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河北及周边地区岩石圈磁场变化及震前异常特征
引用本文:赵慧琴,张海洋,李博,王朝景,刘德强,毛丰龙.河北及周边地区岩石圈磁场变化及震前异常特征[J].西北地震学报,2021,43(5):1008-1013.
作者姓名:赵慧琴  张海洋  李博  王朝景  刘德强  毛丰龙
作者单位:河北省地震局保定地震监测中心站, 河北 保定 071000
基金项目:2021年度震情跟踪定向工作任务青年项目(2021010407);河北省地震科技星火计划重点项目(DZ20190422046)
摘    要:利用2019年度大华北秋季复测156个测点的流动地磁矢量资料,获得河北及周边地区岩石圈磁场半年变化图,分析归纳河北及周边地区岩石圈磁场的总体变化特征,并研究测区内2019年12月3日河北怀安MS3.4地震和2019年12月5日河北丰南MS4.5地震前岩石圈磁场局部变化和异常特征。结果表明:丰南MS4.5地震发生在H矢量的转向区,总强度F负异常的高值区,D要素负异常的高梯度带和Z值变化的高值区;怀安MS3.4地震则发生在H矢量幅值弱化且转向区,D要素零值线附近的正值区和Z值变化的低值区。

关 键 词:流动地磁  岩石圈磁场  地磁矢量  磁异常特征  高梯度带
收稿时间:2021/4/6 0:00:00

Variation and pre-seismic anomaly characteristics of the lithosphericmagnetic field in Hebei Province and its surrounding areas
ZHAO Huiqin,ZHANG Haiyang,LI Bo,WANG Zhaojing,LIU Deqiang,MAO Fenglong.Variation and pre-seismic anomaly characteristics of the lithosphericmagnetic field in Hebei Province and its surrounding areas[J].Northwestern Seismological Journal,2021,43(5):1008-1013.
Authors:ZHAO Huiqin  ZHANG Haiyang  LI Bo  WANG Zhaojing  LIU Deqiang  MAO Fenglong
Institution:Baoding Central Seismic Station, Hebei Earthquake Agency, Baoding 071000, Hebei, China
Abstract:In this paper, the semi annual variation of the lithospheric magnetic field in Hebei and its surrounding areas was obtained by using the data of mobile geomagnetic vector from 156 observation points of North China in autumn 2019, and the overall variation characteristics of lithospheric magnetic field in the study area were analyzed and summarized. Furthermore, the local variation and anomaly characteristics of lithospheric magnetic field before the Huai''an, Hebei MS3.4 earthquake on December 3, 2019 and the Fengnan, Hebei MS4.5 earthquake on December 5, 2019 were studied. The results showed that the epicenter of Fengnan MS4.5 earthquake was located in the turning area of vector H, the high value area of negative anomaly of total intensity F, the high gradient zone of negative anomaly of element D and the high value area of Z value. The Huai''an MS3.4 earthquake occurred in the area where the amplitude of vector H weakened and turned, the positive area near the zero value line of element D and the low value area where the Z value changed.
Keywords:mobile geomagnetism  lithospheric magnetic field  geomagnetic vector  magnetic anomaly characteristics  high gradient zone
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