Frequency dependent anisotropy of porous rocks with aligned fractures
In fractured reservoirs, the wave induced fluid flow between pores and fractures can cause significant dispersion and attenuation of seismic waves. For waves propagating normal to the fractures this effect has been quantified in earlier studies. Here we extend normal incidence results to oblique inc...
| Main Authors: | , , |
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| Format: | Conference Paper |
| Published: |
European Association of Geoscientists and Engineers, EAGE
2011
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| Online Access: | http://hdl.handle.net/20.500.11937/28585 |