|本期目录/Table of Contents|

[1]李延京,刘城,杨广华.格尔木地震台记录2016年门源MS6.4地震震相相关分析*[J].地震研究,2016,39(增刊):128-131.
 LIU Yanjing,LIU Cheng,YANG Guanghua.Relevant Analysis for Phase of Qinghai Menyuan MS6.4 Earthquake in 2016 Recorded by Golmud Seismic Station[J].Journal of Seismological Research,2016,39(增刊):128-131.
点击复制

格尔木地震台记录2016年门源MS6.4地震震相相关分析*(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
39
期数:
2016年增刊
页码:
128-131
栏目:
出版日期:
2016-11-20

文章信息/Info

Title:
Relevant Analysis for Phase of Qinghai Menyuan MS6.4 Earthquake in 2016 Recorded by Golmud Seismic Station
作者:
李延京1刘城12杨广华2
1.青海省地震局 乐都地震台,青海 乐都 810700; 2.青海省地震局 格尔木地震台,青海 格尔木 816000
Author(s):
LIU Yanjing1LIU Cheng12YANG Guanghua2
1. Ledu Seismic Station,Earthquake Administration of Qinghai Province,Ledu 810700,Qinghai,China2. Golmud Seismic Station,Earthquake Administration of Qinghai Province,Golmud 816000,Qinghai,China
关键词:
门源MS6.4地震 格尔木地震台 震相 单台法
Keywords:
Menyuan MS6.4 earthquake diurnal variation of geomagnetic vertical component load-unloading response ratio daily variation amplitude radio
分类号:
P315.73
DOI:
-
摘要:
采用格尔木地震台所记录的地震波形数据对门源MS6.4地震震相进行分析。结果显示:此次地震的震相符合一般近震特征,在对地震波形数据处理过程中,震相有Pn、Pg、Sn、Sg,运用单台定位处理方法估测出地震的震源深度为10 km,与Hypoast定位方法测定结果近似一致,利用初至波估算出格尔木地震台震中距约为756 km。
Abstract:
Based on the seismic waveforms of the Menyuan MS6.4 earthquake recorded by Golmud Seismic Station,we analyzed its phase by using phase analytical software.The results show that the phase characteristics of Menyuan MS6.4 earthquake accord with that of the general near earthquake,which shows Pn、Pg、Sn、Sg phases in the process of seismic waveforms processing. The focal depth is 10 km measured by single station location processing method,which is consistent with the results by Hypoast location method. The epicenter distance of Golmud Seismic Station is 617 km by using of seismic first arrival wave.

参考文献/References:

-

备注/Memo

备注/Memo:
收稿日期:2016-08-23
基金项目:青海省地震局科学基金(2015A05)和青海省地震局政策课题基金(zc201608)联合资助.

更新日期/Last Update: 2016-10-20