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The Method

Claerbout (1992) casts the problem of slope estimation as a univariate optimization problem, based on the observation that the partial differential equation  
 \begin{displaymath}
\left( \frac{\partial}{\partial x} + p \frac{\partial}{\partial t} \right) u(t,x)\end{displaymath} (1)
is zero-valued if the wavefield u(t,x) consists only of plane waves with time slope, or ``stepout,'' p. Claerbout also notes that a cascade of two PDEs annihilates data consisting of plane waves with two slopes, p1 and p2. The analog to equation (1) is:  
 \begin{displaymath}
\left( \frac{\partial}{\partial x} + p_1 \frac{\partial}{\pa...
 ...}{\partial x} + p_2 \frac{\partial}{\partial t} \right) u(t,x),\end{displaymath} (2)
or after expansion,  
 \begin{displaymath}
\left( \frac{\partial^2}{\partial x^2} + (p_1+p_2) \frac{\pa...
 ... t} 
 + p_1 p_2 \frac{\partial^2}{\partial t^2} \right) u(t,x).\end{displaymath} (3)


 
next up previous print clean
Next: Discretizing the problem Up: Brown: Slope estimation Previous: Background
Stanford Exploration Project
11/11/2002