地磁低点位移异常:岷县-漳县M6.6地震可能的震前反映  

Abnormity of Geomagnitics Low-Point Shift:A Possible Seismogenic Reflection of the Minxian-Zhangxian M6.6 Earthquake

作　　者：许康生[1] 曾文浩[1] 

机构地区：[1]中国地震局兰州地震研究所,兰州市东岗西路410号730000

出　　处：《大地测量与地球动力学》2017年第4期425-428,共4页Journal of Geodesy and Geodynamics

基　　金：国家自然科学基金(41474046)~~

摘　　要：选取天水地磁台(TSY)和兰州地磁台(LZH)2011~2013年、乾陵地磁台(QIX))2012~2013年以及成都地磁台(CDP)观测资料,基于小波多尺度分解,提取地磁垂直向日变的最低点时刻,在时间域展现低点位移变化特征。结果表明,从2013-05开始,天水台地磁日变低点时刻表现为持续上升(低点时刻逐渐滞后),2013-07初达到峰值。岷县-漳县地震(2013-07-22 M6.6)发震时间处在低点位移下降段,而其他台站低点位移在震前未出现异常变化。结合其他文献认为,天水地磁低点位移异常可能是这一地震孕育和发生过程在地磁场的反映。In this paper,we use observation data for Tianshui geomagnetic station（TSY）, Lanzhou geomag- netic station （LZH）, Qianling geomagnetic station（QIX）, and Chengdu geomagnetic station（CDP）, based on multi-scale wavelet decomposition, extraction of time of low-point on vertical compenent,and variation process of low-point shift on time. The results show that the low-point shift continues to lag the vertical compenent on Tianshui geomagnetic station （TSY） from May to July 2013. The range of variation lies beyond the normal state, but other stations do not present this abnormal phenomenon. This process shows localized features at Tianshui station; the Minxian-Zhangxian 2013-07-22 M6.6 earthquake occurrence is on down-point time of low-point shift peak, showing the correlation between the anomaly and the earthquake. This may be a reflec- tion of seismogenics in the geomagnetic field. These results have an important reference value in the study of the seismogenic process, mechanism dynamics process of geomagnetic low point shift, and exploration on earthquake prediction.

关 键 词：地磁 低点位移 岷县-漳县地震 地震孕育 

分 类 号：P315[天文地球—地震学]