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A novel three-dimensional model of the fluid stored deep in Earth’s crust along the Cascadia Subduction Zone provides new insight into how the accumulation and release of those fluids may
CORVALLIS, Ore. – A novel three-dimensional model of the fluid stored deep in Earth’s crust along the Cascadia Subduction Zone provides new insight into how the accumulation and release of those fluids may influence seismic activity in the region. The fluid collects near but does not penetrate a thickened section of the crust known as Siletzia lies beneath much of western