Extended Data Fig. 5: Curved sections of the 3D resistivity model just above the upper interface of the subducting slab from various inversion runs. | Nature Geoscience

Extended Data Fig. 5: Curved sections of the 3D resistivity model just above the upper interface of the subducting slab from various inversion runs.

From: Fluid transport and storage in the Cascadia forearc influenced by overriding plate lithology

Extended Data Fig. 5

(a) run#36. (b) run#44. (c) run#45. Panel (d) shows a 3D view of the result shown in panel (c). For run#36 & run#44, the conductive ocean was allowed to vary during inversion, while for run#45 it was frozen. Note that run#44 & run#45 have more sites in Southwestern Oregon.

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