Iss. 650. Novosibirsk, 119 p. (in Russian) .</mixed-citation></citation-alternatives></ref><ref id="cit2"><label>2</label><citation-alternatives><mixed-citation xml:lang="ru">Buslov M.M., Watanabe T., Smirnova L.V., Fujiwara I., Iwata K., de Grave I., Semakov N.N., Travin A.V., Kir’yanova A.P., Kokh D.A., 2003. Role of Strike-Slip Faults in Late Paleozoic – Early Mesozoic Tectonics and Geodynamics of the Altai-Sayan and East Kazakhstan Folded Zone. Russian Geology and Geophysics 44 (1–2), 49–75.</mixed-citation><mixed-citation xml:lang="en">Buslov M.M., Watanabe T., Smirnova L.V., Fujiwara I., Iwata K., de Grave I., Semakov N.N., Travin A.V., Kir’yanova A.P., Kokh D.A., 2003. Role of Strike-Slip Faults in Late Paleozoic – Early Mesozoic Tectonics and Geodynamics of the Altai-Sayan and East Kazakhstan Folded Zone. Russian Geology and Geophysics 44 (1–2), 49–75.</mixed-citation></citation-alternatives></ref><ref id="cit3"><label>3</label><citation-alternatives><mixed-citation xml:lang="ru">Добрецов Н.Л., Ермолов П.В., Хомяков В.Д. Офиолиты и состав фундамента осевой части Зайсанской геосинклинали // Базитовые и ультрабазитовые комплексы Сибири / Ред. Ю.А. Кузнецов. Новосибирск: Наука, 1979. Вып. 441. С. 196–219.</mixed-citation><mixed-citation xml:lang="en">Dobretsov N.L., Ermolov P.V., Khomyakov V.D., 1979. Ophiolites and Basement Composition of the Axial Part of the Zaisan Geosyncline. In: Yu.A. Kuznetsov (Ed.), Basite and Ultrabasite Complexes of Siberia. Iss. 441. Nauka, Novosibirsk, p. 196–219 (in Rus</mixed-citation></citation-alternatives></ref><ref id="cit4"><label>4</label><citation-alternatives><mixed-citation xml:lang="ru">Добрецов Н.Л., Зоненшайн Л.П. Рифейско-нижнепалеозойские офиолиты Северной Евразии. Новосибирск: Наука, 1985. 195 с.</mixed-citation><mixed-citation xml:lang="en">Dobretsov N.L., Zonenshain L.P., 1985. Riphean – Lower Paleozoic Ophiolites of North Eurasia. Nauka, Novosibirsk, 195 p. (in Russian) .</mixed-citation></citation-alternatives></ref><ref id="cit5"><label>5</label><citation-alternatives><mixed-citation xml:lang="ru">Ермолов П.В., Изох Э.П., Пономарёва А.П., Тян В.Д. Габбро-гранитные серии западной части Зайсанской складчатой системы. Новосибирск: Наука, 1977. 249 с..</mixed-citation><mixed-citation xml:lang="en">Ermolov P.V., Izokh E.P., Ponomaryova A.P., Tyan V.D., 1977. Gabbro-Granitic Series of the Western Part of Zaisan Folding System. Nauka, Novosibirsk, 249 p. (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit6"><label>6</label><citation-alternatives><mixed-citation xml:lang="ru">Ермолов П.В., Полянский Н.В., Добрецов Н.Л. Офиолиты Чарского пояса // Офиолиты / Ред. А.А. Абдулин, Е.И. Паталаха. Алма-Ата: Наука, 1981. С. 103–187.</mixed-citation><mixed-citation xml:lang="en">Ermolov P.V., Polyansky N.V., Dobretsov N.L., 1981. Ophiolites of the Chara Belt. In: A.A. Abdulin, E.I. Patalakha (Eds), Ophiolites. Nauka, Alma-Ata, p. 103–178 (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit7"><label>7</label><citation-alternatives><mixed-citation xml:lang="ru">Ермолов П.В., Владимиров А.Г., Изох А.Э. Полянский Н.В., Кузебный B.C., Ревякин П.С., Борцов В.Д. Орогенный магматизм офиолитовых поясов (на примере Восточного Казахстана) // Труды Института геологии и геофизики СО АН СССР. Вып. 651. Новосибирск: Наука, 1983. 210 с.</mixed-citation><mixed-citation xml:lang="en">Ermolov P.V., Vladimirov A.G., Izokh A.E., Polyanskiy N.V., Kuzebny B.S., Revyakin P.S., Bortsov V.D., 1983. Orogenic Magmatism of Ophiolitic Belts (at an Example of East Kazakhstan). Proceedings of the Institute of Geology and Geophysics of the USSR Academy of Sciences. Iss. 651. Nauka, Novosibirsk, 210 p. (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit8"><label>8</label><citation-alternatives><mixed-citation xml:lang="ru">Holland T.J.B., Powell R., 1998. An Internally Consistent Thermodynamic Data Set for Phases of Petrological Interest. Journal of Metamorphic Geology 16 (3), 309–343. https://doi.org/10.1111/J.1525-1314.1998.00140.X.</mixed-citation><mixed-citation xml:lang="en">Holland T.J.B., Powell R., 1998. An Internally Consistent Thermodynamic Data Set for Phases of Petrological Interest. Journal of Metamorphic Geology 16 (3), 309–343. https://doi.org/10.1111/J.1525-1314.1998.00140.X.</mixed-citation></citation-alternatives></ref><ref id="cit9"><label>9</label><citation-alternatives><mixed-citation xml:lang="ru">Хомяков В.Д. Петрология офиолитов Чарской зоны (Восточный Казахстан): Автореф. дис. … канд. геол.-мин. наук. Усть-Каменогорск, 1984. 16 с.</mixed-citation><mixed-citation xml:lang="en">Khomyakov V.D., 1984. Petrology of Ophiolites of Chara Zone (Eastern Kazakhstan). PhD Thesis (Candidate of Geology and Mineralogy). Ust-Kamenogorsk, 16 p. (in Russian)</mixed-citation></citation-alternatives></ref><ref id="cit10"><label>10</label><citation-alternatives><mixed-citation xml:lang="ru">Kurganskaya E.V., Safonova I.Yu., Simonov V.A., 2014. Geochemistry and Petrogenesis of Suprasubduction Volcanic Complexes of the Char Shear Zone (Eastern Kazakhstan). Russian Geology and Geophysics 55 (1), 62–77. https://doi.org/10.1016/j.rgg.2013.12.005.</mixed-citation><mixed-citation xml:lang="en">Kurganskaya E.V., Safonova I.Yu., Simonov V.A., 2014. Geochemistry and Petrogenesis of Suprasubduction Volcanic Complexes of the Char Shear Zone (Eastern Kazakhstan). Russian Geology and Geophysics 55 (1), 62–77. https://doi.org/10.1016/j.rgg.2013.12.005.</mixed-citation></citation-alternatives></ref><ref id="cit11"><label>11</label><citation-alternatives><mixed-citation xml:lang="ru">Lavrent’ev Y.G., Karmanov N.S., Usova L.V., 2015. Electron Probe Microanalysis of Minerals: Microanalyzer or Scanning Electron Microscope? Russian Geology and Geophysics 56 (8), 1154–1161. https://doi.org/10.1016/j.rgg.2015.07.006.</mixed-citation><mixed-citation xml:lang="en">Lavrent’ev Y.G., Karmanov N.S., Usova L.V., 2015. Electron Probe Microanalysis of Minerals: Microanalyzer or Scanning Electron Microscope? Russian Geology and Geophysics 56 (8), 1154–1161. https://doi.org/10.1016/j.rgg.2015.07.006.</mixed-citation></citation-alternatives></ref><ref id="cit12"><label>12</label><citation-alternatives><mixed-citation xml:lang="ru">Полянский Н.В., Добрецов Н.Л., Ермолов П.В., Кузебный В.С. Структура и история развития Чарского офиолитового пояса // Геология и геофизика. 1979. № 5. С. 66–78.</mixed-citation><mixed-citation xml:lang="en">Polyansky N.V., Dobretsov N.L., Ermolov P.V., Kuzebny V.S., 1979. Structure and Development History of the Chara Ophiolitic Belt. Russian Geology and Geophysics 5, 66–78 (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit13"><label>13</label><citation-alternatives><mixed-citation xml:lang="ru">Полянский Н.В., Хомяков В.Д. Геосинклинальные вулканические комплексы Чарского офиолитового пояса. Алма-Ата: Наука, 1981. Т. 40. С. 4–12.</mixed-citation><mixed-citation xml:lang="en">Polyansky N.V., Khomyakov V.D., 1981. Geosynclinal Volcanic Complexes of Chara Ophiolitic Belt. Vol. 40. Nauka, Alma-Ata, p. 4–12 (in Russian) .</mixed-citation></citation-alternatives></ref><ref id="cit14"><label>14</label><citation-alternatives><mixed-citation xml:lang="ru">Safonova I.Yu., Buslov M.M., Iwata K., Kokh D.A., 2004. Fragments of Vendian – Early Carboniferous Oceanic Crust of the Paleo-Asian Ocean in Foldbelts of the Altai-Sayan Region of Central Asia: Geochemistry, Biostratigraphy and Structural Setting. Gondwana Research 7 (3), 771–790. https://doi.org/10.1016/S1342-937X(05)71063-7.</mixed-citation><mixed-citation xml:lang="en">Safonova I.Yu., Buslov M.M., Iwata K., Kokh D.A., 2004. Fragments of Vendian – Early Carboniferous Oceanic Crust of the Paleo-Asian Ocean in Foldbelts of the Altai-Sayan Region of Central Asia: Geochemistry, Biostratigraphy and Structural Setting. Gondwana Research 7 (3), 771–790. https://doi.org/10.1016/S1342-937X(05)71063-7.</mixed-citation></citation-alternatives></ref><ref id="cit15"><label>15</label><citation-alternatives><mixed-citation xml:lang="ru">Safonova I.Yu., Simonov V.A., Kurganskaya E.V., Obut O.T., Romer R.L., Seltmann R., 2012. Late Paleozoic Oceanic Basalts Hosted by the Char Suture-Shear Zone, East Kazakhstan: Geological Position, Geochemistry, Petrogenesis and Tectonic Setting. Journal of Asian Earth Sciences 49, 20–39. https://doi.org/10.1016/j.jseaes.2011.11.015.</mixed-citation><mixed-citation xml:lang="en">Safonova I.Yu., Simonov V.A., Kurganskaya E.V., Obut O.T., Romer R.L., Seltmann R., 2012. Late Paleozoic Oceanic Basalts Hosted by the Char Suture-Shear Zone, East Kazakhstan: Geological Position, Geochemistry, Petrogenesis and Tectonic Setting. Journal of Asian Earth Sciences 49, 20–39. https://doi.org/10.1016/j.jseaes.2011.11.015.</mixed-citation></citation-alternatives></ref><ref id="cit16"><label>16</label><citation-alternatives><mixed-citation xml:lang="ru">Щерба Г.Н., Беспаев Х.А., Дьячков Б.А., Мысник А.М., Ганженко Г.Д., Сапаргалиев Е.М. Большой Алтай (геология и металлогения). Алматы: Гылым, 1998. 395 с.</mixed-citation><mixed-citation xml:lang="en">Shcherba G.N., Bespayev Kh.A., D’yachkov B.A., Mysnik A.M., Ganzhenko G.D., Sapargaliyev E.M., 1998. Large Altai (Geology and Metallogeny). Gylym Publishing House, Almaty, 395 p. (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit17"><label>17</label><citation-alternatives><mixed-citation xml:lang="ru">Travin A.V., 2016. Thermochronology of Early Paleozoic Collisional and Subduction-Collisional Structures of Central Asia. Russian Geology and Geophysics 57 (3), 434–450. https://doi.org/10.1016/j.rgg.2016.03.006.</mixed-citation><mixed-citation xml:lang="en">Travin A.V., 2016. Thermochronology of Early Paleozoic Collisional and Subduction-Collisional Structures of Central Asia. Russian Geology and Geophysics 57 (3), 434–450. https://doi.org/10.1016/j.rgg.2016.03.006.</mixed-citation></citation-alternatives></ref><ref id="cit18"><label>18</label><citation-alternatives><mixed-citation xml:lang="ru">Vladimirov A.G., Kruk N.N., Khromykh S.V., Polyansky O.P., Vladimirov V.G., Travin A.V., Babin G.A., Kuibida M.L., Vladimirov V.D., Chervov V.V., 2008. Permian Magmatism and Lithospheric Deformation in the Altai Caused by Crustal and Mantle Thermal Processes. Russian Geology and Geophysics 49 (7), 468–479. https://doi.org/10.1016/j.rgg.2008.06.006.</mixed-citation><mixed-citation xml:lang="en">Vladimirov A.G., Kruk N.N., Khromykh S.V., Polyansky O.P., Vladimirov V.G., Travin A.V., Babin G.A., Kuibida M.L., Vladimirov V.D., Chervov V.V., 2008. Permian Magmatism and Lithospheric Deformation in the Altai Caused by Crustal and Mantle Thermal Processes. Russian Geology and Geophysics 49 (7), 468–479. https://doi.org/10.1016/j.rgg.2008.06.006.</mixed-citation></citation-alternatives></ref><ref id="cit19"><label>19</label><citation-alternatives><mixed-citation xml:lang="ru">Волкова Н.И., Хлестов В.В., Сухоруков В.П., Хлестов М.В. Геохимия метаморфизованных пиллоу-базальтов Чарской зоны, Северо-Восточный Казахстан // Корреляция алтаид и уралид: магматизм, метаморфизм, стратиграфия, геохронология, геодинамика и металлогения: Материалы Второй международной научной конференции (1–4 апреля 2014 г.). Новосибирск: Изд-во СО РАН, 2014. С. 26–27.</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Khlestov V.V., Sukhorukov V.P., Khlestov M.V., 2014. Geochemistry of Metamorphosed Pillow-Basalts of Chara Zone, North-Eastern Kazakhstan. In: Correlation of Altaides and Uralides: Magmatism, Metamorphism, Stratigraphy, Geochronology, Geodynamics and Metallogeny. Proceedings of the Third International Scientific Conference (April 1–4, 2014). Publishing House of SB RAS, Novosibirsk, p. 26–27 (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit20"><label>20</label><citation-alternatives><mixed-citation xml:lang="ru">Volkova N.I., Khlestov V.V., Sukhorukov V.P., Khlestov M.V., 2016a. Geochemistry of Metamorphosed Pillow Basalts of the Chara Zone, NE Kazakhstan. Doklady Earth Sciences 467, 350–354. https://doi.org/10.1134/S1028334X16040085.</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Khlestov V.V., Sukhorukov V.P., Khlestov M.V., 2016a. Geochemistry of Metamorphosed Pillow Basalts of the Chara Zone, NE Kazakhstan. Doklady Earth Sciences 467, 350–354. https://doi.org/10.1134/S1028334X16040085.</mixed-citation></citation-alternatives></ref><ref id="cit21"><label>21</label><citation-alternatives><mixed-citation xml:lang="ru">Volkova N.I., Simonov V.A., Travin A.V., Stupakov S.I., Yudin D.S., 2016b. Eclogites in the Chara Zone, NE Kazakhstan: New Geochemical and Geochronological Data. Geochemistry International 54, 208–214. https://doi.org/10.1134/S0016702915120101.</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Simonov V.A., Travin A.V., Stupakov S.I., Yudin D.S., 2016b. Eclogites in the Chara Zone, NE Kazakhstan: New Geochemical and Geochronological Data. Geochemistry International 54, 208–214. https://doi.org/10.1134/S0016702915120101.</mixed-citation></citation-alternatives></ref><ref id="cit22"><label>22</label><citation-alternatives><mixed-citation xml:lang="ru">Volkova N.I., Sklyarov E.V., 2007. High-Pressure Complexes of Central Asian Fold Belt: Geologic Setting, Geochemistry, and Geodynamic Implications. Russian Geology and Geophysics 48 (1), 83–90. https://doi.org/10.1016/j.rgg.2006.12.008.</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Sklyarov E.V., 2007. High-Pressure Complexes of Central Asian Fold Belt: Geologic Setting, Geochemistry, and Geodynamic Implications. Russian Geology and Geophysics 48 (1), 83–90. https://doi.org/10.1016/j.rgg.2006.12.008.</mixed-citation></citation-alternatives></ref><ref id="cit23"><label>23</label><citation-alternatives><mixed-citation xml:lang="ru">Волкова Н.И., Тарасова Е.Н., Полянский Н.В., Хомяков В.Д. Петрология высокобарических пород Чарской зоны (Восточный Казахстан) // Петрология магматических и метаморфических комплексов: Материалы Всероссийской петрографической конференции (24–26 ноября 2005 г.). Томск: ЦНТИ, 2005. Вып. 5. T. 1. С. 317–320</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Tarasova E.N., Polyansky N.V., Khomyakov V.D., 2005. Petrology of High-Baric Rocks of Chara Zone (East Kazakhstan). In: Petrology of Magmatic and Metamorphic Complexes. Proceedings of Materials of the All-Russian Petrographic Conference (November 24–26, 2005). Iss. 5. Vol. 1. Publishing House of CSTI, Tomsk, p. 317–320 (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit24"><label>24</label><citation-alternatives><mixed-citation xml:lang="ru">Волкова Н.И., Тарасова Е.Н., Полянский Н.В., Травин А.В., Юдин Д.С. Геохимия и 39Ar-40Ar возраст включений высокобарических пород в серпентинитовом меланже Чарской зоны // Геодинамическая эволюция литосферы Центрально-Азиатского подвижного пояса (от океана к континенту): Материалы научного совещания по Программе фундаментальных исследований ОНЗ РАН (19–22 октября 2004 г.). Иркутск: Изд-во ИЗК СО РАН, 2004. Вып. 2. Т. 1. С. 76–80.</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Tarasova E.N., Polyansky N.V., Travin A.V., Yudin D.S., 2004. Geochemistry and 39Ar-40Ar Age of High-Baric Rocks Inclusions in Serpentinite Melange of the Chara Zone. In: Geodynamic Evolution of the Lithosphere of the Central Asian Mobile Belt (from Ocean to Continent). Proceedings of Scientific Meeting (October 19–22, 2004). Iss. 2. Vol. 1. Publishing House of IEC SB RAS, Irkutsk, p. 76–80 (in Russian).</mixed-citation></citation-alternatives></ref><ref id="cit25"><label>25</label><citation-alternatives><mixed-citation xml:lang="ru">Volkova N.I., Tarasova E.N., Vladimirov A.G., Khomyakov V.D., Polyanskii N.V., 2008. High-Pressure Rocks in the Serpentinite Melange of the Chara Zone, Eastern Kazakhstan: Geochemistry, Petrology, and Age. Geochemistry International 46, 386–401. https://doi.org/10.1134/S0016702908040071.</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Tarasova E.N., Vladimirov A.G., Khomyakov V.D., Polyanskii N.V., 2008. High-Pressure Rocks in the Serpentinite Melange of the Chara Zone, Eastern Kazakhstan: Geochemistry, Petrology, and Age. Geochemistry International 46, 386–401. https://doi.org/10.1134/S0016702908040071.</mixed-citation></citation-alternatives></ref><ref id="cit26"><label>26</label><citation-alternatives><mixed-citation xml:lang="ru">Volkova N.I., Travin A.V., Yudin D.S., 2011. Ordovician Blueschist Metamorphism as a Reflection of Accretion-Collision Events in the Central Asian Orogenic Belt. Russian Geology and Geophysics 52 (1), 72–84. https://doi.org/10.1016/j.rgg.2010.12.006.</mixed-citation><mixed-citation xml:lang="en">Volkova N.I., Travin A.V., Yudin D.S., 2011. Ordovician Blueschist Metamorphism as a Reflection of Accretion-Collision Events in the Central Asian Orogenic Belt. Russian Geology and Geophysics 52 (1), 72–84. https://doi.org/10.1016/j.rgg.2010.12.006.</mixed-citation></citation-alternatives></ref><ref id="cit27"><label>27</label><citation-alternatives><mixed-citation xml:lang="ru">Whitney D.L., Evans B.W., 2010. Abbreviations for Names of Rock-Forming Minerals. American Mineralogist 95 (1), 185–187. https://doi.org/10.2138/am.2010.3371.</mixed-citation><mixed-citation xml:lang="en">Whitney D.L., Evans B.W., 2010. Abbreviations for Names of Rock-Forming Minerals. American Mineralogist 95 (1), 185–187. https://doi.org/10.2138/am.2010.3371.</mixed-citation></citation-alternatives></ref></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
