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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-1944</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 причинах и этапах перестройки речной сети Северо-Сосьвинского Урала в позднем кайнозое</article-title><trans-title-group xml:lang="en"><trans-title>On causes and stages of drainage net changes at the North Sosva Urals during Late Cenozoic</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>Миняйло</surname><given-names>Л. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Minyailo</surname><given-names>L. A.</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>ЗапСибНИГНИ</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1978</year></pub-date><pub-date pub-type="epub"><day>15</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>76</fpage><lpage>81</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Миняйло Л.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Миняйло Л.А.</copyright-holder><copyright-holder xml:lang="en">Minyailo L.A.</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/1944">https://geomorphology.igras.ru/jour/article/view/1944</self-uri><abstract><p>On the Urals area under consideration the drainage net has been found to change not less than four times since Oligocene Main causes of the drainage net changes were the ocean's transgressions and covering the valleys with sediments of transgression cycles. During each new stage the drainage net developed transgressively, following the basin level lowering.</p></abstract><trans-abstract xml:lang="en"><p>On the Urals area under consideration the drainage net has been found to change not less than four times since Oligocene Main causes of the drainage net changes were the ocean's transgressions and covering the valleys with sediments of transgression cycles. During each new stage the drainage net developed transgressively, following the basin level lowering.</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>
