Wave-equation migration velocity analysis by residual moveout fitting |
In wave-equation migration, as for example reverse-time migration, the image is computed from the back-propagated receiver wavefield, , and the forward-propagated source wavefield, , where is the recording time, is the model-coordinate vector, is the source position at the surface, and is the slowness model.
The prestack image, , is computed as the zero lag of the temporal cross-correlation between the spatially-shifted back-propagated receiver wavefield and forward-propagated source wavefield as (Rickett and Sava, 2002):
where is the half subsurface offset, which in this paper I will assume to be horizontal, but it does not need to be in the general case (Biondi and Symes, 2004).
The prestack image as a function of subsurface offset can be transformed to an image as a function of reflection aperture angle, by using a linear operator (Sava and Fomel, 2003). In matrix notation, if is a matrix and is a matrix, the image transformation from subsurface offset into the angle domain can be expressed as:
I introduce an objective function that maximizes the flatness of the angle-domain image along the aperture-angle axis at all spatial locations . This objective function aims at maximizing image flatness not directly as a function of the slowness, but indirectly through the application of an angle-domain moveout operator , which depends on the column vector of moveout parameters .
I define the application of the moveout operators to a prestack image computed by equations 1 and 2 with a background slowness , as
(A-3) |
I further define the stacking operator that sums the image along the aperture-angle axis . I can now introduce the objective function that measures the flatness of the image as:
The fitting problems maximize the zero lag of the cross-correlation between the prestack image computed for a realization of the slowness vector and the moved-out image computed with the background slowness . For the sake of keeping the notation as compact as possible, I combine the independent fitting problems into one by defining the following objective function:
The vector of moveout parameters is therefore the solutions of the following maximization problem:
For velocity estimation in the angle domain, an effective parametrization of the moveout is the "curvature" , that defines the following moveout equation
Wave-equation migration velocity analysis by residual moveout fitting |