Lapusta, Nadia - Division of Geological and Planetary Sciences, California Institute of Technology

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Lapusta, Nadia - Division of Geological and Planetary Sciences, California Institute of Technology

SUBMITTED TO JOURNAL OF GEOPHYSICAL RESEARCH, APRIL 2008 Rate and state friction laws can explain scaling of small
Int J Fract DOI 10.1007/s10704-010-9479-4
REVISION SUBMITTED TO JOURNAL OF GEOPHYSICAL RESEARCH, APRIL 2008 Variability of earthquake nucleation in continuum models of
Geophys. J. Int. () , 117 Analysis of supershear transition regimes in rupture experiments
Rupture modes in laboratory earthquakes: Effect of fault prestress and nucleation conditions
LAPUSTA ET AL.: DYNAMIC ANALYSIS OF SLOWLY LOADED FAULTS 1 To appear in the Journal of Geophysical Research, 2000.
Submitted to Seismological Research Letters4 May 15, 20086
Journal of the Mechanics and Physics of Solids 49 (2001) 18651898
Nucleation and early seismic propagation of small and large events in a crustal earthquake model
Pulse-like and crack-like ruptures in experiments mimicking crustal earthquakes
This article was published in an Elsevier journal. The attached copy is furnished to the author for non-commercial research and
SUBMITTED TO JOURNAL OF GEOPHYSICAL RESEARCH, DEC 17, 2007 Spectral-element modeling of spontaneous earthquake rupture
SUBMITTED TO JOURNAL OF GEOPHYSICAL RESEARCH, JULY 2008 3D boundary-integral modeling of spontaneous1
Threedimensional earthquake sequence simulations with evolving temperature and pore pressure due to shear heating
Spectral element modeling of spontaneous earthquake rupture on rate and state faults: Effect of
Spectralelement simulations of longterm fault slip: Effect of lowrigidity layers on earthquakecycle
Variability of earthquake nucleation in continuum models of rate-and-state faults and implications for
PUBLISHED ONLINE: 25 APRIL 2010 | DOI: 10.1038/NGEO843 Towards inferring earthquake patterns from
Three-dimensional boundary integral modeling of spontaneous earthquake sequences and aseismic slip
Supershear transition due to a free surface in 3-D simulations of spontaneous dynamic rupture on vertical strike-slip faults
Scaling of small repeating earthquakes explained by interaction of seismic and aseismic slip in a rate and