Radiated seismic energy from coda measurements and no scaling in apparent stress with seismic moment
The seismic coda consists of scattered waves that leave the earthquake source in a variety of directions. The averaging of source radiation that results leads to stable ground motion spectra that we use as the basis for a robust measurement of radiated wave energy. We apply an empirical Green's...
| Autores Principales: | , , |
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| Formato: | Artículo (Article) |
| Lenguaje: | Inglés (English) |
| Publicado: |
American Geophysical Union
2010
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| Materias: | |
| Acceso en línea: | https://repository.urosario.edu.co/handle/10336/26837 https://doi.org/10.1029/2009JB006736 |