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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-2685</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>Величина денудационного среза Алдано-Станового региона за меозойско-кайнозоиское время</article-title><trans-title-group xml:lang="en"><trans-title>Scale of the denudation for mesozoic-Cenozoic time in Aldan-Stanovoi region</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>Веселов</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Veselov</surname><given-names>A. M.</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>ВСЕГЕИ</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1987</year></pub-date><pub-date pub-type="epub"><day>15</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>47</fpage><lpage>53</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Веселов А.М., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Веселов А.М.</copyright-holder><copyright-holder xml:lang="en">Veselov A.M.</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/2685">https://geomorphology.igras.ru/jour/article/view/2685</self-uri><abstract><p>Value of the denudation (i. e. mean thickness of rock layer removed by denudation) is defined for different stages of the topographic evolution of the Aldan-Stanovoi region on the basis of analysis of the relief history. Danudation values for Jurassic and Cretaceous stages were obtained using bulk method and amounted to 400 and 300 meters respectively. Variations of the denudation rate are taken into account. For Cretaceous - Paleogene and Neogene-Quaternary stages mean denudation values of 100 to 150 and 50 meters were obtained with considerable variations in different geomorphological structures for the last stage. For Mesozoic - Cenozoic time in the Aldan-Stanovoi region mean denudation value is 1000 meters, maximum value being more than 2000 meters in lonascending blocks, minimum - 100 to 150 meters is blocks of inherited downwarping.</p></abstract><trans-abstract xml:lang="en"><p>Value of the denudation (i. e. mean thickness of rock layer removed by denudation) is defined for different stages of the topographic evolution of the Aldan-Stanovoi region on the basis of analysis of the relief history. Danudation values for Jurassic and Cretaceous stages were obtained using bulk method and amounted to 400 and 300 meters respectively. Variations of the denudation rate are taken into account. For Cretaceous - Paleogene and Neogene-Quaternary stages mean denudation values of 100 to 150 and 50 meters were obtained with considerable variations in different geomorphological structures for the last stage. For Mesozoic - Cenozoic time in the Aldan-Stanovoi region mean denudation value is 1000 meters, maximum value being more than 2000 meters in lonascending blocks, minimum - 100 to 150 meters is blocks of inherited downwarping.</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>
