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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">nature</journal-id><journal-title-group><journal-title xml:lang="ru">Природопользование</journal-title><trans-title-group xml:lang="en"><trans-title>Nature Management</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2079-3928</issn><publisher><publisher-name>Институт природопользования НАН Беларуси</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">nature-30</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>ГЕОЛОГИЯ. ПОЛЕЗНЫЕ ИСКОПАЕМЫЕ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOLOGY. MINERALS</subject></subj-group></article-categories><title-group><article-title>История формирования рельефа южной Беларуси в четвертичное время</article-title><trans-title-group xml:lang="en"><trans-title>Relief forming history of south Belarus area during quaternary period</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>Матвеев</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Matveyev</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Матвеев Алексей Васильевич – академик, доктор геолого-минералогических наук, профессор, главный научный сотрудник.</p><p>ул. Ф. Скорины, 10, 220076, Минск</p></bio><bio xml:lang="en"><p>Aleksey V. Matveyev – Academician, D. Sc. (Geological and Mineralogical), Professor, Chief Researcher, Institute of Nature Management of the National Academy of Sciences of Belarus.</p><p>10, F. Skoriny Str., 220076, Minsk</p></bio><email xlink:type="simple">matveyev@nature-nas.by</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт природопользования НАН Беларуси</institution></aff><aff xml:lang="en"><institution>Institute of Nature Management of the National Academy of Sciences of Belarus</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>28</day><month>10</month><year>2025</year></pub-date><volume>0</volume><issue>1</issue><fpage>83</fpage><lpage>90</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Матвеев А.В., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Матвеев А.В.</copyright-holder><copyright-holder xml:lang="en">Matveyev A.V.</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.nature-journal.by/jour/article/view/30">https://www.nature-journal.by/jour/article/view/30</self-uri><abstract><p>На основании анализа разрезов буровых скважин, опубликованных материалов по палеогеографии и геологии региона построена серия палеогеоморфологических схем, выявлены основные факторы формирования на территории южной Беларуси крупной корытообразной формы земной поверхности и своеобразного «полесского» рельефа (ландшафта), который в близком к современному виде сформировался в муравинское межледниковье. Наиболее распространенными категориями рельефа были заболоченные озерно-аллювиальные и аллювиальные низины, которые с севера, запада и востока окаймлялись ледниковыми равнинами и возвышенностями припятского оледенения, а с юга – несколько тектонической приподнятой поверхностью Украинского Полесья. В послемуравинское время рельеф развивался унаследованно, происходило только некоторое изменение площадей распространения основных генетических типов за счет проявления аллювиальных и озерно-аллювиальных процессов.</p></abstract><trans-abstract xml:lang="en"><p>A series of paleogeomorphological schemes based on the analysis of borehole sections and published materials on paleogeography and geology of the region was constructed. The main formation factors of a large trough-shaped form of the earth’s surface and a kind of “Polesie” relief (landscape) in southern Belarus were revealed. Its modern configuration was formed during the Muravian interglacial. Marshy lacustrine-alluvial and alluvial lowlands were the most common relief categories. They were bordered by glacial plains and highlands of the Pripyatian glaciation from the north, west and east, and by a slightly tectonically uplifted surface of the Ukrainian Polesie from the south. The relief was developing in a hereditary manner in the post-Muravian time. There were only some changes in the areas of the main genetic types’ distribution due to the alluvial and lacustrine-alluvial processes.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>палеорельеф</kwd><kwd>межледниковье</kwd><kwd>факторы формирования рельефа</kwd><kwd>«полесский» рельеф (ландшафт)</kwd></kwd-group><kwd-group xml:lang="en"><kwd>paleorelief</kwd><kwd>interglacial</kwd><kwd>relief formation factors</kwd><kwd>"Polesie" relief (landscape)</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">Ажгиревич, Л. Ф. Буроугольная формация кайнозоя Белоруссии / Л. Ф. Ажгиревич. – Минск, 1981. – 200 с.</mixed-citation><mixed-citation xml:lang="en">Azhgirevich L. F. Burougol'naya formaciya kajnozoya Belorussii [Brown coal formation of the Cenozoic of Belarus]. Minsk, 1981, 200 p. 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