Abstract
Propagating slip pulses in earthquake ruptures (Heaton, 1990) are studied based on a one-dimensional N-degree-of-freedom dynamical spring-slider system with a constant ratio of static to dynamic frictional forces. Results show that for almost all cases in the study, the rise time of ruptures at a particular site is much smaller than the duration of ruptures along the whole fault. A propagating slip pulse is generated along the fault. Hence, simulation results are in agreement with Heaton's propagating slip-pulse model.
Original language | English |
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Pages (from-to) | 100-104 |
Number of pages | 5 |
Journal | Tectonophysics |
Volume | 487 |
Issue number | 1-4 |
DOIs | |
State | Published - May 2010 |
Keywords
- Duration
- Rise time
- Rupture dynamics
- Slip pulses
- Spring-slider model