Slide 2: ../pmprays.gif PmP Example. Top: Sources (triangles) and receivers (circles). Note that only 25% of possible source-receiver pairs are randomly-selected and used in the inversion. (Bottom) Typical ray paths.
Slide 13: ../pmpsummary.gif PmP Example. Summary of results A) True model. B) Starting model. C) Inversion with damping that favors Moho topography. D) Inversion with damping that favors crustal velocity structure.