摘要
通过详细分析上覆于梅江断裂上全新统地层中三个人工探槽剖面 ,得出该断裂是一条全新世活动断层 ,且近 30 0 0年以来 ,至少发生过两次 7级左右强烈地震事件的结论性认识。
The understanding that the Mae Chan Fault is a Holocene active fault and at least two strong earthquakes with about M 7 0 have occurred in the fault in past 3000 years is obtained through analyzing in detail the tree artificial trench profiles overlying on Holocene stratum in the Mae Chan Fault.
出处
《地震研究》
CSCD
北大核心
2001年第1期61-64,共4页
Journal of Seismological Research
