Abstract

<p>In the past decade, there have been several disaster earthquakes occurred in Taiwan.<br>From the observed data of the disaster earthquakes, the stations located in the source<br>rupture direction have obvious directivity pulses, and the distribution of the earthquake<br>disaster is related to the peak ground velocity. Therefore, how to use a large and high-<br>dense seismic database to develop a near-real-time detection system on the earthquake<br>rupture directivity, which is a very important task in Taiwan. In this study, we determine<br>the earthquake rupture directivity using near-field velocity data from 1991 to 2018, which<br>were collected under the Taiwan Strong Motion Instrument Program (TSMIP). The used<br>method is mainly constructed in the interpolation of the peak-ground-velocity map and<br>the directional attenuation regression analysis. Through the analysis of moderate-to-large<br>magnitude (M L > 5.5) seismic events, the source rupture directivity can be detected<br>effectively and quickly by the applied method. The detection results are also comparable<br>with those from the previous source studies. We also find out a linear relationship between<br>the directivity effect and earthquake magnitude. Since the TSMIP station may provide<br>real-time services in the future, the detection system proposed by this research can quickly<br>provide disaster prediction information, which is of great importance for earthquake<br>emergency response and hazard mitigation.</p>

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