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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-2872</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>Корреляционный анализ серии пале геоморфологических карт юго-востока Европейской территории СССР</article-title><trans-title-group xml:lang="en"><trans-title>Correlation between paleogeomorphological maps of the South-East of the European USSR</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>Брылев</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Brylev</surname><given-names>V. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Бендерович</surname><given-names>Л. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Benderovich</surname><given-names>L. Yu.</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>Волгоградский пединститут</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1991</year></pub-date><pub-date pub-type="epub"><day>19</day><month>12</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>49</fpage><lpage>56</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Брылев В.А., Бендерович Л.Ю., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Брылев В.А., Бендерович Л.Ю.</copyright-holder><copyright-holder xml:lang="en">Brylev V.A., Benderovich L.Y.</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/2872">https://geomorphology.igras.ru/jour/article/view/2872</self-uri><abstract><p>A series of paleogeomorphological maps of the Lower Volga region, Manych area, Middle and Lower Don basin and Western Caspian Lowland have been compiled for eleven typical stages of continental evolution since Devonian to the recent time. Main morphostuctural elements are shown on each of the maps. Statistical correlation of the morphostructures' development is carried out using criteria of the rank correlation, inherited and newly formed morphostuctures being identified. Paleohydrological network development has been studied.</p></abstract><trans-abstract xml:lang="en"><p>A series of paleogeomorphological maps of the Lower Volga region, Manych area, Middle and Lower Don basin and Western Caspian Lowland have been compiled for eleven typical stages of continental evolution since Devonian to the recent time. Main morphostuctural elements are shown on each of the maps. Statistical correlation of the morphostructures' development is carried out using criteria of the rank correlation, inherited and newly formed morphostuctures being identified. Paleohydrological network development has been studied.</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>
