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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-2694</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>Речная сеть Южно-Енисейского района (Енисейский кряж) в мелу и палеогене</article-title><trans-title-group xml:lang="en"><trans-title>Drainage network of the Southern Yenisei region (the Yenisei Ridge) at the Cretaceous and Paleogene</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>Чеха</surname><given-names>В. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Chekha</surname><given-names>V. P.</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>ПГО «Красноярскгеология»</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>102</fpage><lpage>106</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Чеха В.П., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Чеха В.П.</copyright-holder><copyright-holder xml:lang="en">Chekha V.P.</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/2694">https://geomorphology.igras.ru/jour/article/view/2694</self-uri><abstract><p>Paleo-geomorphological and litho-facial methods have been used to reconstruct Cretaceous and Paleogene drainage network of the Southern Yenisei region. Former valleys pattern is proved to be essentially different from the recent one, the fact being important 'for gold placers situation and shape.</p></abstract><trans-abstract xml:lang="en"><p>Paleo-geomorphological and litho-facial methods have been used to reconstruct Cretaceous and Paleogene drainage network of the Southern Yenisei region. Former valleys pattern is proved to be essentially different from the recent one, the fact being important 'for gold placers situation and shape.</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>
