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...

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Detalles Bibliográficos
Autores Principales: Baltay, Annemarie, Prieto, German, Beroza, Gregory C.
Formato: Artículo (Article)
Lenguaje:Inglés (English)
Publicado: American Geophysical Union 2010
Acceso en línea:https://repository.urosario.edu.co/handle/10336/26837