Seismicity Pattern Changes Prior to Large Earthquakes -An Approach of the RTL Algorithm
Yi-Xuan Wu
Institute of Geophysics, NationalCentralUniversity, Chungli, Taiwan 320.
ABSTRACT
A statistical method, which is called the Region-Time-Length (RTL) algorithm and takes into account information such as magnitude, occurrence time and place of earthquakes, was applied to earthquake data to investigate seismicity pattern changes prior to large earthquakes. The results indicated that seismic quiescence anomalies generally started a few years before the occurrence of the earthquakes and lasted from 1 to 2.5 years. The duration of the subsequent stage of seismic activation generally lasted several months. An earthquake is most likely to occur once the relevant source region has passed through the quiescence and activation stages. Close investigation of possible artifacts due to the selection of model parameters and the changes of seismological networks are important in identifying real seismicity changes from man-made ones.It indicated that an increased RTL parameter would be a new potentiallyuseful index for the risk alarm of earthquake swarms.
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