|
|
|
|
Exact seismic velocities for TI media and extended Thomsen formulas for stronger anisotropies |
Figures 1-6 present results for the case of vertical fractures having an isotropic distribution of normals (symmetry axes) in the horizontal plane. The resulting medium has VTI symmetry.
A first observation is that the low crack density results for
are nearly constant, showing that
. When this happens for
,
it is also true that
is approximately elliptical. Of course,
the exact results for
are always elliptical, but the
Thomsen and new approximate results are only approximately elliptical.
Secondly, all three velocity models (exact, Thomsen, and the new approximation)
give very similar results for all cases shown when
. There are however
some significant differences among the results for
,
especially for
and
- the largest deviations
from the exact curves being those for Thomsen's approximations (red curves)
in both cases.
|
|---|
|
FIG7
Figure 7. For aligned vertical fractures and HTI symmetry: examples of anisotropic quasi-P compressional wave speed ( |
|
|
|
|---|
|
FIG8
Figure 8. Same as Figure 7 for SH shear wave speed ( |
|
|
|
|---|
|
FIG9
Figure 9. Same as Figure 7 for quasi-SV shear wave speed ( |
|
|
|
|---|
|
FIG10
Figure 10. Same as Figure 7, for a different background medium having Poisson's ratio |
|
|
|
|---|
|
FIG11
Figure 11. Same as Figure 8, but the value of |
|
|
|
|---|
|
FIG12
Figure 12. Same as Figure 9, but the value of |
|
|
|
|
|
|
Exact seismic velocities for TI media and extended Thomsen formulas for stronger anisotropies |