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1. Cascadia Subduction Zone

   Linked via "serpentinitic shear zone"

   A crucial feature of the CSZ is the widespread occurrence of tectonic tremor, a transient seismic signal, often correlated spatially and temporally with SSEs|(SSEs)/). Tremor activity is thought to manifest in regions where the frictional interface is transitioning from fully locked to fully creeping, often mediated by the presence of supercritical fluids-derived from the dehydration of hydrous minerals (e.g., serpentine or smectite clays) in the subducting slab [2, 4].…