Oblique Strike-Slip Faulting of the Cascadia Submarine Forearc: The Daisy Bank Fault Zone off Central Oregon
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American Geophysical Union
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1. Fluid sources and overpressures within the central Cascadia Subduction Zone revealed by a warm, high-flux seafloor seep;Science Advances;2023-01-27
2. Along‐Trench Structural Variations of the Subducting Juan de Fuca Plate From Multichannel Seismic Reflection Imaging;Journal of Geophysical Research: Solid Earth;2018-04
3. Effects of lateral friction on the structural evolution of fold-and-thrust belts: Insights from sandbox experiments with implications for the origin of landward-vergent thrust wedges in Cascadia;Geological Society of America Bulletin;2015-09-28
4. Confidence levels for tsunami-inundation limits in northern Oregon inferred from a 10,000-year history of great earthquakes at the Cascadia subduction zone;Natural Hazards;2009-09-21
5. Geophysical constraints on the surface distribution of authigenic carbonates across the Hydrate Ridge region, Cascadia margin;Marine Geology;2003-11
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