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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-3257</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>Крупные гравитационные смещения и морфоструктурные узлы Малого Кавказа</article-title><trans-title-group xml:lang="en"><trans-title>Large gravitational displacements and morphostructural nodes of the Lesser Caucasus</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>Жидков</surname><given-names>М. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Zhidkov</surname><given-names>M. P.</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>Институт географии РАН</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1996</year></pub-date><pub-date pub-type="epub"><day>20</day><month>03</month><year>2023</year></pub-date><volume>0</volume><issue>2</issue><fpage>72</fpage><lpage>78</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Жидков М.П., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Жидков М.П.</copyright-holder><copyright-holder xml:lang="en">Zhidkov M.P.</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/3257">https://geomorphology.igras.ru/jour/article/view/3257</self-uri><abstract><p>Morphostructural nodes are most important elements of the earthorust block structure. They are formed by lineaments intersections and feature increased rates of enogenic and exogenic processes. A majority of the morphostructural nodes of the Lesser Caucasus are prone to earthquakes of magnitudes not less than 5.5. Field data, aerial photos interpretation and analysis of literature reveal numerous large gravitational mass displacements (landslides, rockfalls, etc.) restricted to highly seismic morphostructural nodes. The largest displacements are recorded in the nodes prone to earthquakes of M = 6.5 or more. The indentification of rnorphostructural nodes liable to form large gravitational displacements is of theoretical and practical interest.</p></abstract><trans-abstract xml:lang="en"><p>Morphostructural nodes are most important elements of the earthorust block structure. They are formed by lineaments intersections and feature increased rates of enogenic and exogenic processes. A majority of the morphostructural nodes of the Lesser Caucasus are prone to earthquakes of magnitudes not less than 5.5. Field data, aerial photos interpretation and analysis of literature reveal numerous large gravitational mass displacements (landslides, rockfalls, etc.) restricted to highly seismic morphostructural nodes. The largest displacements are recorded in the nodes prone to earthquakes of M = 6.5 or more. The indentification of rnorphostructural nodes liable to form large gravitational displacements is of theoretical and practical interest.</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>
