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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-3471</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>Роль тектоники в эволюции рельефа Горного Алтая</article-title><trans-title-group xml:lang="en"><trans-title>The role of neotectonic in the relief evolution of Gorny Altai</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>Новиков</surname><given-names>И. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Novikov</surname><given-names>I. S.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ОИГГМ СО РАН</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1998</year></pub-date><pub-date pub-type="epub"><day>14</day><month>12</month><year>2023</year></pub-date><volume>0</volume><issue>1</issue><fpage>82</fpage><lpage>91</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Новиков И.С., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Новиков И.С.</copyright-holder><copyright-holder xml:lang="en">Novikov I.S.</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/3471">https://geomorphology.igras.ru/jour/article/view/3471</self-uri><abstract><p>A small impact of selective denudation on the relief evolution of Gorny Altai has been established on the basis of geomorphological structure analysis and its relation to geological composition. New model for relief development has been put forward. According to this model vertical movements which have caused the formation of Altai Mts. have taken place due to regional contraction of this area. At first a system of swells separated by troughs appeared during the contraction, and then it was broken by faults, of which shears and thrusts were predominant.</p></abstract><trans-abstract xml:lang="en"><p>A small impact of selective denudation on the relief evolution of Gorny Altai has been established on the basis of geomorphological structure analysis and its relation to geological composition. New model for relief development has been put forward. According to this model vertical movements which have caused the formation of Altai Mts. have taken place due to regional contraction of this area. At first a system of swells separated by troughs appeared during the contraction, and then it was broken by faults, of which shears and thrusts were predominant.</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>
