Tomography iteration trends for crustal model

These results were calculated from repeated iterations of the J-class model. Beginning with the draped-topography 1-D, multiple tomographic inversions of the traveltime data provided improved models. The charts below gauge the success of multiple iterations.

This particular example was executed under the following constraints

inversion parameter file=Jt3-10.prm
max_dT=0.75
damping=0.1
decim=2
nth=600
nazi=500

postscript file