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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-2213</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>Структурно-геоморфологическая характеристика шельфа Керченского и Таманского полуостровов</article-title><trans-title-group xml:lang="en"><trans-title>Structural geomorphological characteristics of the shelf of the Kerch and Taman peninsulas</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>Щербаков</surname><given-names>Ф. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Shcherbakov</surname><given-names>F. 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>Чистяков</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Chistyakov</surname><given-names>A. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Московский государственный университет имени М.В.Ломоносова, Геологический факультет</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>2</issue><issue-title>Геоморфология</issue-title><fpage>80</fpage><lpage>85</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Щербаков Ф.А., Чистяков А.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Щербаков Ф.А., Чистяков А.А.</copyright-holder><copyright-holder xml:lang="en">Shcherbakov F.A., Chistyakov A.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/2213">https://geomorphology.igras.ru/jour/article/view/2213</self-uri><abstract><p>The shelf topography is described as well as parts of continental slope and continental rise near the Kerch and Taman peninsular. The bottom landforms are interpreted in terms of their structure using the data on the peninsulas and shell geology. Main structural elements of SW-NE strike are proved to be distinctly pronounced at the shelf and possibly at continental slope and rise.</p></abstract><trans-abstract xml:lang="en"><p>The shelf topography is described as well as parts of continental slope and continental rise near the Kerch and Taman peninsular. The bottom landforms are interpreted in terms of their structure using the data on the peninsulas and shell geology. Main structural elements of SW-NE strike are proved to be distinctly pronounced at the shelf and possibly at continental slope and rise.</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>
