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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">10.24930/1681-9004-2021-21-5-712-723</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1487</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>К методике определения изотопного состава Sm/Nd и Sr на ICP-MS Neptune Plus с LA приставкой NWR 213</article-title><trans-title-group xml:lang="en"><trans-title>Determination of Sm/Nd and Sr isotopic composition using an ICP-MS Neptune Plus equipped with an NWR 213 attachment for laser ablation</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>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. Акад. Вонсовского, 15</p></bio><bio xml:lang="en"><p>  15 Akad. Vonsovskogo 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. Акад. Вонсовского, 15</p></bio><bio xml:lang="en"><p>  15 Akad. Vonsovskogo st., Ekaterinburg 620110 </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 геохимии УрО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>A.N. Zavaritsky Institute of Geology and Geochemistry uB RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>31</day><month>10</month><year>2021</year></pub-date><volume>21</volume><issue>5</issue><fpage>712</fpage><lpage>723</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Червяковская М.В., Червяковский В.С., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Червяковская М.В., Червяковский В.С.</copyright-holder><copyright-holder xml:lang="en">Chervyakovskaya M.V., Chervyakovskiy V.S.</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.lithosphere.ru/jour/article/view/1487">https://www.lithosphere.ru/jour/article/view/1487</self-uri><abstract><sec><title>Объект исследования</title><p>Объект исследования. Изотопная система Sm/Nd в ряде межлабораторных природных образцов апатита, титанита, алланита, монацита и во внутрилабораторных пробах апатита (из карбонатитов Ильменогорского массива, Южный Урал), монацита (из пегматитов Адуйского гранитного массива и его обрамления, Средний Урал) и титанита (из кальцитовых жил Сарановского месторождения хромита, Средний Урал, и из щелочного пегматита рудника Шпат, Вишневые горы, Южный Урал); изотопная система Sr ряде межлабораторных природных образцов апатита и во внутрилабораторных пробах апатита (из апатит-карбонатной жилы Слюдяногорского месторождения, Иркутская область, и из карбонатитов Ильменогорского массива, Южный Урал).</p></sec><sec><title>Метод</title><p>Метод. Исследование проведено на многоколлекторном масс-спектрометре с индуктивно-связанной плазмой Neptune Plus (ThermoFisher) с приставкой для лазерной абляции NWR 213 (ESI), размещенном в помещении класса чистоты 7 ИСО в ЦКП “Геоаналитик” (ИГГ УрО РАН, г. Екатеринбург). Результаты. В работе описаны методические подходы для изучения изотопных систем Sm/Nd и Sr в природных фосфатных и силикатных минералах методом масс-спектрометрии с индуктивно-связанной плазмой с лазерной абляцией, реализованные на оборудовании ЦКП “Геоаналитик” (ИГГ УрО РАН, г. Екатеринбург). Проведена сравнительная характеристика результатов с литературными данными по исследованию межлабораторных природных образцов, получено удовлетворительное совпадение данных. По разработанным методикам анализа были изучены образцы апатита (анализ Sr изотопной системы) и образцы апатита, монацита, титанита (анализ Sm/Nd изотопной системы). Заключение. Проделанная методическая работа по анализу изотопных систем Sm/Nd и Sr рекомендована для изучения различных минералов: апатит, титанита, алланит, монацит (анализ Sm/Nd изотопной системы); апатит (анализ Sr изотопной системы). Достигнутые погрешности анализа позволяют использовать результаты для интерпретаций различных геохимических процессов.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>Research subject</title><p>Research subject. The Sm/Nd isotope system was investigated using inter-laboratory natural samples of apatite, titanite, allanite, monazite, as well as intra-laboratory samples of apatite (from carbonatites, Ilmenogorsk massif, Ural), monazite (from pegmatites of the Aduy granite massif and its framing, Middle Urals) and titanite (from calcite veins, Saranov skoye chromite deposit, Middle Urals and from alkaline pegmatite, Shpat mine, Vishnevy mountains, South Urals). The Sr isotope system was investigated using inter-laboratory natural apatite samples and intra-laboratory apatite samples (from the apatite-carbonate vein, Slyudyanogorskoe deposit, Irkutsk region and from carbonatites, Ilmenogorsk massif, Ural).</p></sec><sec><title>Methods</title><p>Methods. The research was carried using a Neptune Plus multicollector mass spectrometer with inductively coupled plasma (ThermoFisher) equipped with an NWR 213 (ESI) laser ablation attachment, located in a room of ISO class 7 at the “Geoanalyst” Center for Collective Use (IGG Ural Branch of the Russian Academy of Sciences, Ekaterinburg). Results. The article describes methodological approaches for studying Sm/Nd and Sr isotope systems in natural phosphate and silicate minerals by inductively coupled plasma mass spectrometry with laser ablation, implemented on the equipment of the Center for Collective Use “Geoanalyst” (IGG Ural Branch of the Russian Academy of Sciences, Ekaterinburg). A comparative analysis of the obtained results with those reported in literature showed their satisfactory agreement. The developed analytical approaches were used to study apatite samples (analysis of the Sr isotope system) and those of apatite, monazite, titanite (analysis of the Sr isotope system). Conclusions. The developed approaches to the analysis of Sm/Nd and Sr isotopic systems can be recommended for investigating such minerals, as apatite, titanite, allanite, monazite (analysis of the Sm/Nd isotope system); apatite (analysis of the Sr isotope system). The achieved analysis errors allow the results to be used for interpreting various geochemical processes.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>лазерная абляция</kwd><kwd>изотопный состав Sm/Nd</kwd><kwd>изотопный состав Sr</kwd></kwd-group><kwd-group xml:lang="en"><kwd>laser ablation</kwd><kwd>Sm/Nd isotopic composition</kwd><kwd>Sr isotopic composition</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в ЦКП “Геоаналитик” при финансовой поддержке гранта РФФИ № 20-05-00403 и в рамках темы № AAAA-A18-118053090045-8 государственного задания ИГГ УрО РАН. Дооснащение и комплексное развитие ЦКП “Геоаналитик” ИГГ УрО РАН осуществляется при финансовой поддержке гранта Министерства науки и высшего образования Российской Федерации, Соглашение № 075-15-2021-680</funding-statement><funding-statement xml:lang="en">LA-ICP-MS study was supported by RFBR grant No. 20-05-00403 and the state assignment of Centre for Collective use “Geoanalist” of IGG uB RAS (No. AAAA-A18-118053090045-8). The re-equipment and comprehensive development of the Centre for Collective use “Geoanalist” is fnancially supported by the grant of the Ministry of Science and higher Education of the Russian Federation. Agreement No. 075-15-2021-680</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">Калинин П.В., Роненсон Б.М. (1957) Геолого-структурные особенности и генезис Слюдянских флогопитовых месторождений. 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