Ground Motion Simulations of the SW Iberia Margin: Rupture Directivity and Earth Structure Effects.

Abstract In this study, we focus on the region between Gorringe Bank and the Horseshoe Fault located in the SW Iberia margin, which is believed to be the site of the great 1755 earthquake. We model ground motions using an extended source located near the Horseshoe scarp to generate synthetic wavefor...

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Bibliographic Details
Main Author: Bezzeghoud, M. (author)
Other Authors: Borges, J. F. (author), Caldeira, B. (author)
Format: article
Language:por
Published: 2012
Subjects:
Seismicity
Ground motion
Seismic Source
Rupture Directivity
Earth Structure
Iberia Margin
Online Access:http://hdl.handle.net/10174/3303
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/3303

Internet

http://hdl.handle.net/10174/3303

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