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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">10.33623/0579-9406-2016-1-3-9</article-id><article-id custom-type="elpub" pub-id-type="custom">geolmsu-3</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></article-categories><title-group><article-title>Новый взгляд на состав и строение глубинных оболочек планет земной группы</article-title><trans-title-group xml:lang="en"><trans-title>New insight into the composition and the structure of the terrestrial planet’s deep seated zones</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>Пущаровский</surname><given-names>Д. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Pushcharovsky</surname><given-names>D. Yu.</given-names></name></name-alternatives><email xlink:type="simple">dean@geol.msu.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>Пущаровский</surname><given-names>Ю. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Pushcharovsky</surname><given-names>Yu. M.</given-names></name></name-alternatives><email xlink:type="simple">dean@geol.msu.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московский государственный университет имени М.В. Ломоносова, геологический факультет</institution><country>Russian Federation</country></aff><aff xml:lang="ru" id="aff-2"><institution>Геологический институт РАН</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2016</year></pub-date><pub-date pub-type="epub"><day>28</day><month>02</month><year>2016</year></pub-date><volume>0</volume><issue>1</issue><fpage>3</fpage><lpage>9</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Пущаровский Д.Ю., Пущаровский Ю.М., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Пущаровский Д.Ю., Пущаровский Ю.М.</copyright-holder><copyright-holder xml:lang="en">Pushcharovsky D.Y., Pushcharovsky Y.M.</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/3">https://vestnik.geol.msu.ru/jour/article/view/3</self-uri><abstract><p>Рассмотрены новые подходы, расширяющие представления о составе и строении мантии Земли и планет земной группы. Новые данные указывают на более дробную структуру глубинных оболочек Земли и Луны. Проанализированы результаты экспериментов при высоких давлении и температуре, позволяющие смоделировать изменения структуры и свойств важнейших компонентов состава мантии и ядер Земли, Луны, «газовых» (Юпитера, Сатурна) и ледяных (Урана, Нептуна) «гигантов».</p></abstract><trans-abstract xml:lang="en"><p>The structure and composition of the Earth’s mantle and of the terrestrial planets are considered in the light of the new scientific approaches. These data indicate on the further structural subdivision of the Earth’s inner geospheres and of the Moon’s deep seated zones. The results of HP- and HT-experiments related with the transformation of the main mantle’s and core’s components of the Earth, Moon, gaseus giants (Jupiter and Saturn) and ice giant planets (Uranus and Neptune) reveal the new structure and property changes.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>минеральные трансформации</kwd><kwd>минералогия мантии</kwd><kwd>состав ядер Земли и Луны</kwd></kwd-group><kwd-group xml:lang="en"><kwd>mineral transitions</kwd><kwd>mantle mineralogy</kwd><kwd>composition of the Earth’s and of the Moon’s core</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">Пущаровский Ю.М. О трех парадигмах в геологии // Геотектоника. 1995. № 1. C. 4-11.</mixed-citation><mixed-citation xml:lang="en">Пущаровский Ю.М. О трех парадигмах в геологии // Геотектоника. 1995. № 1. 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