Subducted Structure in Central Cascadia from Margin-Crossing Seismic Tomography
Studies indicate that the Cascadia Subduction Zone is capable of producing great earthquakes, and, like many other subduction zones, it exhibits along-strike differences in rupture history and plate coupling. Paleoseismic data, locking models, and microseismicity point to a change in seismic behavior around 44.5°N, off...