Evidence for Patchy Sediment Underthrusting and a Strong, Drained Outer Accretionary Wedge in Central Cascadia: Implications for Dynamic Slip Conditions

Harold J Tobin, University of Washington Seattle, Earth and Space Sciences, Seattle, WA, United States and Susanna I Webb, University of Wisconsin Madison, Madison, WI, United States
Back to: New Insights on the Cascadia Subduction Zone from Offshore and Amphibious Studies