1 Ocak 2014 Dergi makalesi Açık Erişim

Ergintav, S.; Reilinger, R. E.; Cakmak, R.; Floyd, M.; Cakir, Z.; Dogan, U.; King, R. W.; McClusky, S.; Ozener, H.

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  <identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/113864</identifier>
  <creators>
    <creator>
      <creatorName>Ergintav, S.</creatorName>
      <givenName>S.</givenName>
      <familyName>Ergintav</familyName>
    </creator>
    <creator>
      <creatorName>Reilinger, R. E.</creatorName>
      <givenName>R. E.</givenName>
      <familyName>Reilinger</familyName>
      <affiliation>MIT, Dept Earth Atmospher &amp; Planetary Sci, Cambridge, MA USA</affiliation>
    </creator>
    <creator>
      <creatorName>Cakmak, R.</creatorName>
      <givenName>R.</givenName>
      <familyName>Cakmak</familyName>
      <affiliation>TUBITAK, MRC, Earth &amp; Marine Sci Inst, Kocaeli, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Floyd, M.</creatorName>
      <givenName>M.</givenName>
      <familyName>Floyd</familyName>
      <affiliation>MIT, Dept Earth Atmospher &amp; Planetary Sci, Cambridge, MA USA</affiliation>
    </creator>
    <creator>
      <creatorName>Cakir, Z.</creatorName>
      <givenName>Z.</givenName>
      <familyName>Cakir</familyName>
      <affiliation>Istanbul Tech Univ, Dept Geol, TR-80626 Istanbul, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>Dogan, U.</creatorName>
      <givenName>U.</givenName>
      <familyName>Dogan</familyName>
      <affiliation>Yildiz Tech Univ, Dept Geomat, Istanbul, Turkey</affiliation>
    </creator>
    <creator>
      <creatorName>King, R. W.</creatorName>
      <givenName>R. W.</givenName>
      <familyName>King</familyName>
    </creator>
    <creator>
      <creatorName>McClusky, S.</creatorName>
      <givenName>S.</givenName>
      <familyName>McClusky</familyName>
      <affiliation>Australia Natl Univ, RSES, Canberra, ACT, Australia</affiliation>
    </creator>
    <creator>
      <creatorName>Ozener, H.</creatorName>
      <givenName>H.</givenName>
      <familyName>Ozener</familyName>
    </creator>
  </creators>
  <titles>
    <title>Istanbul'S Earthquake Hot Spots: Geodetic Constraints On Strain Accumulation Along Faults In The Marmara Seismic Gap</title>
  </titles>
  <publisher>Aperta</publisher>
  <publicationYear>2014</publicationYear>
  <dates>
    <date dateType="Issued">2014-01-01</date>
  </dates>
  <resourceType resourceTypeGeneral="Text">Journal article</resourceType>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/113864</alternateIdentifier>
  </alternateIdentifiers>
  <relatedIdentifiers>
    <relatedIdentifier relatedIdentifierType="DOI" relationType="IsIdenticalTo">10.1002/2014GL060985</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">During the past century, a series of predominantly westward migrating M&amp;gt;7 earthquakes broke an similar to 1000km section of the North Anatolian Fault (NAF). The only major remaining seismic gap along the fault is under the Sea of Marmara (Main Marmara Fault (MMF)). We use 20years of GPS observations to estimate strain accumulation on fault segments in the Marmara Sea seismic gap. We report the first direct observations of strain accumulation on the Princes' Islands segment of the MMF, constraining the slip deficit rate to 10-15mm/yr. In contrast, the central segment of the MMF that was thought to be the most likely location for the anticipated gap-filling earthquakes shows no evidence of strain accumulation, suggesting that fault motion is accommodated by fault creep. We conclude that the Princes' Islands segment is most likely to generate the next M&amp;gt;7 earthquake along the Sea of Marmara segment of the NAF.</description>
  </descriptions>
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