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      <source-app name="Horizon">Horizon</source-app>
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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%">Dondin, F.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Lebrun, J. F.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Kelfoun, Karim</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Fournier, N.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Randrianasolo, A.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Sector collapse at Kick 'em Jenny submarine volcano (Lesser Antilles) : numerical simulation and landslide behaviour</title>
        <secondary-title>Bulletin of Volcanology</secondary-title>
      </titles>
      <pages>595-607</pages>
      <keywords>
        <keyword>Kick 'em Jenny</keyword>
        <keyword>Sector collapse</keyword>
        <keyword>Submarine landslide</keyword>
        <keyword>Numerical modelling</keyword>
        <keyword>Rheology</keyword>
        <keyword>VolcFlow</keyword>
        <keyword>Lesser Antilles</keyword>
      </keywords>
      <dates>
        <year>2012</year>
      </dates>
      <call-num>fdi:010055709</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Bulletin of Volcanology</full-title>
      </periodical>
      <isbn>0258-8900</isbn>
      <accession-num>ISI:000300577200019</accession-num>
      <number>2</number>
      <electronic-resource-num>10.1007/s00445-011-0554-0</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010055709</url>
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        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/2012/04/010055709.pdf</url>
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      <volume>74</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Kick 'em Jenny volcano is the only known active submarine volcano in the Lesser Antilles. It lies within a horseshoe-shaped structure open to the west northwest, toward the deep Grenada Basin. A detailed bathymetric survey of the basin slope at Kick 'em Jenny and resulting high-resolution digital elevation model allowed the identification of a major submarine landslide deposit. This deposit is thought to result from a single sector collapse event at Kick 'em Jenny and to be linked to the formation of the horseshoe-shaped structure. We estimated the volume and the leading-edge runout of the landslide to be ca. 4.4 km(3) and 14 km, respectively. We modelled a sector collapse event of a proto Kick 'em Jenny volcano using VolcFlow, a finite difference code based on depth-integrated mass and momentum equations. Our models show that the landslide can be simulated by either a Coulomb-type rheology with low basal friction angles (5.5A degrees-6.5A degrees) and a significant internal friction angle (above 17.5A degrees) or, with better results, by a Bingham rheology with low Bingham kinematic viscosity (0 &lt; nu (B) &lt; 30 m(2)/s) and high shear strength (130 &lt; I-3 a parts per thousand currency signaEuro parts per thousand 180 m(2)/s(2)). The models and the short runout distance suggest that the landslide travelled as a stiff cohesive flow affected by minimal granular disaggregation and slumping on a non-lubricated surface. The main submarine landslide deposit can therefore be considered as a submarine mass slide deposit that behaved like a slump.</abstract>
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