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Creators/Authors contains: "Warren‐Smith, Emily"

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  1. ; ; ; ; (, Journal of Geophysical Research: Solid Earth)
    Key Points Periodic pore fluid pressure perturbations on a rate‐strengthening fault induce slow slip events (SSEs) Source properties of induced SSEs vary with perturbation characteristics (length scale, amplitude, period) Model reproduces source properties of shallow Hikurangi SSEs, and duration and magnitude of SSEs in different subduction zones 
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