1887

Abstract

The peak ground motion parameters, related to earthquake hazard at a given site, are strongly dependent on the source process, the ray path and the local geological conditions. The area of Thiva city, situated in Central Greece, is surrounded by seismogenetic zones characterized by high seismicity level (figure 1). The broad region of Thiva has sustained severe damage from earthquakes occurred in near and moderate distances.

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/content/papers/10.3997/2214-4609.201407206
1998-09-14
2020-04-08
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407206
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