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地震 ›› 2001, Vol. 21 ›› Issue (3): 57-64.

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加卸载响应比方法的空间扫描应用研究

王琤琤, 梅卫萍, 王炜, 杨彩霞, 缪发军   

  1. 1.江苏省地震局,江苏南京 210014;
    2.上海市地震局,上海 200062
  • 收稿日期:2001-03-16 修回日期:2001-04-30 出版日期:2001-07-31 发布日期:2022-06-02
  • 作者简介:王琤琤(1948-),女,江苏无锡人,副研究员,主要从事测震学和地震预报研究。
  • 基金资助:
    “九五”中国地震局科研攻关项目(96-913-01-17)

A study on the practical application of the spatial scanning of loading/unloading response ratio

WANG Zheng-zheng1, MEI Wei-ping1, WANG Wei2, YANG Cai-xia1, MIAO Fa-jun2   

  1. 1. Seismological Bureau of Jiangsu Province, Nanjing 210014, China;
    2. Seismological Bureau of Shanghai Municipality, Shanghai 200062, China
  • Received:2001-03-16 Revised:2001-04-30 Online:2001-07-31 Published:2022-06-02

摘要: 用基于构造应力场资料的加卸载响应比方法,通过应力场参数、最少样本量等多种参数的分区全时空扫描对比,全面总结了大华北地区1970~1999年5级以上地震前的中期和短期时间演化特征: 在最少样本为15时,震前2年左右在震中附近出现Y3≥2的高值异常区,于震前1年收缩、甚至消失,并常常在震前6个月左右时在震中处出现小范围的高值异常。预报效能R评分为0.3~0.5, P评分为0.4~0.6。研究结果还显示, 4级左右的中等地震前也存在Y3的高值异常。

关键词: 加卸载响应比, 全时空扫描, 孕震信息, 时空演化

Abstract: In the paper, a comprehensive investigation has been made on the precursory variations in the loading/unloading response ratio (Called Y value) prior to the earthquakes M≥5 in Northern China during the period of 1970~1999. It is based on a comparison of the results of the ratio's temporal-spatial scanning with different values of related parameters such as the stress field, and the least sample amount. As aresult, the following medium-term and short-term evolution characteristics have been revealed. When the least sample amount is 15, an a noma lous area of high value with Y3≥2 appeared in the vicinity of the epicenter about 2 years before the earthquake. It contracted or even disappeared one year before the earthquake and a small anomalous area with high value usually about 6 months before the earthquake at the epicenter. The R-value of the prediction efficiency assessment is 0.3~0.5 and that of P is 0.4~0.6. The study has also shown that anomalous area of Y3 high value appeared before moderate earthquakes with magnitude about 4 too.

Key words: Loading/unloading response ratio, Temporal-spatial scanning, Seismogenic information, time-space evolution

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