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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%">Leon-Rios, S.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Rietbrock, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bie, L. D.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Beck, S.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Charvis, Philippe</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Comte, D.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Galve, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Meltzer, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Roecker, S.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ruiz, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Segovia, M.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Physical properties controlling earthquake ruptures : two study cases along the South American Subduction Zone</title>
        <secondary-title>Geophysical Research Letters</secondary-title>
      </titles>
      <pages>e2025GL114615 [12 p.]</pages>
      <keywords>
        <keyword>tomography</keyword>
        <keyword>seismology</keyword>
        <keyword>subduction zone</keyword>
        <keyword>seismic slip</keyword>
        <keyword>EQUATEUR</keyword>
        <keyword>CHILI</keyword>
        <keyword>AMERIQUE DU SUD</keyword>
        <keyword>PEDERNALES</keyword>
        <keyword>ANTOFAGASTA</keyword>
      </keywords>
      <dates>
        <year>2025</year>
      </dates>
      <call-num>fdi:010094399</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Geophysical Research Letters</full-title>
      </periodical>
      <isbn>0094-8276</isbn>
      <accession-num>ISI:001536276100001</accession-num>
      <number>14</number>
      <electronic-resource-num>10.1029/2025gl114615</electronic-resource-num>
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          <url>https://www.documentation.ird.fr/intranet/publi/2025-09/010094399.pdf</url>
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      </urls>
      <volume>52</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Seismic velocity models were compared with coseismic slip distributions for two megathrust earthquakes that occurred along the South American subduction zone. By analyzing the distribution of Vp/Vs ratios, we found that seismic anomalies with values higher or lower than the average coincide with the boundaries of the earthquake ruptures. In contrast, the regions characterized by intermediate Vp/Vs values may represent a mechanical "sweet spot" where the physical properties create favorable conditions for sustained rupture propagation. Our methodology, which combines the Vp/Vs distribution and the analysis of coseismic slip models, could reveal the rupture-prone regions and the likely magnitude of potential earthquakes, providing relevant information for seismic hazard assessment.</abstract>
      <custom6>066</custom6>
      <custom7>Chili / Équateur</custom7>
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