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The TTI case

In the case of a tilt in the angle of symmetry of the TI (TTI) medium, the dispersion relations 2 and 3 must be altered to reflect the tilt. Specifically, the wavenumbers should be transformed to the direction of the tilt. In fact, at the reflection point all equations used to develop the mapping in equation (4) hold regardless of the direction of tilt. This implies that the quadratic solution (5) applies with , , and given by Table 1 granted that the wavenumbers are transformed in the direction of the tilt. Considering that $\phi$ is the tilt angle measured from vertical in 2-D, the horizontal (conventional) wavenumbers given by the surface-recorded data are given by

$\displaystyle k_{sc} \equiv k_{sx} \cos\phi - k_{sz} \sin\phi,$

(6)

and

$\displaystyle k_{rc} \equiv k_{rx} \cos\phi - k_{rz} \sin\phi.$

(7)

where $k_{sx}$ and $k_{rx}$ now correspond to the normal-to-the-tilt wavenumber direction and they are related to $k_{sz}$ and $k_{rz}$ (tilt direction wavenumbers), respectively using equations 2 and 3. Based on the above equations, to solve for $k_{sx}$ and $k_{rx}$ needed for the angle gather mapping, we are required to solve a quartic equation that can be represented, with pain, analytically or solved numerically. Alternatively, the formulations for a transversely isotropic medium with tilt constrained to the dip (DTI), introduced by Alkhalifah and Sava (2010), is simpler than those introduced here for a general TI medium, and thus can be used at the velocity model building stage. However, when the assumption of the tilt being normal to the reflector dip fails, for example at salt flank reflections where the tilt is generally not normal to the Salt flank, we will need a general formulation similar to the one developed here.

Next: Conclusions Up: Angle gathers in wave-equation Previous: Synthetic Example

2013-04-02