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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">10.24930/1681-9004-2021-21-1-70-89</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-1399</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>Минералогия спессартин-кварцевых пород Сихотэ-Алиня</article-title><trans-title-group xml:lang="en"><trans-title>Mineralogy of spessartine-quartz rocks of the Sikhote-Alin</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>Перевозникова</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Perevoznikova</surname><given-names>E. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>690022, г. Владивосток, пр. 100-летия Владивостока, 159</p></bio><bio xml:lang="en"><p>159 Sentury of Vladivostok 100th av., Vladivostok 690022</p></bio><email xlink:type="simple">elenavalper@yandex.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>Казаченко</surname><given-names>В. Т.</given-names></name><name name-style="western" xml:lang="en"><surname>Kazachenko</surname><given-names>V. T.</given-names></name></name-alternatives><bio xml:lang="ru"><p>690022, г. Владивосток, пр. 100-летия Владивостока, 159</p></bio><bio xml:lang="en"><p>159 Sentury of Vladivostok 100th av., Vladivostok 690022</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Дальневосточный геологический институт ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Far Eastern Geological Institute, Far Eastern Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>03</day><month>03</month><year>2021</year></pub-date><volume>21</volume><issue>1</issue><fpage>70</fpage><lpage>89</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Перевозникова Е.В., Казаченко В.Т., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Перевозникова Е.В., Казаченко В.Т.</copyright-holder><copyright-holder xml:lang="en">Perevoznikova E.V., Kazachenko V.T.</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/1399">https://www.lithosphere.ru/jour/article/view/1399</self-uri><abstract><p>Объект исследований. Статья посвящена изучению спессартин-кварцевых пород триасовой кремневой формации Сихотэ-Алиня. Объектами исследований служили коренные выходы спессартин-кварцевых пород Горной и Широкопаднинской площадей Малиновского и Ольгинского рудных районов (в Самаркинском и Таухинском террейнах соответственно).  Материалы и методы. Отбор каменного материала проводился штуфным способом. Диагностика минералов выполнялась под микроскопом в проходящем и отраженном свете и заверялась определением их составов. Анализы минералов (в аншлифах) выполнены в ДВГИ ДВО РАН на рентгеноспектральном микроанализаторе JXA8100.  Результаты. Спессартин-кварцевые и марганцевосиликатные породы занимают одинаковое положение в разрезе триасовых отложений Таухинского и Самаркинского террейнов, что свидетельствует о синхронном накоплении осадков (протолитов этих пород) в едином осадочном бассейне. В Таухинском террейне эти породы образовались при контактовом метаморфизме кремнисто-родохрозитовых тел в позднем мелу при становлении гранитоидных массивов Восточно-Сихотэ-Алинского вулканоплутонического пояса, а в Самаркинском террейне – в раннемеловое время при формировании гранитоидных тел Хунгари-Татибинского плутонического пояса. Протолитами кремнисто-родохрозитовых пород и их контактово-метаморфизованных аналогов являлись кремнистые илы биогенной природы. Из-за одинаковой природы протолитов и близких условий метаморфизма марганцевосиликатные и спессартин-кварцевые породы обнаруживают минералогическое сходство. Оно выражается в присутствии многих общих для них минералов, таких как спессартин, члены ильменит-пирофанитового ряда, титанит, монацит, бастнезит, алланит, апатит, циркон, бадделеит, торианит и др. В спессартин-кварцевых породах Сихотэ-Алиня присутствует группа редких в природе минералов: чералит, грэйит, редкая разновидность фтор-глиноземистого титанита, в котором около половины Ti замещено Al, и кармелтазит.  Заключение. Появление (при контактовом метаморфизме кремнисто-родохрозитовых пород в восстановительных условиях) спессартин-кварцевых или, вместо них, марганцевосиликатных пород, сложенных главным образом пироксеноидами, определяляется относительными количествами карбонатного и глинистого вещества в исходных осадках, а также содержаниями в них Ba и щелочей.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. The article is devoted to the study of spessartine-quartz rocks of the Triassic chert formation of the Sikhote-Alin. The research objects involved the outcrops of spessartine-quartz rocks of the Gornaya and Shirokaya Pad areas from Malinovka and Olga ore districts (in the Samarka and Taukha terranes respectively).  Materials and methods. The selection of stone materials was performed manually. The diagnostic of minerals was performed using the microscope in transmitted and reflected light and carried out by the determination of their composion. The polished sections of the minerals were investigated at the FEGI FEB RAS using JXA8100 microanalysers.  Results. Spessartine-quartz and manganese silicate rocks occupy the same position in the section of the Triassic deposits of the Taukha and Samarka terrains. This indicates a synchronous accumulation of sediments (protoliths of these rocks) in a single sedimentary basin. The rocks formed by contact metamorphism in the Late and Early Cretaceous large granitoid massifs. This process is manifested in the presence of a variety of such minerals, as spessartine, members of the ilmenite-pyrophanite series, titanite, monazite, bastnesite, allanite, apatite, zircon, baddeleyite, torianite and others. The rocks under study also include such rare minerals, as cheralite, greyite and a rare variety of fluorine-aluminous titanite.  Conclusion. The occurrence (during contact metamorphism of siliceous-rhodochrosite rocks) of spessartine-quartz or manganesesilicate rocks composed mainly of pyroxenoids, was determined by both the relative amounts of carbonate and clay matter, as well as the concentrations of Ba and alkalis in the initial sediments.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>спессартин-кварцевые породы</kwd><kwd>кремнисто-родохрозитовые породы</kwd><kwd>марганцевосиликатные породы</kwd><kwd>минералогия</kwd><kwd>чералит</kwd><kwd>кармелтазит</kwd><kwd>грэйит</kwd><kwd>триасовая кремневая формация</kwd><kwd>Сихотэ-Алинь</kwd></kwd-group><kwd-group xml:lang="en"><kwd>spessartine-quartz rocks</kwd><kwd>siliceous-rhodochrosite rocks</kwd><kwd>manganesesilicate rocks</kwd><kwd>mineralogy</kwd><kwd>cheralite</kwd><kwd>carmeltazite</kwd><kwd>greyite</kwd><kwd>Triassic chert formation</kwd><kwd>Sikhote-Alin</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Брусницын А.И. 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