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![]() | Non-hyperbolic common reflection surface | ![]() |
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In this appendix, we reproduce the derivation of an analytical expression for reflection traveltime from a hyperbolic reflector in a homogeneous velocity model (Fomel and Stovas, 2010). Similar derivations apply to an elliptic reflector and were used previously in the theory of offset continuation (Stovas and Fomel, 1996; Fomel, 2003).
Consider the source point
and the receiver point
at the
surface
above a 2-D constant-velocity medium and a hyperbolic
reflector defined by the equation
has physical meaning. Substituting this solution into equation (A-2), we obtain, after a number of algebraic simplifications,
The connection with the multifocusing parameters is summarized in Table 1 for the general case and three special cases (a plane dipping reflector, a flat reflector, and a point diffractor). The first two special cases turn the nonhyperbolic CRS equation into the hyperbolic form (8). The last case turns it into the double-square-root form (13).
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Hyperbolic reflector |
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Plane dipping reflector | ||||
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0 |
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Flat reflector | ||||
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0 | 0 |
Point diffractor | ||||
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![]() | Non-hyperbolic common reflection surface | ![]() |
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