Extended Data Fig. 6: Comparison between Vp from seismic tomography24 (a) and (b) and resistivity from the MT (c) and (d), along two profiles in Western Washington.
From: Fluid transport and storage in the Cascadia forearc influenced by overriding plate lithology
Top panels: an east-west profile across the Olympic Mountains; lower panels, the CAFE profile (MT sites along this profile34 are shown in Fig. 1). Note that for the Vp plots cool colors are low velocities (a-b), and are interpreted as subducted sediments and metasediments. These should have low resistivities (hot colors in (c-d). There is a very good agreement between geometries imaged by the two geophysical methods.
