Seismic Hazard and Risk Assessment for Tulbagh, South Africa: Part I – Assessment of Seismic Hazard

被引:0
作者
A. Kijko
S. J. P. Retief
G. Graham
机构
[1] Council for Geoscience,
来源
Natural Hazards | 2002年 / 26卷
关键词
seismic hazard; probabilistic; South Africa; historical data; instrumental data;
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中图分类号
学科分类号
摘要
In this part of our study the probabilistic seismic hazard analysis (PSHA) for Tulbagh was performed. The applied procedure is parametric and consists essentially of two steps. The first step is applicable to the area in the vicinity of Tulbagh and requires an estimation of the area-specific parameters, which, in this case, is the mean seismic activity rate, λ, the Gutenberg-Richter parameter, b, and the maximum regional magnitude, mmax. The second step is applicable to the Tulbagh site, and consists of parameters of distribution of amplitude of the selected ground motion parameter. The current application of the procedure provides an assessment of the PSHA in terms of peak ground acceleration (PGA) and spectral acceleration (SA). The procedure permits the combination of both historical and instrumental data. The historical part of the catalogue only contains the strongest events, whereas the complete part can be divided into several subcatalogues, each assumed complete above a specified threshold of magnitude. In the analysis, the uncertainty in the determination of the earthquake was taken into account by incorporation of the concept of `apparent magnitude'. The PSHA technique has been developed specifically for the estimation of seismic hazard at individual sites without the subjective judgement involved in the definition of seismic source zones, when the specific active faults have not been mapped or identified, and where the causes of seismicity are not well understood. The results of the hazard assessment are expressed as probabilities that specified values of PGA will be exceeded during the chosen time intervals, and similarly for the spectral accelerations. A worst case scenario sketches the possibility of a maximum PGA of 0.30g. The results of the hazard assessment can be used as input to a seismic risk assessment.
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页码:175 / 201
页数:26
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[11]  
Kijko A.(1993)Computation of seismic hazard Ann. Di Geofisica 36 181-200
[12]  
Sellevoll M. A.(1968)Aftershocks and microaftershocks Bull. Seism. Soc. Am. 58 1131-1168
[13]  
Kijko A.(1985)Effects of magnitude uncertainties in the Gutenberg-Richter frequency-magnitude law Bull. Seism. Soc. Am. 75 1681-1697
[14]  
Sellevoll M. A.(1997)Model of strong ground motions from earthquakes in Central and Eastern North America: best estimates and uncertainties Seism. Res. Lett. 68 41-57
[15]  
Kijko A.(1975)On the correlation of seismic intensity scales with the peaks of recorded ground motion Bull. Seism. Soc. Am. 65 139-162
[16]  
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