Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures

An important characteristic of fractured rocks is their high seismic attenuation, which so far has been mainly attributed to wave-induced fluid flow (WIFF) between the fractures and the embedding matrix. The influence of fracture connectivity on seismic attenuation has, however, recently, only been...

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Detalles Bibliográficos
Autores principales:	Rubino, J. Germán, Quintal, Beatriz, Müller, Tobias M., Guarracino, Luis, Jänicke, Ralf, Steeb, Holger, Holliger, Klaus
Formato:	Articulo
Lenguaje:	Inglés
Publicado:	2015
Materias:	Geofísica fractured rocks seismic attenuation WIFF fracture connectivity embedding matrix Biot’s theory
Acceso en línea:	http://sedici.unlp.edu.ar/handle/10915/143073
Aporte de:	SEDICI (UNLP) de Universidad Nacional de La Plata

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