Simulation of macroseismic field in Central Greece

The distribution of seismic intensity is generally influenced by major geological and tectonic features and, on a smaller scale, by local geological conditions, such as the type of surface soil, the surface-to-bedrock soil structure in sedimentary basins and the depth of the saturated zone, The pres...

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Bibliographic Details
Main Authors: J. Drakopoulos, D. Michalopoulou, K. C. Makropoulos, S. Chailas, V. Kouskouna
Format: Article
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1996-06-01
Series:Annals of Geophysics
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