2) Aftershock distribution
余震分布
1.
Comparison of aftershock distribution and sequence type of 3 strong earthquakes (M≥7) from 1970 to 2008 in Sichuan Province
四川3次7级以上地震序列和余震分布特征的对比
3) Strong earthquake distribution
强震分布
4) aftershock distribution size
余震分布尺度
1.
0 in Chinese mainland from 1970 to 2004, for different sequence types and different rupture modes of the main shock, the relationship between aftershock distribution size R and the magnitude of the main shock M0 has been studied statistically.
0地震序列资料,统计研究了中国大陆余震分布尺度与序列最大地震震级M0及最大地震破裂形式之间的关系。
5) cosinusoidal intensity distribution
余弦强度分布
6) strong aftershock
强余震
1.
Phased estimating for the temporal and spatial development of the seismic sequence of the 2008 M8.0 Wenchuan Earthquake and its strong aftershocks
汶川8.0级地震序列的时—空扩展与强余震趋势的阶段性估计
2.
The Grey system theory is used for an attempt to forecast occurrence time of two strong aftershocks of the 2004 North Sumatra earthquake sequence with magnitude of 9.
0级地震序列两次强余震(系指ML≥6)的发震时间进行了尝试性预测。
3.
Using the ground motion attenuation relation, we calculated and compared the effective peak acceleration(EPA) generated by main shocks and their strong aftershocks of 21 earthquake sequences with MS≥7 occurred in Chinese mainland and offing of China during 1966—2002.
应用地震动衰减关系计算了1966年邢台地震以来中国大陆及近海发生的21次MS≥7地震序列的主震和强余震产生的有效峰值加速度,并对计算结果进行了比较分析,发现76。
补充资料：余震
见地震。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条