Relationships Between Fundamental Seismic Hazard Parameters for the Different Source Regions in Turkey

被引:0
作者
Yusuf Bayrak
Ahmet Yilmaztürk
Serkan Öztürk
机构
[1] Karadeniz Technical University,Department of Geophysics
来源
Natural Hazards | 2005年 / 36卷
关键词
Gutenberg–Richter relationship; intensity; magnitude; modal values; seismic hazard;
D O I
暂无
中图分类号
学科分类号
摘要
Turkey has been divided into eight different seismic regions taking into consideration the tectonic environments and epicenters of the earthquakes to examine relationships of the modal values (a/b), the expected maximum magnitudes (Mmax) and the maximum intensities (Imax). For this purpose, the earthquakes for the time period 1900–1992 from the Global Hypocenter Data Base CD-ROM prepared by USGS, and for the time period 1993–2001 from the PDE data and IRIS data are used. Concerning the relationships developed between different magnitude scales and between surface wave magnitudes (MS) and intensity for different source regions in Turkey, we have constructed a uniform catalog of MS. We have estimated the values of Mmax and Imax using the Gumbel III asymptotic distribution. Highest a-values are observed in the Aegean region and the lowest b-values are estimated for the North Anatolian Fault. Maximum values of a/b, Mmax and Imax are related to the eastern and western part of the North Anatolian Fault and the Aegean Arc. The lowest values of all parameters are observed near the Mid Anatolian Fault system. Linear relationships have been calculated between a/b, Mmax and Imax using orthogonal regression. If one of the three parameters is computed, two other parameters can be calculated empirically using these linear relationships. Hazard maps of Mmax and Imax values are produced using these relationships for a grid of equally spaced points at 1°. It is observed that the maps produced empirically may be used as a measure of seismic hazard in Turkey.
引用
收藏
页码:445 / 462
页数:17
相关论文
共 42 条
[1]  
Båth M.(1981)Earthquake recurrence of a particular type PAGEOPH 119 1063-1076
[2]  
Bayrak Y.(2002)Lateral variations of the modal ( J. Geodynamics 34 653-666
[3]  
Yılmaztürk A.(1983)/ Bull. Seism. Soc. Am. 73 831-851
[4]  
Öztürk S.(1979)) values for the different regions of the world Geophys. J. R. Astr. Soc. 59 249-280
[5]  
Bender B.(1984)Maximum likelihood estimation of b values for magnitude grouped data Geophys. J. R. Astr. Soc. 78 475-506
[6]  
Burton P. W.(1976)Seismic risk in southern Europe through to India examined using Gumbel’s third distribution of extreme values Bull. Seism. Soc. Am. 66 843-868
[7]  
Burton W. P.(1985)Seismic Risk in Turkey, the Aegean and eastern Mediterranean: The occurrence of large magnitude earthquakes Tectonophysics 117 295-344
[8]  
McGonigle R.(1966)Seismicity of Northern Anatolia Nature 211 954-956
[9]  
Makropoulos K. C.(1944)A probabilistic assessment of the seismic hazard in Turkey Bull. Seism. Soc. Am. 34 185-188
[10]  
Üçer S. B.(2002)A model for the occurrence of large earthquakes J. Seismol. 6 257-277