A transversely isotropic medium with a tilted symmetry axis normal to the reflector |
To appreciate the simplification attained from this constraint , we initially restrict our discussions to a homogeneous medium. In this case, the zero-offset isochron, which is representative of the equal traveltime surface, is spherical in shape, equivalent to the isotropic medium isochron, with a radius governed by the velocity in the tilt direction, , as follows:
For non zero-offset case, the traveltime isochron is constrained by the
double-square-root (DSR) formula (Claerbout, 1995). Thus, the
total traveltime,
, is a combination of traveltimes from the source
located at (
,
), and the receiver
located at
(
,
) to an image point in the subsurface at location
and is
given by the expression
If we reformulate the DSR equation in terms of changes in time, and thus, focus on the plane-wave relation we end up with the following DSR formula:
Thus, in the non-zero offset case the isochron depends on angle, but it is a single angle for both source and receiver rays and we do not have to worry about relating the two angles, as is the case in VTI and general TTI media. This provides us with analytical relations for plane waves at the reflection point. In this case, both the source and receiver waves have the same wave group velocity that differs along the non-zero offset isochron. In fact, for the zero-dip part of the isochron the reflection angle is at its maximum reducing to zero for a vertical reflector, as seen in Figure 1(b).
Next, we formulate the extended imaging condition, necessary for angle-gather development, for the DTI model. As shown in this section, angle gathers are also necessary for an explicit formulation of downward continuation in a DTI model.
Reflection
Figure 2. A schematic plot of the reflection geometry for a 2tilted transversely isotropic TTI medium with a tilt in the dip direction. The incident and reflection angles are the same given by the group angle . 2Here, and correspond, respectively, to the source and receiver locations, is the distance between the source and the reflector in the direction given by unit vector normal to the reflector with direction described by unit vector , and and are, respectively, the unit vector directions for each of the source and receiver rays with ray angle measured from the normal to the reflector. |
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A transversely isotropic medium with a tilted symmetry axis normal to the reflector |