Figure 1.
(A) A single p-wave velocity model drawn from population L which consists of 20,000 velocity models. The numerically simulated seismic wavefield using an elastic lattice wave propagation method is shown overlain on the models with the source location (shown by the *). (B) A single p-wave velocity model drawn from the population T which consists of 20,000 velocity models. The numerically simulated seismic wavefield is shown overlain on the models. (C) The velocity profile through the model shown in (A) from two different locations in this model. (D) The velocity profile through the model shown in (B) from two different locations in this model. The triangles in (A) and (B) show the location of the synthetic seismic stations at which time varying synthetic seismic data are ‘captured’ during the simulation run.