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Subsurface-offset Hessian

The prestack migration image (subsurface offset domain) for a group of shots positioned at ${\bf x}_s=(x_s,y_s,0)$ and a group of receivers positioned at ${\bf x}_r=(x_r,y_r,0)$ can be given by the adjoint of a linear operator ${\bf L}$ acting on the data-space ${\bf d}({\bf x}_s,{\bf x}_r;\omega)$ as
   \begin{eqnarray}
{\bf m}({\bf x},{\bf h}) &=& {\bf L}'{\bf d}({\bf x}_s,{\bf x}_...
 ...\sideset{}{'}\sum_{{\bf x}}{\bf d}({\bf x}_s,{\bf x}_r;\omega),

\end{eqnarray}
(1)
where ${\bf G}({\bf x},{\bf x}_s;\omega)$ and ${\bf G}({\bf x},{\bf x}_r;\omega)$ are respectively the Green's functions from the shot position ${\bf x}_s$ and from the receiver position ${\bf x}_r$ to a point in the model space ${\bf x}$, and $ {\bf h}=(h_x,h_y)$ is the subsurface offset. The symbols $\sideset{}{'}\sum_{{\bf h}}$ and $\sideset{}{'}\sum_{{\bf x}}$ are spray (adjoint of the sum) operators in the subsurface offset and model space dimensions, respectively. The Green's functions are computed by means of the one-way wave-equation.

The synthetic data can be modeled (as the adjoint of equation 1) by the linear operator ${\bf L}$ acting on the model space ${\bf m}({\bf x},{\bf h})$ with ${\bf x}=(x,y,z)$ and $ {\bf h}=(h_x,h_y)$
   \begin{eqnarray}
{\bf d}({\bf x}_s,{\bf x}_r;\omega)&=&{\bf L}{\bf m}({\bf x},{\...
 ...\bf x}_s}\sideset{}{'}\sum_{\omega}
 {\bf m}({\bf x},{\bf h}),

\end{eqnarray}
(2)
where the symbols $\sideset{}{'}\sum_{{\bf x}_r}$,$\sideset{}{'}\sum_{{\bf x}_s}$, and $\sideset{}{'}\sum_{\omega}$ are spray operators in the shot, receiver, and frequency dimensions, respectively.

The quadratic cost function is
\begin{eqnarray}
S({\bf m}) &=& \frac{1}{2} \sum_{\omega}\sum_{{\bf x}_s}\sum_{{\bf x}_r} 
 \Vert {\bf d} - {\bf d}_{obs} \Vert^2, 
\end{eqnarray} (3)
and its second derivative with respect to the model parameters ${\bf m}({\bf x},{\bf h})$ and ${\bf m}({\bf x'},{\bf h'})$ is the subsurface offset Hessian:
   \begin{eqnarray}
{\bf H}({\bf x,h};{\bf x',h'})&=&\sum_{\omega}
\sum_{{\bf x}_s...
 ...f x}_r;\omega) {\bf G}({\bf x'-h'},{\bf x}_r;\omega). \nonumber

\end{eqnarray}
The next subsection shows how to use the subsurface-offset domain Hessian to compute the angle Hessian following the Fomel (2004) approach.


next up previous print clean
Next: Angle-domain Hessian Up: Expanding Hessian dimensionality Previous: Expanding Hessian dimensionality
Stanford Exploration Project
1/16/2007