Figure 3. Non-linear 2D inversion of MT and CSEM data. Left: converged MT data inversion. The dashed black lines enclose the prominent low resistivity channel interpreted as partial melt at the LAB. Right: converged CSEM data inversion that shows decreasing resistivity beneath fault scarps at the outer rise and a low resistivity channel that follows the plate interface in the forearc margin, and which represent hydration and sediment subduction, respectively.
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