gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2023-14-4-0711gtcrust-1719Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSLA-ICP-MS ТРЕКОВОЕ ДАТИРОВАНИЕ АПАТИТА ИЗ ИНТРУЗИВНЫХ ТЕЛ СИБИРСКОЙ ТРАППОВОЙ ПРОВИНЦИИ: МЕТОД, ПЕРВЫЕ РЕЗУЛЬТАТЫ И ИХ ИНТЕРПРЕТАЦИЯLA-ICP-MS APATITE FISSION-TRACK DATING OF THE SIBERIAN TRAPS INTRUSIONS: METHOD, FIRST RESULTS AND THEIR INTERPRETATIONhttps://orcid.org/0000-0002-0265-8047БагдасарянТ. Э.BagdasaryanT. E.

119991, Москва, Ленинские горы, 1

123242, Москва, ул. Большая Грузинская, 10, стр. 1

1 Leninskie Gory, Moscow 119991

10-1 Bolshaya Gruzinskaya St, Moscow 123242

https://orcid.org/0000-0001-5237-6614ХубановВ. Б.KhubanovV. B.

670047, Улан-Удэ, ул. Сахьяновой, 6а, Республика Бурятия

6а Sakhyanova St, Ulan-Ude 670047, Republic of Buryatia

https://orcid.org/0000-0001-8364-0529ВеселовскийР. В.VeselovskiyR. V.

119991, Москва, Ленинские горы, 1

123242, Москва, ул. Большая Грузинская, 10, стр. 1

1 Leninskie Gory, Moscow 119991

10-1 Bolshaya Gruzinskaya St, Moscow 123242

roman.veselovskiy@ya.ruhttps://orcid.org/0000-0001-5599-5760ЗайцевВ. А.ZaitsevV. A.

119991, Москва, ул. Косыгина, 19

19 Kosygin St, Moscow 119991

https://orcid.org/0000-0003-1044-7175МалышевС. В.MalyshevS. V.

199034, Санкт-Петербург, наб. Университетская, 7-9

7-9 Universitetskaya Emb, Saint Petersburg 199034

Московский государственный университет им. М.В. Ломоносова; Институт физики Земли им. О.Ю. Шмидта РАНРоссияLomonosov Moscow State University; Schmidt Institute of Physics of the Earth, Russian Academy of SciencesRussian FederationГеологический институт им. Н.Л. Добрецова СО РАНРоссияDobretsov Geological Institute, Siberian Branch of the Russian Academy of SciencesRussian FederationИнститут геохимии и аналитической химии им. В.И. Вернадского РАНРоссияVernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of SciencesRussian FederationСанкт-Петербургский государственный университетРоссияSaint Petersburg UniversityRussian Federation202316082023144711711Copyright © Багдасарян Т.Э., Хубанов В.Б., Веселовский Р.В., Зайцев В.А., Малышев С.В., 20232023Багдасарян Т.Э., Хубанов В.Б., Веселовский Р.В., Зайцев В.А., Малышев С.В.Bagdasaryan T.E., Khubanov V.B., Veselovskiy R.V., Zaitsev V.A., Malyshev S.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/1719

В статье представлены результаты трекового анализа апатита, впервые выполненного в Институте физики Земли им. О.Ю. Шмидта РАН с использованием метода масс-спектроскопии с индуктивно связанной плазмой и лазерной абляцией (LA-ICP-MS, Геологический институт им. Н.Л. Добрецова Сибирского отделения РАН) для двух интрузивных тел Сибирской пермско-триасовой трапповой провинции: щелочно-ультраосновного плутона Маган (две пробы) и Контайской интрузии (одна проба). Полученный трековый возраст составляет 217.6±18.6 и 238.8±35.8 млн лет – для интрузии Маган и 150.0±23.0 млн лет (2σ) для Контайской интрузии и маркирует время, прошедшее с момента их остывания ниже 120 °С. Распределение длин треков в зернах апатита из исследованных образцов свидетельствует об их быстром остывании до приповерхностных температур. Приводится подробное описание используемой методики, а также показано, что результаты трекового анализа, выполненного по принципу «образец-в-образец» классическим методом внешнего детектора и методом LA-ICP-MS в модификации зета-калибровки, совпадают в пределах погрешности метода.

In this paper we present the results on apatite fission-track dating, which was first performed at the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, using the laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS, Dobretsov Geological Institute, Siberian Branch of the Russian Academy of Sciences) for two intrusions of the Siberian Permian-Triassic large igneous province: Magan alkaline-ultramafic pluton (two samples) and Kontay intrusion (one sample). The obtained AFT ages are 217.6±18.6 and 238.8±35.8 Ma (95% confidence) for the Magan intrusion and 150.0±23.0 Ma for the Kontay intrusion and mark the time since they have been cooled below 120 °C. The distributions of track lengths in apatite grains from the studied samples indicate their rapid cooling to near-surface temperatures. We provide a detailed description of the method used, and also demonstrate that the results of fissiontrack analysis performed on the "sample-to-sample" principle by the classical external detector method (EDM) and the LA-ICP-MS method in the modification of the zeta calibration coincide within the age uncertainty.

трековый анализтрековое датированиеапатитLA-ICP-MSтермохронологиягеохронологияСибирские траппыapatite fission-track analysisapatite fission-track datingapatiteLA-ICP-MSthermochronologygeochronologySiberian trapsАвторы благодарят М.М. Буслова (ИГМ СО РАН), А.В. Куликову (ИГМ СО РАН) и Ю.А. Бишаева (ИГМ СО РАН) за помощь в пробоподготовке, а также рецензентов, чьи замечания значительно улучшили качество статьи. Лабораторные исследования проводились на оборудовании ЦКП «Петрофизика, геомеханика и палеомагнетизм» ИФЗ РАН. Исследование выполнено при финансовой поддержке РФФИ, грант №20-35-90066, а также в рамках государственного задания ИФЗ РАН. Работа выполнена в рамках фундаментальных исследований ИФЗ РАН и ГИН СО РАН (базовый проект № гос. рег. АААА-А21-121011390002-2).The study was conducted with the financial support of the Russian Foundation for Basic Research, grant 20-35-90066, and part of the state assigmnent of the IPE RAS. 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The authors declare that there are no conflicts of interest present.