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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">geolmsu</journal-id><journal-title-group><journal-title xml:lang="ru">ВЕСТНИК МОСКОВСКОГО УНИВЕРСИТЕТА. СЕРИЯ 4. ГЕОЛОГИЯ</journal-title><trans-title-group xml:lang="en"><trans-title>Moscow University Bulletin. Series 4. Geology</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0579-9406</issn><publisher><publisher-name>Издательский Дом МГУ</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.33623/0579-9406-2019-2-94-103</article-id><article-id custom-type="elpub" pub-id-type="custom">geolmsu-314</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>КРАТКИЕ СООБЩЕНИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>SHORT MESSAGES</subject></subj-group></article-categories><title-group><article-title>Свидетельство кумулусной кристаллизации и локальные проявления эклогитового метаморфизма в оливиновом габбро комплекса Марун-Кеу (Полярный Урал)</article-title><trans-title-group xml:lang="en"><trans-title>Evidence of cumulate crystallization and local development of the eclogite-facies metamorphism in the olivine gabbro of the Marun-Keu complex, Polar Urals, Russia</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>Лю</surname><given-names>И.</given-names></name><name name-style="western" xml:lang="en"><surname>Liu</surname><given-names>Y. Y.</given-names></name></name-alternatives><bio xml:lang="ru"><p>геологический факультет, кафедра петрологиии, аспирант</p></bio><email xlink:type="simple">yingyuan1990@gmail.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>Перчук</surname><given-names>А. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Perchuk</surname><given-names>A. L.</given-names></name></name-alternatives><bio xml:lang="ru"><p>геологический факультет, кафедра петрологиии, профессор, зав. кафедрой, докт. геол.-минерал. н.</p></bio><email xlink:type="simple">alp@geol.msu.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Зиновьева</surname><given-names>Н. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Zinovieva</surname><given-names>N. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>геологический факультет, кафедра петрологиии, зав. лабораторией, докт. геол.-минерал. н.</p></bio><email xlink:type="simple">nzinov@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московский государственный университет имени М.В. Ломоносова</institution><country>Russian Federation</country></aff><aff xml:lang="ru" id="aff-2"><institution>Московский государственный университет имени М.В. Ломоносова;&#13;
Институт экспериментальной минералогии РАН имени Д.С. Коржинского</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>28</day><month>04</month><year>2019</year></pub-date><volume>0</volume><issue>2</issue><fpage>94</fpage><lpage>103</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Лю И.Y., Перчук А.Л., Зиновьева Н.Г., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Лю И., Перчук А.Л., Зиновьева Н.Г.</copyright-holder><copyright-holder xml:lang="en">Liu Y.Y., Perchuk A.L., Zinovieva N.G.</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://vestnik.geol.msu.ru/jour/article/view/314">https://vestnik.geol.msu.ru/jour/article/view/314</self-uri><abstract><p>Приведены результаты детального петрологического исследования меланократового оливинового габбро, частично преобразованного при эклогитовом метаморфизме. В породе установлены структурные признаки кумулусной кристаллизации на магматическом этапе. Наибольшим изменениям во время эклогитового метаморфизма подверглись плагиоклазы, по которым развивается мелко-скрытозернистый агрегат, сложенный минералами высокобарного парагенезисом. На этом же этапе по периферии плагиоклазовых (фельзических) доменов на контактах с (Fe, Mg)-минералами сформировались коронарные структуры. Минеральная термобарометрия и метод моделирования фазовых равновесий показали близкие параметры метаморфизма – температуру Т=680±60 ᵒC давление Р=2,2±0,4 ГПа, соответствующие установленным нами ранее условиям образования эклогитов и гранат-амфиболового перидотита из этого же комплекса.</p></abstract><trans-abstract xml:lang="en"><p>The paper presents the results of a detailed petrological study of olivine gabbro transformed to different extent by eclogite-facies metamorphism. Textural features of cumulate crystallization in the rock are presented. Plagioclases underwent the greatest alteration and replaced by finegrained aggregate during eclogite-facies metamorphism. Corona textures are developed along the boundaries of the plagioclase (felscic) domains at the contacts with (Fe,Mg)-minerals during eclogite facies event. The mineral thermobarometry and phase equilibrium modeling provide P-T metamorphic conditions in relatively narrow range of temperature 680±60 ᵒC and pressure Р=2,2±0.4 GPa. This is in a good agreement with the previously established conditions for the formation of eclogites and garnet-amphibole peridotite from the same complex.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>эклогитовый метаморфизм</kwd><kwd>габбро</kwd><kwd>кумулат</kwd><kwd>коронарная структура</kwd><kwd>Полярный Урал</kwd><kwd>Марун-Кеу</kwd></kwd-group><kwd-group xml:lang="en"><kwd>eclogite-facies metamorphism</kwd><kwd>gabbro</kwd><kwd>cumulate</kwd><kwd>corona texture</kwd><kwd>Polar Urals</kwd><kwd>Marun-Keu</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">Куликова К.В. Редкоземельные элементы в породах и минералах из эклогитов района Слюдяной Горки (хребет Марункеу, Полярный Урал) // Петрология и минералогия севера Урала и Тимана. Сыктывкар, 2005. С. 115–124.</mixed-citation><mixed-citation xml:lang="en">Куликова К.В. 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