Prograde Rayleigh-wave motion in the valley of Mexico
A theory of prograde particle motion of Rayleigh waves for a layer over a half-space is derived and compared withobservations in the valley of Mexico. We compute synthetic seismograms for a simplified model of the Texcoco site. Theearthquake of 19 September 1985, M 8.1, featured prograde motion of R...
Kaydedildi:
| Yayımlandı: | Geofísica Internacional |
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| Asıl Yazarlar: | , , , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Universidad Nacional Autónoma de México
2006
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| Konular: | |
| Online Erişim: | https://www.redalyc.org/articulo.oa?id=56845301 |
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