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We obtained high-precision locations for 5250 earthquakes in the Iquique segment of the northern Chilean subduction zone from two temporary local seismic networks around 21°S. A double seismic zone in the downgoing Nazca slab can be clearly identified. One band of seismicity is located at the plate interface and a second one 20–25km deeper in the oceanic mantle. It can be traced updip to uncommon...

High-resolution image of the North Chilean subduction zone: seismicity, reflectivity and fluids