首页|2021年9月16日四川泸县Ms6.0地震前地磁扰动异常特征分析

2021年9月16日四川泸县Ms6.0地震前地磁扰动异常特征分析

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选取四川地区3个地磁扰动台站的观测数据,利用基于脉冲幅度法的地磁垂直强度极化方法,对2021年9月16日四川泸县Ms6.0地震前的地磁扰动异常演化特征进行分析.研究结果表明:(1)在中强地震前,台站的垂直强度极化值和超阈值极化值频次逐日变化均会出现高值异常,其中频次异常呈现先增强后降低,再增强-降低的形态;(2)发生异常变化的多个台站距离震中300 km范围内,时间上属准同步变化;(3)地震多发生在异常出现的一个月后,频次异常值往往是研究时段的最高值;(4)机理上,这些异常演化形态和特征是由岩石的破裂特性决定的,一定程度上反映了地震的孕育过程;(5)这种震前的地磁扰动异常与外源场无关.
Characteristics of geomagnetic disturbance anomalies before the Luxian,Sichuan Ms6.0 earthquake on September 16,2021
Based on the observational data from three geomagnetic disturbance stations in the Si-chuan area,the evolution characteristics of geomagnetic disturbance anomalies before the Ms6.0 earthquake in Luxian County,Sichuan Province,on September 16,2021,were analyzed using the geomagnetic vertical intensity polarization method,which is based on the pulse amplitude method.Results show that before the moderate-to-strong earthquake,the vertical intensity polar-ization values at the stations,as well as the frequency of polarization values exceeding the thresh-old,exhibit high-value anomalies.These frequency anomalies followed a pattern of initially increasing,then decreasing,and finally exhibiting an increasing-decreasing trend.Many stations exhibiting abnormal changes are located within 300 km of the epicenter,with the anomalies occurring in a quasi-synchronous manner over time.Most earthquakes tend to occur within one month after the anomalies,and the frequency of outliers often reaches its maximum value during the study period.In terms of the underlying mechanism,the evolution patterns and characteris-tics of these anomalies are influenced by the fracture properties of rocks,which reflect,to some extent,the earthquake preparation process.Furthermore,the geomagnetic disturbance anomaly before the earthquake is unrelated to external magnetic field variations.

geomagnetic disturbancegeomagnetic vertical intensity polarization methodLuxian Ms6.0 earthquakeabnormal characteristics

王玮铭、冯志生、朱培育、廖晓峰、何畅、张致伟

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四川省地震局,四川成都 610041

江苏省地震局,江苏南京 210000

上海市地震局,上海 200001

地磁扰动 地磁垂直强度极化法 泸县Ms6.0地震 异常特征

2025

地震工程学报
中国地震局兰州地震研究所,中国地震学会,清华大学,中国土木工程学会

地震工程学报

北大核心
影响因子:1.191
ISSN:1000-0844
年,卷(期):2025.47(1)