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地震 ›› 2006, Vol. 26 ›› Issue (3): 53-63.

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北京及邻近地区中等以上地震地下流体异常识别与特征研究

杨明波1, 王吉易2, 刘喜兰3, 王力1, 赵文忠1, 鲁跃1, 张洪魁1   

  1. 1.北京市地震局, 北京 100080;
    2.河北省地震局, 河北 石家庄 050021;
    3.天津市地震局, 天津 300201
  • 收稿日期:2006-02-23 修回日期:2006-03-24 发布日期:2021-11-01
  • 作者简介:杨明波(1966-), 男, 山东莒县人, 1997年获硕士学位, 副研究员, 主要从事地震监测预报等研究。
  • 基金资助:
    北京市“十五”科技攻关项目(H030630090190)

Study on recognition of fluid anomaly and its characteristics for moderately strong earthquakes in Beijing region and its adjacent area

YANG Ming-bo1, WANG Ji-yi2, LIU Xi-lan3, WANG Li1, ZHAO Wen-zhong1, LU Yue1, ZHANG Hong-kui1   

  1. 1. Earthquake Administration of Beijing Municipality, Beijing 100080;
    2. Earthquake Administration of Hebei province, Shijiazhuang 050021;
    3. Earthquake Administration of Tianjin Municipality, Tianjin 300201, China
  • Received:2006-02-23 Revised:2006-03-24 Published:2021-11-01

摘要: 系统分析了北京及其邻区多年积累的震例资料, 提出该区的地下流体异常分为趋势上升型中期异常、 转折型中短期异常、 突发型短期异常和短临异常等类型。 运用“同一化”思路、 从属函数、 剩余曲线及原始曲线均方差等异常判定方法, 提取了中等以上地震, 特别是5级以上地震的中、 短、 临异常实例。 通过对流体异常特征的统计分析, 给出了北京及邻近地区的中期、 中短期、 短期和短临异常的时间分布特征, 并对地震前各阶段异常的超前时间进行了总结, 该时间可作为发震时间的预测指标。 在实际应用中可为该区的震情判定提供依据。

关键词: 地下流体异常, 同一化, 中等地震, 北京及其邻区

Abstract: This paper systematically analyzed the data of earthquake cases in Beijing and its adjacent area accumulated for many years, and point out that fluid anomaly can be divided by medium-term anomaly, medium-short term anomaly, short-term anomaly and short-imminent anomaly. Using “identity” idea and anomaly criterion of slave function, remain-curve and original-curve deviation etc, a set of medium-term, short-term and imminent-term anomaly of the moderately strong earthquakes, especially those with intensity ≥Ⅴ, above magnitude 5 earthquakes are extracted. Through statistics and analysis of fluid anomaly characteristics, this paper obtained the time distribution characteristics of fluid anomaly of the moderately strong earthquakes, especially those with intensity ≥Ⅴ, earthquakes in Beijing and its adjacent area, and summarized the leading time of each phases anomaly before the earthquakes, which can be regarded as index of occurrence time of earthquakes. It can provide reference for earthquake monitoring in this area.

Key words: Fluid anomaly, Identity, Moderately strong earthquake, Beijing and its adjacent area

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