Attenuation relation of Arias intensity for Zagros Mountains region (Iran)

被引:18
|
作者
Rajabi, Ali M. [1 ]
Khamehchiyan, M. [1 ]
Mahdavifar, Mohammad R. [2 ]
Del Gaudio, V. [3 ]
机构
[1] Tarbiat Modares Univ, Engn Geol Dept, Tehran, Iran
[2] IIEES, Geotech Engn Res Ctr, Tehran, Iran
[3] Univ Bari, Dipartimento Geol & Geofis, I-70125 Bari, Italy
关键词
Attenuation relationship; Zagros; Arias intensity; Earthquake-induced landslides; TIME-PROBABILISTIC EVALUATION; LANDSLIDE HAZARD; EQUATIONS;
D O I
10.1016/j.soildyn.2009.09.008
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Arias intensity is considered as a shaking parameter Suitable for characterizing earthquake impact on ground stability. Within the framework of a Study aimed at providing tools for the assessment of hazards related to earthquake-induced slope failures, Arias intensity attenuation relations were determined for the Zagros Mountains region, an active tectonic belt elongated NW-SE in the western and south-western part of Iran. The calculation of relation coefficients was based on strong-motion data of earthquakes located in the Zagros area and recorded by Iranian stations managed by the Building and Housing Research Center of Iran (BHRC). Five models of attenuation relation were considered and their coefficients were estimated through a least-square regression analysis. The relations obtained were then applied to a data sample different from that used for regression and the root mean square (RMS) of residuals was examined in order to compare effectiveness of different relations in probabilistic estimates. Furthermore a comparison made with attenuation relations obtained for Alborz and the central part of Iran showed significant differences possibly related to structural differences. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:110 / 118
页数:9
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