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地震 ›› 2000, Vol. 20 ›› Issue (z1): 65-69.

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地震预报中地震学异常的统计研究

吴富春, 许俊奇, 张宪, 董星宏   

  1. 陕西省地震局 ,陕西 西安 710068
  • 收稿日期:2000-05-08 修回日期:2000-05-29 出版日期:2000-09-30 发布日期:2022-09-23
  • 作者简介:吴富春 (1941-) ,男 ,江苏宜兴人 ,研究员 ,主要从事地震学、地震分析预报、工程地震等研究。
  • 基金资助:
    地震科学联合基金资助项目(95-07-431)

The statistical study on seismological anomalies in earthquake prediction of China

WU Fu-chun, XU Jun-qi, ZHANG Xian, DONG Xing-hong   

  1. Seismological Bureau of Shaanxi Province, Xi'an 710068, China
  • Received:2000-05-08 Revised:2000-05-29 Online:2000-09-30 Published:2022-09-23

摘要: 利用 1988年以来全国地震趋势会商会所提出的各类地震学异常 ,研究其与下一年大陆地震的对应关系。9年内 46种地震学方法所提出的 932项异常资料表明: 1989~ 1993年 ,用地震学预报地震方法的数量有一个增大过程; 各种方法所提出异常对应地震的比率在 0~ 48% ,平均约为 28% ,这也与中国地震预报中预报区数的成功率相当 ; 统计预报、区域应力场增强、地震条带、小震调制比、 b 值等方法有较高的地震对应率, 而地震活动异常平静、分数维、异常震群、C 值、 地震窗等方法地震对应率稍差; 用地震学方法预报地震最成功的年份在 1989年, 最差年份为 1990 年 ; 与预报区数的成功比率一样, 其地震的对应比率并未随时间的推后而有所提高。各种地震学方法的物理内涵及其与地震孕育的内在联系及各种地震学方法间相互关联问题是今后用地震 学方法预报地震的研究课题。

关键词: 地震学, 预报方法, 异常, 统计研究

Abstract: By using various seismological anomalies obtained from the National Workshop on Earthquake Tendency from 1988 to 1996, the relationship between the anomalies in a certain year and the earthquakes occurred in the Chinese mainland in the next year is studied.The data of 932 anomalies obtained from more than 46 predictio nmethods of seismology in the past nine years show that the numbers of the prediction methods of seismology increased from 1988 to 1996. The corresponding ratios for different seismological anomalies with moderate or larger earthquakes are between 0 and 48%, the average value is 28% which is numerically equal to the correct ratio of the forecasting regional number in Chinese earthquake prediction. The methods of the statistical prediction, the streng thening of regional stress field, the seismic bands, the modulation ratio of small earthquakes and the b -value have higher corresponding ratios with earthquakes. The methods of the anomaloust ranquility of seismic activity, the fractal dimension, the a nomalous earthquake swarm, the C -value and the earthquake windows have lower corresponding ratios with earthquakes. The year that has the highest forecasting ratio is 1989, and the year that has the lowest forecasting ratio is 1990. As the same as the forecasting regional number, the corresponding ratio of seismological anomaly does not increase when time goes on. The following questions may be further studied in the future: the physical meaning of every seismological prediction method and the inner relationship between the seismological anomaly and the earthquakes.

Key words: Seism ology, Prediction method, Anomaly, Sta tistical study

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