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京西北盆岭构造区强震复发概率模型及地震潜势的定量评估 被引量:10

PROBABILITY MODEL FOR STRONG EARTHQUAKE RECURRENCE AND QUANTITATIVE ESTIMATES OFSEISMIC POTENTIAL IN THE BASINN-AND-RANGE PROVINCE,NORTHWEST OF BEIJING
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摘要 基于京西北盆岭构造区活动构造的定量化研究成果 ,视强震复发间隔为一随机变量 ,借鉴NB模型的建模方法 ,结合强震复发过程中存在分形规律的思想 ,建立京西北模型———强震复发间隔的均一化值服从正态分布N(1.0 0 0 3,0 .2 4 6 4 2 ) ;京西北盆岭构造区未来可能发生地震概率较高的断裂是 :天镇 -阳高盆地北缘断裂、阳原盆地南缘断裂、延庆盆地北缘断裂辛韩段、矾山盆地北缘断裂燕水段。 Based on the results of quantitative research on active faults,and especially the detailed investigation and systematic summary on paleoearthquakes in the basin-and-range province,northwest of Beijng by Ran Yongkang et al., a catalog of strong earthquakes since 25ka B.P. (including historical earthquakes) has been compiled for the 15 individual segments of 7 active faults in this area. Furthermore,this catalog is used to estimate the strong earthquake recurrence interval (T),average strong earthquake recurrence interval (T a) and value of normalized function (T/T a) for all specific fault segments in the light of the thought of the NB model.In these estimations,the recurrence intervals of strong earthquakes on 2 specific segments are estimated separately for longer-interval and shorter-interval,and correspondingly their T a and T a/T values are estimated in the same manner.The reason is that we found that the recurrence of characteristic earthquakes follows a fractal-law,i.e. the recurrence of characteristic earthquake follows a quasi-periodic model with longer quiet and active periods,while within the active period it follows a quasi-periodic model with shorter interval.Moreover,the recurrence of small earthquakes within the relatively short active period may follow a clustering model. As the 15 fault segments have a similar tectonic environment,it is considered that they have a similar recurrence model of strong earthquakes.Therefore, the obtained 35 T/T a values are treated as an equal basis for the statistical analysis.The result of statistic analysis shows that the distribution of normalized strong earthquake recurrence internal follows a normal distribution with mean (μ) equal to 1.000 3 and standard deviation (σ) of 0.246 4,and we call it the Northwest Beijing model.Using this model and also comparing with the NB model,we have estimated the probabilities of strong earthquake occurrence on 25 segments of 15 faults in the basin-and-range province,northwest of Beijing.The results indicate that the potential fault segments for the occurrence of future strong earthquake should be the North marginal fault of the Tiznzhen-Yanggao basin,the South marginal fault of the Yangyuan basin,the Xingwei segment of the North marginal fault of the Yanqing basin,the Yanshui segment of the North marginal fault of the Fanshan basin,and the South marginal fault of the Xuanhua basin.
出处 《地震地质》 EI CSCD 北大核心 2002年第1期91-100,共10页 Seismology and Geology
基金 国家重点基础研究发展规划项目 (95 130 10 5 ) 中国地震局重点项目 (95 0 4 0 80 3)共同资助 中国地震局地质研究所论著 2 0 0 2B0 0 0 7
关键词 京西北岭构造区 强震复发概率模型 地震潜势 地震 概率分布 定量评估 活动构造 Earthquake,Probability distribution, Model of northwest Beijing,Quantitative estimates
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