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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-2886</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>Методика научных исследований</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Scientific Research Methods</subject></subj-group></article-categories><title-group><article-title>О методике палеогеоморфологических реконструкций субаквального рельефа бассейнов карбонатонакопления</article-title><trans-title-group xml:lang="en"><trans-title>On methods of paleogeomorphological reconstructions of bottom topography</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>Кузнецов</surname><given-names>В. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Kuznetsov</surname><given-names>V. G.</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 институт нефти и газа им. И.М. Губкина</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1991</year></pub-date><pub-date pub-type="epub"><day>22</day><month>12</month><year>2022</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>32</fpage><lpage>38</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кузнецов В.Г., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Кузнецов В.Г.</copyright-holder><copyright-holder xml:lang="en">Kuznetsov V.G.</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/2886">https://geomorphology.igras.ru/jour/article/view/2886</self-uri><abstract><p>A method of reconstruction of paleobasins depth is developed based on integrated results of analysis facies, thickness and pattern of stratification, taking into consideration specific features of carbonates and salts accumulation. As an example, carbonate - saline series of the Vendian - Cambrian age within the Siberian platform is considered.</p></abstract><trans-abstract xml:lang="en"><p>A method of reconstruction of paleobasins depth is developed based on integrated results of analysis facies, thickness and pattern of stratification, taking into consideration specific features of carbonates and salts accumulation. As an example, carbonate - saline series of the Vendian - Cambrian age within the Siberian platform is considered.</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>
