HR: 0830h
AN: S41C-0094 [PDF]
TI: Spatial and scale-dependent friction parameter derived from earthquake rate changes after a stress step
by the 1999, Chi-Chi, Taiwan, earthquake
AU: * Wang, W
EM: seiwhwg@eq.ccu.edu.tw
AF: Institute of Applied geophysics, National Chung Cheng University, 160, Shanshin, Minghsiung, Chiayi,
621
Taiwan
AU: Chang, S
EM: sph8801@eq.ccu.edu.tw
AF: Institude of Seismology, National Chung Cheng University, 160, Shanshin, Minghsiung, Chiayi, 621
Taiwan
AB:
DieterichÝs fomulation for earthquake clustering derived from stability analysis of a spring-slider system with slowness law
suggests that earthquake rate changes can be used as a stress meter for near-surface deformation and a tool for evaluation
of the probability for the future large earthquakes. While employing this theory, most studies implicitly assumed friction
parameters are spatially and magnitude independent. This assumption, however, needs to be justified. We conduct
genetic-algorithm inversion to simultaneously obtain the spatial variation of long-term stressing rate and friction parameter
based on the earthquake rate changes before and after the 1999, Chi-Chi, Taiwan, earthquake. We found that the long-term
stressing rate from this inversion agrees well with GPS observations. Our results also suggest that the rupture
characteristics of the Chi-Chi earthquake may be attributed to the spatial variation in A$\sigma$ (rate constitutive
parameter and normal stress). Moreover, we found that A$\sigma$ systematically decreases with earthquake magnitude, which
implies that DieterichÝs fomulation for earthquake clustering is implicitly magnitude-dependent. Since stress drop derived
form seismic moment release does not strongly correlate with earthquake magnitude, the magnitude-dependent friction parameter
derived from this method may reflect the friction behavior of characteristic asperities only instead of the entire rupture
area.
DE: 7209 Earthquake dynamics and mechanics
DE: 7215 Earthquake parameters
DE: 7230 Seismicity and seismotectonics
SC: Seismology [S]
MN: 2003 Fall Meeting