摘要
中条山北麓断裂是运城盆地的主控断裂.作为第四纪以来的活动断裂,其活动情况与运城盆地及周边的地震活动间存在一定的关系.采用异常参数R值法和年滑动速率比法对布设在此断裂的流动水准场地观测数据进行分析,发现2种数据分析方法结合起来能更准确地发现观测数据的异常变化,研究结果可为运城盆地及周边地区的地震预测研究提供参考.
Fault at the north piedmont of Zhongtiao Mountain is the main fault in Yuncheng basin.As active faults since Quaternary,the activity of faults is related to the seismicity of Yuncheng basin and its surrounding areas.In this paper,anomalous parameter R value method and annual slip rate ratio method are used to analyze the observation data of flow leveling sites located in this fault.It is found that the combination of the two data processing methods can more accurately detect the anomalous changes of the observed data,and provide a reference for earthquake prediction in Yuncheng basin and its surrounding areas.
作者
李晓锐
刘国俊
常姣
姚林鹏
李民
LI Xiaorui;LIU Guojun;CHANG Jiao;YAO Linpeng;LI Min(Xiaxian Central Seismological Station,Shangxi Eartjquake Agency,Shanxi Province 044400,China;National Continental Rift Valley Dynamics Observatory of Taiyuan,Shanxi Province 030025,China)
出处
《地震地磁观测与研究》
2020年第1期78-84,共7页
Seismological and Geomagnetic Observation and Research
基金
山西省地震局科研项目“基于Python的ObsPy包在地震震相自动拾取中的应用研究”(项目编号:SBK-2026)。
关键词
中条山北麓断裂
跨断层水准
地震活动
分析方法
fault at the north piedmont of Zhongtiao Mountain
fault-cross leveling
seismic activity
analytical methods