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- W2353873670 abstract "An MS6. 6 earthquake occurred at the boundary between M inxian and Zhangxian Counties on Jul. 22,2013. Studying the cross fault deformation of seismogenic structure area before and after the M inxian-Zhangxian MS6. 6 earthquake,we found that the deformation anomaly appeared in Sidian,M ajietan and M aoyugou sites before the earthquake. The deformation in single period were 2 ~ 7 times than the average value,and the duration of deformation anomaly was less than 4 months before the earthquake in these three sites. The deformation recovered to average value in 4 months after the earthquake except for M aoyugou site. The impending deformation ΔV in Sidian site( 5. 5mm) was about 2 times than that in M ajietan and M aoyugou sites,which were due to the main dynamic source was from the activity of North margin of Western Qinlin Fault,so the deformation anomaly in main fault was larger than that of branch fault. The characteristic of Lintan-Tanchang Fault is the diversity of activity,and the activity of the eastern section of active faults is stronger than that in the western part.The recurrence period of M inxian-Zhangxian earthquake is about( 220 ± 40) a,the magnitude of it is from 6. 0to 6. 6." @default.
- W2353873670 created "2016-06-24" @default.
- W2353873670 creator A5081828254 @default.
- W2353873670 date "2014-01-01" @default.
- W2353873670 modified "2023-09-23" @default.
- W2353873670 title "Research on Cross-fault Deformation Abnormity of Minxian-Zhangxian M_S6. 6 Earthquake in Gansu in 2013" @default.
- W2353873670 hasPublicationYear "2014" @default.
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