An energy-based approach to estimate seismic attenuation due to wave-induced fluid flow in heterogeneous poroelastic media

Wave-induced fluid flow (WIFF) due to the presence of mesoscopic heterogeneities is considered as one of the main seismic attenuation mechanisms in the shallower parts of the Earth’s crust. For this reason, several models have been developed to quantify seismic attenuation in the presence of heterog...

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Autores principales: Solazzi, Santiago Gabriel, Rubino, Jorge Germán, Müller, Tobias M., Milani, Marco, Guarracino, Luis, Holliger, Klaus
Formato: Articulo
Lenguaje:Inglés
Publicado: 2016
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/103086
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