Advantages of Shear Wave Seismic in Morrow Sandstone Detection
Figure 8
Wave propagation snapshots for (a) P-wave, (b) S-wave and (c) PS-wave using Model 1c. We observe that amplitude of multiples due to shallow anhydrite layers is stronger than the reflection from the top of Morrow A sandstone in P- and PS-wave snapshot. Whereas the Morrow A sandstone response is stronger than the amplitude of multiples in S-wave snapshot.
