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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">dan</journal-id><journal-title-group><journal-title xml:lang="ru">Доклады Национальной академии наук Беларуси</journal-title><trans-title-group xml:lang="en"><trans-title>Doklady of the National Academy of Sciences of Belarus</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1561-8323</issn><issn pub-type="epub">2524-2431</issn><publisher><publisher-name>The Republican Unitary Enterprise Publishing House "Belaruskaya Navuka"</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.29235/1561-8323-2019-63-6-755-760</article-id><article-id custom-type="elpub" pub-id-type="custom">dan-843</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>НАУКИ О ЗЕМЛЕ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>EARTH SCIENCES</subject></subj-group></article-categories><title-group><article-title>Условия формирования пород русиновского комплекса кристаллического фундамента Беларуси</article-title><trans-title-group xml:lang="en"><trans-title>formation сonditions of the rocks from the Rusinovsky complex of the crystalline basement of Belarus</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>Гуринович</surname><given-names>М. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Hurynovich</surname><given-names>M. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Гуринович Марина Петровна – науч. сотрудник. </p><p>ул. Купревича, 7, 220141, Минск</p></bio><bio xml:lang="en"><p>Hurynovich Marina Petrovna – Researcher. </p><p>7, Kuprevich Str., 220141, Minsk</p></bio><email xlink:type="simple">marfapk88@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии</institution></aff><aff xml:lang="en"><institution>Institute for Geology</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>07</day><month>01</month><year>2020</year></pub-date><volume>63</volume><issue>6</issue><fpage>755</fpage><lpage>760</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Гуринович М.П., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Гуринович М.П.</copyright-holder><copyright-holder xml:lang="en">Hurynovich M.P.</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://doklady.belnauka.by/jour/article/view/843">https://doklady.belnauka.by/jour/article/view/843</self-uri><abstract><p>Определены условия формирования ультрабазит-базитовых пород русиновского комплекса кристаллического фундамента Беларуси на основе петролого-геохимических данных. Показано, что породы русиновского комплекса разделяются на две петрохимические серии: магнезиальную и титано-железистую. Особенности редкоэлементного состава пород указывают на расплавление и переработку первоначального состава магмы, а также ее коровую контаминацию. По условиям формирования породы комплекса близки к островодужным образованиям.</p></abstract><trans-abstract xml:lang="en"><p>Based on the petrological and geochemical data, the formation conditions of the ultrabasic-basic rocks of the Rusinovsky complex of the crystalline basement of Belarus are determined. It is shown that the rocks of the Rusinovsky complex are divided into two petrochemical series: magnesian and titanium-ferruginous. The peculiarities of the rare-element rock composition indicate the melting and processing of the original composition of magma, and its crust contamination. According to the formation conditions of the rock, the complex is close to island-arc formations.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>кристаллический фундамент</kwd><kwd>русиновский комплекс</kwd><kwd>ультабазит-базиты</kwd><kwd>условия формирования</kwd></kwd-group><kwd-group xml:lang="en"><kwd>crystalline basement</kwd><kwd>rusinovsky complex</kwd><kwd>ultrabasic-basites</kwd><kwd>formation conditions</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">Железорудные формации докембрия Белоруссии / А. С. Махнач [и др.]. – Минск: Наука и техника, 1974. – 144 с.</mixed-citation><mixed-citation xml:lang="en">Makhnach A. S., Dominikovskii G. G., Pasyukevich V. I., Stasevich A. I., Shvarkov S. L., Kolotovskii A. S., Il’kevich G. I. Iron ore formations of Precambrian Belarus. Minsk, Nauka i tekhnika Publ., 1974. 144 p. 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