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A seismic attenuation zone below Popocatépetl volcano inferred from coda waves of local earthquakes
Using a single scattering model, weighted averages of the quality factor <Qc> were estimated at 6 Hz for coda wavewindows 25s after S-wave arrival at depths ranging from 2 to 10 km and magnitudes between 2 and 3. Considering Qc-1 as intrinsicattenuation, we find a zone of seismic wave attenuat...
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| Publicado no: | Geofísica Internacional |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Universidad Nacional Autónoma de México
2005
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| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=56844205 |
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