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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-2023-14-3-0699</article-id><article-id custom-type="elpub" pub-id-type="custom">gtcrust-1694</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>40Ar/39Ar ДАТИРОВАНИЕ МАРУЯМАИТА (КАЛИЙСОДЕРЖАЩИЙ ТУРМАЛИН) ИЗ АЛМАЗОНОСНЫХ ПОРОД КОКЧЕТАВСКОГО МАССИВА</article-title><trans-title-group xml:lang="en"><trans-title>40Ar/39Ar DATING OF MARUYAMAITE (K-DOMINANT TOURMALINE) FROM DIAMOND-BEARING METAMORPHIC ROCKS OF THE KOKCHETAV MASSIF</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>Корсаков</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Korsakov</surname><given-names>A. V.</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><email xlink:type="simple">korsakov@igm.nsc.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>Юдин</surname><given-names>Д. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Yudin</surname><given-names>D. 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>Мусияченко</surname><given-names>К. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Musiyachenko</surname><given-names>K. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>630090, Новосибирск, пр-т Академика Коптюга, 3; V6T 1Z4, Ванкувер, Канада</p></bio><bio xml:lang="en"><p>Andrey V. Korsakov.</p><p>3 Academician Koptyug Ave, Novosibirsk 630090; Vancouver V6T 1Z4, Canada</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>Демин</surname><given-names>С. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Demin</surname><given-names>S. P.</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-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; Университет Британской Колумбии</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; University of British Columbia</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>18</day><month>06</month><year>2023</year></pub-date><volume>14</volume><issue>3</issue><fpage>699</fpage><lpage>699</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Корсаков А.В., Юдин Д.С., Мусияченко К.А., Демин С.П., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Корсаков А.В., Юдин Д.С., Мусияченко К.А., Демин С.П.</copyright-holder><copyright-holder xml:lang="en">Korsakov A.V., Yudin D.S., Musiyachenko K.A., Demin S.P.</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/1694">https://www.gt-crust.ru/jour/article/view/1694</self-uri><abstract><p>Проведено 40Ar/39Ar исследование маруямаита (калийсодержащий турмалин) из турмалин-кварц-полевошпатовых пород, вскрытых в пределах главного штрека штольни Кумды-Кольского месторождения технических алмазов (Кокчетавский массив, Северный Казхстан). Получены 40Ar/39Ar спектры, в которых выделяются четкие плато С совпадающими В пределах ошибки значениями возраста - датировки 502.3±8.0, 502.2±8.0, 506.0±8.0 млн лет по турмалину. Эти датировки значительно моложе возраста пород, образованных на этапе высокобарического метаморфизма, фиксируемого комплексом методов - 530±2 млн лет. Таким образом, формирование богатых турмалином пород Кумды-Кольского месторождения не связано с высокобарическим этапом метаморфизма, то есть образование маруямаита происходило на более позднем низкобарическом этапе. K/Ar система в турмалине может быть использована для датирования метасоматических и метаморфических процессов, так как показано, что такие датировки совпадают даже для кристаллов турмалина с различным содержанием калия.</p></abstract><trans-abstract xml:lang="en"><p>40Ar/39Ar analyses were made on maruyamaite (potassium-dominant tourmaline) from tourmaline-quartz-feldspar rocks discovered within the Kumdy-Kol microdiamond deposit (Kokchetav massif, North Kazakhstan). Turmaline yielded well-defined 40Ar/39Ar plateau age spectra whose values coincide within the error - ages of 502.3±8.0, 502.2±8.0, 506.0±8.0 Ma. These ages are much younger than the age of 530±2 Ma determined for high-pressure metamorphism by different methods. Thus, the formation of tourmaline-rich rocks of the Kumdy-Kol deposit cannot be associated with the high-pressure metamorphic events, and, therefore, testifies in favor of the low-pressure nature of maruyamaite. Based on the coincidence of age data for tourmaline crystals with different potassium contents, it can be concluded that the K/Ar system in tourmaline can be used for dating metasomatic and metamorphic processes.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Ar-Ar датирование</kwd><kwd>маруямаит</kwd><kwd>алмаз</kwd><kwd>метаморфизм высоких давлений</kwd><kwd>Кокчетав</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Ar-Ar dating</kwd><kwd>maruyamaite</kwd><kwd>diamond</kwd><kwd>high pressure metamorphism</kwd><kwd>Kokchetav</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследования выполнены при поддержке РНФ (грант 18-17-00186). Отбор образцов начинался в рамках государственного задания ИГМ СО РАН.</funding-statement><funding-statement xml:lang="en">The study was supported by the Russian Science Foundation (grant 18-17-00186). 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