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大同地震台远震波形走时残差的计算和应用
引用本文:白伟利,郝雪景,高存英,苏燕红,彭丽娟. 大同地震台远震波形走时残差的计算和应用[J]. 地震地磁观测与研究, 2021, 42(5): 30-35. DOI: 10.3969/j.issn.1003-3246.2021.05.005
作者姓名:白伟利  郝雪景  高存英  苏燕红  彭丽娟
作者单位:1.中国山西 037000 山西省地震局大同中心地震台;2.中国山西 030025 太原大陆裂谷动力学国家野外科学观测研究站
基金项目:中国地震局监测、预报、科研三结合课题(项目编号:3JH-202001018)
摘    要:选取大同地震台记录的2010-2019年531个Ms≥5.0地震事件,根据发震区域的不同对其波形走时残差进行分析,得到不同发震区域地震波形的平均走时残差.结果 表明,日本、喜马拉雅地区地震波形的走时残差总体为负值,平均残差分别为-1.51 s、-0.70 s;斐济、中国台湾地区、南美洲西海岸地区大多为正值,平均残差为0...

关 键 词:地震波走时  走时残差

Calculation and application of seismic wave travel time residuals at Datong Seismic Station for teleseismic events
BAI Weili,HAO Xuejing,GAO Cunying,SU Yanhong,PENG Lijuan. Calculation and application of seismic wave travel time residuals at Datong Seismic Station for teleseismic events[J]. Seismological and Geomagnetic Observation and Research, 2021, 42(5): 30-35. DOI: 10.3969/j.issn.1003-3246.2021.05.005
Authors:BAI Weili  HAO Xuejing  GAO Cunying  SU Yanhong  PENG Lijuan
Affiliation:1.Datong Central Seismic Station of Shanxi Earthquake Agency, Shanxi Province 037000, China;2.National Field Scientific Observation and Research Station of Taiyuan Continental Rift Dynamics, Taiyuan 030025, China
Abstract:This paper collects seismic records at Datong Seismic Station for 531 M ≥ 5.0 earthquakes from 2010 to 2019, classifies them according to their epicenter region, and obtains the average travel time residuals for different regions. The results show that:the seismic wave travel time residuals for earthquakes in Japan and the Himalayas are negative, and their average residuals are -1.51 s and -0.7 s, respectively; the travel time residuals for earthquakes in Fiji, Taiwan, and the west coast of South America are densely positive, with the average residuals of 0.79 s, 1.83 s, and 1.86 s, respectively. At the same time, it is found that in the presence of interference, referring to the calculation results of the average travel time residuals in different regions, the identification of the first arrival phases can be better carried out by judging the positional relationship of the actual first arrival phase and the theoretical first arrival phase.
Keywords:seismic wave travel time   travel time residual
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