摘要
依据神户海洋气象台、大阪气象台、神户港岛、神户大学、神户本山小学、尼崎及大阪福岛的强震记录,分析了强地震的走时和传播特性,指出大阪盆地的厚沉积层是造成St波在神户和大阪到时发生延迟的原因,由于断层在空间上的分布造成一些强震记录的波形差异。
The real cases of adding storeys to buildings were recounted,it was suggested that the factors of earthquake resistance of build site,structure and material should be paid attention before the storeys will be added to the original building,especially which the buildings lacat at the focal monitoring and preparedness areas.
出处
《山西地震》
1997年第3期54-57,共4页
Earthquake Research in Shanxi
关键词
强震观测
地震波传播
地震
日本兵库县
Earthquake resistance reinforcement Aseismic design Buildings