Delineation of seismic source zones based on seismicity parameters and probabilistic evaluation of seismic hazard using logic tree approach

被引:12
作者
Vipin, K. S. [1 ]
Sitharam, T. G. [2 ]
机构
[1] Indian Inst Sci, Bangalore 560012, Karnataka, India
[2] Indian Inst Sci, Dept Civil Engn, Bangalore 560012, Karnataka, India
关键词
Source zone; PSHA; logic tree; site response; PHA; PGA; Sa; local site effects; MOTION PREDICTION EQUATIONS; INCOMPLETE DATA FILES; EARTHQUAKE HAZARD; SPECTRAL ACCELERATION; MAGNITUDE; INDIA; CATALOGS;
D O I
10.1007/s12040-013-0300-4
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The delineation of seismic source zones plays an important role in the evaluation of seismic hazard. In most of the studies the seismic source delineation is done based on geological features. In the present study, an attempt has been made to delineate seismic source zones in the study area (south India) based on the seismicity parameters. Seismicity parameters and the maximum probable earthquake for these source zones were evaluated and were used in the hazard evaluation. The probabilistic evaluation of seismic hazard for south India was carried out using a logic tree approach. Two different types of seismic sources, linear and areal, were considered in the present study to model the seismic sources in the region more precisely. In order to properly account for the attenuation characteristics of the region, three different attenuation relations were used with different weightage factors. Seismic hazard evaluation was done for the probability of exceedance (PE) of 10% and 2% in 50 years. The spatial variation of rock level peak horizontal acceleration (PHA) and spectral acceleration (Sa) values corresponding to return periods of 475 and 2500 years for the entire study area are presented in this work. The peak ground acceleration (PGA) values at ground surface level were estimated based on different NEHRP site classes by considering local site effects.
引用
收藏
页码:661 / 676
页数:16
相关论文
共 44 条
[1]   Unusual lithospheric structure and evolutionary pattern of the cratonic segments of the South Indian shield [J].
Agrawal, PK ;
Pandey, OP .
EARTH PLANETS AND SPACE, 2004, 56 (02) :139-150
[2]  
Aki K., 1965, B EARTHQ RES I TOKYO, V43, P237, DOI DOI 10.1111/J.1365-246X.-2008.04059.X
[3]   Probabilistic seismic hazard analysis for Bangalore [J].
Anbazhagan, P. ;
Vinod, J. S. ;
Sitharam, T. G. .
NATURAL HAZARDS, 2009, 48 (02) :145-166
[4]  
[Anonymous], 2000, SEISM ATL IND
[5]  
[Anonymous], 2001, 368 BSSC FEMA
[6]   Earthquake ground-motion prediction equations for eastern North America [J].
Atkinson, Gail M. ;
Boore, David M. .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2006, 96 (06) :2181-2205
[7]  
BENDER B, 1983, B SEISMOL SOC AM, V73, P831
[8]  
Bhatia S, 1997, ANN GEOFIS, V42, P1154
[9]   On the use of logic trees for ground-motion prediction equations in seismic-hazard analysis [J].
Bommer, JJ ;
Scherbaum, F ;
Bungum, H ;
Cotton, F ;
Sabetta, F ;
Abrahamson, NA .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2005, 95 (02) :377-389
[10]  
Budnitz R.J., 1997, NUREG/CR-6372