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沂沭断裂带小震震源参数特征分析

李翠芹 张正帅 郑建常 戴宗辉

李翠芹,张正帅,郑建常,戴宗辉,2023. 沂沭断裂带小震震源参数特征分析. 震灾防御技术,18(2):274−283. doi:10.11899/zzfy20230208. doi: 10.11899/zzfy20230208
引用本文: 李翠芹,张正帅,郑建常,戴宗辉,2023. 沂沭断裂带小震震源参数特征分析. 震灾防御技术,18(2):274−283. doi:10.11899/zzfy20230208. doi: 10.11899/zzfy20230208
Li Cuiqin, Zhang Zhengshuai, Zheng Jianchang, Dai Zonghui. Characteristics of Seismic-source Spectral Parameters of Small Earthquakes in Yishu Fault Zone[J]. Technology for Earthquake Disaster Prevention, 2023, 18(2): 274-283. doi: 10.11899/zzfy20230208
Citation: Li Cuiqin, Zhang Zhengshuai, Zheng Jianchang, Dai Zonghui. Characteristics of Seismic-source Spectral Parameters of Small Earthquakes in Yishu Fault Zone[J]. Technology for Earthquake Disaster Prevention, 2023, 18(2): 274-283. doi: 10.11899/zzfy20230208

沂沭断裂带小震震源参数特征分析

doi: 10.11899/zzfy20230208
基金项目: 中国地震科学实验场地震可预测性国际合作项目(2018YFE0109700);山东省地震局一般项目(YB2006);中国地震局震情跟踪定向工作任务(2021010121);中国地震科学实验场的地震可预测性国际合作研究(2018YFE0109700)
详细信息
    作者简介:

    李翠芹,女,生于1987年。硕士,工程师。主要从事数字地震学方面的研究。E-mail:licuiqin12@163.com

    通讯作者:

    张正帅,男,生于1989年。硕士,工程师。主要从事地震波理论与应用方面的研究。E-mail:zhangzs1989@126.com

Characteristics of Seismic-source Spectral Parameters of Small Earthquakes in Yishu Fault Zone

  • 摘要: 利用山东台网记录的2010—2020年沂沭断裂带范围内的地震波形资料,基于高频截止模型,以理论震源谱对观测震源谱之间的最小绝对残差值作为目标函数,使用稳健的最小二乘法估计模型参数,得到93个地震震源谱的特征参数和震源参数,对不同震源参数之间的定标关系及视应力的时空特征进行分析。研究结果表明,高频截止模型的理论震源谱对观测震源谱有较好的拟合效果,能够明显改善拐角频率识别效果,因此该模型更适用于观测震源谱;沂沭断裂带中小地震的拐角频率为2~15 Hz,与矩震级有较好的相关关系,震级越大,拐角频率越低;地震矩$ {M}_{0} $与震级$ {M}_{{\mathrm{L}}} $在单对数坐标系下存在较好的线性关系,利用稳健函数线性拟合,可表示为$ \mathrm{log}{M}_{0}=1.096{M}_{{\mathrm{L}}}+9.78 $;地震视应力的时间分布特征表明,沂沭断裂带2012—2014年地震视应力偏高,地震强度和频次明显增加,2016年后地震视应力有所降低,地震强度和频次有所降低;沂沭断裂带地震多发生在高视应力内部和边缘地区,断裂带中南部的莒南-临沂和断裂带北段的安丘段存在明显高视应力集中区,这些区域为沂沭带未来可能发生中强地震的潜在震源区,有必要对高视应力区的地球物理特征进行监测。
  • 图  1  数据资料

    Figure  1.  Data sheet

    图  2  山东地区56个台站的场地响应(苗庆杰等,2016

    Figure  2.  The site responses of 56 stations in Shandong province(Miao et al., 2016

    图  3  2012年5月10日莒县ML2.3地震计算实例

    Figure  3.  Calculation example of the Juxian ML2.3 earthquake on May 10, 2012

    图  4  部分地震震源谱拟合结果

    Figure  4.  Partial seismic source spectrum fitting results

    图  5  震源参数之间的定标关系

    Figure  5.  Scaling relation among source parameters

    图  6  拐角频率随时间的变化曲线

    Figure  6.  Variation of corner frequency with time

    图  7  视应力随时间演化曲线

    Figure  7.  Variation of apparent stress with time

    图  8  视应力空间分布特征

    Figure  8.  Spatial distribution of differential apparent stress

    图  9  视应力深度分布与地震波速度结构关系

    Figure  9.  Relationship between apparent stress depth distribution and seismic wave velocity structure

  • 晁洪太, 李家灵, 崔昭文等, 1994. 郯庐断裂带中段全新世活断层的特征滑动行为与特征地震. 内陆地震, 8(4): 297—304 doi: 10.16256/j.issn.1001-8956.1994.04.002

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  • 收稿日期:  2022-04-11
  • 刊出日期:  2023-06-30

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