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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">10.24930/1681-9004-2024-24-2-214-225</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-2056</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>Важнейшие структурные типы в неорганической химии и минералогии: новые данные</article-title><trans-title-group xml:lang="en"><trans-title>Major structural types in inorganic chemistry and mineralogy: New data</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>Еремин</surname><given-names>Н. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Eremin</surname><given-names>N. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Геологический факультет, кафедра кристаллографии и кристаллохимии</p><p>119234, г. Москва, ГСП-1, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>Nikolay N. Eremin</p><p>Department of Crystallography and Crystal Chemistry, Geological Facility</p><p>1 Leninskie Gory, Mosсow 119234</p></bio><email xlink:type="simple">neremin@mail.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>Гурбанова</surname><given-names>О. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Gurbanova</surname><given-names>O. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Геологический факультет, кафедра кристаллографии и кристаллохимии</p><p>119234, г. Москва, ГСП-1, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>Olga A. Gurbanova</p><p>Department of Crystallography and Crystal Chemistry, Geological Facility</p><p>1 Leninskie Gory, Mosсow 119234</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>Подображных</surname><given-names>А. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Podobrazhnykh</surname><given-names>A. D.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Геологический факультет, кафедра кристаллографии и кристаллохимии</p><p>119234, г. Москва, ГСП-1, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>Andrey D. Podobrazhnykh</p><p>Department of Crystallography and Crystal Chemistry, Geological Facility</p><p>1 Leninskie Gory, Mosсow 119234</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>Ионидис</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Ionidis</surname><given-names>N. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Геологический факультет, кафедра кристаллографии и кристаллохимии</p><p>119234, г. Москва, ГСП-1, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>Nikita A. Ionidis</p><p>Department of Crystallography and Crystal Chemistry, Geological Facility</p><p>1 Leninskie Gory, Mosсow 119234</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>Шванская</surname><given-names>Л. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Schvanskaya</surname><given-names>L. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Геологический факультет, кафедра кристаллографии и кристаллохимии</p><p>119234, г. Москва, ГСП-1, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>Larisa V. Schvanskaya</p><p>Department of Crystallography and Crystal Chemistry, Geological Facility</p><p>1 Leninskie Gory, Mosсow 119234</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>Еремина</surname><given-names>Т. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Eremina</surname><given-names>T. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Геологический факультет, кафедра кристаллографии и кристаллохимии</p><p>119234, г. Москва, ГСП-1, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>Tatiana A. Eremina</p><p>Department of Crystallography and Crystal Chemistry, Geological Facility</p><p>1 Leninskie Gory, Mosсow 119234</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>03</day><month>05</month><year>2024</year></pub-date><volume>24</volume><issue>2</issue><fpage>214</fpage><lpage>225</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Еремин Н.Н., Гурбанова О.А., Подображных А.Д., Ионидис Н.А., Шванская Л.В., Еремина Т.А., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Еремин Н.Н., Гурбанова О.А., Подображных А.Д., Ионидис Н.А., Шванская Л.В., Еремина Т.А.</copyright-holder><copyright-holder xml:lang="en">Eremin N.N., Gurbanova O.A., Podobrazhnykh A.D., Ionidis N.A., Schvanskaya L.V., Eremina T.A.</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/2056">https://www.lithosphere.ru/jour/article/view/2056</self-uri><abstract><p>Объект исследования. Структурные типы с различными стехиометрическими соотношениями между химическими элементами. Цель. Анализ распространенности структурных типов с различными стехиометрическими соотношениями между химическими элементами, а именно простые вещества, бинарные соединения, тройные соединения со стехиометрией ABX3, тройные соединения со стехиометрией AB2X4. Общие положения. Анализ проводился с помощью актуальных на сегодняшний момент баз структурных данных неорганических соединений ICSD (Inorganic Crystal Structure Database) и PCD (Pearson’s Crystal Data), определено количество записей с наиболее распространенными структурными типами по состоянию на 2013 и 2023 г., приведены их классификационные обозначения в разных базах данных и годах, проанализированы ранги структурных типов по минералам и неорганическим соединениям. Для всех рассмотренных структурных типов указаны минералы, кристаллизующиеся в этих структурных типах, по данным ISCD 2023, с выборкой только по числу зарегистрированных в IMA минералов (International Mineralogical Association – Commission on New Minerals, Nomenclature and Classiﬁcation) по состоянию на март 2023 г. Также для всех кристаллизующихся в рассмотренных структурных типах минералов приведены русскоязычные названия минералов в соответствии с базой данных WWW-МИНКРИСТ. Выводы. Для каждого стехиометрического соотношения определены наиболее вероятные причины его реализации в тех или иных структурных типах. Исходя из кристаллохимических принципов обсуждена “популярность” структурных типов среди неорганических соединений и минералов и указаны факторы, оказывающие наибольшее влияние на это.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. Structural types with different stoichiometric correlations between chemical elements. Aim. To analyze the prevalence of structural types with different stoichiometric correlations between chemical elements, such as simple substances with binary compounds, triple compounds with stoichiometry ABX3, triple compounds with stoichiometry AB2X4. Key points. The analysis was conducted using the databases of inorganic compounds ICSD (Inorganic Crystal Structure Database) and PCD (Pearson’s Crystal Data). The number of entries with the most typical structural types for 2013 and 2023 are determined. Their classifications in various databases for different years are given. The ranks of structural types for minerals and inorganic compounds are analyzed. The minerals crystallized in all the considered structural types are indicated according to the 2023 ISCD data, sampling only by the number of minerals registered in IMA (International Mineralogical Association – Commission on New Minerals, Nomenclature and Classification) for March 2023. The Russian names of minerals are presented in accordance with the database WWW-MINCRIST for the minerals crystallizing in all the structural types under consideration. Conclusions. The most probable causes for the realization of each stoichiometric correlation in various structural types are determined. The prevalence of certain structural types among inorganic compounds and minerals, as well as the underlying reasons, are discussed based on the principles of crystal chemistry.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>структурный тип</kwd><kwd>минералы</kwd><kwd>неорганические соединения</kwd><kwd>ранги структурных типов</kwd></kwd-group><kwd-group xml:lang="en"><kwd>structural type</kwd><kwd>minerals</kwd><kwd>inorganic compounds</kwd><kwd>ranks of structural types</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках госбюджетной темы № АААА-А16-116033010121-7 “Новые минералы и синтетические аналоги: кристаллогенезис и особенности кристаллохимии”.</funding-statement><funding-statement xml:lang="en">The study was funded by the state budget research project No. AAAA-A16-116033010121-7 “New minerals and synthetic analogues: crystallogenesis and features of crystal chemistry”.</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">Бокий Г.Б. 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