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华北地震区岩石圈磁异常场零值线与中强震震中分布关系
引用本文:顾春雷,张毅,顾左文,王行舟,王雷,徐如刚,朱志春.华北地震区岩石圈磁异常场零值线与中强震震中分布关系[J].西北地震学报,2012,34(2):174-179.
作者姓名:顾春雷  张毅  顾左文  王行舟  王雷  徐如刚  朱志春
作者单位:1. 中国科学技术大学地球与空间科学系,安徽合肥230026;安徽省地震局,安徽合肥230031
2. 安徽省地震局,安徽合肥,230031
3. 中国地震局地球物理研究所,北京,100081
基金项目:地震行业科研专项200908029-03-02
摘    要:通过对华北地震区岩石圈磁异常场各分量的零值线分布以30km为缓冲半径建立缓冲区,并对缓冲区内1900年以来MS4.0及以上大陆地震进行统计,探讨华北地区岩石圈磁异常场零值线分布与中强震震中位置关系,发现7.0级以上地震震中分布与岩石圈磁异常场磁偏角、N向分量、E向分量以及垂直分量零值线的分布位置关系密切,其中震中分布与磁偏角的相关性最高,达83.3%。

关 键 词:岩石圈磁异常  零值线  缓冲区  中强震震中  华北地震区

Relationship between Zero-value-line of Abnormal Geomagnetic Field in Lithosphere and Strong-moderate Earthquake Epicenters in North China Seismic Region
GU?Chun-lei,ZHANG?Yi,Gu?Zuo-wen,WANG?Xing-zhou,WANG?Lei,XU?Ru-gang and ZHU?Zhi-chun.Relationship between Zero-value-line of Abnormal Geomagnetic Field in Lithosphere and Strong-moderate Earthquake Epicenters in North China Seismic Region[J].Northwestern Seismological Journal,2012,34(2):174-179.
Authors:GU?Chun-lei  ZHANG?Yi  Gu?Zuo-wen  WANG?Xing-zhou  WANG?Lei  XU?Ru-gang and ZHU?Zhi-chun
Institution:1.College of Earth and Space Science,University of Science and Technology of China,Hefei 230026,China; 2.Earthquake Administration of Anhui Province,Hefei 230031,China;3.Institute of Geophysics,CEA,Beijing 100081,China)
Abstract:We build the buffer zones with a 30 km radius from the zero-value-lines of all components of the abnormal geomagnetic field in lithosphere of north China seismic region,and statistical analyze all the MS≥4.0 earthquakes in the buffer zones since 1900.The results indicate that there are close relativities among the epicenter distribution of large earthquakes with MS≥7.0 and the zero-value-lines of geomagnetic declination,north component,east component and vertical component of the abnormal geomagnetic field,and the epicenter distribution has the highest relation to the geomagnetic declination with proportion 83.3%.
Keywords:Abnormal geomagnetic field in lithosphere  Zero-value-line  Buffer zone  Strong-moderate earthquake epicenter  North China seismic region
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