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利用sPL震相测定2022年山西古交ML4.1地震震源深度

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选取2022年2月20日山西古交ML4.1地震事件波形,筛选出震中距在10~70 km之间的5个地震台站,基于sPL震相特征对波形数据进行处理,在震中距23 km的GUJ台观测到sPL震相.使用山西2015一维地壳速度模型,通过SEIS-CAP软件计算该地震的震源机制解,并利用F-K方法计算理论地震图,与观测波形拟合对比,确定该地震震源深度约4 km.sPL震相方法、CAP方法测定的震源深度和正式编目结果基本一致,表明利用sPL震相测定山西古交ML4.1地震震源深度是可靠的.
Determination of Focal Depth of 2022 Gujiao ML4.1 Earthquake in Shanxi Province by sPL Seismic Phase
The seismic event waveform of Shanxi Gujiao ML4.1 earthquake on February 20,2022 is selected,five seismic stations with epicenter between 10 and 70 km are selected,and the waveform data are processed based on the characteristics of sPL phase.sPL phase is observed at GUJ station with epicenter 23 km away.Using the one-dimensional crust velocity model of Shanxi 2015,SEIS-CAP software is used to calculate the focal mechanism solution of the earthquake,and F-K method is used to calculate the theoretical seismogram,and compared with the observed waveform,the focal depth of the earthquake is determined to be about 4 km.The focal depth measured by sPL phase method and CAP method is basically consistent with the official cataloging results,which indicates that the focal depth of Shanxi Gujiao ML4.1 earthquake measured by sPL phase method is reliable.

focal depthfocal mechanism solutionGujiao earthquakesPL seismic phaseF-K method

王卓君、窦立婷、冯凯宇、吕睿、梁永烨、刘雪娇

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山西省地震局,山西 太原

太原大陆裂谷动力学国家野外科学观测研究站,山西 太原

震源深度 震源机制解 古交地震 sPL震相 F-K方法

中国地震局监测、预报、科研三结合课题

3JH-202302055

2024

科学技术创新
黑龙江省科普事业中心

科学技术创新

影响因子:0.842
ISSN:1673-1328
年,卷(期):2024.(6)
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