Complexity of seismicity due to highly rate‐dependent friction
- 10 November 1996
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 101 (B11) , 25321-25336
- https://doi.org/10.1029/96jb02095
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- Analysis of the relationship between seismic moment and fault length for large crustal strike‐slip earthquakes between 1977–92Geophysical Research Letters, 1996
- Dynamical weakening of faults by acoustic fluidizationNature, 1996
- Self-healing slip pulse on a frictional surfaceJournal of the Mechanics and Physics of Solids, 1995
- Model of earthquake recurrence: Role of elastic wave radiation, relaxation of friction, and inhomogeneityJournal of Geophysical Research, 1995
- Variations in rupture process with recurrence interval in a repeated small earthquakeNature, 1994
- Earthquake nucleation on faults with rate-and state-dependent strengthTectonophysics, 1992
- Spontaneous processes for nucleation, dynamic propagation, and stop of earthquake ruptureGeophysical Research Letters, 1992
- Strike‐slip earthquakes on quasi‐vertical transcurrent faults: Inferences for general scaling relationsGeophysical Research Letters, 1992
- Intrinsic properties of a Burridge-Knopoff model of an earthquake faultPhysical Review A, 1991
- Mechanical model of an earthquake faultPhysical Review A, 1989