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<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<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-2207</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>Анализ продольного профиля долин при морфоструктурных исследованиях</article-title><trans-title-group xml:lang="en"><trans-title>Valley profile analysis for morphostructural studies</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>Воскресенский</surname><given-names>К. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Voskresensky</surname><given-names>K. 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>Московский государственный университет имени М.В.Ломоносова, Географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1980</year></pub-date><pub-date pub-type="epub"><day>30</day><month>08</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>48</fpage><lpage>53</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Воскресенский К.С., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Воскресенский К.С.</copyright-holder><copyright-holder xml:lang="en">Voskresensky K.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/2207">https://geomorphology.igras.ru/jour/article/view/2207</self-uri><abstract><p>A longitudinal profile of a valley is discussed which is drawn considering -the river's discharge. Analysis- of such reduced profile makes possible to distinguish the influence of rocks resistance and of differentiated tectonic movements as well as to estimate them quantitatively. 50 tributaries of the Burinda River (the Amur drainage basin) have been analyzed using the described technique and a schematic map of relative block movements have been compiled.</p></abstract><trans-abstract xml:lang="en"><p>A longitudinal profile of a valley is discussed which is drawn considering -the river's discharge. Analysis- of such reduced profile makes possible to distinguish the influence of rocks resistance and of differentiated tectonic movements as well as to estimate them quantitatively. 50 tributaries of the Burinda River (the Amur drainage basin) have been analyzed using the described technique and a schematic map of relative block movements have been compiled.</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>
