摘要
对SQIP地震学中期预测方法在华北地区的中期预测效果进行了重新评价，回溯性全时空扫描检验报准率R值约为0．67～0．68。做了方法中短期和短期预测指标的提取尝试。结果表明综合参量P值异常区由最大出现收缩后，平均约7个月左右发生未来主震，其中6个月内的震例约占有“收缩”震例的53％～54％，在3个月内的约占33％～35％；部分震例发生在异常区消失后7～8个月内。表明P值异常区“收缩”（或消失）一定程度上可以作为中、强地震的中短期预测标志。
The effect of SQIP method on the medium range earthquake prediction in Northern China are reevaluated, the R values calculated by Xu grade criterion are 0.67 - 0. 68 using the retrospective all time-space scan. And the medium-short and short range prediction index of this method is also extracted. The results show that after the anomaly region of synthetical parameter P shrinking about 7 months in average, main earthquake would accure. Among them 53% -54% events accured in 6 months after the shrinking, the 33% -35% events were in 3 months, and a few of events accured after the anomaly region disappeared for 7 - 8 months. Therefore, the anomaly region of synthetical parameter P shrinking or disappearing can be the medium-short range or short range predicting index for moderate strong earthquake.
出处
《西北地震学报》
CSCD
北大核心
2006年第2期167-171,共5页
Northwestern Seismological Journal
基金
"十五"国家重点科技攻关项目子专题(2004BA601B01-01-01)
关键词
SQIP方法
华北
地震预报
综合参量
预测指标
SQIP method
Northern China
Earthquake prediction
Synthesis parameter
Prediction index
