摘要
本文从地震力的角度来分析1918年南澳大震烈度异常的原因。潮阳、潮安和云霄一带的烈度异常的主要是莫霍界面上的反射波S_(11)所造成;惠来、漳州和佛县一带的烈度异常主要是由于莫霍界面和地表面上各反射一次的反射波S_(11)所造成.
The reason of the intensity anomaly of Nanao earthquake in 1918 was discussed in this paper from the angle of earthquake mechanics. The intensity anomaly in the Chaoyang, CHaoan and Yunxiao areas is principally due to the reflected waves S11 from the Moho surface. The intensity anomoly in the Huilai, Zhangzhou and Futan areas is principally due to the waves S11 reflected once from the surface of the earth and Mobo surface.
出处
《华南地震》
1989年第1期44-46,共3页
South China Journal of Seismology
