A shallow slow slip event with Mw 6.6 was captured in the Copiapó ridge, Chile, with migrating seismic swarms indicating fluid pressure pulses as the likely initiation mechanism.
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Seismic swarms unveil the mechanisms driving shallow slow slip dynamics in the Copiap\'o ridge, Northern Chile
A shallow slow slip event with Mw 6.6 was captured in the Copiapó ridge, Chile, with migrating seismic swarms indicating fluid pressure pulses as the likely initiation mechanism.