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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-2704</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>Зависимость вертикального расчленения рельефа дна юго-восточного сектора Индийского океана от глубины</article-title><trans-title-group xml:lang="en"><trans-title>Vertical dissection of the ocean floor as related to the ocean depth within the SE sector of the Indian Ocean</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>Кара</surname><given-names>В. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Kara</surname><given-names>V. I.</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>Спириденко</surname><given-names>Л. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Spiridenko</surname><given-names>L. I.</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>НИПИОкеангеофизика</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1987</year></pub-date><pub-date pub-type="epub"><day>15</day><month>11</month><year>2022</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>49</fpage><lpage>56</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кара В.И., Спириденко Л.И., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Кара В.И., Спириденко Л.И.</copyright-holder><copyright-holder xml:lang="en">Kara V.I., Spiridenko L.I.</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/2704">https://geomorphology.igras.ru/jour/article/view/2704</self-uri><abstract><p>Analysis of digital model of the SE Indian floor topography using specially developed software revealed the range of the ocean floor vertical dissection to be related to the ocean depth. Six topographic levels have been indentified differing in the character of the relation. The paper describes the relation and tries to explain it by the earthcrust evolution.</p></abstract><trans-abstract xml:lang="en"><p>Analysis of digital model of the SE Indian floor topography using specially developed software revealed the range of the ocean floor vertical dissection to be related to the ocean depth. Six topographic levels have been indentified differing in the character of the relation. The paper describes the relation and tries to explain it by the earthcrust evolution.</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>
