潜在地震破裂面源模型及在概率地震危险性分析中的应用方法  

POTENTIAL RUPTURE SURFACE MODEL AND ITS APPLICATION ON PROBABILISTIC SEISMIC HAZARD ANALYSIS

作　　者：胥广银[1] 高孟潭[1] 

机构地区：[1]中国地震局地球物理研究所,中国北京100081

出　　处：《地震学报》2007年第3期285-294,共10页Acta Seismologica Sinica

基　　金：地震科学联合基金项目(104065);科研院所社会公益研究专项(2005DIB3J119)资助.

摘　　要：目前国内外常用的概率地震危险性分析方法中,一般把未来可能发生的地震震源(潜在震源)简化为点源或者是线源.但对于较大震级的地震,仍然采用点源或线源模型来描述潜在震源显然是不合理的.为此,在概率地震危险性分析方法中本文提出了潜在地震破裂面源模型,并以1999年9月21日台湾集集7.6级地震的车笼埔断层为例,探讨了其在地震危险性分析中的应用方法.结果表明:①采用潜在地震破裂面源模型是合理的,因为它可以模拟地震破裂面与地震动影响场的三维展布特征,尤其适用于较大震级地震的近场区域;②潜在地震破裂面源的大小、产状,对近震源场点的地震危险性分析和地震区划结果有明显的控制影响.Potential sources are simplified as point sources or linear sources in current probabilistic seismic hazard analysis （PSHA） methods. Focus size of large earthquakes is considerable, and fault rupture attitudes may have great influence upon the seismic hazard of a site which is near the source. Under this circumstance, it is unreasonable to use the simplified potential source models in the PSHA, so a potential rupture surface model is proposed in this paper. Adopting this model, we analyze the seismic hazard near the Chelungpu fault that generated the Chi-Chi （Jiji） earthquake with magnitude 7.6 and the following conclusions are reached. ① This model is reasonable on the base of focal mechanism, especially for sites near potential earthquakes with large magnitude;② The attitudes of potential rupture surfaces have great influence on the results of probabilistic seismic hazard analysis and seismic zoning.

关 键 词：潜在震源 地震破裂面产状 潜在地震破裂面源 概率地震危险性分析 地震区划 

分 类 号：P315.9[天文地球—地震学]