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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-2194</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>Палеорельеф визейского возраста на территории Удмуртии</article-title><trans-title-group xml:lang="en"><trans-title>Visean paleo-relief at the Udmurtian territory</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>Атласман</surname><given-names>Ю. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Atlasman</surname><given-names>Yu. E.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Камское отделение ВНИГНИ</institution><country>Russian Federation</country></aff><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>1</issue><issue-title>Геоморфология</issue-title><fpage>71</fpage><lpage>76</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Атласман Ю.Е., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Атласман Ю.Е.</copyright-holder><copyright-holder xml:lang="en">Atlasman Y.E.</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/2194">https://geomorphology.igras.ru/jour/article/view/2194</self-uri><abstract><p>Sedimentation of the Visean terrigenous series at the Udrnurtian territory was analysed from the paleogeornorphological point of view. For Malinovian, Bobrikovian and Tula ages paleogeomorphological schemes l:500000 were drawn, based on sediments thickness, the latter being reconstructed considering sediments compression, sand content etc. Main geomorphic features of the area can be described for Visean age on the base of the investigation carried out, and zones can be outlined promising for non-anticlinal oil and gas deposits.</p></abstract><trans-abstract xml:lang="en"><p>Sedimentation of the Visean terrigenous series at the Udrnurtian territory was analysed from the paleogeornorphological point of view. For Malinovian, Bobrikovian and Tula ages paleogeomorphological schemes l:500000 were drawn, based on sediments thickness, the latter being reconstructed considering sediments compression, sand content etc. Main geomorphic features of the area can be described for Visean age on the base of the investigation carried out, and zones can be outlined promising for non-anticlinal oil and gas deposits.</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>
