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2010—2016年南北地震带岩石圈磁场变化分析
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  • 英文篇名:Lithospheric geomagnetic field variation in the North-South Seismic Belt from 2010 to 2016
  • 作者:冯丽丽
  • 英文作者:Feng Lili;Qinghai Earthquake Agency;
  • 关键词:南北地震带 ; 岩石圈磁场变化 ; 小波分解 ; 芦山地震
  • 英文关键词:North-South Seismic Belt;;lithospheric magnetic field variation;;wavelet decomposition;;Lushan earthquake
  • 中文刊名:DZXB
  • 英文刊名:Acta Seismologica Sinica
  • 机构:青海省地震局;
  • 出版日期:2019-03-15
  • 出版单位:地震学报
  • 年:2019
  • 期:v.41
  • 基金:青海省地震科学基金(2017A01);; 2017年震情跟踪定向工作任务(2017010402)共同资助
  • 语种:中文;
  • 页:DZXB201902009
  • 页数:10
  • CN:02
  • ISSN:11-2021/P
  • 分类号:103-112
摘要
利用小波分解对2010—2016年南北地震带(21°N—37°N,97°E—109°E)区域6期岩石圈磁场年变化数据进行处理,并对2011年6月以来该区域发生的M_S≥5.0强震震中区的岩石圈磁场变化空间分布及时间演化特征进行了系统分析。结果显示:震级与岩石圈磁场ΔX,ΔY,ΔZ分量变化的相关系数分别为0.26,-0.26,0.15,即二者无显著相关性;震中处岩石圈磁场分量变化的最大幅值分别为18.46,14.98,-15.54 nT。对岩石圈磁场变化进行小波分解的结果表明:MS7.0地震前两年出现显著基底异常,其尺度可能达到上千千米;M_S6.0地震前一年也出现显著基底异常,但异常尺度较小;M_S5.0地震前尚未观测到明确的基底或中层异常。
        This paper processed six issues of annual variation data of lithospheric magnetic field from 2010 to 2016 in the North-South Seismic Belt(21°N-37°N,97°E-109°E) by using wavelet decomposition,and systematically analyzed the annual variation of lithospheric magnetic field in epicenters of strong earthquakes(M_S≥5.0) since June of 2011. The results show that correlative coefficients between earthquake magnitude and lithospheric magnetic field components ΔX,ΔY,ΔZ are 0.26,-0.26,0.15,respectively,which means there is no significant correlation between the two parameters;the maximum variation amplitude of lithospheric magnetic field components ΔX,ΔY,ΔZ in the epicenters of strong earthquakes are 18.46,14.98,-15.54 nT,respectively. The wavelet decomposition results show that there is significant variation on basic layers with maximum scale of one thousand kilometers in two years before MS7.0 earthquakes,and significant variation also appears on basic layer in one year before M_S6.0 earthquakes,but the scale is smaller;as to before MS5.0 earthquakes,no significant anomalies have been found on basic layer or middle layer.
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