最大加速度記録を用いた簡易断層位置推定法の適用性について

抄録

In this study, the applicability of the method to identify the location of earthquake fault after the eventusing the records of peak acceleration observed at ground surface is described. The applicable limit is defined as the standard deviation of the identified location of an fault line in relation to the magnitude and the length of fault line. Finally, the results of identification in 1995 Hyogoken-Nanbu eathquake is discussed