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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">10.24930/2500-302X-2026-26-1-81-99</article-id><article-id custom-type="edn" pub-id-type="custom">KPCDNL</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-2453</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>Микроэлементный состав, текстура, катодолюминесценция, комбинационное рассеяние, ЛА-ИСП-МС U-Pb датирование и Lu-Hf изотопный состав циркона Bai-1-2023 из песков комплекса заливов оз. Байкал “Бухта Песчаная” как потенциального стандарта раннепротерозойского возраста</article-title><trans-title-group xml:lang="en"><trans-title>Trace element composition, texture, cathodoluminescence, Raman scattering, LA–ICP–MS U–Pb dating, and Lu–Hf isotopic composition of zircon Bai-1-2023 from sands of the Peschanaya Bay complex of Lake Baikal as a potential Early Proterozoic age standard</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>Вотяков</surname><given-names>С. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Votyakov</surname><given-names>S. L.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г. Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>Sergey L. Votyakov</p><p>15 Academician Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">zaitseva.mv1991@gmail.com</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>Червяковская</surname><given-names>М. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Chervyakovskaya</surname><given-names>M. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г. Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>Maria V. Chervyakovskaya</p><p>15 Academician Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">zaitseva.mv1991@gmail.com</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>Червяковский</surname><given-names>В. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Chervyakovskiy</surname><given-names>V. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г. Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>Vasiliy S. Chervyakovskiy</p><p>15 Academician Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">zaitseva.mv1991@gmail.com</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>Панкрушина</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Pankrushina</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г. Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>Elizaveta A. Pankrushina</p><p>15 Academician Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">zaitseva.mv1991@gmail.com</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>Булатов</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Bulatov</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г. Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>Vladislav A. Bulatov</p><p>15 Academician Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">zaitseva.mv1991@gmail.com</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>Чебыкин</surname><given-names>Н. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Chebykin</surname><given-names>N. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г. Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>Nikolai S. Chebykin</p><p>15 Academician Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">zaitseva.mv1991@gmail.com</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>Мандрыгина</surname><given-names>Д. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Mandrygina</surname><given-names>D. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>620110, г. Екатеринбург, ул. Академика Вонсовского, 15</p></bio><bio xml:lang="en"><p>Daria A. Mandrygina</p><p>15 Academician Vonsovsky st., Ekaterinburg 620110</p></bio><email xlink:type="simple">zaitseva.mv1991@gmail.com</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>Иванов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>664033, г. Иркутск, ул. Лермонтова, 128</p></bio><bio xml:lang="en"><p>Alexei V. Ivanov</p><p>128 Lermontov st., Irkutsk 664033</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Институт геологии и геохимии им. академика А.Н. Заварицкого УрО РАН<country>Россия</country></aff><aff xml:lang="en">A.N. Zavaritsky Institute of Geology and Geochemistry, UB RAS<country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru">Институт земной коры СО РАН<country>Россия</country></aff><aff xml:lang="en">Institute of the Earth’s Crust, SB RAS<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2026</year></pub-date><pub-date pub-type="epub"><day>21</day><month>02</month><year>2026</year></pub-date><volume>26</volume><issue>1</issue><fpage>81</fpage><lpage>99</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Вотяков С.Л., Червяковская М.В., Червяковский В.С., Панкрушина Е.А., Булатов В.А., Чебыкин Н.С., Мандрыгина Д.А., Иванов А.В., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Вотяков С.Л., Червяковская М.В., Червяковский В.С., Панкрушина Е.А., Булатов В.А., Чебыкин Н.С., Мандрыгина Д.А., Иванов А.В.</copyright-holder><copyright-holder xml:lang="en">Votyakov S.L., Chervyakovskaya M.V., Chervyakovskiy V.S., Pankrushina E.A., Bulatov V.A., Chebykin N.S., Mandrygina D.A., Ivanov A.V.</copyright-holder><license 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/2453">https://www.lithosphere.ru/jour/article/view/2453</self-uri><abstract><p>Поиск и обоснование геохронологических стандартов, проведение их межлабораторного “слепого” тестирования – актуальные задачи в области аналитической геохимии. В ЦКП ИЗК СО РАН в качестве геохронологического стандарта U-Pb возраста предложен циркон Bai-1-2023 из песка заливов оз. Байкал “Бухта Песчаная”, продукта разрушения гранитов рапакиви Приморского комплекса Западного Предбайкалья.  Результаты. В работе представлены данные “слепого” анализа U-Pb и Lu-Hf изотопного состава выборки из более 100 зерен циркона Bai-1-2023. По данным микрозондового и ЛА-ИСП-МС анализа, локальной спектроскопии комбинационного рассеяния света и катодолюминесценции изучен состав зерен, их текстура и однородность; результаты сопоставлены с таковыми для международных образцов сравнения циркона Mud Tank, 91500, Temora-2, GJ-1, Plesovice. Для выборки из 25 зерен циркона выделены две статистически обособленные, конкордантные возрастные популяции 1871 ± 8.1 и 1781 ± 5.7 млн лет (37 ЛА-ИСП-МС определений; параметр дисконкордантности 207Pb/206Pb и 206Pb/238U возрастов для большинства точек менее 5–6%; для единичных – 10–17%); более древняя из которых близка к ИР-ТИМС датировкам (1859 ± 16 и 1853.6 ± 6.5 млн лет). Наличие двух популяций не сопровождается ясно различимыми изменениями состава зерен циркона и их текстуры, ядер, оболочек и трещин. Полученные ЛА-ИСП-МС данные для изотопных отношений 176Hf/177Hf и 176Lu/177Hf использованы для расчета параметра εHf(t) и значения модельного возраста источника TDM, которые составляют –13.7…–6.5 и 2.5–2.7 млрд лет соответственно. Как по зернам, так и в пределах каждого зерна циркона фиксируются значимые вариации положения колебательной моды ν3(SiO4) (от 1003.4 до 1006.6 см–1) и ее ширины (от 4.8 до 9.8 см–1), а также значений накопленной авторадиационной и эквивалентной доз – Dα = (0.64–2.47)·1018 и Dαэк = (0.20–0.52)·1018 α-расп/г соответственно. Показано, что зерна циркона Bai-1-2023 соответствуют II–III стадиям разупорядочения структуры минерала. Яркость катодолюминесценции варьирует по зернам более чем на порядок; спектры носят сложный суперпозиционный характер; выделяется ряд широких полос Аi, Вi, Сi в ближней УФ, сине-зеленой и желтой областях; проанализировано положение точек для циркона на тройной Аi-Вi-Сi дискриминационной диаграмме. Показано, что зерна циркона Bai-1-2023 по спектроскопическим свойствам и степени радиационной деструкции перекрывают ряд ОС циркона 91500 → Temora-2 → GJ-1 → Plesovice. Выводы. Циркон Bai-1-2023 может быть рекомендован в качестве вторичного стандарта возраста для контроля правильности ЛА-ИСП-МС анализа. </p></abstract><trans-abstract xml:lang="en"><p>The search for and substantiation of geochronological standards, as well as their interlaboratory testing, are current tasks in the field of analytical geochemistry. Zircon Bai-1-2023 from the sands of the bays of Lake Baikal (“Peschanaya Bay”), a product of the destruction of rapakivi granites of the Primorsky Complex of the Western Cis-Baikal region, has been proposed by the Institute of the Earth’s Crust SB RAS as a U–Pb geochronological standard. Results. This paper presents the results of an interlaboratory, “blind” U–Pb and Lu–Hf isotope study of more than 100 Bai-1-2023 zircon grains. Grain composition, texture, and homogeneity were analyzed by the methods of microprobe and LA–ICP–MS analysis, local Raman and cathodoluminescence spectroscopy. The results were compared with those obtained for international reference materials of zircon Mud Tank, 91500, Temora-2, GJ–1, and Plesovice. For 25 grains (37 LA–ICP– MS determination rounds), two statistically isolated, concordant age populations of 1871 ± 8.1 and 1781 ± 5.7 Ma were identified; for most points, the discordance parameter for 207Pb/206Pb and 206Pb/238U ages was less than 5–6%; for single ones – 10–17%. One population showed an age close to IR-TIMS dating (1859 ± 16 and 1853.6 ± 6.5 Ma). The presence of two populations  is not accompanied by clearly distinguishable changes in the composition of zircon grains and their texture, cores, shells, and cracks. LA–ICP–MS data were obtained for 176Hf/177Hf and 176Lu/177Hf isotope ratios. The parameter εHf(t) and the model age of the source TDM were calculated as follows εHf(t)= –13.7 ÷ –6.5 and TDM = 2.5– 2.7 Ga. For zircon grains, significant variations in the position of the vibrational mode ν3(SiO4) (1003.4– 1006.6 cm-1) and its width FWHM  (4.8–9.8 cm-1), as well as the values of accumulated autoradiation and equivalent doses – (0.64–2.47) and (0.20– 0.52)·1018 α-decay/g, respectively, were established. Bai-1-2023 zircon was shown to correspond to II–III stages of the mineral disorder. Cathodoluminescence brightness of zircon grains varied by more than an order of magnitude. In the spectra, a number of broad bands Ai, Bi, Ci in the near UV, blue–green, and yellow regions were distinguished. The position of points for Bai-1-2023 zircon on the triple Ai–Bi–Ci discrimination diagram was analyzed. Spectroscopic properties of Bai-1-2023 zircon and the degree of its radiation damage were shown to overlap the properties of the reference materials  91500 → Temora-2→ GJ–1 → Plesovice. Conclusions. Zircon Bai-1-2023 can be recommended as a secondary age reference material for verifying the accuracy of LA–ICP–MS analysis.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>циркон</kwd><kwd>масс-спектрометрия</kwd><kwd>образец сравнения</kwd><kwd>катодолюминесценция</kwd><kwd>комбинационное рассеяние света</kwd></kwd-group><kwd-group xml:lang="en"><kwd>zircon</kwd><kwd>mass spectrometry</kwd><kwd>reference sample</kwd><kwd>cathodoluminescence</kwd><kwd>Raman spectroscopy</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Результаты получены в ЦКП “Геоаналитик” ИГГ УрО РАН в рамках госзадания № 123011800012-9.</funding-statement></funding-group><funding-group xml:lang="en"><funding-statement>The results were obtained at the Geoanalyst Collective Use Center of the IGG UB RAS within the framework of state assignment No. 123011800012-9</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">Вотяков С.Л., Червяковская М.В., Щапова Ю.В., Панкрушина Е.А., Михалевский Г.Б., Червяковский В.С. 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