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Small velocity anomalies can create AVO effects by focusing
the reflected seismic wavefield. This impedes AVO analysis. The AVO
anomalies caused by focusing are distinguishable by surface-consistent
patterns. () named this phenomenon
focusing-effect AVO (FEAVO).
In this paper, I present and discuss the
feasibility of a method whose application to FEAVO-affected 2D and 3D
datasets would produce an estimate of the anomalies.
The goal is to determine a velocity field accurate enough to generate a
FEAVO-free prestack volume by downward continuing the wavefield
through the FEAVO-generating anomalies.
The accurate velocity model
should be obtained by using the inversion method known as wave
equation migration velocity analysis (WEMVA) (),
with a fitting goal
modified so that it is specifically geared toward extracting FEAVO effects.
I have continued that line of work by going into more depth with
regard to each of the aspects of the study. I will respect the same
structure. The material presented at each point consists of the
progress in knowledge and research accomplished since the
previous paper.
I begin with a review of previous work
used as a basis for my work,
then I explain my approach and show evidence
of its validity.
Next: Previous work by others
Up: R. Clapp: STANFORD EXPLORATION
Previous: Vlad: REFERENCESFocusing-effect AVO
Stanford Exploration Project
11/11/2002