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GEOPHYSICAL RESEARCH LETTERS, VOL. ???, XXXX, DOI:10.1029/, A mechanism for preseismic steady rupture fronts1
 

Summary: GEOPHYSICAL RESEARCH LETTERS, VOL. ???, XXXX, DOI:10.1029/,
A mechanism for preseismic steady rupture fronts1
observed in laboratory experiments2
Y. Kaneko
Institute of Geophysics and Planetary Physics, Scripps Institution of3
Oceanography, University of California - San Diego, La Jolla, USA4
J.-P. Ampuero
Division of Geological and Planetary Sciences, California Institute of5
Technology, Pasadena, USA6
Y. Kaneko, Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography,
Univerisity of California - San Diego, 9500 Gilman Drive MC 0225, La Jolla, California 92093,
USA. (ykaneko@ucsd.edu)
J.-P. Ampuero, Division of Geological and Planetary Sciences, California Institute of Tech-
nology, 1200 E. California Boulevard MC 252-21, Pasadena, California 91125, USA. (am-
puero@gps.caltech.edu)
D R A F T October 8, 2011, 6:25pm D R A F T
X - 2 KANEKO AND AMPUERO: MODELING PRESEISMIC STEADY RUPTURE
It has been shown that the onset of frictional instability is characterized7
by a transition from stable, quasi-static rupture growth to unstable, inertially-8
controlled high-speed rupture. In particular, slow rupture fronts propagat-9

  

Source: Ampuero, Jean Paul - Division of Geological and Planetary Sciences, California Institute of Technology

 

Collections: Geosciences