1887

Abstract

second and third layers decreases from south west towards the north east of the study area. Attentive to the velocity distribution of the P and S wave velocity, the Poisson’s ratio distribution as well as attenuation coefficient obtained for the identified layers of the area under investigation in the Bam city, it is concluded that the low velocity layer with high thickness and attenuation coefficient of the first layer can be attributed to be the cause of the strong motion vibration of the soil due to Bam earthquake on 26th December 2003 in the city.

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/content/papers/10.3997/2214-4609.20144900
2010-09-06
2024-04-20
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20144900
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