Extended Data Fig. 4: Convergence for the preferred inversion.
From: Forearc seismogenesis in a weakly coupled subduction zone influenced by slab mantle fluids
Convergence for the preferred inversion run40. Top left: r.m.s. misfit as a function of iteration. Top right panel: model roughness. Bottom left panel: iteration time. Bottom right panel: Lagrange multiplier search at each iteration step.
