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@ARTICLE{BarSinai:22907,
      author       = {Bar Sinai, Y. and Brener, E.A. and Bouchbinder, E.},
      title        = {{S}low rupture of frictional interfaces},
      journal      = {Geophysical research letters},
      volume       = {39},
      issn         = {0094-8276},
      address      = {Washington, DC},
      publisher    = {American Geophysical Union},
      reportid     = {PreJuSER-22907},
      pages        = {L03308},
      year         = {2012},
      note         = {We thank O. Ben-David and J. Fineberg for numerous
                      insightful discussions. EB acknowledges support of the James
                      S. McDonnell Foundation, the Minerva Foundation with funding
                      from the Federal German Ministry for Education and Research,
                      the Harold Perlman Family Foundation and the William Z. and
                      Eda Bess Novick Young Scientist Fund.},
      abstract     = {The failure of frictional interfaces and the spatiotemporal
                      structures that accompany it are central to a wide range of
                      geophysical, physical and engineering systems. Recent
                      geophysical and laboratory observations indicated that
                      interfacial failure can be mediated by slow slip rupture
                      phenomena which are distinct from ordinary, earthquake-like,
                      fast rupture. These discoveries have influenced the way we
                      think about frictional motion, yet the nature and properties
                      of slow rupture are not completely understood. We show that
                      slow rupture is an intrinsic and robust property of simple
                      non-monotonic rate-and-state friction laws. It is associated
                      with a new velocity scale c(min), determined by the friction
                      law, below which steady state rupture cannot propagate. We
                      further show that rupture can occur in a continuum of
                      states, spanning a wide range of velocities from c(min) to
                      elastic wave-speeds, and predict different properties for
                      slow rupture and ordinary fast rupture. Our results are
                      qualitatively consistent with recent high-resolution
                      laboratory experiments and may provide a theoretical
                      framework for understanding slow rupture phenomena along
                      frictional interfaces. Citation: Bar Sinai, Y., E. A.
                      Brener, and E. Bouchbinder (2012), Slow rupture of
                      frictional interfaces, Geophys. Res. Lett., 39, L03308,
                      doi:10.1029/2011GL050554.},
      keywords     = {J (WoSType)},
      cin          = {PGI-2},
      ddc          = {550},
      cid          = {I:(DE-Juel1)PGI-2-20110106},
      pnm          = {Grundlagen für zukünftige Informationstechnologien},
      pid          = {G:(DE-Juel1)FUEK412},
      shelfmark    = {Geosciences, Multidisciplinary},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000300241500003},
      doi          = {10.1029/2011GL050554},
      url          = {https://juser.fz-juelich.de/record/22907},
}