Ground Motion Simulations of the SW Iberia Margin: Rupture Directivity and Earth Structure Effects.
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 waveforms using...
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| Outros Autores: | , |
| Formato: | article |
| Idioma: | por |
| Publicado em: |
2012
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| Assuntos: | |
| Texto completo: | http://hdl.handle.net/10174/3298 |
| País: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/3298 |