1 Ocak 2011 Dergi makalesi Açık Erişim

Bouchon, Michel; Karabulut, Hayrullah; Aktar, Mustafa; Ozalaybey, Serdar; Schmittbuhl, Jean; Bouin, Marie-Paule

DataCite XML

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/92405</identifier>
  <creators>
    <creator>
      <creatorName>Bouchon, Michel</creatorName>
      <givenName>Michel</givenName>
      <familyName>Bouchon</familyName>
    </creator>
    <creator>
      <creatorName>Karabulut, Hayrullah</creatorName>
      <givenName>Hayrullah</givenName>
      <familyName>Karabulut</familyName>
    </creator>
    <creator>
      <creatorName>Aktar, Mustafa</creatorName>
      <givenName>Mustafa</givenName>
      <familyName>Aktar</familyName>
    </creator>
    <creator>
      <creatorName>Ozalaybey, Serdar</creatorName>
      <givenName>Serdar</givenName>
      <familyName>Ozalaybey</familyName>
      <affiliation>Marmara Res Ctr, Earth &amp; Marine Sci Inst, TUBITAK, TR-41470 Gebze, Kocaeli, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Schmittbuhl, Jean</creatorName>
      <givenName>Jean</givenName>
      <familyName>Schmittbuhl</familyName>
    </creator>
    <creator>
      <creatorName>Bouin, Marie-Paule</creatorName>
      <givenName>Marie-Paule</givenName>
      <familyName>Bouin</familyName>
    </creator>
  </creators>
  <titles>
    <title>Extended Nucleation Of The 1999 M-W 7.6 Izmit Earthquake</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2011</publicationYear>
  <dates>
    <date dateType="Issued">2011-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/92405</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1126/science.1197341</relatedIdentifier>
  </relatedIdentifiers>
  <rightsList>
    <rights rightsURI="http://www.opendefinition.org/licenses/cc-by">Creative Commons Attribution</rights>
    <rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
  </rightsList>
  <descriptions>
    <description descriptionType="Abstract">Laboratory and theoretical studies suggest that earthquakes are preceded by a phase of developing slip instability in which the fault slips slowly before accelerating to dynamic rupture. We report here that one of the best-recorded large earthquakes to date, the 1999 moment magnitude (M-w) 7.6 Izmit (Turkey) earthquake, was preceded by a seismic signal of long duration that originated from the hypocenter. The signal consisted of a succession of repetitive seismic bursts, accelerating with time, and increased low-frequency seismic noise. These observations show that the earthquake was preceded for 44 minutes by a phase of slow slip occurring at the base of the brittle crust. This slip accelerated slowly initially, and then rapidly accelerated in the 2 minutes preceding the earthquake.</description>
  </descriptions>
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