冯向东, 王晓山, 陈婷, 张素欣. 晋冀蒙交界地区最小一维速度模型[J]. 华北地震科学, 2017, 35(4): 16-21. DOI: 10.3969/j.issn.1003-1375.2017.04.003
引用本文: 冯向东, 王晓山, 陈婷, 张素欣. 晋冀蒙交界地区最小一维速度模型[J]. 华北地震科学, 2017, 35(4): 16-21. DOI: 10.3969/j.issn.1003-1375.2017.04.003
FENG Xiang-dong, WANG Xiao-shan, CHEN Ting, ZHANG Su-xin. 1-D Minimum Velocity Model of Shanxi-Hebei-Inner Mongolia Border Area[J]. North China Earthquake Sciences, 2017, 35(4): 16-21. DOI: 10.3969/j.issn.1003-1375.2017.04.003
Citation: FENG Xiang-dong, WANG Xiao-shan, CHEN Ting, ZHANG Su-xin. 1-D Minimum Velocity Model of Shanxi-Hebei-Inner Mongolia Border Area[J]. North China Earthquake Sciences, 2017, 35(4): 16-21. DOI: 10.3969/j.issn.1003-1375.2017.04.003

晋冀蒙交界地区最小一维速度模型

1-D Minimum Velocity Model of Shanxi-Hebei-Inner Mongolia Border Area

  • 摘要: 收集整理晋冀蒙交界地区2014年9月1日至2016年5月28日间448次1.0级以上地震事件的6 678条P波和6 103条S波到时资料,采用震源位置-速度结构的联合反演方法,使用Velest程序计算了晋冀蒙交界地区"最小一维速度模型",并利用这一模型对该地区1 763次地震进行了重新定位。结果显示:重新定位后震源深度分布集中于5~20 km区间,趋于正态分布,定位结果有显著改善。

     

    Abstract: In this study, we collected 6 678 P-wave traveltimes and 6 013 S-wave traveltimes in the Shanxi-Hebei-Inner-Mongolia border area. On basis of these data, using the simultaneous inversion methods in the Velest program for hypocenter-velocity structure, we present a 1-D minimum velocity model of the study area. With the 1-D minimum velocity model, we relocate 1 763 earthquakes in the Shanxi-Hebei-Inner-Mongolia border area. The result shows that:the hypocenter depth is mostly between 5 km to 20 km.

     

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