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  <front>
    <journal-meta>
      <journal-title-group>
        <journal-title xml:lang="ru">Жизнь Земли. Междисциплинарный научно-практический журнал</journal-title>
        <journal-title xml:lang="en">Life of the Earth</journal-title>
      </journal-title-group>
    </journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.29003/m3550.0514-7468.2023_45_3/341-354</article-id>            <article-id pub-id-type="publisher-id">1725</article-id>
      <title-group>
        <article-title xml:lang="ru">Физическое моделирование условий формирования краевых плато на примере структур Северной Атлантики</article-title>        <trans-title-group xml:lang="en"><trans-title>Physical modeling of the formation conditions of marginal plateaux on the example of structures in the North Atlantic Ocean</trans-title></trans-title-group>      </title-group>
      <contrib-group>
                    <contrib contrib-type="author">
              <string-name xml:lang="ru">Агранов Г.Д., Дубинин Е.П., Грохольский А.Л.</string-name>              <string-name xml:lang="en">Agranov, G.D., Dubinin, E.P., Grokholskii, A.L.</string-name>            </contrib>
              </contrib-group>

            <pub-date pub-type="epub" iso-8601-date="2023-09-06">
        <day>06</day>
        <month>09</month>
        <year>2023</year>
      </pub-date>
      
      <volume>45</volume>      <issue>3</issue>      <fpage>341</fpage>      <lpage>354</lpage>
            <history>
                <date date-type="accepted" iso-8601-date="2023-09-06">
  <day>06</day>
  <month>09</month>
  <year>2023</year>
</date>
      </history>
      
      <abstract xml:lang="ru"><p>Рассматриваются особенности образования краевых плато в ранний период раскрытия Северной Атлантики. Океаническое раскрытие между Гренландией и Европой (образование Северной Атлантики) началось примерно 50–55 млн лет назад после длительного периода рифтогенеза, за которым последовало формирование спредингового хребта Эгир и образование бассейна Норвежской котловины. С этого момента началось формирование серии специфических структур – краевых плато. В&nbsp;статье с помощью метода физического моделирования рассмотрены условия их формирования. Выделены три группы структур и проведена их типизация по механизму образования. Каждому из типов структур была посвящена серия экспериментов. Проведено сопоставление экспериментальных результатов с предполагаемой моделью формирования и эволюции краевых плато.</p></abstract>      <trans-abstract xml:lang="en"><p>Peculiarities of the formation of marginal plateaus in the early period of the opening of the North Atlantic Ocean are considered. The oceanic opening between Greenland and Europe (formation of the North Atlantic Ocean) began approx. 50–55 Mya after a long period of rifting, followed by the formation of the Aegir spreading ridge and the formation of the basin of the Norwegian Deep. Since that moment, the formation of a series of specific structures (marginal plateaus) began. The article considers conditions for their formation, using the physical modeling method. Three groups of structures were distinguished and typified according to the formation mechanism. A series of experiments was performed to each type of structures. Experimental results are compared with our proposed model for the formation and evolution of marginal plateaux.</p></trans-abstract>
      <kwd-group xml:lang="ru"><kwd>Северная Атлантика</kwd><kwd>краевые плато</kwd><kwd>плато Воринг</kwd><kwd>плато Ермак</kwd><kwd>плато Моррис-Джесуп</kwd><kwd>пассивная окраина</kwd><kwd>физическое моделирование</kwd></kwd-group>      <kwd-group xml:lang="en"><kwd>North Atlantic Ocean</kwd><kwd>marginal plateaux</kwd><kwd>Vøring Plateau</kwd><kwd>Yermak Plateau</kwd><kwd>Morris Jesup Rise</kwd><kwd>passive margin</kwd><kwd>physical modeling</kwd></kwd-group>
          </article-meta>
  </front>
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