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2013年岷县6.6级地震前天水台磁通门秒数据异常提取分析
引用本文:倪晓寅,冯志生,陈莹.2013年岷县6.6级地震前天水台磁通门秒数据异常提取分析[J].西北地震学报,2016,38(S2):203-207.
作者姓名:倪晓寅  冯志生  陈莹
作者单位:福建省地震局, 福建 福州 350003,江苏省地震局, 江苏 南京 210014,福建省地震局, 福建 福州 350003
基金项目:2015年度震情跟踪定向工作任务“基于秒数据的地磁转换函数强震前变化特征研究”(2015010407)
摘    要:基于GM4磁通门磁力仪秒数据,分析研究了2008-2014年天水地磁台的地磁极化值和转换函数变化,结果表明在2013年岷县6.6级地震前天水台地磁极化值和转换函数存在不同程度的异常:(1)转换函数|A|和|B|在震前均出现了下降-转折-上升的异常变化,在上升至最高点时发生了岷县6.6级地震;(2)较短的周期转折上升变化更明显,幅度也更大,如|A|的20~80 s和|B|的20~110 s;(3)3.20 s、50 s和80 s周期的帕金森矢量方位角在震前出现转向并指向震中的现象;(4)4.5~100 s周期的极化值Yzh在震前3个月出现2次超3倍均方差的高值异常。

关 键 词:地磁场  秒采样  转换函数  极化  地震
收稿时间:2016/2/5 0:00:00

Extraction and Analysis of Anomalies of the Second Data from GM4 Fluxgate Magnetometer at Tianshui Station before the 2013 Minxian MS6.6 Earthquake
NI Xiao-yin,FENG Zhi-sheng and CHEN Ying.Extraction and Analysis of Anomalies of the Second Data from GM4 Fluxgate Magnetometer at Tianshui Station before the 2013 Minxian MS6.6 Earthquake[J].Northwestern Seismological Journal,2016,38(S2):203-207.
Authors:NI Xiao-yin  FENG Zhi-sheng and CHEN Ying
Institution:Earthquake Administration of Fujian Province, Fuzhou 350003, Fujian, China,Earthquake Administration of Jiangsu Province, Nanjing 210014, Jiangsu, China and Earthquake Administration of Fujian Province, Fuzhou 350003, Fujian, China
Abstract:On July 22, 2013, an earthquake occurred in Minxian County, Gansu Province, whose epicenter was located 154 km from the Tianshui seismic station. Geomagnetic three-component second sample observations at Tianshui station were initiated in 2007 through a GM4 fluxgate magnetometer. Here, we analyze the change of the geomagnetic polarization value and the transform function at Tianshui station from 2008 to 2014 based on the second data of GM4 fluxgate magnetometer. The results indicate that the geomagnetic polarization value and the transform function show different degrees of anomaly before the Minxian MS6.6 earthquake.(1) The transform function exhibited down turning recovery before the earthquake. In fact, the earthquake occurred just as the transform function reached the maximum.(2)The short-term increase was more obvious than the long-term trend, and the rising amplitude was larger.(3) Before the earthquake,the Parkinson vector azimuth in the periods of 20 s, 50 s, and 80 s was rotated and directed to the epicenter.(4) In April 2013, three months before the earthquake, the geomagnetic polarization at Tianshui station showed two anomalies of high values exceeding three times the mean square deviation.
Keywords:geomagnetic field  second sample  transform function  polarization  earthquake
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