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Chapter
Structural Relationship Between the 2008 M8 Wenchuan and 2013 M7 Lushan Earthquakes Viewed by Fault-Zone Trapped Waves
We analyzed waveform data recorded at seismic network and temporal stations for aftershocks of the 2013 M7 Lushan earthquake and the 2008 M8 Wenchuan earthquake in both time and frequency. Prominent fault-zone tr...
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Article
Changes in source parameters of foreshocks and aftershocks of the 2001 M S=6.0 Yajiang, Sichuan, earthquake
In this paper changes in focal mechanisms, parameters of wave spectra, and stress drops for the M S=5.0 foreshock and M S=6.0 mainshock in February 2001 in Yajiang ...
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Article
Earthquake focal mechanisms and stress field in Sichuan-Yunnan area determined using P wave polarity and short period P and S waveform data
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Article
A real time processing system of seismic waves using personal computers — Function and characteristics
The real-time processing system of CTSN performs following: A/D conversion; automatic event detection; event data saving; automatic measure of P and S arrivals; event location and print out the calculated resu...
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Article
Attenuation of coda waves and Q c value beneath the Chengdu telemetered seismic network
Based on the single scattering model of coda power spectrum analysis, digital waveform data of 50 events recorded by the real-time processing system of the Chengdu telemetry network are analyzed to estimate the Q
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Article
Temporal changes in shear wave splitting after theM=5.2 shimian earthquake of June 9, 1989
Just after the occurrence of anM=5.2 earthquake in Shimian, Sichuan, two three-component seismometers were set up near the epicenter of the earthquake. Field observations were made for the four-year period from 1...