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📄 kirchhoff.tex

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\section{Time-shift imaging in Kirchhoff migration}The imaging condition described in the preceding sectionhas an equivalent formulation in Kirchhoff imaging.Traditional construction of common-image gathers usingKirchhoff migration is represented by the expression\beq \label{eqn:KirOld}\RR \lp \mm,\ho \rp =\sum_{\mo} \Uo \left[\mo,\ho,         t_s \lp \mm,\mo-\ho \rp +        t_r \lp \mm,\mo+\ho \rp    \right]\;,\eeqwhere $\Uo\lp\mo,\ho,t\rp$ is the recorded wavefield at the surface as a function of surface midpoint $\mo$ and offset $\ho$ (Figure~\ref{fig:kir}).$t_s$ and $t_r$ stand for traveltimes from sources and receivers at coordinates $\mo-\ho$ and $\mo+\ho$ to points in the subsurface at coordinates $\mm$.For simplicity, the amplitude and phase correction term $A \lp \mm,\mo,\ho \rp \frac{\partial}{\partial t}$is omitted in \req{KirOld}.% ------------------------------------------------------------\inputdir{XFig}\plot{kir}{width=3.0in}{Notations for Kirchhoff imaging.S is a source and R is a receiver.}% ------------------------------------------------------------The time-shift imaging condition can be implemented in Kirchhoff imaging using a modificationof \req{KirOld} that is equivalent to \reqs{imgT} and \ren{imgTw}:\beq \label{eqn:KirNew}\RR \lp \mm,\tt \rp=\sum_{\mo} \sum_{\ho}\Uo \left[                \mo,\ho,               t_s \lp \mm,\mo-\ho \rp +              t_r \lp \mm,\mo+\ho \rp + 2 \tt    \right] \;.\eeqImages obtained by Kirchhoff migration as discussed in \req{KirNew} differ from image constructed with \req{KirOld}.Relation~\ren{KirNew} involves a double summation oversurface midpoint $\mo$ and offset $\ho$ to produce an image at location $\mm$. Therefore, the entire input data contributespotentially to every image location.This is advantageous because migrating usingrelation~\ren{KirOld} different offsets $\ho$ independentlymay lead to imaging artifacts as discussed by \cite{GEO69-02-05620575}.After Kirchhoff migration using relation~\ren{KirNew},images can be converted to the angle domain using \req{angT}.

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