作者: Peng Zhao , Zhigang Peng
DOI: 10.1111/J.1365-246X.2009.04385.X
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摘要: SUMMARY We systematically investigate spatial variations of temporal changes and depth extent damage zones along the Calaveras fault that ruptured during 1984 Morgan Hill earthquake by waveform analysis 333 sets repeating earthquakes. We use a sliding window cross-correlation technique to measure traveltime in waveforms generated each cluster. find clear delays S- early S-coda waves for events immediately after main shock. The amplitudes time decrease logarithmically with since shock, indicating time-dependent recovery (healing) process following abrupt coseismic changes. largest are observed at station CCO is closest rupture zone this larger clusters top 6 km, depth. In comparison, other five stations much smaller, do not show relationship hypocentral suggest these mostly occur few hundred metres near-surface layers, while likely associated around well developed kilometres upper crust. Our results consistent inference widespread non-linearity layers strong ground motions nearby large earthquakes, localized damages flower-type structures active faults based on previous studies recent 3-D numerical simulations.