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we develop a theoretical model to describe the dispersion and attenuation of oblique incident P and SV waves, where the rock is composed of a microcracked porous background and aligned fractures. We investigate the multiple attenuation mechanisms of FB-WIFF, ES, microcrack squirt flow, and Biot flow and their coupling effects.
Aligned fractures; P- and SV-wave dispersion and attenuation; microcracked porous rock; FB-WIFF; ES; squirt flow
Aligned fractures; P- and SV-wave dispersion and attenuation; microcracked porous rock; FB-WIFF; ES; squirt flow
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