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地震 ›› 2013, Vol. 33 ›› Issue (1): 56-64.

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宁夏及邻区地震震源衰减模型及震源参数研究

金春华1, 盛菊琴1, 田小慧1, 赵翠萍2   

  1. 1.宁夏地震局, 宁夏 银川 750001;
    2.中国地震局地震预测研究所, 北京 100036
  • 收稿日期:2012-03-21 修回日期:2012-09-17 出版日期:2013-01-31 发布日期:2020-10-16
  • 作者简介:金春华(1979-),女,青海乐都人,工程师,从事地壳速度结构及地震新参数方面的研究工作。
  • 基金资助:
    中国地震局台站三结合项目(201224)

Seismic Attenuation Model and Source Parameters in Ningxia and its Adjacent Areas

JIN Chun-hua1, SHENG Ju-qin1, TIAN Xiao-hui1, ZHAO Cui-ping2   

  1. 1. Earthquake Administration of Ningxia Hui Autonomous Region, Yinchuan 750001, China;
    2. Insitute of Earthquake Science, CEA, Beijing 100036, China
  • Received:2012-03-21 Revised:2012-09-17 Online:2013-01-31 Published:2020-10-16

摘要: 选取2003年1月至2011年12月宁夏及邻区发生的201个ML2.0以上地震事件进行反演, 用经验格林函数计算得到本区地震震源谱衰减模型。 在已知非弹性衰减系数和场地响应的条件下, 计算得到震源谱并研究了近震震级与拐角频率、 地震矩、 震源破裂半径及应力降之间的关系。 详细分析了震源参数误差大小及各种误差影响因素。 对剩余应力降时空演化特征分析研究结果表明: 高剩余应力降集中分布在宁夏北部宁蒙交界地区、 低剩余应力降分布在宁夏中部同心、 中卫一带, 银川盆地中南部的吴灵地区和宁夏南部海原断裂带中东段剩余应力降变化较为明显, 在时间分布上这两个区域剩余应力降在中强地震前均有降低—增强的趋势。

关键词: 震源谱衰减模型, 震源参数误差, 剩余应力降, 宁夏及邻区

Abstract: 201 events of ML≥2.0 are selected from January 2003 to December 2011 in Ningxia and its adjacent areas for inversion. Seismic spectral attenuation models are calculated by empirical Green function. On the base of known inelastic attenuation coefficient and site response, the source spectra are calculated and the relationship between local magnitude and corner frequency, seismic moments, rupture radius and stress drop are studied. Magnitude of error of seismic source parameters and influence factors are analyzed in detail. Temporal evolution characteristics of residual stress drop analysis results show that high residual stress drop is concentrated in the northern Ningxia and Inner Mongolia border region, low in Tongxin and Zhongwei area of central Ningxia. Residual stress drop changes more obviously in the Wuling area of south-central Yinchuan basin and middle-east Haiyuan fault of southern Ningxia. On these two regions, residual stress drops have decrease-enhancement trend in temporal distribution before strong earthquakes.

Key words: Source Spectrum Attenuation, Source parameters, Residual stress drop, Ningxia and its adjacent area

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