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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">46906</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Mega-earthquake on 11 March 2011 in Japan and aftershock process dynamics' development</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Mega-earthquake on 11 March 2011 in Japan and aftershock process dynamics' development</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Tikhonov</surname>
       <given-names>I N</given-names>
      </name>
      <name xml:lang="en">
       <surname>Tikhonov</surname>
       <given-names>I N</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Institute of Marine Geology and Geophysics of Far Eastern Branch of RAS, Yuzhno-Sakhalinsk, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Marine Geology and Geophysics of Far Eastern Branch of RAS, Yuzhno-Sakhalinsk, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>12</volume>
   <issue>1</issue>
   <fpage>1</fpage>
   <lpage>9</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-11-10T01:11:30+03:00">
     <day>10</day>
     <month>11</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46906/view">https://rjes.ru/en/nauka/article/46906/view</self-uri>
   <abstract xml:lang="ru">
    <p>The article provides data on seismic activity and recurrence periods of strongest (M ge; 7.6 earthquakes for the historical and instrumental periods of observations in epicenter area of a mega-event. It was shown that a period of recurrence of strongest events in this area was about 40 years. To the east of Honshu island a long seismic gap (~800nbsp;km was discovered, located to the south of latitude 39oN and filled recently with aftershocks of the 11.03.2011 mega-earthquake.  Significant analogues in aftershocks dynamics of the 2011 Great Japan Earthquake with aftershock sequences of the Sumatra-Andaman 2004, Mw = 9.3 and Simushir 2006, Mw = 8.3 earthquakes were described. A similarity over time for the first event and over space field of aftershocks' epicenters for the second event was noted. The author suggested a possibility of occurrence of a recurrent strong event with magnitude approximately equal to 8, shifted along the main thrust towards the deep oceanic trench. </p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The article provides data on seismic activity and recurrence periods of strongest (M ge; 7.6 earthquakes for the historical and instrumental periods of observations in epicenter area of a mega-event. It was shown that a period of recurrence of strongest events in this area was about 40 years. To the east of Honshu island a long seismic gap (~800nbsp;km was discovered, located to the south of latitude 39oN and filled recently with aftershocks of the 11.03.2011 mega-earthquake.  Significant analogues in aftershocks dynamics of the 2011 Great Japan Earthquake with aftershock sequences of the Sumatra-Andaman 2004, Mw = 9.3 and Simushir 2006, Mw = 8.3 earthquakes were described. A similarity over time for the first event and over space field of aftershocks' epicenters for the second event was noted. The author suggested a possibility of occurrence of a recurrent strong event with magnitude approximately equal to 8, shifted along the main thrust towards the deep oceanic trench. </p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Large earthquake</kwd>
    <kwd>recurrence of the large earthquakes</kwd>
    <kwd>seismic gap</kwd>
    <kwd>mega-earthquake</kwd>
    <kwd>aftershock sequence</kwd>
    <kwd>strongest aftershock</kwd>
    <kwd>field of aftershocks' epicenters</kwd>
    <kwd>probable scenario</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Large earthquake</kwd>
    <kwd>recurrence of the large earthquakes</kwd>
    <kwd>seismic gap</kwd>
    <kwd>mega-earthquake</kwd>
    <kwd>aftershock sequence</kwd>
    <kwd>strongest aftershock</kwd>
    <kwd>field of aftershocks' epicenters</kwd>
    <kwd>probable scenario</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
 <back>
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</article>
