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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">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-3441</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>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Влияние тектонических особенностей на формирование ледникового рельефа Белоруссии</article-title><trans-title-group xml:lang="en"><trans-title>Tectonic influence on glacial landforms formation in Byelorussia</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>Нечипоренко</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Nechiporenko</surname><given-names>L. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Институт геохимии и геофизики АН Белоруссии</institution><country>Belarus</country></aff><pub-date pub-type="collection"><year>1997</year></pub-date><pub-date pub-type="epub"><day>06</day><month>12</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>83</fpage><lpage>87</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Нечипоренко Л.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Нечипоренко Л.А.</copyright-holder><copyright-holder xml:lang="en">Nechiporenko L.A.</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://geomorphology.igras.ru/jour/article/view/3441">https://geomorphology.igras.ru/jour/article/view/3441</self-uri><abstract><p>Tectonic deformations had a strong influence on the distribution of glaciation at Byelorussia during Pleistocene. Velocity and direction of ice movements were repeatedly changed that affected the completeness of Pleistocene stratigraphy, thickness and distribution of separate layers. Very clearly tectonic influence shows at distribution and size of marginal glacial complexes and in their inner structure. Linear elements of glacial relief controlled by faults are frequent.</p></abstract><trans-abstract xml:lang="en"><p>Tectonic deformations had a strong influence on the distribution of glaciation at Byelorussia during Pleistocene. Velocity and direction of ice movements were repeatedly changed that affected the completeness of Pleistocene stratigraphy, thickness and distribution of separate layers. Very clearly tectonic influence shows at distribution and size of marginal glacial complexes and in their inner structure. Linear elements of glacial relief controlled by faults are frequent.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
