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...
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| 發表在: | Geofísica Internacional |
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| Principais autores: | , |
| 格式: | Artigo |
| 語言: | Inglês |
| 出版: |
Universidad Nacional Autónoma de México
2005
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| 主題: | |
| 在線閱讀: | https://www.redalyc.org/articulo.oa?id=56844205 |
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