Intermediate‐Depth Earthquakes Controlled by Incoming Plate Hydration Along Bending‐Related Faults
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DOI: 10.1029/2018gl081585
Abstract: Intermediate‐depth earthquakes (focal depths 70–300 km) are enigmatic with respect to their nucleation and rupture mechanism and the properties controlling their spatial distribution. Several recent studies have shown a link between intermediate‐depth earthquakes and the… read more here.
Keywords: bending related; related faults; intermediate depth; depth earthquakes ... See more keywords