Using a Synthetic Borehole Model to Determine the Pore Aspect Ratio Dependence of Velocities from Acoustic Well-Logging Data

<div>The received waveforms from one borehole model. The differential arrival times of P- and S-waves between the two receivers (R1 and R2 in Figure <a href="../fig4/">4</a>) are used to calculate the wave velocities.</div>

Geofluids

fig5

Figure 5

Figure 5: Using a Synthetic Borehole Model to Determine the Pore Aspect Ratio Dependence of Velocities from Acoustic Well-Logging Data 