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 attenuation be...
Gardado en:
| Publicado en: | Geofísica Internacional |
|---|---|
| Principais autores: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Universidad Nacional Autónoma de México
2005
|
| Assuntos: | |
| Acceso en liña: | https://www.redalyc.org/articulo.oa?id=56844205 |
| Tags: |
Sen Etiquetas, Sexa o primeiro en etiquetar este rexistro!
|