INTEGRATED 2D GEOPHYSICAL MODELING OVER THE JUAN DE FUCA PLATE
In our analysis, we have integrated multiple geophysical data from public sources, namely gravity and magnetic fields with seismic reflections and refractions. Our constructed 2D geophysical model starts from the Axial segment of the JdF spreading ridge. On the western side of the profile, gravity model requires lower densities of the mantle rocks associated with the Cobb hotspot. There are also two bathymetric seamounts near the oceanic ridge that have both gravity and magnetic signatures. Our profile crosses the pseudofault zones that require lower crustal densities with respect to adjacent oceanic crusts. We interpret this as evidence of extensive faulting in that region making the pseudofaults zones of weakness within the JdF plate. Our modeling also suggests the presence of a buried seamount beneath the accretionary prism that appears to be in contact with the Siletz terrane of the continental domain. This buried seamount may potentially influence the overall subduction process and may be related to the lack of earthquakes in this region.