Next: Shallow-origin FEAVO effects
Up: R. Clapp: STANFORD EXPLORATION
Previous: The new approach
As stated by (), the heuristic for proving
that the inversion approach is feasible comprises three steps:
- 1.
- Proving that shallow-origin FEAVO anomalies are visible in the
angle domain
and
wave-equation methods correctly handle the deep-origin FEAVO effects
in synthetic data. That was first accomplished by
() and in this paper I present
some improved results.
- 2.
- Proving that the anomalies can be extracted in the angle domain. I
will show that in the case of simple velocity distributions, the
shape of the anomalies is described by very simple analytical
formulas and I will discuss ways to extract them.
- 3.
- Proving that the extracted anomalies can be transformed back to the
initial domain, updating the guess. In particular, that the
linearized downward continuation does not render FEAVO effects
unrecognizable.
Next: Shallow-origin FEAVO effects
Up: R. Clapp: STANFORD EXPLORATION
Previous: The new approach
Stanford Exploration Project
11/11/2002