Near‐surface versus fault zone damage following the 1999 Chi‐Chi earthquake: Observation and simulation of repeating earthquakes. Issue 4 (6th April 2015)

• Record Type: Journal Article
• Authors: Chen, Kate Huihsuan; Furumura, Takashi; Rubinstein, Justin
• Is Part Of: Journal of geophysical research. Volume 120:Issue 4(2015:Apr.)
• Page Start: 2426
• Page End: 2445
• Publication Date: 2015-04-06
• Subjects: Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1002/2014JB011719
• Languages: English
• ISSNs: 2169-9313

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>We observe crustal damage and its subsequent recovery caused by the 1999 <italic>M</italic>7.6 Chi‐Chi earthquake in central Taiwan. Analysis of repeating earthquakes in Hualien region, ~70 km east of the Chi‐Chi earthquake, shows a remarkable change in wave propagation beginning in the year 2000, revealing damage within the fault zone and distributed across the near surface. We use moving window cross correlation to identify a dramatic decrease in the waveform similarity and delays in the <italic>S</italic> wave coda. The maximum delay is up to 59 ms, corresponding to a 7.6% velocity decrease averaged over the wave propagation path. The waveform changes on either side of the fault are distinct. They occur in different parts of the waveforms, affect different frequencies, and the size of the velocity reductions is different. Using a finite difference method, we simulate the effect of postseismic changes in the wavefield by introducing <italic>S</italic> wave velocity anomaly in the fault zone and near the surface. The models that best fit the observations point to pervasive damage in the near surface and deep, along‐fault damage at the time of the Chi‐Chi earthquake. The footwall stations show the combined effect of near‐surface and the fault zone damage, where the velocity reduction (2–7%) is twofold to threefold greater than the fault zone damage observed in the hanging wall stations. The physical models obtained here allow us to monitor the temporal evolution and recovering process of the Chi‐Chi fault zone damage.</p> </abstract>