Thermal environment of the Southern Washington region of the Cascadia subduction zone
Author:
Affiliation:
1. School of Oceanography University of Washington Seattle Washington USA
2. College of Earth, Ocean and Atmospheric Sciences Oregon State University Corvallis Oregon USA
Funder
National Science Foundation
U.S. Department of Energy
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016JB013839
Reference109 articles.
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3. Evidence for Great Holocene Earthquakes Along the Outer Coast of Washington State
4. Atwater B. F. andE.Hemphill‐Haley(1997) Recurrence intervals for great earthquakes of the past 3 500 years at northwest Willapa Bay Washington Prof. Pap. 1576 U.S. Geol. Surv. Menlo Park Calif.
5. The Washington continental slope: Quaternary tectonics and sedimentation
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1. Late Quaternary Surface Displacements on Accretionary Wedge Splay Faults in the Cascadia Subduction Zone: Implications for Megathrust Rupture;Seismica;2024-04-30
2. An introductory review of the thermal structure of subduction zones: I—motivation and selected examples;Progress in Earth and Planetary Science;2023-07-28
3. Focusing Effects of Teleseismic Wavefields by the Subducting Plate Beneath Cascadia;Journal of Geophysical Research: Solid Earth;2023-06
4. Fluid sources and overpressures within the central Cascadia Subduction Zone revealed by a warm, high-flux seafloor seep;Science Advances;2023-01-27
5. Methane Plume Emissions Associated With Puget Sound Faults in the Cascadia Forearc;Geochemistry, Geophysics, Geosystems;2021-12-29
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