1) aftershock sequence
余震序列
1.
0 earthquake s aftershock sequence.
0级地震余震序列的震源机制解。
2.
On the basis of Aki and Chouet s single scattering theory of coda waves for local earthquakes,we estimated the Qc-value of coda at the source region using the digital waveform data of the aftershock sequence of the Ning er MS6.
94;测量结果显示宁洱地震余震序列的尾波值Qc较低,表明宁洱震源区属于构造运动较为活跃区。
3.
The character of principle compressive stress of the aftershock sequence varying with time presents the complex stress state in the earthquake zone.
0余震的垂直分量在频率域内进行地震矩张量反演,对反演结果进行了讨论,并用最小二乘法回归了地震矩M0、矩震级MW和地方震震级ML之间的关系;根据对余震序列主压应力轴随时间的变化特点,分析了震区复杂的应力状态。
2) main shock-after shock type
主震-余震型序列
3) aftershock sequence characteristic
余震序列特征
4) main shock after shock type sequence
主余震型序列
5) Epidemic Type Aftershock Sequence
传染型余震序列模型
6) aftershock series of Jiujiang-Ruichang earthquake
九江-瑞昌余震序列
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