首页|2023年10月24日甘肃肃北MS5.5地震震源机制及发震构造

2023年10月24日甘肃肃北MS5.5地震震源机制及发震构造

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收集到青海和甘肃区域地震台网记录的宽频带地震波形和震相观测数据,利用ISOLA近震全波形方法对2023 年 10 月 24 日甘肃肃北MS5.5 地震进行矩张量反演,得到震源机制解和矩心深度;通过双差定位方法获得地震序列精定位结果和时空分布特征,并结合该地区构造背景对发震构造进行分析.获得肃北MS5.5 地震震源机制解参数为:节面Ⅰ的走向、倾角和滑动角为 170°、73°和 108°,节面Ⅱ的走向、倾角和滑动角为 300°、24°和 42°,震源矩心深度为 4 km;重定位后,此次地震序列震中集中分布在长约 22 km、宽约 10 km的区域内,地震丛集的优势方向为NNW-SSE向.通过对震源机制解、定位结果、区域构造背景等进行分析,推测震源机制解节面Ⅰ为发震断层面,此次地震为发生在隐伏断层上的一次逆冲兼有走滑型地震事件,发震断裂与周边主要断裂的性质一致.
The Focal Mechanism Solution and Seismogenic Structure of the Subei MS 5.5 Earthquake in Gansu on October 24th,2023
This article collected broadband seismic waveform and phase data recorded by the Qinghai and Gansu regional seismic networks.The focal mechanism solution and centroid depth of the Subei MS5.5 earthquake in Gansu on October 24th,2023 were obtained by performing centroid moment tensor inversion with ISOLA software.The precise hypocenter results and spatio-temporal distribution characteristics of the earthquake sequence were obtained through the double-difference relocation method,and an analysis of the seismogenic structures was conducted based on the structural background of the area.The focal mechanism solution parameters of the Subei MS5.5 earthquake are as follows:the strike,dip and slip angles of nodal plane Ⅰ are 170°,73°and 108°,respectively.The strike,dip and slip angles of nodal plane Ⅱ are 300°,24° and 42°,respectively.The main shock centroid depth is 4 km.After relocation,the epicenter of the earthquake sequence was concentrated in a region about 22 km long and 10 km wide,and the dominant direction of the earthquake cluster was NNW-SSE.Based on the analysis of focal mechanism solution,relocation results and regional tectonic background,we infer that the focal mechanism solution plane I is the seismogenic fault plane,and the earthquake is a predominantly thrust faulting with strike-slip event occurring on the hidden fault,and the seismogenic fault has the same property as the surrounding major faults.

focal mechanismfull moment tensorSubei earthquakeseismogenic structureearthquake relocation

张潇、李振月、郭祥云、崔华伟、盛书中、王甘娇、米梓菲、徐仁义

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东华理工大学地球物理与测控技术学院,南昌 330013

中国地震局地球物理研究所,北京 100081

山东省地震局,济南 250014

江西省地震局,南昌 330036

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震源机制 全矩张量 肃北地震 发震构造 地震重定位

国家自然科学基金国家自然科学基金东华理工大学博士科研启动基金

4170405342364005DHBK2019084

2024

华北地震科学
河北省地震局

华北地震科学

CSTPCD
影响因子:0.598
ISSN:1003-1375
年,卷(期):2024.42(2)
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