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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-2022-13-5-0673</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1584</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>МАГМАТИЧЕСКИЕ ПОРОДЫ ТЕКТУРМАССКОГО АККРЕЦИОННОГО КОМПЛЕКСА, ЦЕНТРАЛЬНЫЙ КАЗАХСТАН: ГЕОЛОГИЧЕСКАЯ ПОЗИЦИЯ И ГЕОДИНАМИЧЕСКИЕ ОБСТАНОВКИ ФОРМИРОВАНИЯ</article-title><trans-title-group xml:lang="en"><trans-title>MAGMATIC ROCKS OF THE TEKTURMASS ACCRETIONARY COMPLEX, CENTRAL KAZAKHSTAN: GEOLOGICAL POSITION AND GEODYNAMIC SETTINGS OF FORMATION</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>Гурова</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Gurova</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, ул. Пирогова, 1</p><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>1 Pirogov St, Novosibirsk 630090</p><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>Сафонова</surname><given-names>И. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Safonova</surname><given-names>I. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, ул. Пирогова, 1</p><p>630090, Новосибирск, пр-т Академика Коптюга, 3</p></bio><bio xml:lang="en"><p>1 Pirogov St, Novosibirsk 630090</p><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>Савинский</surname><given-names>И. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Savinsky</surname><given-names>I. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, ул. Пирогова, 1</p></bio><bio xml:lang="en"><p>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>Антонюк</surname><given-names>Р. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Antonyuk</surname><given-names>R. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>100019, Караганда, ул. Ипподромная, 5</p></bio><bio xml:lang="en"><p>5 Ippodromnaya St, Karaganda 100019</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>Орынбек</surname><given-names>Т. Ж.</given-names></name><name name-style="western" xml:lang="en"><surname>Orynbek</surname><given-names>T. Zh.</given-names></name></name-alternatives><bio xml:lang="ru"><p>100019, Караганда, ул. Ипподромная, 5</p></bio><bio xml:lang="en"><p>5 Ippodromnaya St, Karaganda 100019</p></bio><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Новосибирский государственный университет; Институт геологии и минералогии им. В.С. Соболева СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Novosibirsk State University; 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>Новосибирский государственный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Novosibirsk State University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Институт проблем комплексного освоения недр</institution><country>Казахстан</country></aff><aff xml:lang="en"><institution>Institute for the Study of Complex Mineral Development</institution><country>Kazakhstan</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>10</day><month>12</month><year>2022</year></pub-date><volume>13</volume><issue>5</issue><fpage>673</fpage><lpage>673</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Гурова А.В., Сафонова И.Ю., Савинский И.А., Антонюк Р.М., Орынбек Т.Ж., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Гурова А.В., Сафонова И.Ю., Савинский И.А., Антонюк Р.М., Орынбек Т.Ж.</copyright-holder><copyright-holder xml:lang="en">Gurova A.V., Safonova I.Y., Savinsky I.A., Antonyuk R.M., Orynbek T.Z.</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/1584">https://www.gt-crust.ru/jour/article/view/1584</self-uri><abstract><p>В статье представлен обзор геологического строения и новые данные по петрографии и химическому составу вулканических пород Тектурмасского аккреционного комплекса (ТАК). Обсуждается их возраст, условия петрогенезиса и вероятные тектонические обстановки формирования. Показано, что ТАК и связанный с ним офиолитовый пояс являются частью орогена тихоокеанского типа позднекембрийско-ордовикского возраста, образованного на активной окраине Палеоазиатского океана. Выделены магматические комплексы преимущественно основного состава (базальты, долериты, габбро) преимущественно толеитовой серии. По содержанию TiO2 базальты и андезибазальты можно разделить на три группы: высоко-Ti, средне-Ti и низкo-Ti. Геологическая позиция и геохимические характеристики магматических пород ТАК предполагают образование cредне-Ti базальтов в обстановке срединно-океанического хребта, высоко-Ti и щелочных андезитов – в обстановке океанического острова/симаунта, а низко-Ti вулканитов – в надсубдукционной обстановке.</p></abstract><trans-abstract xml:lang="en"><p>The paper provides an overview of the geological structure and presents new data on petrography and geochemistry of igneous rocks of the Tekturmas accretionary complex (TAC). Consideration is being given to the age, petrogenesis and probable tectonic settings of formation of igneous rocks. It is shown that the TAC and adjacent ophiolite belt are parts of the Late Cambrian – Ordovician Pacific-type orogenic belt formed at an active margin of the Paleo-Asian Ocean. The TAC is dominated mainly by tholeiitic mafic igneous rocks (basalt, dolerite, gabbro). There are recognized three groups of rocks: high-Ti, medium-Ti and low-Ti. Geological and geochemical features of TAC igneous rocks suggest their formation in three tectonic settings: mid-ocean ridge (medium-Ti), oceanic island/seamount (high-Ti) and over subduction zones (low-Ti).</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Палеоазиатский океан</kwd><kwd>Центрально-Азиатский складчатый пояс</kwd><kwd>поздний кембрий</kwd><kwd>ордовик</kwd><kwd>офиолиты</kwd><kwd>петрография</kwd><kwd>геохимия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Paleo-Asian Ocean</kwd><kwd>Central Asian Orogenic Belt</kwd><kwd>Late Cambrian</kwd><kwd>Ordovician</kwd><kwd>ophiolites</kwd><kwd>petrography</kwd><kwd>geochemistry</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при поддержке Российского научного фонда (проект № 21-77-20022, геохимия), Министерства науки и высшего образования РФ (проекты № FSUS-2020-0039 НГУ и № 0330-2019-0003 ИГМ СО РАН, региональная геология, петрография) и Министерства науки и высшего образования Казахстана (проект № АР08855920, локальная геология, полевые работы).</funding-statement><funding-statement xml:lang="en">The study was supported by the Russian Science Foundation (project 21-77-20022, geochemistry), the Ministry of Science and Higher Education of the Russian Federation (projects FSUS-2020-0039 and 0330-2019-0003 regional geology and petrography) and the Ministry of Science and Higher Education of Kazakhstan (project AR08855920; local geology, field work).</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">An A.-R., Choi S.H., Yu Y., Lee D.-С., 2016. 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