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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-3135</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>Природа генеральных черт рельефа дна океана (кинематика плит, рифтогенные хребты и трансформные разломы океанической литосферы)</article-title><trans-title-group xml:lang="en"><trans-title>Nature of general features of the ocean floor topography (plate kinematics, riftogenic ridges and transform faults in the oceanic lithosphere)</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>Ушаков</surname><given-names>С. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Ushakov</surname><given-names>S. 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, географический факультет</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1994</year></pub-date><pub-date pub-type="epub"><day>01</day><month>03</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>13</fpage><lpage>22</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Ушаков С.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Ушаков С.А.</copyright-holder><copyright-holder xml:lang="en">Ushakov S.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/3135">https://geomorphology.igras.ru/jour/article/view/3135</self-uri><abstract><p>In the article the history of establishment of the plate tectonics theory and its influence on modification of knowledge of the endogenous sea floor geomorphology is stated briefly. Kinematics of main plates and age of sea floor, or more exactly - the time of cooling of the oceanic lithosphere, are examined as the principal plate tectonics reasons determined the nature of general features of the Earth's face. It is noted that a location of riftogenic mid-ocean ridges in young spreading ocean basins is determined by the character of tension and the lithosphere breaking up in rifting zones. It is considered an influence of transform faults on the pattern of the sea floor topography of the World Ocean.</p></abstract><trans-abstract xml:lang="en"><p>In the article the history of establishment of the plate tectonics theory and its influence on modification of knowledge of the endogenous sea floor geomorphology is stated briefly. Kinematics of main plates and age of sea floor, or more exactly - the time of cooling of the oceanic lithosphere, are examined as the principal plate tectonics reasons determined the nature of general features of the Earth's face. It is noted that a location of riftogenic mid-ocean ridges in young spreading ocean basins is determined by the character of tension and the lithosphere breaking up in rifting zones. It is considered an influence of transform faults on the pattern of the sea floor topography of the World Ocean.</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>
