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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 pub-id-type="doi">10.15356/0435-4281-2005-3-98-101</article-id><article-id custom-type="elpub" pub-id-type="custom">geomorf-474</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>О СООТНОШЕНИИ СКОРОСТЕЙ СОВРЕМЕННОЙ ДЕНУДАЦИИ И ТЕКТОНИЧЕСКИХ ПОДНЯТИЙ ЭПИГЕОСИНКЛИНАЛЬНЫХ ГОР ЕВРАЗИИ</article-title><trans-title-group xml:lang="en"><trans-title>THE RECENT DENUDATION RATE AND UPLIFT VELOCITY OF EPIGEOSYNCLINAL MOUNTAINS OF EURASIA</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>Мамина</surname><given-names>Л. Р.</given-names></name><name name-style="western" xml:lang="en"><surname>Mamina</surname><given-names>L. R.</given-names></name></name-alternatives><email xlink:type="simple">geomorfologiya@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Казанский (Приволжский) федеральный университет, Казань</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Kazan (Volga region) Federal University, Kazan</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2005</year></pub-date><pub-date pub-type="epub"><day>14</day><month>07</month><year>2015</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>98</fpage><lpage>101</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Мамина Л.Р., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Мамина Л.Р.</copyright-holder><copyright-holder xml:lang="en">Mamina L.R.</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/474">https://geomorphology.igras.ru/jour/article/view/474</self-uri><abstract><p>Recent mechanical denudation rate in Alps, Carpathians, West and East Caucasus, and Himalayas was estimated by the sediment discharge data. The values obtained were compared with tectonic uplift velocities. Everywhere within the axial zone of the mountains the tectonic uplift predominates denudation in ratio 1.8:1 - 6.4:1. This indicates the continuous upward evolution of mountains. Recent rates of mountains uplift are higher than average rates for the whole neotectonic stage.</p><p><ext-link xlink:href="https://www.elibrary.ru/item.asp?id=9148988" ext-link-type="uri">Статья в библиотеке elibrary.ru</ext-link></p></abstract><trans-abstract xml:lang="en"/><kwd-group xml:lang="ru"><kwd>Денудация</kwd><kwd>тектоника</kwd><kwd>эпигеосинклиналь</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Denudation</kwd><kwd>tectonics</kwd><kwd>epigeosynclinal</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">Лопатин Д.В. Эрозия и сток наносов//Природа. 1950. № 7. 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