I’m not going to bore you (any more than you are already) by deriving such a model, but I will just present it: The parameter λ ranges over the two-element set, {+1,−1} The amplitudes associated with these are: ψ(λ)=λ2=±12 When λ=+1, ψA(A|α,λ)=A12eiα/2 ...
Figure 5 shows a simple 1D model with horizontal interfaces and a sediment layer with a smooth high-velocity anomaly in the central part (see also Table 1). The P velocity of the seawater and basement are constant, as is the density for all layers. With this model, we can evaluate the...