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A wider seismogenic zone at Cascadia due to fluid circulation in subducting oceanic crust

Geology (2012) 40 (10): 899–902.
This article has been cited by the following articles in journals that are participating in CrossRef Cited-by Linking.
Disentangling the Roles of Subducted Volatile Contributions and Mantle Source Heterogeneity in the Production of Magmas Beneath the Washington Cascades
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Pressure-driven processes explain the decreasing magnetization of the subducting oceanic crust in the Japan Trench
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Thermally Significant Fluid Seepage Through Thick Sediment on the Juan de Fuca Plate Entering the Cascadia Subduction Zone
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Cascadia Subduction Zone Fault Heterogeneities From Newly Detected Small Magnitude Earthquakes
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Deformation of the Juan de Fuca Plate Beneath the Central Cascadia Continental Margin (44°-45°N) in Response to an Upper Plate Load
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Fluid sources and overpressures within the central Cascadia Subduction Zone revealed by a warm, high-flux seafloor seep
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Geodynamic studies of southwestern Canada: subduction zone processes and backarc mantle dynamics
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Canadian Journal of Earth Sciences (2023) 60 (9): 1283.
Spatial variations of the effective elastic thickness and internal load fraction in the Cascadia subduction zone
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Assessing Margin‐Wide Rupture Behaviors Along the Cascadia Megathrust With 3‐D Dynamic Rupture Simulations
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Systematic characterization of morphotectonic variability along the Cascadia convergent margin: Implications for shallow megathrust behavior and tsunami hazards
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Bayesian inversion of surface heat flow in subduction zones: a framework to refine geodynamic models based on observational constraints
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Geophysical Journal International (2020) 222 (1): 103.
Heat Flow Evidence for Hydrothermal Circulation in Oceanic Crust Offshore Grays Harbor, Washington
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Thermal State, Slab Metamorphism, and Interface Seismicity in the Cascadia Subduction Zone Based On 3‐D Modeling
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Geophysical Research Letters (2017) 44 (18): 9242.
Heat flow bounds over the Cascadia margin derived from bottom simulating reflectors and implications for thermal models of subduction
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Thermal environment of the Southern Washington region of the Cascadia subduction zone
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Journal of Geophysical Research: Solid Earth (2017) 122 (8): 5852.
Invited review paper: Some outstanding issues in the study of great megathrust earthquakes—The Cascadia example
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Effect of hydrothermal circulation on slab dehydration for the subduction zone of Costa Rica and Nicaragua
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Physics of the Earth and Planetary Interiors (2016) 255: 66.
Three-Dimensional Thermal Model of the Costa Rica-Nicaragua Subduction Zone
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Modeled temperatures and fluid source distributions for the Mexican subduction zone: Effects of hydrothermal circulation and implications for plate boundary seismic processes
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Relationships among temperature, dehydration of the subducting Philippine Sea plate, and the occurrence of a megathrust earthquake, low-frequency earthquakes, and a slow slip event in the Tokai district, central Japan
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Slab melting beneath the Cascade Arc driven by dehydration of altered oceanic peridotite
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Gravity anomalies, crustal structure, and seismicity at subduction zones: 2. Interrelationships between fore‐arc structure and seismogenic behavior
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Tomographic imaging of the Cascadia subduction zone: Constraints on the Juan de Fuca slab
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Segmentation of plate coupling, fate of subduction fluids, and modes of arc magmatism in Cascadia, inferred from magnetotelluric resistivity
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Relationship between the Cascadia fore-arc mantle wedge, nonvolcanic tremor, and the downdip limit of seismogenic rupture
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Geochemistry, Geophysics, Geosystems (2014) 15 (4): 1580.
Downdip landward limit of Cascadia great earthquake rupture
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Global analysis of the effect of fluid flow on subduction zone temperatures
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