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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Narteau, C.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Byrdina, Svetlana</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Shebalin, P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Schorlemmer, D.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Common dependence on stress for the two fundamental laws of statistical seismology</title>
        <secondary-title>Nature</secondary-title>
      </titles>
      <pages>642-U113</pages>
      <dates>
        <year>2009</year>
      </dates>
      <call-num>fdi:010048437</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Nature</full-title>
      </periodical>
      <isbn>0028-0836</isbn>
      <accession-num>ISI:000272277900039</accession-num>
      <number>7273</number>
      <electronic-resource-num>10.1038/nature08553</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010048437</url>
        </related-urls>
        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/2009/12/010048437.pdf</url>
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      </urls>
      <volume>462</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Two of the long-standing relationships of statistical seismology are power laws: the Gutenberg-Richter relation(1) describing the earthquake frequency-magnitude distribution, and the Omori-Utsu law(2) characterizing the temporal decay of aftershock rate following a main shock. Recently, the effect of stress on the slope (the b value) of the earthquake frequency-magnitude distribution was determined(3) by investigations of the faulting-style dependence of the b value. In a similar manner, we study here aftershock sequences according to the faulting style of their main shocks. We show that the time delay before the onset of the power-law aftershock decay rate ( the c value) is on average shorter for thrust main shocks than for normal fault earthquakes, taking intermediate values for strike-slip events. These similar dependences on the faulting style indicate that both of the fundamental power laws are governed by the state of stress. Focal mechanisms are known for only 2 per cent of aftershocks. Therefore, c and b values are independent estimates and can be used as new tools to infer the stress field, which remains difficult to measure directly.</abstract>
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      <custom1>UR157</custom1>
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