Dynamic seismic signatures of saturated porous rocks containing two orthogonal sets of fractures: Theory versus numerical simulations
The dispersion and attenuation of seismicwaves are potentially important attributes for the noninvasive detection and characterization of fracture networks. A primary mechanism for these phenomena is wave-induced fluid flow (WIFF), which can take place between fractures and their embedding backgroun...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Blackwell Publishing Ltd
2018
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| Online Access: | http://hdl.handle.net/20.500.11937/67572 |