Do seismic waves sense fracture connectivity?
A defining characteristic of fractured rocks is their very high level of seismic attenuation, which so far has been assumed to be mainly due to wave-induced fluid flow (WIFF) between the fractures and the pore space of the embedding matrix. Using oscillatory compressibility simulations based on the...
Guardado en:
| Autores principales: | Rubino, Jorge Germán, Guarracino, Luis, Müller, Tobias M., Holliger, Klaus |
|---|---|
| Formato: | Articulo |
| Lenguaje: | Inglés |
| Publicado: |
2013
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| Materias: | |
| Acceso en línea: | http://sedici.unlp.edu.ar/handle/10915/102664 https://ri.conicet.gov.ar/11336/21935 |
| Aporte de: |
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